From 0d7feff349f335a13dd22035fd84621cdf990601 Mon Sep 17 00:00:00 2001 From: ggserver Date: Sat, 3 Aug 2024 07:57:19 +0000 Subject: [PATCH] Add updates up until 2024-08-03 07:55:09 --- .../87/038187EBFFA41D08055F2E8B8D8FFEB5.xml | 851 ++++++++++++++++++ .../1C/03841C0BFF88FFE3C976F88FFDAFB896.xml | 203 +++++ .../1C/03841C0BFF88FFE4C976FEEEFB75BDA9.xml | 222 +++++ .../1C/03841C0BFF88FFE4CAD0FABBFCF1BA4F.xml | 146 +++ .../1C/03841C0BFF88FFE4CAD0FEEEFEF0BE7A.xml | 146 +++ .../1C/03841C0BFF8AFFE4C976FA1CFEFDBBAB.xml | 181 ++++ .../1C/03841C0BFF8AFFE6C976FDFAFB71BE19.xml | 122 +++ .../1C/03841C0BFF8DFFE0C976F8C8FD73BFE0.xml | 191 ++++ .../1C/03841C0BFF8DFFE1C976FC65FA14BC6A.xml | 134 +++ .../1C/03841C0BFF8DFFE1CAD0F82FFB46B8D3.xml | 157 ++++ .../1C/03841C0BFF8FFFE3CAD0F8A8FB71B8D3.xml | 168 ++++ .../1C/03841C0BFF8FFFE3CAD0FB87FE46BC75.xml | 135 +++ .../87/039687F3FFAFFFAEFF6CFEC960032F1E.xml | 107 +++ .../87/03988783FFA7FF9B83FEFB32F42FFB3D.xml | 147 +++ 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data/FF/13/87/FF1387C3C315256013E8F47DFB18FED8.xml create mode 100644 data/FF/13/87/FF1387C3C31E256F104EF6D8FE0EFAF2.xml diff --git a/data/03/81/87/038187EBFFA41D08055F2E8B8D8FFEB5.xml b/data/03/81/87/038187EBFFA41D08055F2E8B8D8FFEB5.xml new file mode 100644 index 00000000000..a17a43fd5e6 --- /dev/null +++ b/data/03/81/87/038187EBFFA41D08055F2E8B8D8FFEB5.xml @@ -0,0 +1,851 @@ + + + +Eupelmus niger (Hymenoptera: Eupelmidae), a Parasitoid of the Endangered Hawaiian Yellow-faced Bee Hylaeus anthracinus (Hymenoptera: Colletidae) + + + +Author + +Magnacca, Gary A. P. Gibson Paul D. Krushelnycky Karl N. + +text + + +Proceedings of the Hawaiian Entomological Society + + +2022 + +54 + + +77 +92 + + + +journal article +0073-134X + + + + + + + +Eupelmus +( +Eupelmus +) +niger +Ashmead + + + + + + + + + + +Eupelmus niger + +Ashmead,1901:315 + + + +(key), 316–317 (description). Published +type +information: +one female +taken in +January +, +Lahaina +, +Maui +[ +Hawai‘i +]. + + + + + +Material examined +. +Type material +. + +Holotype +♀ +( +NHMUK +), photographs only examined (see methods).Type labels: Type / Lahaina, Maui, coast 1.97 / + +Eupelmus niger +Ash + +♀ +Type / B.M. +TYPE HYM +. 5.979 / +NHMUK010370259 +. + + + +Holotype +point-mounted ( +Figs. 2A,B +); contorted ( +Fig. 2B +); missing right antenna beyond pedicel ( +Fig. 2H +), ovipositor sheaths ( +Figs. 2A,B +), and apical two tarsomeres of right mesotarsus ( +Fig. 3F +insert). + + +Other material +. + +USA +. + +Hawai‘i + +: O‘ahu, nr. + +Makapu Pt. + +[misspelling of Makapuʻu Pt], +Aug +54, +J.W.Beardsley +,rearedex.wood + +Tournefortia + +( +1♀ +CNC +). O‘ahu +Is. +, +Kahuku +, +James Campbell Nat. Wildlife Refuge +, + + +4m + +. + +, +P. Krushelnycky +— +21.69470°N +157.95286°W +, + +22.XI.2021 + +, ex. + +Hylaeus anthracinus + +nest / coll# PDK1092, spec/ lot# +PKSP52275 +( +1♂ +CNC +) + +; + +21.69470°N +157.95286°W +, + +23.XI.2021 + +, ex. + +Hylaeus anthracinus + +nest / coll# PDK1093, spec/ lot# +PKSP52276 +( +1♀ +CNC +) + +; + +21.70147°N +157.95875°W +, + +6.XII.2021 + +, ex. + +Hylaeus + +nest / coll # PDK1094, spec/lot# +PKSP52277 +( +1♀ +, +1♂ +CNC +) + +; + +21.69794°N +157.95644°W +, + +7.XII.2021 + +, ex. + +Hylaeus anthracinus + +nest / coll# PDK1097, spec/ lot# +PKSP52267 +( +1♀ +CNC +) + +; + +21.69470°N +157.95286°W +, + +7.XII.2021 + +, ex. + +Hylaeus anthracinus + +nest / coll# PDK1097, spec/ lot# +PKSP52266 +( +1♂ +CNC +) + +; + +21.69702°N +157.95567°W +, + +22.IX.2021 + +, ex. + +Hylaeus anthracinus + +nest / coll# PDK 1088, spec/lot# +PKSP51219 +( +1♀ +, +2♂ +HDOA +) + +; + +21.70147°N +157.95875°W +, + +24.IV.2022 + +, ex. + +Hylaeus + +nest / coll# PDK 1155—spec/ lot# +PKSP52304 +( +1♀ +BPBM +) + +, + +spec/ lot# +PKSP52305 +( +1♀ +BPBM +) + +, + +spec/ lot# +PKSP52306 +( +1♂ +BPBM +) + +, + +spec/ lot# +PKSP52307 +( +1♀ +BPBM +) + +, + +spec/lot# +PKSP52308 +( +1♂ +BPBM +) + +; + +21.70210°N +157.95966°W +, + +14.IV.2022 + +, ex. bee nests, probably + +Hylaeus + +/ coll# PDK1157— spec/lot# +PKSP52326 +( +1♀ +UHIM +) + +, + +spec/lot# +PKSP52327 +( +1♀ +UHIM +) + +, + +spec/lot# +PKSP52328 +( +1♂ +UHIM +) + +, + +spec/lot# +PKSP52329 +( +1♂ +UHIM +) + +, + +spec/lot# +PKSP52330 +( +1♂ +UHIM +) + +, + +spec/lot# +PKSP52331 +( +1♀ +UHIM +) + +; + +Kāne‘ohe +, +Marine Corps Base Hawai‘i +, + +4 m + +, +P. Krushelnycky +— +21.45625°N +157.75508°W +, + +5.XII.2021 + +, ex. + +Hylaeus + +nest / coll# PDK1096—spec/lot# +PSKP52263 +( +1♂ +CNC +) + +, + +spec/lot# +PSKP52264 +( +1♀ +CNC +) + +, + +spec/lot# +PSKP52265 +( +1♂ +CNC +) + +; + +21.45625°N +157.75508°W +, + +6.IV.2022 + +, ex. bee nests, probably + +Hylaeus + +/ coll# PDK1154—spec/lot# +PSKP52322 +( +1♀ +BPBM +) + +, + +spec/lot# +PSKP52323 +( +1♀ +BPBM +) + +, + +spec/lot# +PSKP52324 +( +1♂ +BPBM +) + +, + +spec/lot# +PSKP52325 + +( +1♀ + + + +BPBM +); +21.45392°N +157.74825°W +, + +13.IV.2022 + + +, ex. + +Hylaeus + +nest / coll# PDK1156—spec/lot# + +PSKP52332 +( +1♂ +UHIM +), spec/lot + +# + +PSKP52333 +( +1♀ +UHIM +) + +. + + + + +Diagnosis. +Both sexes of + +E. niger + +are readily differentiated from those of all other known macropterous Hawaiian + +Eupelmus + +by a combination of hair-like body setae and extensively, darkly infuscate fore wings ( +Figs. 3D, E +, +5D +). Most Hawaiian + +Eupelmus +species + +have hyaline or essentially hyaline fore wings or those females with partly infuscate fore wings have white, lanceolate to spatulate setae on the body ( +Gibson 1995 +, e.g. Figs. 89, 182, Gibson and Fusu 2016, Figs. 77a–d). Both sexes are also atypically dark though with variably distinct metallic lusters under some angles of light depending on the +type +of light used ( +Figs. 2 +, +3A–C +, +4 +, +5A–C, E +), including the legs at least basal of the tarsi ( +Figs. 2D +, +4B +), and the ovipositor sheaths other than the extreme apex ( +Figs. 3J, K +), whereas at least females of other Hawaiian + +Eupelmus + +usually are a brighter green to blue and have more extensively pale legs and/or ovipositor sheaths. + + + + +Description. +FEMALE (habitus: +Figs. 2A–D +). Length of uncontorted individual, including ovipositor sheaths, about 6.0– +7.3 mm +. Head ( +Figs. 2G, H +, +3A, B +) dark, almost black, but with slight green to greenish-blue or violaceous lusters in part under some angles of light ( +Figs. 2G +, +3A, C +); setae dark, hair-like. Maxillary and labial palpi dark. Antenna dark except for paler micropilose sensory region of clava ( +Fig. 3C +). Mesosoma ( +Figs. 2E, F +) similarly dark with dark hair-like setae as head except as follows: frontal surface of prepectus pale ( +Fig. 2F +); mesonotum and propodealcallarregionswithslightgreen, blue and/or violaceous lusters under different angles of light, the scutellar-axillar complex in particular more distinctly and extensively violaceous under most angles of light, and acropleuron with very slight blue to violaceous luster under some angles of light. Fore wing ( +Figs. 3D, E +) with costal cell and/or base of basal cell variably distinctly brownish-infuscate, but at least mostly subhyaline to hyaline compared to more darkly, distinctly brownish-infuscate disc beyond level of base of parastigma, though disc progressively paler posterior of about level of medial fold and apically beyond venation; costal cell dorsally with row of dark setae nearleadingmarginonlyoveraboutapical one-third, but ventrally almost completely setose; basal cell entirely setose and with line of setae along mediocubital fold continuous to disc so as to differentiate bare cubital and vanal areas posterior of basal cell and oblique, rectangular speculum behind base of parastigma anterior to mediocubital setal line beyond basal cell, the disc otherwise uniformly setose except for oblique linea calva. Legs ( +Figs. 2C, D +) similarly dark as mesosoma, including row of mesotibial apical pegs and mesotarsal pegs ( +Fig. 3F +), except pro- and mesotarsi variably paler, brown to yellowish or white except for darker setae ( +Fig. 3F +), and metatarsus variably extensively pale, with at least extreme base ( +Figs. 3G, H +) and sometimes entire basitarsus ( +Fig. 3I +) white. Gaster ( +Figs. 2C, D +) dark with dark hair-like setae and obscure metallic lusters under some angles of light similar to head and mesosoma, the basal tergite dorsally sometimes with more distinct green luster; ovipositor sheaths entirely dark except for extreme apex ( +Figs. 3J, K +). + + +Head in dorsal view ( +Figs. 3A, B +) with interocular distance about 0.3× head width; in lateral view ( +Fig. 2D +) lenticular with face evenly convex and parascrobal region smoothly merged with frons; vertex alutaceous-imbricate, frons above level of scrobal depression coriaceous to indistinctly coriaceous-reticulate with setiferous punctures lateral anterior ocellus, parascrobal region and lower face more distinctly reticulate with setiferous punctures except for smooth, bare clypeal apex and more coriaceous paraclypeal region apically, scrobes and scrobal depression transversely reticulate to reticulate-rugulose and bare, and interantennal prominence more finely coriaceous to coriaceous-imbricate with setiferous punctures; OOL: POL: LOL: MPOD about 0.5–0.6: 1.6–1.8: 1.4–1.5: 1.0. Antenna ( +Fig. 3C +) with scape slightly curved, about 5.0–5.5× as long as wide and of similar width throughout; pedicel about 1.5–2.0× as long as wide; fl1 about 1.2–1.4× longer than wide and 0.55–0.66× as long as pedicel; fl2 about 2.3× as long as wide or length of fl1, and subsequent preclaval flagellomeres progressively shorterandwider,withfl3 about 1.9–2.3×, fl4about 2.2×, fl5 about1.5–1.6×,fl6about 1.3–1.4×, fl7 about 1.0–1.2× and fl8 about 0.9–1.0× as long as wide; clava about 2.2–2.3× as long as wide and about 0.7– 0.75×combined length of preceding three flagellomeres, with micropilose sensory region ventrally over apical two clavo- meres. Mesonotum ( +Fig. 2E +) with anteromedial lobe of mesoscutum transversely reticulate-imbricate to strigose anteriorly but increasingly more coriaceous medially to reticulate posteriorly compared to more distinctly reticulate posteriorly depressed region; lateral lobe minutely coriaceous and bare dorsolongitudinally, and coriaceous to coriaceous-reticulate with setiferous punctures laterally; scutellar-axillar complex low convex, mostly coriaceous with setiferous punctures exceptscutellummediolongitudinallyand posterior frenal area bare. Acropleuron ( +Fig. 2F +) shallowly reticulate anteriorly and posteriorly of much more minutely sculptured mesal region, the reticulations posterior of mesal region larger than anteriorly. Fore wing ( +Figs. 3D, E +) with cc: mv: pmv: stv = 4.0–4.7: 3.7–4.0: 1.2: 1.0, with stigma curved apically at abrupt angle relative to stigmal vein. Middle leg with row of 6–8 mesotibial apical pegs; mesotarsus ( +Fig. 3F +) with symmetrical peg pattern on basitarsus and pegs clear- ly differentiated into two rows apically; second tarsomere with 5 or 6, third tarsomere with 2 or 3, and fourth tarsomere with 1 or 2 pegs on either side. Propodeum with medial depression broadly V-shaped and extended almost to posterior margin ( +Fig. 2E +); callus with sparse setae not ob- structing view of cuticle ( +Fig. 2F +). Gaster ( +Figs. 2C, D +) not atypically modified, with posterodorsal margins of Gt1–Gt4 deeply emarginate ( +Fig. 2C +), posterior margin of Gt5 rounded and extending over medially divided Gt7 to base of syntergum ( +Fig. 3J +); syntergum dorsally ( +Fig. 3J +) strongly transverse to sublinear anterior of sclerotized anal plate comprising most of dorsal surface and extending to base of constriction separating exposed ovipositor sheaths from concealed second valvifers. Ovipositor sheaths in dorsal view ( +Fig. 3J +) with lateral margins out-curved so as to be widest medially and narrowed basally and apically, in lateral view ( +Fig. 2K +) length measured from apex of gaster about 1.0–1.1× as long as metatarsis (cf. + + +Figs. 3I, K +) and about 1.1–1.2× as long as mv. + + +MALE (habitus: +Figs. 4A, B +). Length +3.6–5.3 mm +. Head ( +Figs. 4C, D +), including maxillary and labial palpi ( +Fig. 4E +), and body color and setation similar to female, almost black with slight green to violaceous lusters under some angles of light, except tarsi mostly pale, white to yellowish, other than darker brown apical tarsomeres ( +Fig. 5F +) or sometimes metatarsus with only basitarsus pale and subsequent tarsomeres darker brown ( +Fig. 5G +). Fore wing ( +Fig. 5D +) similar in color to female, the extreme base brownish-infuscate but basally mostly hyaline to subhyaline to level about equal with apex of costal cell and with bare region of disc paler infuscate relative to surrounding setose region, the disc also paler posterior to level of medial fold and apically beyond venation; setal pattern similar to female except speculum continuous with linea calva, the bare regions not separated by setae. + + +Head in dorsal view ( +Fig. 4D +) with interocular distance slightly less than 0.5× head width; vertex smoothly rounded into occiput; vertex transversely reticulate to reticulate-imbricate ( +Fig. 4D +), frons above level of scrobal depression ( +Figs. 4C, D +) coriaceous-reticulate, the surface of most cells slightly depressed, to variably more distinctly reticulate and with setiferous punctures lateral of anterior ocellus, parascrobal region and lower face more distinctly reticulate with setiferous punctures except for smooth, bare clypeal apex and minutely coriaceous paraclypeal region, scrobes and scrobal depression transversely reticulate-strigose and bare, and interantennal prominence finely coriaceous to almost smooth except for setiferous punctures and shiny mediolongitudinally ( +Figs. 4C, E, F +); lower face and gena near malar sulcus with longer, but straight to only slightly curved dark setae ( +Fig. 4E +); OOL: POL: LOL: MPOD = 0.6–0.7: 2.3–2.4: 1.4–1.6: 1.0. Antenna ( +Fig. 4F +) with scape sub- rectangular, about 2.6–2.8× as long as wide; pedicel about 1.5× as long as apical width, ventrally with line of apically curved setae; fl1 strongly transverse but extensively setose with more than one row of setae, and subsequent preclaval flagellomeres with single row of mps apically and dense, short setae, with fl2 slightly longer than apical width, but fl3–fl8 all about as long as wide to slightly wider than long apically; clava about twice as long as wide and about as long as combined length of preceding two flagellomeres. Mesonotum ( +Fig. 5A +) reticulate, the reticulations somewhat larger posteriorly on middle lobe than lateral lobe lateral of notauli; scutellar-axillar sculpture pattern and setation similar to female, the scutellum more finely sculptured and bare mediolongitudinally and with bare frenal area; prepectus and mesofemoral depression similarly reticulate ( +Fig. 5B +); acropleuron reticulate anteriorly to coriaceous posteriorly; upper and lower mesepimeron not divided by line or pit, with upper mesepimeron almost smooth, only obscurely coriaceous relative to more coarsely coriaceous-reticulate lower mesepimeron. Metapleuron coriaceous to coriaceous-reticulate. Propodeum ( +Fig. 5C +) with complete median carina and a few short longitudinal carinae extending anteriorly from propodeal foramen ( +Figs. 5C, E +), and with posterolateral angle projecting into short denticle ( +Figs. 5C, E +: arrow), but panels otherwise finely coriaceous; callar region with line of dark setae anterior to spiracle and sparsely setose lateral of spiracle. Petiole smooth, shiny, transverse. Gaster dorsally ( +Fig. 5E +) entirely coriaceous and either entirely, uniformly setose beyond Gt2 or tergites variably broadly bare basally depending on inflation of gaster telescoping seg- ments, but with Gt1 dorsally and Gt2 dorsomedially bare. + + + +Figure 4. + +Eupelmus niger + +♂ reared from + +Hylaeus anthracinus + +. +A +, dorsal habitus; +B +, lateral habitus; +C +, frontal head; +D +, dorsal head; +E +, lower face; +F +, antenna. + + + + +Figure 5. + +Eupelmus niger + +♂ reared from + +Hylaeus anthracinus + +. +A +, dorsal mesosoma; +B +, lateral mesosoma; +C +, propodeum; +D +, fore wing; +E +, gaster and propodeum, dorsolateral; +F +, mesotarsus; +G +, metatarsus. + + + +Variation +. The metallic lusters evident in the plates of illustrations of both sexes, taken using the fibre optic light source, are more intense and extensive than when viewed using the halogen light source on which the descriptions are based.Further, the Makapuʻu female is more dark brown than black and the fore wings somewhat paler brown, more similar to those of the +holotype +( +Fig. 3D +) than the dark brown infuscation of our reared females ( +Fig. 3E +). Both differences may result from the +holotype +and Makapuʻu specimen being older and, as a result, at least the Makapuʻu female possibly being somewhat faded. The metatarsi of both the +holotype +( +Fig. 3G +) and the Makapuʻu female are almost completely brown except for the extreme base, but extent of the pale metatarsal region varies in our reared specimens (cf. +Figs. 3H, I +). The Makapuʻu female differs from both the +holotype +and our reared females in having one or two setae within the fore wing speculum so that the speculum is less conspicuous. The Makapuʻu female also has Gt7 more extensively exposed and an apical portion of the second valvifers visible beyond the syntergum basal to the ovipositor sheath constriction so that the sheaths super- ficially appear somewhat longer, but both differences likely are an artefact resulting from shrivelling of the gaster during air-drying. The ovipositor sheaths of the +holotype +are missing ( +Figs. 2A, B +), but the original description states they were the length of the hind tarsi and black. The original description also states the wings of the +holotype +to be “subhyaline, clear hyaline at extreme base” (Ashmead 1910, p. 326), though the fore wing disc of the +holotype +is extensively brownish-infuscate ( +Fig. 2D +). + + + + +Distribution +. +USA +. +Hawai‘i +: Maui, O‘ahu. + + + + +Hosts +. + +Hylaeus +( +Nesoprosopis +) +anthracinus +(F. Smith) + +, + +Hylaeus +( +Indialaeus +) +strenuus +(Cameron) + +. + + + + +Remarks. +In the unpublished manuscript of C. Yoshimoto, +six specimens +( +6♀ +in one version, +3♀ +and +3♂ +in another version) are listed with similar data as the examined Makapuʻu Pt. female. The manuscript does not include the specimens being reared from + +Tournefortia + +wood, but provides the additional information they were collected +August 1954 +, and “appar- ently parasite of +Nesoprosopis +sp.”. Also listed from the same site was a “pupa found in bee nest with remains of bee pupae in + +Tournefortia + +twig.” However, we were unable to locate any of these other specimens. Another +six females +with different collection and host data were also listed under + +E. niger + +in the manuscript, including +two females +collected by Bridwell stated as deposited in the +United States +National Museum of Natural History, +Washington +, DC (USNM). These +two specimens +were located in the USNM, but photographs provided to us of the specimens revealed that one of the two is a male and neither is + +E. niger + +, the specimens having hyaline wings and a brighter green body color. Along with the Makapuʻu Pt. female under the name + +E. niger + +in the CNC is a male with the same data as +one specimen +cited in the manuscript as a female. It is possible that the manuscript sex citation is incorrect, but the CNC male is not + +E. niger + +. Because of the discrepancies between the manuscript and observed specimens we do not cite the collection data of the other manuscript-listed specimens. + + + + \ No newline at end of file diff --git a/data/03/84/1C/03841C0BFF88FFE3C976F88FFDAFB896.xml b/data/03/84/1C/03841C0BFF88FFE3C976F88FFDAFB896.xml new file mode 100644 index 00000000000..7e4d6d6def9 --- /dev/null +++ b/data/03/84/1C/03841C0BFF88FFE3C976F88FFDAFB896.xml @@ -0,0 +1,203 @@ + + + +Badenian Small Gastropods From Lăpugiu De Sus (Făget Basin, Romania). Rissoidae Family + + + +Author + +TĂMAȘ A. + + + +Author + +TĂMAȘ D. M. + + + +Author + +POPA M. V. + +text + + +Acta Palaeontologica Romaniae + + +2013 + +9 + + +1 + + +57 +66 + + + +journal article +10.5281/zenodo.13189681 +1842-371x +13189681 + + + + + + +Alvania +( +Alvania +) +ampulla +( +Eichwald, 1853 +) + + + + + + + +Fig. +2g + + + +1853 + +Riss. ampulla +m. - + +Eichwald, p. 274 + + +1954 + +Alvania montagui +var. +ampulla +Eichw. + +- Friedberg, p. 376, pl. 22, fig 12 + + +1966 + +Rissoa +( +Alvania +) +montagui miocaenica +Sacco + +- Strausz, p. 74, pl. 46, fig. 19, 20 + + +1971 + +Alvania +( +Alvania +) +montagui ampulla +(Eichwald) + +- Rado, pl. 4, fig. 70, 86 + + +1975 + +Alvania +( +Alvania +) +montagui ampulla +(Eichwald) + +- Bałuk, p. 79, pl. 9, fig. 9 + + +1981 + +Alvania montagui ampulla +(Eichwald) + +- Krach, p. 49, pl. 15, fig. 13-15 + + +2000 + +Alvania +( +Alvania +) +montagui ampulla +(Eichwald) + +- Popa and Ianoliu, p. 84, pl. 2, fig. 5 + + +2004 + +Alvania +( +Alvania +) +ampulla +(Eichwald) + +- Kowalke and Harzhauser, p. 119, fig. 6D + + +Material: +44 specimens +, + +19 from L5, 11 from Lp2 and 14 Lp10 ( +one specimen +PMBBU 23856 +) + + + +Description: Conical shell with 5-6 whorls; up to +2.25 mm +in height and +1.37 mm +in width. In adult specimens, the protoconch is only partly preserved; juvenile specimens show protoconch with two convex whorls ornamented with fine spiral threads. Teleoconch with slightly convex whorls and canaliculate suture. The last whorl is about 70% of the total shell height. It is ornamented with more-pronounced 16-20 axial ribs intersected by 6 spiral threads. Towards the base, additional 3-4 spiral threads. Oval aperture, slightly sharper towards the top. The inner lip partly covers the umbilicus while the external one shows inner denticles and external varix. + + +Distribution: identified in +Austria +( +Kowalke and Harzhauser, 2004 +), +Poland +( +Friedberg, 1954 +; +Bałuk, 1975 +; +Krach, 1981 +), +Hungary +( +Strausz, 1966 +), +Romania +( +Rado, 1971 +; +Popa and Ianoliu, 2000 +). + + + + \ No newline at end of file diff --git a/data/03/84/1C/03841C0BFF88FFE4C976FEEEFB75BDA9.xml b/data/03/84/1C/03841C0BFF88FFE4C976FEEEFB75BDA9.xml new file mode 100644 index 00000000000..9eeaf006179 --- /dev/null +++ b/data/03/84/1C/03841C0BFF88FFE4C976FEEEFB75BDA9.xml @@ -0,0 +1,222 @@ + + + +Badenian Small Gastropods From Lăpugiu De Sus (Făget Basin, Romania). Rissoidae Family + + + +Author + +TĂMAȘ A. + + + +Author + +TĂMAȘ D. M. + + + +Author + +POPA M. V. + +text + + +Acta Palaeontologica Romaniae + + +2013 + +9 + + +1 + + +57 +66 + + + +journal article +10.5281/zenodo.13189681 +1842-371x +13189681 + + + + + + +Alvania +( +Alvania +) +perregularis +(Sacco, 1895) + + + + + + +Fig. 2f + + +1895 + +Acinus Mariae + + +? +var. +perregularis +Sacc. + +– Sacco, 18, p. 25 + + +1954 + +Alvania perregularis +Sacco + +- Friedberg, p. 377, pl. 22, fig 14, 15 + + +1960 + +Alvania +( +Alvania +) +perregularis +(Sacco) + +- Kojumdgieva and Strachimirov, p. 100, pl. 30, fig. 16 a, b 1966 + +Rissoa +( +Alvania +) +perregularis +Sacco + +- Strausz, p. 73, pl. 46, fig. 12, 13 + + +1973 + +Alvania perregularis +Sacco + +– Bohn-Havas, p. 1037, pl. 3, fig. 1,2 + + +partim 1975 + +Alvania +( +Turbona +) +perregularis +(Sacco) + +– Bałuk, p. 85, pl. 9, fig. 14,15 + + +1981 + +Alvania (Turbona) perregularis +(Sacco) + +- Švagrovskỳ, p. 118, pl. 36, fig. 4 + + +partim 1981 + +Alvania perregularis +Sacco + +- Krach, p. 51, pl. 15, fig. 6 + + +1993 + +Alvania perregularis +Sacco + +- Șuraru and Papp, pl. V, fig 18 + + +2000 + +Alvania (Turbona) perregularis +(Sacco) + +- Popa and Ianoliu, p. 84, pl. 2, fig. 6 + + +2004 + +Alvania +( +Alvania +) +perregularis +(Sacco) + +– Kowalke and Harzhauser, p. 120, fig. 7B + + +Material: +eight specimens +, + +one from L5, one from L2, one from Lp4, and five from Lp10 ( +one specimen +PMBBU 23855 +) + + + +Description: Conical shell consisting of six whorls; up to +2.63 mm +in height and +1.55 mm +in width. Protoconch is consisting of about 2.75 convex whorls ornamented with finely grained spiral threads. The transition to the teleoconch is well-defined. The teleoconch shows flat whorls with canaliculate suture. Ornamentation represented by up to 37 axial ribs intersected by up to 14 spiral threads resulting in reticulated pattern with fine knots at the junctions. The last whorl represents about 70% of the total shell height. Drop-like aperture with inner lip partly covering the umbilicus. External lip with inner denticles. The shell shows varices both on the aperture area, and on other locations on the whorls. + + +Distribution: identified in +Czech Republic +( +Kowalke and Harzhauser, 2004 +), +Poland +( +Friedberg, 1954 +; +Bałuk, 1975 +; +Krach, 1981 +), Slovacia (Švagrovskỳ, 1981), +Hungary +( +Strausz, 1966 +; Bohn – Havas, 1973), +Bulgaria +( +Kojumdgieva and Strachimirov, 1960 +), +Romania +( +Șuraru and Papp, 1993 +; +Popa and Ianoliu, 2000 +). + + + + \ No newline at end of file diff --git a/data/03/84/1C/03841C0BFF88FFE4CAD0FABBFCF1BA4F.xml b/data/03/84/1C/03841C0BFF88FFE4CAD0FABBFCF1BA4F.xml new file mode 100644 index 00000000000..32e145c9236 --- /dev/null +++ b/data/03/84/1C/03841C0BFF88FFE4CAD0FABBFCF1BA4F.xml @@ -0,0 +1,146 @@ + + + +Badenian Small Gastropods From Lăpugiu De Sus (Făget Basin, Romania). Rissoidae Family + + + +Author + +TĂMAȘ A. + + + +Author + +TĂMAȘ D. M. + + + +Author + +POPA M. V. + +text + + +Acta Palaeontologica Romaniae + + +2013 + +9 + + +1 + + +57 +66 + + + +journal article +10.5281/zenodo.13189681 +1842-371x +13189681 + + + + + + +Alvania +( +Alvania +) +productilis +Boettger, 1906 + + + + + + +Fig. 2e + + +1906 + +Alvania +( +Alvania +) +productilis + +n. sp. +- Boettger, p. 156, nr. 539 + + +1934 + +Alvania +( +Alvania +) +productilis +Boettger + +- Zilch, p. 212, pl. 5, fig. 83 + + +1975 + +Alvania +( +Alvania +) +productilis +Boettger + +- Bałuk, p. 81, pl. 9, fig. 6 + + +1981 + +Alvania +( +Alvania +) +productilis +(Boettger) + +- Švagrovskỳ, p.117, pl. 36, fig. 6, 7 + + +Material: +two specimens + +from L5 ( +one specimen +PMBBU 23854 +) + + + +Description: Conical shell consisting of five whorls, up to +2.10 mm +in height and +1.25 mm +in width. + +Protoconch consists of two convex whorls ornamented with spiral threads; the transition to the teleoconch is not well noticeable. Teleoconch with convex whorls and a well-defined suture. On the first whorl there are 20 axial ribs intersected by four spiral threads. The last whorl represents about 70% of the total shell height; it is ornamented with 20 axial ribs intersected by spiral threads. The base is ornamented with four spiral threads. The aperture is drop-like. The inner lip covers the umbilicus, while the external none is thickened due to a varix; it presents inner denticles. + +Distribution: identified in +Poland +( +Bałuk, 1975 +), Slovacia (Švagrovskỳ, 1981), +Romania +(Boettger, 1906; +Zilch, 1934 +) + + + + \ No newline at end of file diff --git a/data/03/84/1C/03841C0BFF88FFE4CAD0FEEEFEF0BE7A.xml b/data/03/84/1C/03841C0BFF88FFE4CAD0FEEEFEF0BE7A.xml new file mode 100644 index 00000000000..7986deb576a --- /dev/null +++ b/data/03/84/1C/03841C0BFF88FFE4CAD0FEEEFEF0BE7A.xml @@ -0,0 +1,146 @@ + + + +Badenian Small Gastropods From Lăpugiu De Sus (Făget Basin, Romania). Rissoidae Family + + + +Author + +TĂMAȘ A. + + + +Author + +TĂMAȘ D. M. + + + +Author + +POPA M. V. + +text + + +Acta Palaeontologica Romaniae + + +2013 + +9 + + +1 + + +57 +66 + + + +journal article +10.5281/zenodo.13189681 +1842-371x +13189681 + + + + + + +Alvania +( +Alvania +) +oceani +( +d'Orbigny, 1852 +) + + + + + + +Fig. 2d + + +1852 + +Rissoa oceani +d’Orb. + +- d’Orbigny, p. 29, nr. 368 1954 + +Alvania oceani +d'Orb. + +- Friedberg, p. 377, pl. 22, fig. 13 + + +1975 + +Alvania +( +Alvania +) +oceani +(d'Orbigny) + +- Bałuk, p. 82, pl. 9, fig. 17 + + +1981 + +Alvania oceani +d'Orbigny + +- Krach, p. 49, pl. 15, fig. 1 + + +2004 + +Alvania +( +Alvania +) +oceani +(d'Orbigny) + +- Kowalke and Harzhauser, p. 120, fig. 7A. + + +Material: +two specimens +, + +one from L5 and one from Lp2 ( +one specimen +PMBBU 23859 +) + + + +Description: Elongated conical shell with five whorls; up to +2.7 mm +in height and +1.40 mm +in width. The protoconch is only partly preserved, as more than 2 convex whorls. Ornamentation is not visible under the stereomicroscope. Teleoconch with flattened first whorls and a last convex whorl with canaliculate suture. Ornamentation consisting of rounded axial ribs intersected by finer spiral threads; the latter become more pronounced towards the base of the shell. The last whorl represents about 65% of the total shell height. It is ornamented with 21 axial ribs intersected by 8 spiral threads. The shell base is covered by 5 spiral threads. Drop-like aperture, with inner lip covering the umbilicus and external lip showing inner denticles. Varices are present on the last-but-one whorl and in the aperture area. Distribution: identified in +Austria +( +Kowalke and Harzhauser, 2004 +), +Poland +( +Friedberg, 1954 +; +Bałuk, 1975 +; +Krach, 1981 +). + + + + \ No newline at end of file diff --git a/data/03/84/1C/03841C0BFF8AFFE4C976FA1CFEFDBBAB.xml b/data/03/84/1C/03841C0BFF8AFFE4C976FA1CFEFDBBAB.xml new file mode 100644 index 00000000000..f2bd875f9b7 --- /dev/null +++ b/data/03/84/1C/03841C0BFF8AFFE4C976FA1CFEFDBBAB.xml @@ -0,0 +1,181 @@ + + + +Badenian Small Gastropods From Lăpugiu De Sus (Făget Basin, Romania). Rissoidae Family + + + +Author + +TĂMAȘ A. + + + +Author + +TĂMAȘ D. M. + + + +Author + +POPA M. V. + +text + + +Acta Palaeontologica Romaniae + + +2013 + +9 + + +1 + + +57 +66 + + + +journal article +10.5281/zenodo.13189681 +1842-371x +13189681 + + + + + + +Rissoa costeiensis +Kowalke and Harzhauser, 2004 + + + + + + +Fig. 2c + + +2004 + +Rissoa costeiensis + +sp. nov. +- Kowalke and Harzhauser, p. 117, fig. 5B + + + +Material: +12 specimens +, 10 from L5, one from Lp2 and one from Lp10 ( +one specimen +PMBBU 23852 +) Description: Conical, elongated shell reaching up to +3 mm +in height and +1.5 mm +in width, with six whorls. The protoconch includes three convex whorls. The teleoconch shows convex whorls with incised suture and ornamentation consisting of prominent axial ribs with higher convexity in their median part. Fine spiral threads noticeable in the interspaces between the axial ribs, more prominent in the inferior half of the whorl. The last whorl is about 60% from the total height of the shell. It is ornamented with 16 axial ribs intersected by 12 spiral threads. Toward the base, 6-8 additional spiral threads are visible. Oval aperture, the inner lip partly covers the umbilicus, while the external one is thickened because of the varix + +. + + + +Fig. 2 - a + +Rissoa acuticosta +(Sacco, 1895) + +. +b + +Rissoa clotho +Hörnes, 1856 + +. +c + +Rissoa costeiensis +Kowalke & Harzhauser, 2004 + +. +d + +Alvania +( +Alvania +) +oceani +( +d'Orbigny, 1852 +) + +. +e + +Alvania +( +Alvania +) +productilis +Boettger, 1906 + +. +f + +Alvania +( +Alvania +) +perregularis +(Sacco, 1895) + +. +g + +Alvania +( +Alvania +) +ampulla +( +Eichwald, 1853 +) + +. +h + +Alvania +( +Alvania +) +helenae +Boettger, 1901 + +. +i + +Alvania +( +Alvania +) +transiens +(Sacco, 1895) + +. + + + +Distribution: identified in +Romania +( +Kowalke and Harzhauser, 2004 +). + + + + \ No newline at end of file diff --git a/data/03/84/1C/03841C0BFF8AFFE6C976FDFAFB71BE19.xml b/data/03/84/1C/03841C0BFF8AFFE6C976FDFAFB71BE19.xml new file mode 100644 index 00000000000..34532d62310 --- /dev/null +++ b/data/03/84/1C/03841C0BFF8AFFE6C976FDFAFB71BE19.xml @@ -0,0 +1,122 @@ + + + +Badenian Small Gastropods From Lăpugiu De Sus (Făget Basin, Romania). Rissoidae Family + + + +Author + +TĂMAȘ A. + + + +Author + +TĂMAȘ D. M. + + + +Author + +POPA M. V. + +text + + +Acta Palaeontologica Romaniae + + +2013 + +9 + + +1 + + +57 +66 + + + +journal article +10.5281/zenodo.13189681 +1842-371x +13189681 + + + + + + +Rissoa clotho +Hörnes, 1856 + + + + + + +Fig. 2b + + +1856 + +Rissoa clotho + +sp. nov. +- Höernes, p. 574, pl. 48, fig. 20 a,b + + +1975 + +Turboella +( +Turboella +) +clotho +(Hörnes) + +- Bałuk, p. 70, pl. 8, fig. 8 + + +2004 + +Rissoa clotho +Hörnes + +- Kowalke and Harzhauser, p.117, fig. 4D + + +Material: +13 specimens +, + +five from L5, four form Lp2, one from Lp3and three from Lp10 ( +one specimen +PMBBU 23851 +) + + + +Description: Conical-elongated shell consisting of six whorls reaching up to +3 mm +in height and +1.5 mm +in width. The protoconch is build-up of 2.25 convex whorls. The teleoconch displays convex whorls separated by an incised suture. Ornamentation consists of prominent axial ribs that become more convex over the suture. On the last whorls, in their lower half, one can notice fine spiral threads, more obvious on the last whorl. This latter represents about 55% of the total shell height and is ornamented with 12 axial ribs. Oval aperture, the inner lip covers the umbilicus while the external lip displays varices. + + +Distribution: identified in +Austria +( +Kowalke and Harzhauser, 2004 +), +Poland +( +Bałuk, 1975 +). + + + + \ No newline at end of file diff --git a/data/03/84/1C/03841C0BFF8DFFE0C976F8C8FD73BFE0.xml b/data/03/84/1C/03841C0BFF8DFFE0C976F8C8FD73BFE0.xml new file mode 100644 index 00000000000..818fd7f68ec --- /dev/null +++ b/data/03/84/1C/03841C0BFF8DFFE0C976F8C8FD73BFE0.xml @@ -0,0 +1,191 @@ + + + +Badenian Small Gastropods From Lăpugiu De Sus (Făget Basin, Romania). Rissoidae Family + + + +Author + +TĂMAȘ A. + + + +Author + +TĂMAȘ D. M. + + + +Author + +POPA M. V. + +text + + +Acta Palaeontologica Romaniae + + +2013 + +9 + + +1 + + +57 +66 + + + +journal article +10.5281/zenodo.13189681 +1842-371x +13189681 + + + + + + +Rissoina (Rissoina) pusilla +( +Brocchi, 1814 +) + + + + + + +Fig. 3f + + +1814 + +Turbo pusillus + +nob. – Brocchi, p. 181, pl. 6, fig. 5 1954 + +Rissoina pusilla +Brocc. + +- Friedberg, p. 356, pl. 20, fig 22 + + +1960 + +Rissoina +( +Rissoina +) +podolica +Cossmann + +- Kojumdgieva & Strachimirov, p. 102, pl. 30, fig. 19 + + +1960 + +Rissoina pusilla podolica +Cossmann + +- Strausz, p. 79, pl. 12, fig. 23-28 + + +part 1975 + +Risoina +( +Rissoina +) +podolica +Cossmann + +- Bałuk, p. 90, pl. 10, fig. 11 + + +1981 + +Rissoina +( +Rissoina +) +podolica +Cossmann + +- Švagrovskỳ, p. 122, pl. 38, fig. 1-4 + + +1981 + +Rissoina podolica +Cossmann + +- Krach, p 51, pl. 15, fig. 25, 26, 34, 35 + + +1993 + +Rissoina podolica +Cossmann + +- Șuraru & Papp, pl. V, fig. 22 + + +2004 + +Rissoina (Rissoina) pusilla +(Brocchi) + +- Landau et al., p. 52, pl 12, fig. 1 + + +Material: +two specimens + +from Lp4 ( +one specimen +PMBBU 23864 +) + + + +Description: Elongated, incompletely preserved shell; up to +5.25 mm +in height and +2.5 mm +in width, first whorls not included. Teleoconch with more than five flattened whorls and incised suture. Ornamentation consisting of fine axial ribs showing a straight orientation on the first whorls and a slightly sinusoidal one towards the last ones. There are 22 to 24 ribs on the last whorl. Numerous extremely fine spiral threads present in the interspaces between the axial rib areas. Three spiral threads are more prominent on the last-but-one supra-suture whorl and nine on the last whorl towards the base of the shell. Oval, siphonostome oblique aperture; umbilicus covered by labrum, the latter thickened due to the presence of a varix. + + +Distribution: identified in: +Austria +( +Kowalke & Harzhauser, 2004 +), +Poland +( +Friedberg, 1954 +; +Bałuk, 1975 +; +Krach, 1981 +), Slovacia (Švagrovskỳ, 1981), +Hungary +( +Strausz, 1966 +), +Bulgaria +( +Kojumdgieva and Strachimirov, 1960 +), +Romania +( +Șuraru and Papp, 1993 +). + + + + \ No newline at end of file diff --git a/data/03/84/1C/03841C0BFF8DFFE1C976FC65FA14BC6A.xml b/data/03/84/1C/03841C0BFF8DFFE1C976FC65FA14BC6A.xml new file mode 100644 index 00000000000..4bebd84ac2c --- /dev/null +++ b/data/03/84/1C/03841C0BFF8DFFE1C976FC65FA14BC6A.xml @@ -0,0 +1,134 @@ + + + +Badenian Small Gastropods From Lăpugiu De Sus (Făget Basin, Romania). Rissoidae Family + + + +Author + +TĂMAȘ A. + + + +Author + +TĂMAȘ D. M. + + + +Author + +POPA M. V. + +text + + +Acta Palaeontologica Romaniae + + +2013 + +9 + + +1 + + +57 +66 + + + +journal article +10.5281/zenodo.13189681 +1842-371x +13189681 + + + + + + +Rissoina (Rissoina) vindobonensis +Sacco, 1895 + + + + + + +Fig. 3e + + +1895 + +Rissoina bruguieri vindobonensis +Sacc. + +- Sacco, 18, p. 35 + + +1960 + +Rissoina +( +Rissoina +) +vindobonensis +(Sacco) + +- Kojumdgieva and Strachimirov, p.102, pl. 30, fig. 20 a, b 1975 + +Rissoina +( +Rissoina +) +vindobonensis +Sacco + +- Bałuk, p. 91, pl. 10, fig. 6,7 + + +1981 + +Rissoina +( +Rissoina +) +vindobonensis +(Sacco) + +- Krach, p 52, pl. 15, fig. 23, 24, 29, 30 + + + +Material: +one specimen +from L5 ( +PMBBU 23863 +) Description: Slender, elongated turriculated shell with more than six whorls; up to +4.3 mm +in height and +1.90 mm +in width + +. + +Protoconch not fully preserved. Teleoconch with 5.5 slightly-convex whorls and incised suture. Ornamentation consisting of opisthocline axial ribs, more pronounced on the first whorls and finer on the last one. Fine spiral threads in the interspaces between the axial rib area. The last whorl represents 60% of the total shell height. Ornamentation is represented by 22 axial ribs alternating with fine spiral threads. The shell’s base is ornamented with fine more pronounced spiral threads. Large and inclined aperture; covered umbilicus and external lip thickened by varix. + +Distribution: identified in: +Polonia +( +Bałuk, 1975 +; +Krach, 1981 +), +Bulgaria +( +Kojumdgieva and Strachimirov, 1960 +). + + + + \ No newline at end of file diff --git a/data/03/84/1C/03841C0BFF8DFFE1CAD0F82FFB46B8D3.xml b/data/03/84/1C/03841C0BFF8DFFE1CAD0F82FFB46B8D3.xml new file mode 100644 index 00000000000..7955dc795cc --- /dev/null +++ b/data/03/84/1C/03841C0BFF8DFFE1CAD0F82FFB46B8D3.xml @@ -0,0 +1,157 @@ + + + +Badenian Small Gastropods From Lăpugiu De Sus (Făget Basin, Romania). Rissoidae Family + + + +Author + +TĂMAȘ A. + + + +Author + +TĂMAȘ D. M. + + + +Author + +POPA M. V. + +text + + +Acta Palaeontologica Romaniae + + +2013 + +9 + + +1 + + +57 +66 + + + +journal article +10.5281/zenodo.13189681 +1842-371x +13189681 + + + + + + +Rissoina +( +Phosinella +) +steinabrunnensis +Sacco 1895 + + + + + + +Fig. 3d + + +1895 + +Rissolina lamellosa + +var. + +Steinabrunnensis +Sacc. + +– Sacco, 18, p. 37 + + +1966 + +Rissoina +( +Phosinella +) +steinabrunnensis +Sacco + +- Strausz, p. 80, pl. 12, fig. 15-18 + + +1975 + +Rissoina +( +Phosinella +) +steinabrunnensis +Sacco + +- Bałuk, p. 95, pl. 10, fig. 4,5 + + +1981 + +Rissoina steinabrunnensis +Sacco + +- Krach, p 52, pl. 15, fig. 27, 28 + + +2006 + +Rissoina +( +Phosinella +) +steinabrunnensis +Sacco + +- Bałuk, p. 189, pl. 4, fig. 1 + + +Material: +two specimens + +from L5 ( +one specimen +PMBBU 23862 +) + + + +Description: Slender and elongated turriculated shell with about seven whorls; up to +4.20 mm +in height and +1.90 mm +in width. Protoconch consisting of about 2.5 convex whorls lacking ornamentation. Teleoconch with convex whorls and deep suture. Ornamentation consisting of prominent axial ribs, arched underneath the suture; this leads to an overall scalariform shell morphology. Fine spiral threads cross-cut the axial ribs. The last whorl represents about 55% of the total shell height. It is ornamented with 17 axial ribs intersected by 13 fine spiral threads, more pronounced towards the base. The oval aperture has an oblique orientation. Weakly incised anterior canal peristome and labrum with external varix. + + +Distribution: identified in: +Poland +( +Bałuk, 1975 +, +2006 +; +Krach, 1981 +), +Hungary +( +Strausz, 1966 +). + + + + \ No newline at end of file diff --git a/data/03/84/1C/03841C0BFF8FFFE3CAD0F8A8FB71B8D3.xml b/data/03/84/1C/03841C0BFF8FFFE3CAD0F8A8FB71B8D3.xml new file mode 100644 index 00000000000..945dec229f2 --- /dev/null +++ b/data/03/84/1C/03841C0BFF8FFFE3CAD0F8A8FB71B8D3.xml @@ -0,0 +1,168 @@ + + + +Badenian Small Gastropods From Lăpugiu De Sus (Făget Basin, Romania). Rissoidae Family + + + +Author + +TĂMAȘ A. + + + +Author + +TĂMAȘ D. M. + + + +Author + +POPA M. V. + +text + + +Acta Palaeontologica Romaniae + + +2013 + +9 + + +1 + + +57 +66 + + + +journal article +10.5281/zenodo.13189681 +1842-371x +13189681 + + + + + + +Alvania +( +Alvania +) +transiens +(Sacco, 1895) + + + + + + +Fig. 2i + + +1895 + +Alvania sculpta + + +? var. +transiens + +– Sacco, 18, p. 27 1954 + +Alvania venus +var. +danubiensis +Cossm. et Peyr. + +- Friedberg, p. 379, pl. 22, fig 17 + + +1966 + +Rissoa +( +Alvania +) +venus danubiensis +Cossmann and Peyrot + +- Strausz, p. 72, pl. 46, fig. 17,18 + + +1975 + +Alvania +( +Acinulus +) +venus transiens +Sacco + +– Bałuk p. 86, pl. 9, fig. 18,19 + + +1981 + +Alvania venus transiens +Sacco + +- Krach, p 51, pl. 15, fig. 9-12 + + +2004 + +Alvania +( +Alvania +) +transiens +(Sacco) + +- Kowalke and Harzhauser, p. 121, fig. 7C + + +Material: +five specimens +, + +three from L5 and two from Lp10 ( +one specimen +PMBBU 23858 +) + + + +Description: Elongated conical shell consisting of six whorls; up to +3.25 mm +in heights and +1.60 mm +in width. Protoconch consisting of about 2.75 convex whorls ornamented with spiral threads. Teleoconch with slightly convex whorls and canaliculate suture. Ornamentation consisting of axial ribs intersected by spiral threads of equal intensity. This leads to the formation of a reticulated network with sharp knots at the intersection. The last whorl is about 65% of the total shell; ornamented with 16–21 axial ribs and six spiral threads. Two additional well-defined spiral threads are noticeable towards the base. Drop-like aperture; the inner lip covers the umbilicus, external lip shows an external varix and inner denticles. + + +Distribution: identified in +Poland +( +Friedberg, 1954 +; +Bałuk, 1975 +; +Krach, 1981 +), +Hungary +( +Strausz, 1966 +), +Austria +( +Kowalke and Harzhauser, 2004 +). + + + + \ No newline at end of file diff --git a/data/03/84/1C/03841C0BFF8FFFE3CAD0FB87FE46BC75.xml b/data/03/84/1C/03841C0BFF8FFFE3CAD0FB87FE46BC75.xml new file mode 100644 index 00000000000..9c66ac98791 --- /dev/null +++ b/data/03/84/1C/03841C0BFF8FFFE3CAD0FB87FE46BC75.xml @@ -0,0 +1,135 @@ + + + +Badenian Small Gastropods From Lăpugiu De Sus (Făget Basin, Romania). Rissoidae Family + + + +Author + +TĂMAȘ A. + + + +Author + +TĂMAȘ D. M. + + + +Author + +POPA M. V. + +text + + +Acta Palaeontologica Romaniae + + +2013 + +9 + + +1 + + +57 +66 + + + +journal article +10.5281/zenodo.13189681 +1842-371x +13189681 + + + + + + +Alvania +( +Alvania +) +helenae +Boettger, 1901 + + + + + + +Fig. 2h + + +1901 + +Alvania +( +Alvania +) +helenae + +n. sp. +- Boettger, p. 140, nr. 432 + + +1934 + +Alvania +( +Alvania +) +helenae +Boettger + +- Zilch, p. 211, pl. 5, fig 81 + + +1975 + +Alvania +( +Alvania +) +helenae +Boettger + +- Bałuk, p. 81, pl. 9, fig. 10 + + +Material: +four specimens + +from L5 ( +one specimen +PMBBU 23857 +) + + + +Description: Elongated conical shell with 5 whorls; up to +2.75 mm +in heights and +1.63 mm +in width. Protoconch consisting of about two convex whorls ornamented with spiral threads. Teleoconch with convex whorls ornamented with pronounced axial ribs intersected by finer spiral threads; knots form at the intersection. The last-but-one whorl shows one varix. The last whorl represents 65–70% of the total shell height; ornamented with 14-18 axial ribs intersected by 6 spiral threads. Towards the base, four additional spiral threads are noticeable. Drop-like aperture, with the inner lip covering the umbilicus. External lip with inner denticles and external varix. + + +Distribution: identified in +Poland +( +Bałuk, 1975 +), +Romania +( +Boettger, 1901 +; +Zilch, 1934 +). + + + + \ No newline at end of file diff --git a/data/03/96/87/039687F3FFAFFFAEFF6CFEC960032F1E.xml b/data/03/96/87/039687F3FFAFFFAEFF6CFEC960032F1E.xml new file mode 100644 index 00000000000..1a4bb3ce5c4 --- /dev/null +++ b/data/03/96/87/039687F3FFAFFFAEFF6CFEC960032F1E.xml @@ -0,0 +1,107 @@ + + + +Lower Cretaceous Calcareous Algae And Foraminifera From Trbušnica (Vardar Zone, Serbia) + + + +Author + +Bucur, Ioan I. +Babeş-Bolyai University, Department of Geology and Center for Integrated Geological Studies, str. M. Kogălniceanu nr. 1, + + + +Author + +Polavder, Svetlana +Faculty of Ecology and Environmental Protection, Department of Geology, Union-Nikola Tesla University, Cara Dusana 62 - 64, 11 000 Beograd, Serbia. polavder @ open. telekom. rs +polavder@open.telekom.rs + + + +Author + +Radoičić, Rajka +Kralja Petra I, 38, 11158 Beograd, Serbia. rajkaradoicic @ gmail. com +rajkaradoicic@gmail.com + +text + + +Acta Palaeontologica Romaniae + + +2014 + +2014-11-18 + + +10 + + +1 - 2 + + +1 +2 + + + +journal article +10.5281/zenodo.13190103 +1842-371x +13190103 + + + + + + +Andreiella rajkae +Bucur, 2014 + + + + + + +( +Fig. 5 e +) + + + +Andreiella rajkae + +was recently described by +Bucur (2014) +from Upper Barremian – lowermost Aptian (lower Bedoulian) limestones in the Hăghimaş Mountains (Eastern Carpathians, +Romania +). It is characterized by a cylindrical thallus with a narrow main stem and two orders of laterals. The first order laterals, large and clubshaped, gradually broaden from the proximal to the distal part where they slightly narrow towards the exterior. The secondary laterals are short and vesiculiform to ovoid in shape. Calcification forms an irregular sleeve around the distal end of the primary laterals, embedding the secondary ones. + + +A single specimen was identified in the studied samples from Trbušnica ( +Fig. 5 e +), however it is very representative for the species. Until this study, + +A. rajkae + +has been identified in only three sites: Mount Rujen (Vardar zone, +Macedonia +) (Radoičić, 2002), Bicaz Gorges (Hăghimaş Mountains, Eastern Carpathians, +Romania +) ( +Bucur & Săsăran, 2011 +; +Bucur, 2014 +), and Munella Platform ( +Albania +) (Schlagintweit, unpublished; +Bucur, 2014 +). Thus, Trbušnica represents the fourth location for this species. + +Dimensions (mm): D = 2.60; d = 0.60; p (distal) = 0.30; p’ = 0.07. + + + \ No newline at end of file diff --git a/data/03/98/87/03988783FFA7FF9B83FEFB32F42FFB3D.xml b/data/03/98/87/03988783FFA7FF9B83FEFB32F42FFB3D.xml new file mode 100644 index 00000000000..f990079ec07 --- /dev/null +++ b/data/03/98/87/03988783FFA7FF9B83FEFB32F42FFB3D.xml @@ -0,0 +1,147 @@ + + + +Zagrosella Rigaudii N. Gen., N. Sp., A New Biokovinoidean Foraminifer From The Maastrichtian Of Iran + + + +Author + +Schlagintweit, Felix +Lerchenauerstr. 167, 80935 Munich, Germany, * Corresponding author: felix. schlagintweit @ gmx. de +felix.schlagintweit@gmx.de + + + +Author + +Rashidi, Koorosh +Department of Geology, Payame Noor University, Po Box 19395 - 3697 Tehran, Iran, kooroshrashidi @ pnu. ac. ir +kooroshrashidi@pnu.ac.ir + +text + + +Acta Palaeontologica Romaniae + + +2017 + +2017-03-15 + + +13 + + +1 + + +3 +13 + + + +journal article +10.5281/zenodo.13189884 +1842-371x +13189884 + + + + + +Family + +Biokovinidae +Gušić, 1977 + + + + + + +Remarks: +Loeblich and Tappan (1987 +, p. 91) defined the +Biokovinidae +as follows: “Test enrolled, at least in early stage, later may uncoil; wall coarsely perforated, in section appearing almost keriothecal, and honeycomb-like in transverse section; aperture simple, single, or multiple. Jurassic”. +Loeblich and Tappan (1987) +included the three genera + +Biokovina +Gušić, 1977 + +, + +Bosniella +Gušić, 1977 + +, and + +Chablaisia +Septfontaine, 1978 + +. The presence of internal structures (here: pillars) is not mentioned by +Loeblich and Tappan (1987) +, but + +Biokovina + +possesses endoskeletal pillars. +Mikhalevich (2004 +, p. 257) in addition included the presence of “phrenothekalike structures and endoskeletal elements (pillars)” in the diagnosis of the +Biokovinidae +. Concerning the “phrenothekalike structures” reference is made to comments included in the species comparison later in the present paper. Mikhalevich transferred + +Chablaisia + +to the pfenderinids and removed + +Bosniella + +from the +Biokovinidae +due to the lack of endoskeletal structures. In the recent classification of agglutinated benthic foraminifera provided by +Kaminski (2014) +, the +Biokovinidae +includes the three genera + +Biokovina + +(with endoskeleton; no exoskeleton), + +Bosniella + +(neither endo- nor exoskeleton), and + +Trochamijiella +Athersuch, Banner & Simmons, 1992 + +(without endoskeleton; with exoskeleton), taxa with and without internal structures. It is worth mentioning that + +Trochamijiella + +does not fit the family diagnosis provided by Loeblich and Tappan due to the lack of a perforated wall. The new genus + +Zagrosella + +is here placed into the family +Biokovinidae +with strict application of the diagnosis provided by +Loeblich and Tappan (1987) +. In fact, at the actual state of knowledge there aren’t other families of complex larger benthic foraminifera (with or without Cretaceous representatives) with equivalent or similar morphology and wall structure in which the Maastrichtian taxon from +Iran +can be accommodated. In any case, + +Zagrosella + +fits the diagnosis of the superfamily +Biokovinoidea Gušić +(= Biokovinacea Gušić in +Loeblich and Tappan, 1987 +) whose range was indicated as Lower Jurassic (Middle Jurassic) to Maastrichtian, thereby becoming one of its youngest representatives. + + + + \ No newline at end of file diff --git a/data/03/9D/87/039D87CD6E331E09A367FAE2792A382B.xml b/data/03/9D/87/039D87CD6E331E09A367FAE2792A382B.xml new file mode 100644 index 00000000000..183484ed68b --- /dev/null +++ b/data/03/9D/87/039D87CD6E331E09A367FAE2792A382B.xml @@ -0,0 +1,96 @@ + + + +Latest Jurassic - Early Cretaceous Dasycladalean Algae (Chlorophyta) From The Morand Drilling At Montricher (Canton Of Vaud, Switzerland) + + + +Author + +Granier, Bruno +Department of Ecology and Evolutionary Biology, The University of Kansas, 1200 Sunnyside Avenue, Lawrence, Kansas 66045, USA (bgranier @ ku. edu) +bgranier@ku.edu + + + +Author + +Clavel, Bernard +24, ch. des Champs d’Amot, 74140 Messery, France (b. clavel 1 @ orange. fr) + + + +Author + +Charollais, Jean +Département de Géologie et de Paléontologie, Sciences de la Terre et de l ¹ Environnement, 13, r. des Maraîchers, 1211 Genève 4, Switzerland (jdcharollais @ bluewin. ch) +jdcharollais@bluewin.ch + + + +Author + +MarcWeidmann +3, sentier du Molard, 1805 Jongny, Switzerland (weidmann-dutoit @ bluewin. ch) +weidmann-dutoit@bluewin.ch + +text + + +Acta Palaeontologica Romaniae + + +2014 + +2014-09-29 + + +10 + + +1 - 2 + + +1 +2 + + + +journal article +10.5281/zenodo.13189719 +1842-371x +13189719 + + + + + + +Falsolikanella danilovae +(Radoičić +ex +Barattolo) + + + + + + +( +Fig. 3 +g-h; +Fig. 7h +) + + +It is known as a typical Urgonian species; however, it is lacking in uppermost Barremian and Bedoulian strata ( + +Clavel +et al. +, 2007 + +, 2013). Here we find it in both the “Urgonien jaune” and the “Urgonien blanc”. + + + + \ No newline at end of file diff --git a/data/03/9D/87/039D87CD6E331E0FA367F9D77EB83EE1.xml b/data/03/9D/87/039D87CD6E331E0FA367F9D77EB83EE1.xml new file mode 100644 index 00000000000..6ae3a7c8416 --- /dev/null +++ b/data/03/9D/87/039D87CD6E331E0FA367F9D77EB83EE1.xml @@ -0,0 +1,107 @@ + + + +Latest Jurassic - Early Cretaceous Dasycladalean Algae (Chlorophyta) From The Morand Drilling At Montricher (Canton Of Vaud, Switzerland) + + + +Author + +Granier, Bruno +Department of Ecology and Evolutionary Biology, The University of Kansas, 1200 Sunnyside Avenue, Lawrence, Kansas 66045, USA (bgranier @ ku. edu) +bgranier@ku.edu + + + +Author + +Clavel, Bernard +24, ch. des Champs d’Amot, 74140 Messery, France (b. clavel 1 @ orange. fr) + + + +Author + +Charollais, Jean +Département de Géologie et de Paléontologie, Sciences de la Terre et de l ¹ Environnement, 13, r. des Maraîchers, 1211 Genève 4, Switzerland (jdcharollais @ bluewin. ch) +jdcharollais@bluewin.ch + + + +Author + +MarcWeidmann +3, sentier du Molard, 1805 Jongny, Switzerland (weidmann-dutoit @ bluewin. ch) +weidmann-dutoit@bluewin.ch + +text + + +Acta Palaeontologica Romaniae + + +2014 + +2014-09-29 + + +10 + + +1 - 2 + + +1 +2 + + + +journal article +10.5281/zenodo.13189719 +1842-371x +13189719 + + + + + + +Selliporella neocomiensis +(Radoičić) + + + + + + +( +Fig. 3f +) + + +This species, also known as + +Diplopora johnsoni +Praturlon + +, is commonly referred to the Tithonian-Berriasian interval. Younger occurrences (Hauterivian) are probably erroneous dating ( +Granier & Deloffre, 1993 +; +Bucur & Săsăran, 2003 +). The unique specimen was found in the transition between the Vions and Pierre Châtel formations. + + +The organogenus + +Carpathoporella +Dragastan, 1995 + +, possibly refers to skeletal remains very similar to isolated calcified laterals of Selliporellas; these bioclasts might be broken pieces of a discrete species. According to +Schlagintweit and Gawlick (2009) +, this +form refers +to octocorallian debris, a view that we do not share. We identify Carpathoporellas in both Urgonian units + + + + \ No newline at end of file diff --git a/data/03/9D/87/039D87CD6E351E0CA367F9D77E373F02.xml b/data/03/9D/87/039D87CD6E351E0CA367F9D77E373F02.xml new file mode 100644 index 00000000000..de92b7a08d9 --- /dev/null +++ b/data/03/9D/87/039D87CD6E351E0CA367F9D77E373F02.xml @@ -0,0 +1,384 @@ + + + +Latest Jurassic - Early Cretaceous Dasycladalean Algae (Chlorophyta) From The Morand Drilling At Montricher (Canton Of Vaud, Switzerland) + + + +Author + +Granier, Bruno +Department of Ecology and Evolutionary Biology, The University of Kansas, 1200 Sunnyside Avenue, Lawrence, Kansas 66045, USA (bgranier @ ku. edu) +bgranier@ku.edu + + + +Author + +Clavel, Bernard +24, ch. des Champs d’Amot, 74140 Messery, France (b. clavel 1 @ orange. fr) + + + +Author + +Charollais, Jean +Département de Géologie et de Paléontologie, Sciences de la Terre et de l ¹ Environnement, 13, r. des Maraîchers, 1211 Genève 4, Switzerland (jdcharollais @ bluewin. ch) +jdcharollais@bluewin.ch + + + +Author + +MarcWeidmann +3, sentier du Molard, 1805 Jongny, Switzerland (weidmann-dutoit @ bluewin. ch) +weidmann-dutoit@bluewin.ch + +text + + +Acta Palaeontologica Romaniae + + +2014 + +2014-09-29 + + +10 + + +1 - 2 + + +1 +2 + + + +journal article +10.5281/zenodo.13189719 +1842-371x +13189719 + + + + + + +Deloffrella quercifoliipora +Granier & Michaud + + + + + + +( + +Fig. +6m + +) + +Selected references: + + +1987 + +Deloffrella quercifoliipora + +n.gen. +n.sp.- +Granier +& +Michaud, Pl. +I +, figs. 1-10, +San Ricardo Formation +, +Kimmeridgian-Tithonian +, +Poblado Catorce +, +Chiapas +( +Mexico +) + + + +1990 + +Deloffrella quercifoliipora + +.- Conrad & Varol, Fig. 8 (right),? Hauterivian, +Elburz +( +Iran +) + + + +2013b + +Deloffrella quercifoliipora +Granier & Michaud. + +- Granier, +Fig. 4.10 +, Morand borehole, - + +271m + +, +Vions Formation +, +Upper Berriasian +, +Montricher +, +Vaud +( +Switzerland +) + + + +Initially described from uppermost Jurassic strata in +Chiapas +, +Mexico +( +Granier & Michaud, 1987 +), this random sections of verticils of + +Actinoporella +sp. + +, Pierre Châtel Formation, Middle Berriasian, sample 319. + + + +Fig. 4 +a to n (scale bar: 500 µm): +a +random sections of laterals of + +Rajkaella bartheli + +, transition Pierre Châtel - Goldberg formations, Lower-Middle Berriasian, sample 320; +b +section of a lateral of + +Rajkaella bartheli + +, transition Pierre Châtel - Goldberg formations, Lower-Middle Berriasian, sample 320; +c +transverse section of a charophyte stalk, + +Charaxis +sp. + +, Goldberg Fm, Lower Berriasian, sample 324; +d +axial sections of charophyte stalks, + +Charaxis +sp. + +, Goldberg Fm, Lower Berriasian, sample 325; +e +transverse section of a charophyte stalk, Goldberg Fm, Lower Berriasian, sample 325; +f +axial section of a charophyte oogonium, Goldberg Fm, Lower Berriasian, sample 321; +g +tufts of secondary laterals of + +Rajkaella bartheli +, Pierre Châtel Formation, Middle Berriasian + +, sample 303; +h +tufts of secondary laterals of + +Rajkaella bartheli +, Pierre Châtel Formation, Middle Berriasian + +, sample 316; +i +section of a lateral of + +Rajkaella bartheli +, Pierre Châtel Formation, Middle Berriasian + +, sample 319; +j +tufts of secondary laterals of + +Rajkaella bartheli +, Pierre Châtel Formation, Middle Berriasian + +, sample 303; +k +section of a lateral of + +Rajkaella bartheli +, Pierre Châtel Formation, Middle Berriasian + +, sample 319; +l +deep tangential section of a verticil of + +Actinoporella +sp. + +(note: the corona structure is visible), "Urgonien jaune", Upper Hauterivian, sample 114; +m +oblique section of a verticil of + +Actinoporella +sp. + +, Pierre Châtel Formation, Middle Berriasian, sample 319; n + + + + +Fig. 5 a +to +p +(scale bar: 250 µm): +a +random section of + +Terquemella +sp. + +, "Urgonien jaune", Upper Hauterivian, sample 107; +b +random section of + +Terquemella +sp. + +, "Urgonien jaune", Upper Hauterivian, sample 128; +c +subtransverse section of + +Deloffrella hauteriviana + +, " Pierre jaune", Lower Hauterivian, sample 171; +d +section of a lateral of + +Rajkaella minima +, Vions Fm + +, Upper Berriasian, sample 287; +e +section of a lateral of + +Rajkaella minima +, Pierre Châtel Formation, Middle Berriasian + +, sample 312; +f +subtransverse section of + +Salpingoporella steinhauseri +, Pierre Châtel Formation, Middle Berriasian + +, sample 307; +g +oblique section of + +Salpingoporella steinhauseri +, Pierre Châtel Formation, Middle Berriasian + +, sample 307; +h +tangential section of + +Salpingoporella steinhauseri +, Pierre Châtel Formation, Middle Berriasian + +, sample 307; +i +oblique section of a verticil of + +Actinoporella +sp. + +(note: the corona structure is visible), Pierre Châtel Formation, Middle Berriasian, sample 301; +j +oblique section of a verticil of + +Clypeina parasolkani +, Pierre Châtel Formation, Middle Berriasian + +, sample 310; +k +subaxial section of a verticil of + +Clypeina parasolkani +, Pierre Châtel Formation, Middle Berriasian + +, sample 310; +l +oblique section of a verticil of + +Clypeina parasolkani +, Pierre Châtel Formation, Middle Berriasian + +, sample 310; +m +subtransverse section of a verticil of + +Clypeina parasolkani +, Pierre Châtel Formation, Middle Berriasian + +, sample 309; +n +oblique section of + +Clypeina +aff. +parasolkani + +(two fertile verticils visible), transition Vions - Pierre Châtel formations, Middle-Upper Berriasian, sample 291.8; +o +subaxial section of + +Clypeina +aff. +parasolkani + +(three fertile verticils visible), transition Vions - Pierre Châtel formations, Middle-Upper Berriasian, sample 291.8; +p +oblique section of + +Otternstella lemmensis +, Pierre Châtel Formation, Middle Berriasian + +, sample 317 + + + +Tethyan species has been reported several times from discrete localities ( +Senegal +, +Algiers +, +Romania +, +Iran +, +etc. +). Its total stratigraphic range spans the Kimmeridgian to the Aptian times ( +Granier & Deloffre, 1993 +). Here it is found only in the Vions Formation. + + + + \ No newline at end of file diff --git a/data/03/9D/87/039D87CD6E351E0FA0C1FAE27E313864.xml b/data/03/9D/87/039D87CD6E351E0FA0C1FAE27E313864.xml new file mode 100644 index 00000000000..1fcea08d006 --- /dev/null +++ b/data/03/9D/87/039D87CD6E351E0FA0C1FAE27E313864.xml @@ -0,0 +1,96 @@ + + + +Latest Jurassic - Early Cretaceous Dasycladalean Algae (Chlorophyta) From The Morand Drilling At Montricher (Canton Of Vaud, Switzerland) + + + +Author + +Granier, Bruno +Department of Ecology and Evolutionary Biology, The University of Kansas, 1200 Sunnyside Avenue, Lawrence, Kansas 66045, USA (bgranier @ ku. edu) +bgranier@ku.edu + + + +Author + +Clavel, Bernard +24, ch. des Champs d’Amot, 74140 Messery, France (b. clavel 1 @ orange. fr) + + + +Author + +Charollais, Jean +Département de Géologie et de Paléontologie, Sciences de la Terre et de l ¹ Environnement, 13, r. des Maraîchers, 1211 Genève 4, Switzerland (jdcharollais @ bluewin. ch) +jdcharollais@bluewin.ch + + + +Author + +MarcWeidmann +3, sentier du Molard, 1805 Jongny, Switzerland (weidmann-dutoit @ bluewin. ch) +weidmann-dutoit@bluewin.ch + +text + + +Acta Palaeontologica Romaniae + + +2014 + +2014-09-29 + + +10 + + +1 - 2 + + +1 +2 + + + +journal article +10.5281/zenodo.13189719 +1842-371x +13189719 + + + + + + +Clypeina sulcata +(Alth) + + + + + + +( +Fig. 3 +j-l) + + +This well known species, which may appear in the literature as + +Cl. jurassica +Favre + +in +Favre & Richard, is the second species of dasycladalean algae listed here that is mineralized with calcite instead of aragonite ( +Conrad & Varol, 1990 +; +Granier, 2012 +). It is found only in the lowermost Pierre Châtel Formation. + + + + \ No newline at end of file diff --git a/data/03/9D/87/039D87CD6E351E0FA0C1FCCA7EA73DA7.xml b/data/03/9D/87/039D87CD6E351E0FA0C1FCCA7EA73DA7.xml new file mode 100644 index 00000000000..06b00ce9c6c --- /dev/null +++ b/data/03/9D/87/039D87CD6E351E0FA0C1FCCA7EA73DA7.xml @@ -0,0 +1,87 @@ + + + +Latest Jurassic - Early Cretaceous Dasycladalean Algae (Chlorophyta) From The Morand Drilling At Montricher (Canton Of Vaud, Switzerland) + + + +Author + +Granier, Bruno +Department of Ecology and Evolutionary Biology, The University of Kansas, 1200 Sunnyside Avenue, Lawrence, Kansas 66045, USA (bgranier @ ku. edu) +bgranier@ku.edu + + + +Author + +Clavel, Bernard +24, ch. des Champs d’Amot, 74140 Messery, France (b. clavel 1 @ orange. fr) + + + +Author + +Charollais, Jean +Département de Géologie et de Paléontologie, Sciences de la Terre et de l ¹ Environnement, 13, r. des Maraîchers, 1211 Genève 4, Switzerland (jdcharollais @ bluewin. ch) +jdcharollais@bluewin.ch + + + +Author + +MarcWeidmann +3, sentier du Molard, 1805 Jongny, Switzerland (weidmann-dutoit @ bluewin. ch) +weidmann-dutoit@bluewin.ch + +text + + +Acta Palaeontologica Romaniae + + +2014 + +2014-09-29 + + +10 + + +1 - 2 + + +1 +2 + + + +journal article +10.5281/zenodo.13189719 +1842-371x +13189719 + + + + + + +Angioporella fouryae +Masse +et al. + + + + + + +( +Fig. 6o +; +Fig. 7l, n +) + +We identified it only in the “Urgonien jaune”. + + + \ No newline at end of file diff --git a/data/03/9D/87/039D87CD6E351E0FA367FDE379463D0B.xml b/data/03/9D/87/039D87CD6E351E0FA367FDE379463D0B.xml new file mode 100644 index 00000000000..e2e8a9acb0f --- /dev/null +++ b/data/03/9D/87/039D87CD6E351E0FA367FDE379463D0B.xml @@ -0,0 +1,96 @@ + + + +Latest Jurassic - Early Cretaceous Dasycladalean Algae (Chlorophyta) From The Morand Drilling At Montricher (Canton Of Vaud, Switzerland) + + + +Author + +Granier, Bruno +Department of Ecology and Evolutionary Biology, The University of Kansas, 1200 Sunnyside Avenue, Lawrence, Kansas 66045, USA (bgranier @ ku. edu) +bgranier@ku.edu + + + +Author + +Clavel, Bernard +24, ch. des Champs d’Amot, 74140 Messery, France (b. clavel 1 @ orange. fr) + + + +Author + +Charollais, Jean +Département de Géologie et de Paléontologie, Sciences de la Terre et de l ¹ Environnement, 13, r. des Maraîchers, 1211 Genève 4, Switzerland (jdcharollais @ bluewin. ch) +jdcharollais@bluewin.ch + + + +Author + +MarcWeidmann +3, sentier du Molard, 1805 Jongny, Switzerland (weidmann-dutoit @ bluewin. ch) +weidmann-dutoit@bluewin.ch + +text + + +Acta Palaeontologica Romaniae + + +2014 + +2014-09-29 + + +10 + + +1 - 2 + + +1 +2 + + + +journal article +10.5281/zenodo.13189719 +1842-371x +13189719 + + + + + + +Conradella bakalovae +(Conrad & Peybernès) + + + + + + +( + +Fig. +6g + +) + + +According to +Masse and Bucur (2002) +the range of + +Conradella bakalovae +(Conrad & Peybernès) + +spans "the Hauterivian (?) - Early Aptian interval". Its record in sample 134 near the base of "Urgonien jaune" validates at least a Late Hauterivian age for its older occurrence. + + + + \ No newline at end of file diff --git a/data/03/9D/87/039D87CD6E351E0FA367FEDF79513C17.xml b/data/03/9D/87/039D87CD6E351E0FA367FEDF79513C17.xml new file mode 100644 index 00000000000..1a562bb5ecb --- /dev/null +++ b/data/03/9D/87/039D87CD6E351E0FA367FEDF79513C17.xml @@ -0,0 +1,92 @@ + + + +Latest Jurassic - Early Cretaceous Dasycladalean Algae (Chlorophyta) From The Morand Drilling At Montricher (Canton Of Vaud, Switzerland) + + + +Author + +Granier, Bruno +Department of Ecology and Evolutionary Biology, The University of Kansas, 1200 Sunnyside Avenue, Lawrence, Kansas 66045, USA (bgranier @ ku. edu) +bgranier@ku.edu + + + +Author + +Clavel, Bernard +24, ch. des Champs d’Amot, 74140 Messery, France (b. clavel 1 @ orange. fr) + + + +Author + +Charollais, Jean +Département de Géologie et de Paléontologie, Sciences de la Terre et de l ¹ Environnement, 13, r. des Maraîchers, 1211 Genève 4, Switzerland (jdcharollais @ bluewin. ch) +jdcharollais@bluewin.ch + + + +Author + +MarcWeidmann +3, sentier du Molard, 1805 Jongny, Switzerland (weidmann-dutoit @ bluewin. ch) +weidmann-dutoit@bluewin.ch + +text + + +Acta Palaeontologica Romaniae + + +2014 + +2014-09-29 + + +10 + + +1 - 2 + + +1 +2 + + + +journal article +10.5281/zenodo.13189719 +1842-371x +13189719 + + + + + +Genus + +Pseudoclypeina +Radoičić + + + + + + +( +Fig. 7o +) + + +Within a verticil, as for the genus + +Clypeina +(Michelin) + +, the primary laterals merge in their proximal part. Some species have a second order of laterals, others have three orders. Specimens referable to this genus have two orders of laterals and are found only in the “Urgonien blanc”. + + + + \ No newline at end of file diff --git a/data/03/9D/87/039D87CD6E361E01A367F8387EF73EE1.xml b/data/03/9D/87/039D87CD6E361E01A367F8387EF73EE1.xml new file mode 100644 index 00000000000..8ce07cab537 --- /dev/null +++ b/data/03/9D/87/039D87CD6E361E01A367F8387EF73EE1.xml @@ -0,0 +1,343 @@ + + + +Latest Jurassic - Early Cretaceous Dasycladalean Algae (Chlorophyta) From The Morand Drilling At Montricher (Canton Of Vaud, Switzerland) + + + +Author + +Granier, Bruno +Department of Ecology and Evolutionary Biology, The University of Kansas, 1200 Sunnyside Avenue, Lawrence, Kansas 66045, USA (bgranier @ ku. edu) +bgranier@ku.edu + + + +Author + +Clavel, Bernard +24, ch. des Champs d’Amot, 74140 Messery, France (b. clavel 1 @ orange. fr) + + + +Author + +Charollais, Jean +Département de Géologie et de Paléontologie, Sciences de la Terre et de l ¹ Environnement, 13, r. des Maraîchers, 1211 Genève 4, Switzerland (jdcharollais @ bluewin. ch) +jdcharollais@bluewin.ch + + + +Author + +MarcWeidmann +3, sentier du Molard, 1805 Jongny, Switzerland (weidmann-dutoit @ bluewin. ch) +weidmann-dutoit@bluewin.ch + +text + + +Acta Palaeontologica Romaniae + + +2014 + +2014-09-29 + + +10 + + +1 - 2 + + +1 +2 + + + +journal article +10.5281/zenodo.13189719 +1842-371x +13189719 + + + + + +Genus + +Oroseina +Dieni +et al. + + + + + + +( +Fig. 7 +s-u) + + + +Fig. 6 +a to o (scale bar: 250 µm): +a +oblique section of + +Salpingoporella annulata +, Pierre Châtel Formation, Middle Berriasian + +, sample 317; +b +oblique section of + +Salpingoporella annulata +, Pierre Châtel Formation, Middle Berriasian + +, sample 317; +c +subtransverse section of + +Salpingoporella annulata +, Pierre Châtel Formation, Middle Berriasian + +, sample 317; +d +oblique section of + +Falsolikanella campanensis +, Vions Fm + +, Upper Berriasian, sample 270; +e +deep tangential section of + +Pseudoactinoporella fragilis + +, "Urgonien jaune", Upper Hauterivian, sample 101; +f +oblique section of + +Pseudoactinoporella fragilis + +, "Urgonien jaune", Upper Hauterivian, sample 107; +g +oblique section of + +Conradella bakalovae + +, "Urgonien jaune", Upper Hauterivian, sample 134; +h +oblique section of a verticil of + +Clypeina parasolkani +, Pierre Châtel Formation, Middle Berriasian + +, sample 309; +i +oblique section of a verticil of + +Clypeina parasolkani +, Pierre Châtel Formation, Middle Berriasian + +, sample 293; +j +oblique section of a verticil of + +Clypeina parasolkani +, Pierre Châtel Formation, Middle Berriasian + +, sample 293; +k +subaxial section of a verticil of + +Clypeina parasolkani +, Pierre Châtel Formation, Middle Berriasian + +, sample 309; +l +subtransverse section of a verticil of + +Clypeina parasolkani +, Pierre Châtel Formation, Middle Berriasian + +, sample 309; +m +deep tangential section of + +Deloffrella quercifoliipora +, Vions Fm + +, Upper Berriasian, sample 271; +n +random section of + +Cymopolia +sp. + +or + +Neomeris +sp. + +, "Urgonien jaune", Upper Hauterivian, sample 115; +o +oblique section of + +Angioporella fouryae + +, "Urgonien jaune", Upper Hauterivian, sample 129 + + + + +Fig. 7 +a to o (scale bar: 250 µm): +a +tangential to oblique section of + +Salpingoporella muehlbergii + +, "Urgonien blanc", Upper Hauterivian, sample 42; +b +transverse section of + +Salpingoporella muehlbergii + +, "Urgonien blanc", Upper Hauterivian, sample 42; +c +oblique section of + +Salpingoporella muehlbergii + +, "Urgonien blanc", Upper Hauterivian, sample 42; +d +oblique section of + +Salpingoporella genevensis + +, "Urgonien blanc", Upper Hauterivian, sample 40; +e +oblique section of + +Suppiluliumaella +sp. + +, "Urgonien jaune", Upper Hauterivian, sample 96; +f +oblique section of + +Suppiluliumaella +sp. + +, "Urgonien jaune", Upper Hauterivian, sample 96; +g +oblique section of + +Suppiluliumaella +sp. + +, "Urgonien jaune", Upper Hauterivian, sample 96; +h +oblique section of a verticil of + +Falsolikanella danilovae + +, "Urgonien jaune", Upper Hauterivian, sample 116; +i +transverse section of + +Salpingoporella melitae + +, "Urgonien blanc", Upper Hauterivian, sample 42; +j +oblique section of + +Cylindroporella +sp. + +, "Urgonien blanc", Upper Hauterivian, sample 71; +k +oblique section of + +Salpingoporella heraldica + +, "Urgonien jaune", Upper Hauterivian, sample 115; +l +oblique section of + +Angioporella fouryae + +, "Urgonien jaune", Upper Hauterivian, sample 115; +m +subtransverse section of + +Suppiluliumaella +sp. + +, "Urgonien jaune", Upper Hauterivian, sample 96; +n +tangential section of a sterile verticil of + +Angioporella fouryae + +, "Urgonien jaune", Upper Hauterivian, sample 115; +o +tangential section of a verticil of + +Pseudoclypeina +sp. + +, "Urgonien blanc", Upper Hauterivian, sample 72; +p +to u (scale bar: 500 µm): p oblique section of + +Deloffrella hauteriviana + +, "Urgonien blanc", Upper Hauterivian, sample 37.85; q subtransverse section of + +Dissocladella + +? sp., "Urgonien blanc", Upper Hauterivian, sample 90; +r +oblique section of + +Deloffrella hauteriviana + +, "Urgonien blanc", Upper Hauterivian, sample 37.85; +s +axial section of + +Oroseina +sp. + +, "Urgonien jaune", Upper Hauterivian, sample 114; +t +random section of + +Oroseina +sp. + +, "Urgonien jaune", Upper Hauterivian, sample 112; +u +tangential section of + +Oroseina +sp. + +, "Urgonien jaune", Upper Hauterivian, sample 112. + + + +In the “Urgonien jaune”, we identified few “rosette”-like structures, which are referred to + +Oroseina +Dieni et al. + + + + + \ No newline at end of file diff --git a/data/03/9D/87/039D87CD6E361E0CA0C1FCF77E34382B.xml b/data/03/9D/87/039D87CD6E361E0CA0C1FCF77E34382B.xml new file mode 100644 index 00000000000..c5ba5eb687a --- /dev/null +++ b/data/03/9D/87/039D87CD6E361E0CA0C1FCF77E34382B.xml @@ -0,0 +1,138 @@ + + + +Latest Jurassic - Early Cretaceous Dasycladalean Algae (Chlorophyta) From The Morand Drilling At Montricher (Canton Of Vaud, Switzerland) + + + +Author + +Granier, Bruno +Department of Ecology and Evolutionary Biology, The University of Kansas, 1200 Sunnyside Avenue, Lawrence, Kansas 66045, USA (bgranier @ ku. edu) +bgranier@ku.edu + + + +Author + +Clavel, Bernard +24, ch. des Champs d’Amot, 74140 Messery, France (b. clavel 1 @ orange. fr) + + + +Author + +Charollais, Jean +Département de Géologie et de Paléontologie, Sciences de la Terre et de l ¹ Environnement, 13, r. des Maraîchers, 1211 Genève 4, Switzerland (jdcharollais @ bluewin. ch) +jdcharollais@bluewin.ch + + + +Author + +MarcWeidmann +3, sentier du Molard, 1805 Jongny, Switzerland (weidmann-dutoit @ bluewin. ch) +weidmann-dutoit@bluewin.ch + +text + + +Acta Palaeontologica Romaniae + + +2014 + +2014-09-29 + + +10 + + +1 - 2 + + +1 +2 + + + +journal article +10.5281/zenodo.13189719 +1842-371x +13189719 + + + + + + +Dissocladella intercedens +Bakalova + + + + + + +( +Fig. 3i +) + +Selected references: + +1975 + +Petrascula bursiformis +(Etallon) + +.- Dragastan, Pl. XL, fig. 3, Upper Tithonian, Fagetul Ciucului Mts. ( +Romania +) + + +1978 + +Dissocladella intercedens + +sp.n. +- Bakalova, Pl. 1, figs. 4 & 6 (detail of 4), Brestnica Formation, Upper Tithonian - Lower Berriasian, borehole Várbica (Varbitsa, +Bulgaria +) + + +1993 + +Dissocladella +aff. +intercedens +Bakalova. + +- Bucur, Pl. 1, figs. 5, 7-18, Crivina marls, Upper Berriasian-Lower Valanginian, Illidia, Reşiţa Zone ( +Romania +) + + +1994 + +Dissocladella +aff. +intercedens +Bakalova. + +- Bucur, Pl. XIV, fig. 9 [= +Bucur, 1993 +, Pl. 1, fig. 7] + + +The specimen found in sample 241.60 from the Lower Valanginian "Calcaires roux" is the unique section of this species ( +Fig. 3i +). + + +In addition to this species we ascribe, with some reservation, to this genus one tiny specimen of a tubular verticillated alga with two orders of laterals ( +Fig. 7q +). It was found in the “Urgonien blanc”. + + + + \ No newline at end of file diff --git a/data/03/9D/87/039D87CD6E361E0CA0C1FEF97E113D28.xml b/data/03/9D/87/039D87CD6E361E0CA0C1FEF97E113D28.xml new file mode 100644 index 00000000000..1a6d280f040 --- /dev/null +++ b/data/03/9D/87/039D87CD6E361E0CA0C1FEF97E113D28.xml @@ -0,0 +1,114 @@ + + + +Latest Jurassic - Early Cretaceous Dasycladalean Algae (Chlorophyta) From The Morand Drilling At Montricher (Canton Of Vaud, Switzerland) + + + +Author + +Granier, Bruno +Department of Ecology and Evolutionary Biology, The University of Kansas, 1200 Sunnyside Avenue, Lawrence, Kansas 66045, USA (bgranier @ ku. edu) +bgranier@ku.edu + + + +Author + +Clavel, Bernard +24, ch. des Champs d’Amot, 74140 Messery, France (b. clavel 1 @ orange. fr) + + + +Author + +Charollais, Jean +Département de Géologie et de Paléontologie, Sciences de la Terre et de l ¹ Environnement, 13, r. des Maraîchers, 1211 Genève 4, Switzerland (jdcharollais @ bluewin. ch) +jdcharollais@bluewin.ch + + + +Author + +MarcWeidmann +3, sentier du Molard, 1805 Jongny, Switzerland (weidmann-dutoit @ bluewin. ch) +weidmann-dutoit@bluewin.ch + +text + + +Acta Palaeontologica Romaniae + + +2014 + +2014-09-29 + + +10 + + +1 - 2 + + +1 +2 + + + +journal article +10.5281/zenodo.13189719 +1842-371x +13189719 + + + + + + +Zergabriella embergeri +(Bouroullec & Deloffre) + + + + + + +( +Fig. 3a +, d-e) + +Selected references: + +1987 + +Macroporella embergeri +Bouroullec & Deloffre. + +- Bucur & Oros, Pl. VI, fig. 3, Crivina marls, Upper Beriasian-Valanginian, Illidia, Reşiţa Zone ( +Romania +) 1989 + +Zergabriella embergeri + +, +n.gen., n.comb. +- Granier, synonymy to date, Pl. 1, figs. 1-7; Pl. 2, figs. 1-9, various localities + + +2010 + +Zergabriella embergeri + +.- Granier, synonymy to date, +Figs. 1-5 +, Pls. 1-4, various localities. + + +This is a third species that becomes mineralized with calcite instead of aragonite ( +Granier, 2012 +). It is found in both Vions and Chambotte formations. + + + + \ No newline at end of file diff --git a/data/03/9D/87/039D87CD6E361E0CA367FC717F5B39BF.xml b/data/03/9D/87/039D87CD6E361E0CA367FC717F5B39BF.xml new file mode 100644 index 00000000000..3bd7d727ad8 --- /dev/null +++ b/data/03/9D/87/039D87CD6E361E0CA367FC717F5B39BF.xml @@ -0,0 +1,156 @@ + + + +Latest Jurassic - Early Cretaceous Dasycladalean Algae (Chlorophyta) From The Morand Drilling At Montricher (Canton Of Vaud, Switzerland) + + + +Author + +Granier, Bruno +Department of Ecology and Evolutionary Biology, The University of Kansas, 1200 Sunnyside Avenue, Lawrence, Kansas 66045, USA (bgranier @ ku. edu) +bgranier@ku.edu + + + +Author + +Clavel, Bernard +24, ch. des Champs d’Amot, 74140 Messery, France (b. clavel 1 @ orange. fr) + + + +Author + +Charollais, Jean +Département de Géologie et de Paléontologie, Sciences de la Terre et de l ¹ Environnement, 13, r. des Maraîchers, 1211 Genève 4, Switzerland (jdcharollais @ bluewin. ch) +jdcharollais@bluewin.ch + + + +Author + +MarcWeidmann +3, sentier du Molard, 1805 Jongny, Switzerland (weidmann-dutoit @ bluewin. ch) +weidmann-dutoit@bluewin.ch + +text + + +Acta Palaeontologica Romaniae + + +2014 + +2014-09-29 + + +10 + + +1 - 2 + + +1 +2 + + + +journal article +10.5281/zenodo.13189719 +1842-371x +13189719 + + + + + + +Triploporella +? +praturloni +(Dragastan) + +, +nov. comb. + + + + + +( +Fig. 3 +b-c) + + +Originally ascribed to the genus + +Macroporella +(Pia) + +, a Seletonnellacean alga, this species has features such as euspondyly, +i.e. +, having laterals arranged in verticils, and cladospory, +i.e. +, with cysts in its primary laterals ( +Bucur, 1985 +), that exclude it. Alternatively it could have been reascribed to the genus + +Salpingoporella + +(Pia +in +Trauth), a Triploporellacean alga. However due to its huge number of primaries per verticils and their general shape, thin and elongated, I prefer to refer it to the genus + +Triploporella +(Steinmann) + +. The question mark following the generic name stands for a species left in open nomenclature as the occurrence of short secondaries is not documented yet. It is a fourth and last species studied that is mineralized with calcite instead of aragonite ( +Granier, 2012 +). + +Our specimens were found in the "Calcaires roux". + +Daycladales of uncertain affinity + + +Genus + +Cylindroporella +Johnson + + + +( +Fig. 7j +) + + +The genus + +Cylindroporella +Johnson + +comprises a number of species of uncertain affinities. Following revisions, some species were transferred to the genera + +Montiella + +L. & J. Morellet and + +Fourcadella +Granier & Berthou + +, +etc +. Here only the few algal remains presenting a neck-like structure (as illustrated by +Granier, 1987b +, Pl. 34, figs. f-g as " + +Cylindroporella barnesii +Johnson + +") are referred to this genus. They are found at the top of the “Urgonien blanc”. + + + + \ No newline at end of file diff --git a/data/03/A1/D9/03A1D95EFFE9FFB8FDF99690FF0DFDB3.xml b/data/03/A1/D9/03A1D95EFFE9FFB8FDF99690FF0DFDB3.xml new file mode 100644 index 00000000000..e97db1b0c9c --- /dev/null +++ b/data/03/A1/D9/03A1D95EFFE9FFB8FDF99690FF0DFDB3.xml @@ -0,0 +1,229 @@ + + + +Description of Nesophrosyne melemele sp. n., an Endemic Hawaiian Leafhopper (Hemiptera: Cicadellidae: Deltocephalinae: Opsiini) Associated with Myoporum sandwicense (Scrophulariaceae) + + + +Author + +Bennett, Michael D. Denis Gordon M. + +text + + +Proceedings of the Hawaiian Entomological Society + + +2017 + +49 + + +47 +50 + + + +journal article +0073-134X + + + + + + + +Nesophrosyne melemele +Denis & Bennett + + + + + + + +Diagnosis +. +Length +: male = +2.88 mm +, female = +3.58 mm +. Yellow colored species. Head and vertex rounded. Frontoclypeus with a dark narrow (stylized) heart-shaped marking. Yellow saddle mark present. Aedeagus with pronounced distal processes, hooking laterally to almost 1/3 length of aedeagal arms. + + + + + +Description. +Dorsum + +( +Figure 1A +): Yellow colored species. Head rounded with vertex weakly produced. Pronotum predominately yellow with posterior edge light brown, extending 1/2 pronotal length and tapering towards lateral edges. Scutellum yellow; centrally split by diffuse dark vertical triangle that is variable in width and length; further subdivided by thin bowed dark horizontal line curving posteriorly. Forewing cells hyaline to infuscate, darkest forms with cells dark brown colored; veins darkly colored throughout; outer anteapical cell present. Clavus with diffuse yellow saddle mark with anterolateral margins fading to dark brown; yellow color broadening towards anterior claval edges. + + + +Figure 1. + +Nesophrosyne melemele + + +sp. n. + +endemic to Kauai: (A) dorsal and ventral habitus, (B) male pygofer lateral view, (C) connective dorsal view, (D) style dorsal view, (E) aedeagus posterior view, and (F) aedeagus lateral view. + + + +Venter +( +Figure 1A +): Face with clypellus yellow. Gena and lorum yellow. Antennal sockets yellow. Frontoclypeus broadly dark or brownish; vertex and edges pale, tapering towards posterior base creating a stylized heart-shaped mark on face. Thoracic plates dark. Legs pale. Ventral abdominal segments pale with infused dark bands along anterior edges. + + +Genitalia +( +Figure 1B–F +): Pygofer bluntly rounded with posterior apex rising to near dorsal edge; dorsal edge flat; ventral lobe reduced with ventral edge angled towards apex; 7 macro setae irregularly distributed. Subgenital plate with dense setae distributed along its lateral edges. Aedeagus with paired aedeagal arms widely splayed, rising conspicuously higher than central apodeme; gonopore preapical; apical processes elongate, extending just above gonopore and hooking to approximately 1/3 length of aedeagal arms. Style with apophysis curved, widening at base; preapical lobe with flat lateral and posterior edges, appearing angular; articulating arm short and triangular; posterior appendages with microsetae. Connective close in length to styles with posterior edge notched; anterior arms bowed and widely splayed with ends hooking mesad. + + + + +Distribution: +Hawaiian Islands, Kauai, Polihale Beach. Elevation: 3 meters + + + + + +Measurements: +Body + +: male (n = 7) = +2.89 mm +(2.7–3.0 mm); female (n = 5) = +3.58 mm +(3.2–4.0 mm). +Genitalia: +(n = 4): pygofer = +0.45 mm +( +0.44–0.45 mm +); style = +0.34 mm +( +0.33–0.35 mm +); connective = +0.27 mm +( +0.26–0.28 mm +); aedeagus lateral length = +0.28mm +( +0.27–0.30 mm +); aedeagus posterior height = +0.26 mm +( +0.24–0.28 mm +). + + + + +Type material: + +Holotype +: +1 male +, +Hawaiian Islands +, +Kauai +, +Polihale State Park +. GPS: +22.29222222 +, +159.95972222 +. +Elevation +: + + +3 m + +. + +Collected on + +5-Jan-2010 + +. +Host +plant: + +Myoporum sandwicense + +. +Coll. G.M. Bennett. Deposited +at the +University +of +Hawaii +Insect Museum +, +Honolulu +, +Hawaii +, +USA +. + + + + + +Paratype +material: + +7 males +and +5 females +with the same locality information and collection date as the +holotype +material (see above) + +. Additional material was also deposited in the University of +Hawaii + +Insect Museum, Honolulu, +Hawaii +, +USA + +. + + + + +Etymology: +Melemele is the Hawaiian word for yellow. It was chosen to describe the predominately yellow body coloration observed in male and females of this species. + + + +Notes: +Host plant + +: + +Myoporum sandwicense +. + +Previous work referred to this species under the provisional designation as +“N. sp. 126” +(Bennett and O’Grady 2012). + + + + \ No newline at end of file diff --git a/data/03/B1/87/03B187C0FFC7CC3202BCADF9FC0C8454.xml b/data/03/B1/87/03B187C0FFC7CC3202BCADF9FC0C8454.xml new file mode 100644 index 00000000000..1743884d86b --- /dev/null +++ b/data/03/B1/87/03B187C0FFC7CC3202BCADF9FC0C8454.xml @@ -0,0 +1,183 @@ + + + +Persiella Pseudolituus N. Gen., N. Sp., And Flabelloperforata Tarburensis N. Gen., N. Sp., Two New Larger Benthic Foraminifera From The Upper Maastrichtian Of Iran + + + +Author + +Schlagintweit, Felix +Lerchenauerstr. 167, 80935 Munich, Germany, felix. schlagintweit @ gmx. de +felix.schlagintweit@gmx.de + + + +Author + +Rashidi, Koorosh +Department of Geology, Payame Noor University, Po Box 19395 - 3697 Tehran, Iran, kooroshrashidi @ pnu. ac. ir +kooroshrashidi@pnu.ac.ir + +text + + +Acta Palaeontologica Romaniae + + +2017 + +2018-01-23 + + +13 + + +2 + + +3 +19 + + + +journal article +1842-371x + + + + + + +Persiella pseudolituus + +n. sp. + + + + + +Figs. 3C–D +, pars, 9–12, 13D–F + + +2013 + +Loftusia morgani + +– Pirbaluti et al., +Fig. 8.10 +Origin of the name: +The species name refers to seemingly similarities to the species + +Pseudocyclammina lituus +Yokoyama. + + + + + + +Holotype +: + +Almost centered axial section illustrated in +Figure 12G +, thin-section SNSB-BSPG +2016 V 16 +(original thin-section Rt 113). + + + +Paratypes +: + +Specimens in figs. 9A–G, 10, 11A–B, F, H, M. + + + + +Description: +Test free, subglobular (coiled forms) to elongate (uncoiling forms), early stage planispirally (occasionally streptospirally, +Fig. 11a +) coiled and involute with up to two and a half whorls present. The test periphery is broadly rounded; with slight axial depressions on both sides (biumbonate). The protoconch is rather large, subspherical to elliptical, and connected to the second chamber (?deuteroconch) by multiple openings ( +Fig. 12j +). + + +Chambers increasing continuously in width and only moderately in height, with many as thirteen chambers in the final whorl. In the coiled part, the septa are strongly oblique with five to six chambers in the first, and ten to eleven chambers in the second whorl. Only rarely the adult stage is uncoiling, uniserial and rectilinear with at least up to six chambers ( +Fig. 9e–f +). Here the septa are convex, in direction of growth. Exoskeleton (beams and rafters) coarse, deep, and forming a network that in tangential sections displays a rounded pattern ( +Fig. 12a–b, f +). Foramen basal to multiple in the juvenile stage, later multiple. In some sections it appears as that the foramina are disposed in continuity between successive chambers ( +Fig. 12 f, i +). No endoskeleton present. Wall dark microgranular (?to finely agglutinating), with thin imperforate outer layer (epiderm) underlain by a layer of fine, parallel, and unbranching pseudokeriotheca-like pores. + + +Dimensions (in mm): + +equatorial diameter (uncoiling forms) = up to 2.5 +axial diameter (thickness) = up to 1.35 +ratio ed/ad (uncoiling forms) = 1.5–1.9 (juvenile specimens ~1.2) +height (uncoiling forms) = up to 3.0 +diameter proloculus = up to 0.65 (mostly 0.25–0.45) thickness septa = 0.075–0.15 + +diameter foramina = +0.035 +–0.075 + +thickness epidermis = ~0.0075 +wall thickness (epidermis + fine alveolar layer) = 0.04– 0.065 + +diameter parapores = +0.0075 +–0.015 + + + + +Remarks: + +Persiella pseudolituus + +has been confounded one time with + +Loftusia morgani +Cox + +(see synonymy). + +L. morgani + +is a large size foraminifer (up to +44.5 mm +in length and up to +8 mm +in diameter), morphologically different, with endoskeleton, just a name a view differences (e.g., +Cox, 1937 +; +Meriç and Görmüş, 2001 +.). From a morphological aspect and also general appearance in sections, + +Persiella pseudolituus + +shows similarities with the Late Jurassic to earliest Cretaceous + +Pseudocyclammina lituus +(Yokoyama) + +( +Fig. 13 +). Leaving apart the generic differences, the test of + +P. lituus + +is more compressed (ratio equatorial diameter/axial diameter about 2), the proloculus is smaller ( +0.24–0.26 mm +), and the number of chambers in the last whorl are less (5–6; all data acc. to +Hottinger, 1967 +, p.63). + + + + \ No newline at end of file diff --git a/data/03/BB/87/03BB87F2FFA6C97BFF4736B1467EFEB4.xml b/data/03/BB/87/03BB87F2FFA6C97BFF4736B1467EFEB4.xml new file mode 100644 index 00000000000..3ba2e5c0ca8 --- /dev/null +++ b/data/03/BB/87/03BB87F2FFA6C97BFF4736B1467EFEB4.xml @@ -0,0 +1,129 @@ + + + +Calcareous Algae (Dasycladales, Udoteaceae) From The Cenomanian Altamira Formation Of Northern Cantabria, Spain + + + +Author + +Schlagintweit, Felix +Lerchenauerstr. 167, 80935 Munich, Germany, felix. schlagintweit @ gmx. de +felix.schlagintweit@gmx.de + + + +Author + +Wilmsen, Markus +Senckenberg Naturhistorische Sammlungen, Königsbrücker Landstrasse 159, 01109 Dresden, Germany, markus. wilmsen @ senckenberg. de +markus.wilmsen@senckenberg.de + +text + + +Acta Palaeontologica Romaniae + + +2014 + +2014-09-17 + + +10 + + +1 - 2 + + +1 +2 + + + +journal article +10.5281/zenodo.13189697 +1842-371x +13189697 + + + + + + +Trinocladus tripolitanus +Raineri, 1922 + + + + + + +Figs. 3 +b-c (pars), 6m-u + + +*1922 + +Trinocladus tripolitanus + +n. gen., n. sp. +- Raineri: 79, pl. 3, figs 15-16, Upper Cretaceous of Lybia. + + +1982 + +Trinocladus tripolitanus +Raineri + +- Conrad & Peybernès, p. 777, pl. 1, figs. 1-4. + + +1983 + +Trinocladus tripolitanus +Raineri + +- Schroeder & Willems, figs. 4.11 and 4.12. + + +1987 + +Trinocladus tripolitanus +Raineri + +- Reitner, pl. 33, fig. 4, pl. 44, fig. 2. + + + + +Remarks: + +T. tripolitanus + +is one of the most common algae observed in the Altamira Formation. Relying on the detailed description of Raineri (1922) and +Pia (1936) +, just a few remarks are given here. First of all, we note the common occurrence of slightly club-shaped thallus fragments ( +Figs. 6r, s +), and an occasional occurrence of a secondary widening of the main axis at the levels of the laterals ( +Fig. 6r +). In rare cases, the calcareous skeleton around the primaries is more or less completely dissolved given the outline of rounded embayments ( +Fig. 6u +). The main axis may be outlined just by a thin calcareous envelope. + + +According to +Reitner (1987 +, fig. 110, and p. 210), + +T. tripolitanus + +is restricted to the reef flat areas, platform sands (shoals) and the open lagoon of the Albian- Cenomanian carbonate platforms of northern +Spain +. It ranges up to the Santonian–Campanian boundary ( +Barattolo, 2002 +, tab. 2). + + + + \ No newline at end of file diff --git a/data/03/EE/87/03EE87ECFFA6FFB044DBD405B9B48046.xml b/data/03/EE/87/03EE87ECFFA6FFB044DBD405B9B48046.xml new file mode 100644 index 00000000000..8a7c2c3b566 --- /dev/null +++ b/data/03/EE/87/03EE87ECFFA6FFB044DBD405B9B48046.xml @@ -0,0 +1,302 @@ + + + +Upper Cretaceous Rudist-Bearing Mixed Siliciclastic-Carbonate And - Volcanoclastic Deposits From Strâmturii Valley, Borod Basin, Northern Apuseni Mountains: Description, Microfacies And Depositional Environments + + + +Author + +Săsăran, Liana +Babeş-Bolyai University, Department of Geology and Center for Integrated Geological Studies, 1 Mihail Kogălniceanu Street, 400084 Cluj-Napoca, Romania; liana. sasaran @ ubbcluj. ro; * Corresponding author: emanoil. sasaran @ ubbcluj. ro; ioan. bucur @ ubbcluj. ro +liana.sasaran@ubbcluj.ro + + + +Author + +Săsăran, Emanoil +Babeş-Bolyai University, Department of Geology and Center for Integrated Geological Studies, 1 Mihail Kogălniceanu Street, 400084 Cluj-Napoca, Romania; liana. sasaran @ ubbcluj. ro; * Corresponding author: emanoil. sasaran @ ubbcluj. ro; ioan. bucur @ ubbcluj. ro +liana.sasaran@ubbcluj.ro + + + +Author + +Bucur, Ioan I. +Babeş-Bolyai University, Department of Geology and Center for Integrated Geological Studies, 1 Mihail Kogălniceanu Street, 400084 Cluj-Napoca, Romania; liana. sasaran @ ubbcluj. ro; * Corresponding author: emanoil. sasaran @ ubbcluj. ro; ioan. bucur @ ubbcluj. ro +liana.sasaran@ubbcluj.ro + +text + + +Acta Palaeontologica Romaniae + + +2018 + +2018-05-06 + + +14 + + +1 + + +3 +20 + + + +journal article +10.5281/zenodo.13190185 +1842-371x +13190185 + + + + + + + +Bournonia excavata +d'Orbigny, 1842 + + + + + + + +Fig. 7 +a-b + + +1842 + +Radiolites excavata + +- d’Orbigny, p. 156, 185. + + +1850 + +Radiolites excavata + +d’Orbigny- p. 215, pl. 556. + + +1907 + +Bournonia excavata +(d’Orbigny) + +- Toucas, p. 27, pl. 2, figs. 11-13a. + + +1912 + +Bournonia excavata +(d’Orbigny) + +- Parona, p. 285, fig. 4. + + +1968 + +Bournonia excavata +(d’Orbigny) + +- Pejović, pl. 5, fig. 2. + + +1989 + +Bournonia excavata +(d’Orbigny) + +- Cestari and Sirna, p.145, fig.3. + + +1992 + +Bournonia excavata +(d’Orbigny) + +- Vicens, p. 185, pl. 74, fig. 1. + + +1995 + +Bournonia excavata +(d’Orbigny) + +- Caffau and Pleničar, p. 230; pl. 7, figs. 2, 2a; pl. 12, fig.3. + + +1995 + +Bournonia excavata +(d’Orbigny) + +- Cestari and Sartorio, p.136. + + +1995 + +Bournonia excavata +(d’Orbigny) + +- Scott, p. 303, pl.2, figs. 3-4; text-fig. 6-D. + + +1999 +Bournonia excavata (d’Orbigny) +- Sirna & Paris, p.51, pl. X, fig. 3. + + +2002 + +Bournonia excavata +(d’Orbigny) + +- Caffau, p. 92-94, figs.2-3. + + +2005 + +Bournonia excavata +(d’Orbigny) + +- Pleničar, p. 80, pl.28 figs. 1-2. + + +2007 + +Bournonia excavata +(d’Orbigny) + +- Macé-Bordy, p. 99-100, fig. 9D-E. + + +2008 + +Bournonia excavata +(d’Orbigny) + +- Pons and Vicens, p. 230, fig. 14C. + +Material: one RV (24078-BBU-MPS). + +Description: Lower attached RV is conical, height up to +55 mm +(incomplete) ( +Fig. 7 +a-b). The ornamentation of the shell as well as the outer shell layer from the anterior side of RV is entirely removed probably due to erosion. In ventral side only Pb is visible as a prominent costa that corresponds to downfolds of the laminae of the outer shell layer. Vb is broken but its location can be easily recognized. Vb and Pb are separated by a narrow furrow, +9 mm +wide, concav (Ib). In the transverse section, the contour of the RV is oval to quadrangular, with a flat posteroventral side, having a diameter of about +30 mm +antero-posterior and +40 mm +dorsal-ventral ( +Fig. 7a +). The elements of the myocardinal apparatus are visible (pm) and (am) and the (at) and (pt) ( +Fig. 7a +); the ligamental ridge is absent. Transverse sections of the RV indicate two well defined layers. The inner layer is less +1 mm +thick and is represented by calcite spar. The thickness of the outer shell layer varies from +3-4 mm +in dorsal and posterior side to +10 mm +in area of Pb. The outer shell layer has a prismatic structure, typical for the + +Bournonia + +genus. + + +Remarks: Specimens very similar with + +Bournonia excavata +d’Orbigny + +have been reported by +Douvillé (1910 +, +1913 +, +1915 +) and recently by +Abdel-Gawad et al. (2011) +from Turonian deposits in +Egypt +. This fact has a great implication extending to Turonian stratigraphical ranges of species + +B. excavata +Also + +, detailed taxonomical studies on small shelled species of + +B. fourtaui + +and + +B. africana + +are required, because of their morphological similarities with + +B. excavata +( +Steuber, 1999 +) + +. If these three species formed a single species ( +Steuber, 1999 +) thus + +Bournonia excavata +(d’Orbigny, 1850) + +has priority according to the rules of International Commission on Zoological Nomenclature (ICZN, Ride et al., 1999). + + +Age: middle Santonian in Spain ( +Vicens et al, 1998 +; +Pons and Vicens, 2008 +) and +France +( +Toucas, 1907 +); late Santonian–early Campanian in +Croatia +(Polšac and Mamuzic, 1969), +Italy +( +Sirna and Paris, 1999 +), +Romania +( +Lupu, 1976 +), +Slovenia +( +Pleničar, 2005 +); late CampanianMaastrichtian in southern +Italy +( +Cestari and Sirna, 1989 +) and +Guatemala +- Carribean Province ( +Scott, 1995 +); Maastrichtian in +Montenegro +( +Pejović, 1968 +) + + + + \ No newline at end of file diff --git a/data/03/EE/87/03EE87ECFFA6FFBE477DD5F3BF9085BE.xml b/data/03/EE/87/03EE87ECFFA6FFBE477DD5F3BF9085BE.xml new file mode 100644 index 00000000000..bd4a19fca76 --- /dev/null +++ b/data/03/EE/87/03EE87ECFFA6FFBE477DD5F3BF9085BE.xml @@ -0,0 +1,243 @@ + + + +Upper Cretaceous Rudist-Bearing Mixed Siliciclastic-Carbonate And - Volcanoclastic Deposits From Strâmturii Valley, Borod Basin, Northern Apuseni Mountains: Description, Microfacies And Depositional Environments + + + +Author + +Săsăran, Liana +Babeş-Bolyai University, Department of Geology and Center for Integrated Geological Studies, 1 Mihail Kogălniceanu Street, 400084 Cluj-Napoca, Romania; liana. sasaran @ ubbcluj. ro; * Corresponding author: emanoil. sasaran @ ubbcluj. ro; ioan. bucur @ ubbcluj. ro +liana.sasaran@ubbcluj.ro + + + +Author + +Săsăran, Emanoil +Babeş-Bolyai University, Department of Geology and Center for Integrated Geological Studies, 1 Mihail Kogălniceanu Street, 400084 Cluj-Napoca, Romania; liana. sasaran @ ubbcluj. ro; * Corresponding author: emanoil. sasaran @ ubbcluj. ro; ioan. bucur @ ubbcluj. ro +liana.sasaran@ubbcluj.ro + + + +Author + +Bucur, Ioan I. +Babeş-Bolyai University, Department of Geology and Center for Integrated Geological Studies, 1 Mihail Kogălniceanu Street, 400084 Cluj-Napoca, Romania; liana. sasaran @ ubbcluj. ro; * Corresponding author: emanoil. sasaran @ ubbcluj. ro; ioan. bucur @ ubbcluj. ro +liana.sasaran@ubbcluj.ro + +text + + +Acta Palaeontologica Romaniae + + +2018 + +2018-05-06 + + +14 + + +1 + + +3 +20 + + + +journal article +10.5281/zenodo.13190185 +1842-371x +13190185 + + + + + + + +Gorjanovicia endrissi +Böhm, 1927 + + + + + + + +Fig. 7c + + +1927 + +Radiolites endrissi + +n. sp. +Böhm, p. 210, pl. 14, figs 1-7. + + +1967 + +Gorjanovicia lipparinii + +- Polšak, p. 107, pl. 67, fig. 31. + + + + +2011 + +Gorjanovicia endrissi +( +Böhm, 1927 +) + +- Fenerci-Masse et al., p. 2, text-fig. 1; p.8, text-fig. 5; p.17-18, text-figs. 12-13. + + + + +Material: one fragment of lower valve. (sample no. 24079 +BBU-MPS +) + + +Description: The shape of right valve is cylindro-conical, +30-60 mm +in length, characterized by a compact shell structure. The transverse section is circular to oval in shape and the diameter ranges from 18x +25 mm +to 36x +40 mm +. The ornamentation consists of well-developed longitudinal costae, which are acute ribs in small specimen and blunt or roundish costae in larger specimen. + + +The outer shell layer is +3-4 mm +thick and composed of compact prismatic calcite. The ligamental ridge is well developed, having +3 mm +length in small specimen and +7 mm +in the other and generally +1 mm +wide ( +Fig. 7c +). The extremity of the ligamental ridge is triangular and truncated. The ventral band (Vb) is +5-10 mm +wide and concave located between two rounded costae. The posterior band of the +two specimens +is flat, 10 and +15 mm +wide respectively and has three fine rounded costae ( +Fig. 7c +). The interband is narrower than the bands, forming a shallow groove, +9-10 mm +wide between two pronounced ribs ( +Fig. 7c +). + + +Discussion. A revision of all described + +Gorjanovicia +species + +and of their diagnostic taxonomic criteria has been made by +Fenerci-Masse et al. (2011) +so that three taxonomic groups, each defined by a key species are currently recognized based on quantitave analisys of morphological characters: + +Gorjanovicia endrissi +(Boehm) + +, + +G. ugarensis + + + + +Fig. 5 a, b +Microfacies from the second rudist-bearing lithosome. +a, c-e +Bioclastic-extraclastic floatstone; frequent bioclasts are represented by rudist fragments, echinoderm fragments and bivalves fragments; the rudist shells are fragment- ed and perforated (a, d). +b +Bioclastic-extraclastic rudstone/grainstones with rudist, echinoderm fragments and red algae fragments. + + + + +Fig. 6 a, b +Extraclastic sediments from the rudist-bearing lithosomes; they are represented by metamorphic lithoclasts (quartzite, crystalline schists), monomineral quartz, muscovite and biotite (crossed polars). +c, d +Tuffites with altered volcanic glass and various crystalloclasts, angular quartz, biotite and calcite (c- plane-polarized light; d - crossed polars). + + + +Sliskovic´ and + +G. kvarneri +Polšak. Our + +specimens are similar with + +Gorjanovicia lipparinii + +described by +Polšak (1967) +from +Istria +in Santonian-lower Campanian deposits. Actually, this species is considered as junior synonym of + +Gorjanovicia endrissi +Böhm + +( +sensu +Fenerci-Masse et al., 2011 +) being assimilated into this taxonomic group. Group of + +Gorjanovicia endrissi + +is characterized by flat anterior band ( +AB +), generally concave interband (I) and flat or concave posterior band ( +PB +), numerous costae and ornamented PB. The broad variations of morphological characters within this group are regarded as echophenotypic variations ( +Fenerci-Masse et al., 2011 +). + + +Age and distribution: Coniacian in +Greece +( +Steuber, 1999 +); late Santonian in +Slovenia +( +Pleničar and Jurkovsek, 1998 +), Santonian-early Campanian in +Croatia +( +Polšak and Mamuzic, 1969 +; +Polšak, 1967 +; +Polšak et al, 1982 +), +Italy +( +Caffau and Pleničar, 1995 +), +Romania +(this study) and early Maastrichtian in +Turkey +( +Fenerci, 1999 +). + + + + \ No newline at end of file diff --git a/data/03/EE/87/03EE87ECFFA8FFBF44DBD10BBCB38068.xml b/data/03/EE/87/03EE87ECFFA8FFBF44DBD10BBCB38068.xml new file mode 100644 index 00000000000..73ac7ace145 --- /dev/null +++ b/data/03/EE/87/03EE87ECFFA8FFBF44DBD10BBCB38068.xml @@ -0,0 +1,280 @@ + + + +Upper Cretaceous Rudist-Bearing Mixed Siliciclastic-Carbonate And - Volcanoclastic Deposits From Strâmturii Valley, Borod Basin, Northern Apuseni Mountains: Description, Microfacies And Depositional Environments + + + +Author + +Săsăran, Liana +Babeş-Bolyai University, Department of Geology and Center for Integrated Geological Studies, 1 Mihail Kogălniceanu Street, 400084 Cluj-Napoca, Romania; liana. sasaran @ ubbcluj. ro; * Corresponding author: emanoil. sasaran @ ubbcluj. ro; ioan. bucur @ ubbcluj. ro +liana.sasaran@ubbcluj.ro + + + +Author + +Săsăran, Emanoil +Babeş-Bolyai University, Department of Geology and Center for Integrated Geological Studies, 1 Mihail Kogălniceanu Street, 400084 Cluj-Napoca, Romania; liana. sasaran @ ubbcluj. ro; * Corresponding author: emanoil. sasaran @ ubbcluj. ro; ioan. bucur @ ubbcluj. ro +liana.sasaran@ubbcluj.ro + + + +Author + +Bucur, Ioan I. +Babeş-Bolyai University, Department of Geology and Center for Integrated Geological Studies, 1 Mihail Kogălniceanu Street, 400084 Cluj-Napoca, Romania; liana. sasaran @ ubbcluj. ro; * Corresponding author: emanoil. sasaran @ ubbcluj. ro; ioan. bucur @ ubbcluj. ro +liana.sasaran@ubbcluj.ro + +text + + +Acta Palaeontologica Romaniae + + +2018 + +2018-05-06 + + +14 + + +1 + + +3 +20 + + + +journal article +10.5281/zenodo.13190185 +1842-371x +13190185 + + + + + + + +Praeradiolites subtoucasi +Toucas, 1907 + + + + + + + +Fig. 7 +d-e. + + +1907 + +Praeradiolites subtoucasi + +n.sp. +- +Toucas, p. 31, pl. 3, figs. 8, 9. + + +1954 + +Praeradiolites subtoucasi + +Toucas- Astre, p. 61, 76- 77, 83, pl. 6, figs. 1, 2. + + +1962 + +Praeradiolites +cf. +subtoucasi + +Toucas- Astre, p. 306, 308. + + +1965 + +Praeradiolites subtoucasi + +Toucas- Pamouktchiev, p. 37, pl. 4, fig. 1, text-fig. 6. + + +1976 + +Praeradiolites subtoucasi + +Toucas- Lupu, p. 126, pl. 17, figs. 4,5a-b, pl. 39, fig. 6. + + +1977 + +Praeradiolites subtoucasi + +Toucas- Pons, p. 69, pl. 50, figs. 1a-d. + + +1992 + +Praeradiolites subtoucasi + +Toucas- Vicens, p. 201, pl. 75, figs. 1-15, pl. 76, figs. 3-4, pl. 79, figs. 1-5. + + +1995 + +Praeradiolites +cf. +subtoucasi + +Toucas- Morris & Skelton, p. 292, pl.6, figs.3,4. + + +1999 + +Praeradiolites subtoucasi + +Toucas- Fenerci, p. 90- 94, text-figs. 3.28, 3.29, pl. VII, figs. 1-7. + + +2004 + +Praeradiolites subtoucasi + +Toucas- Fenerci, p. 93, pl. 1, figs. 1-6. + + +2006 + +Praeradiolites subtoucasi + +Toucas- Pons and Vicens, p. 15-16, fig. 13F, fig. 14G. + + +2012 + +Praeradiolites subtoucasi + +Toucas- Pons et al., p. 690, fig. 11B. + + +2013 + +Praeradiolites subtoucasi + +Toucas- Özer et al., p. 35-36, pl. II, figs. A-F; pl. III, figs. A-H. + +Material: two lower valves (samples nos.24080, 24081 BBU-MPS). + +Description: The shape of RV is conical to cylindrical in both specimens, having 38 and +42 mm +in length and its surface is ornamented with horizontal growth lines. Diameter of RV near to the commissure is +30 mm +(24081 BBU-MPS) and +35 mm +(24080 BBU-MPS) with an oval contour in transverse sections ( +Fig. 7d, e +). The outer shell layer is generally thin, ranging from +3 to 8 mm +thickness on the dorsal side, were cellular structures alternate with thin calcitic compact layers. In ventral side of both RVs the outer shell layer is very eroded and the radial bands (Vb and Pb) are represented by two longitudinal grooves that show approximately the same width ( +Fig. 7d, e +). The Ib is represented by longitudinal costae and has a width ranges from +4 to 7 mm +. The ligamental ridge (L) is long (5 respectively +7 mm +) has a thin stem and is rounded at its extremity ( +Fig. 7d, e +). The cardinal apparatus is preserved showing the teeth (at and pt) and the posterior (pm) and anterior myophores (am) ( +Fig. 7e +). + + +Discussion and remarks: +Vicens (1992) +designated + +Praeradiolites aristidis ( +Munier-Chalmas, 1888) + +and + +Praeradiolites echennensis ( +Astre, 1954 +) + +as synonyms of + +Praeradiolites subtoucasi +( +Toucas, 1907 +) + +. Instead, +Steuber (1999) +described from +Greece +species of + +Praeradiolites echennensis ( +Astre, 1954 +) + +that can be distinguished from the other two species ( + +P. aristidis + +and + +P. subtoucasi + +) therefore considered + +P. echennensis + +as valid species. + + +Age and distribution: late Santonian-early Campanian in +France +( +Astre, 1962 +), +Spain +( +Vicens, 1992 +), +Romania +( +Lupu, 1976 +; +Săsăran et al., 2010 +); Maastrichtian in +Croatia +( +Gušić and Jelaska, 1990 +; +Steuber et al., 2005 +), +Oman +( +Morris and Skelton, 1995 +), +Turkey +( +Fenerci, 1999 +, +2004 +), +Iraq +( +Özer et al., 2013 +). + + + + \ No newline at end of file diff --git a/data/03/EE/87/03EE87ECFFA9FFBD477DD2C7BC508295.xml b/data/03/EE/87/03EE87ECFFA9FFBD477DD2C7BC508295.xml new file mode 100644 index 00000000000..dc918db77fd --- /dev/null +++ b/data/03/EE/87/03EE87ECFFA9FFBD477DD2C7BC508295.xml @@ -0,0 +1,221 @@ + + + +Upper Cretaceous Rudist-Bearing Mixed Siliciclastic-Carbonate And - Volcanoclastic Deposits From Strâmturii Valley, Borod Basin, Northern Apuseni Mountains: Description, Microfacies And Depositional Environments + + + +Author + +Săsăran, Liana +Babeş-Bolyai University, Department of Geology and Center for Integrated Geological Studies, 1 Mihail Kogălniceanu Street, 400084 Cluj-Napoca, Romania; liana. sasaran @ ubbcluj. ro; * Corresponding author: emanoil. sasaran @ ubbcluj. ro; ioan. bucur @ ubbcluj. ro +liana.sasaran@ubbcluj.ro + + + +Author + +Săsăran, Emanoil +Babeş-Bolyai University, Department of Geology and Center for Integrated Geological Studies, 1 Mihail Kogălniceanu Street, 400084 Cluj-Napoca, Romania; liana. sasaran @ ubbcluj. ro; * Corresponding author: emanoil. sasaran @ ubbcluj. ro; ioan. bucur @ ubbcluj. ro +liana.sasaran@ubbcluj.ro + + + +Author + +Bucur, Ioan I. +Babeş-Bolyai University, Department of Geology and Center for Integrated Geological Studies, 1 Mihail Kogălniceanu Street, 400084 Cluj-Napoca, Romania; liana. sasaran @ ubbcluj. ro; * Corresponding author: emanoil. sasaran @ ubbcluj. ro; ioan. bucur @ ubbcluj. ro +liana.sasaran@ubbcluj.ro + +text + + +Acta Palaeontologica Romaniae + + +2018 + +2018-05-06 + + +14 + + +1 + + +3 +20 + + + +journal article +10.5281/zenodo.13190185 +1842-371x +13190185 + + + + + + + +Sphaerulites boreaui +Toucas, 1908 + + + + + + + +Fig. 7 +j-k. + + +1908 + +Sphaerulites boreaui + +nov. sp. +- Toucas, p. 56, pl.9, fig.6, text-figs. 28-29. + + +1976 + +Sphaerulites boreaui + +Toucas- Lupu, p. 129, pl.20, fig.1a-b. + + +2000 + +Sphaerulites +cf. +boreaui + +Toucas- Pleničar and Jurkovsek, p. 59, pl.3, fig.1. + + +Material: +1 specimen +, both valves (BBU-MPS-24084). + + +Description: The shape of right valve is conical, rapidly expanding, having +40 mm +height and +110 mm +diameter antero-posterior. Growth lamellae of RV are subhorizontal, markedly expanded. In postero-ventral area, radial structures are not visible because the valves are broken. Left valve is slightly convex, thin and smaller than RV, measuring +15 mm +heigh and +60 mm +the antero-posterior diameter ( +Fig. 7j +). In transverse section through the valves near the commissure, the ligament ridge is visible having a long pedicle, +16 mm +length, and expand- ed distal end ( +Fig. 7k +); two dorsal cavities developed between the ligament ridge and the myocardinal apparatus ( +Fig. 7k +). The cellular outer shell layer of RV has variable thickness; largest toward the anterior side, with cells extremely radially elongated giving the appearance of radial ridges ( +Fig. 7k +). + + + +Fig. 7 a, b + +Bournonia excavata +d'Orbigny, 1847 + +, (inventory no. 24078 BBU-MPS =no.1246 sample field); +a +transverse section through RV close to the commissure, showing the myocardinal elements: anterior and posterior tooth and myophores (am, pm) of the opposite valve; +b +view of flat posteroventral side of RV; +c + +Gorjanovicia endrissi +(Böhm) + +(24079 BBU-MPS) – transverse section of RV showing compact layer, concave ventral band (Vb); Ib- narrow and wide Pb with 3 fine rounded costae; +d +, +e + +Praeradiolites subtoucasi +(Toucas) + +: +d +transverse section through RV (24080-BBU-MPS), unknown commissure. The outer shell layer from ventral side is eroded thus the radial bands are missing. +e +transverse section on other specimen (24081-BBUMPS) having outer shell layer partially broken but preserve the myocardinal apparatus. +f, g + +Radiolites squamosus +(d'Orbigny) + +: +f +specimen with both valves showing convex LV, very eroded and the ornamentations of RV consist in dense growth lamellae (sample no. 24082 BBU-MPS); +g +ventral side of RV of the same specimen showing radial bands (Vb and Pb) with folds upward to commissure and the narrow interband (Ib). +h-i + +Radiolites nouleti +(Bayle) + +(sample no. 24083 BBU-MPS): +h +large conical RV, thick-shelled, with dense folded growth lamellae, slightly ondulated in large interband (Ib); +i +transverse section in RVof the same specimen, showing thick cellular outer shell layer, ligamental ridge and accessory cavities. +j, k + +Sphaerulites boreaui +(Toucas) + +(sample no. 24084 BBU-MPS), +j +specimen with both valves, top view, showing LV, thin and smaller than lower valve and large RV with expanded, sub-horizontal growth lamellae; +k +transverse section through RV, showing thickness of cellular + + + +outer shell layer, positions of radial bands (Vb and Pb), the length of ligamental ridge and myocardinal apparatus. Remarks: Our specimen is similar with species of + +Sphaerulites boreaui + +previously described by +Lupu (1976) +from Late Santonian deposits from RoȘia Basin. + + +Age and distribution: early-middle Santonian in +France +( +Toucas, 1907 +), late Santonian-early Campanian in +Bosnia-Herzegovina +( +Sliskovic, 1971 +), +Slovenia +( +Pleničar and Jurkovsek, 2000 +), +Romania +( +Lupu, 1976 +) and +Spain +( +Vicens, 1992 +). + + + + \ No newline at end of file diff --git a/data/03/EE/87/03EE87ECFFA9FFBF44DBD1C4B82B8794.xml b/data/03/EE/87/03EE87ECFFA9FFBF44DBD1C4B82B8794.xml new file mode 100644 index 00000000000..60aef250c89 --- /dev/null +++ b/data/03/EE/87/03EE87ECFFA9FFBF44DBD1C4B82B8794.xml @@ -0,0 +1,169 @@ + + + +Upper Cretaceous Rudist-Bearing Mixed Siliciclastic-Carbonate And - Volcanoclastic Deposits From Strâmturii Valley, Borod Basin, Northern Apuseni Mountains: Description, Microfacies And Depositional Environments + + + +Author + +Săsăran, Liana +Babeş-Bolyai University, Department of Geology and Center for Integrated Geological Studies, 1 Mihail Kogălniceanu Street, 400084 Cluj-Napoca, Romania; liana. sasaran @ ubbcluj. ro; * Corresponding author: emanoil. sasaran @ ubbcluj. ro; ioan. bucur @ ubbcluj. ro +liana.sasaran@ubbcluj.ro + + + +Author + +Săsăran, Emanoil +Babeş-Bolyai University, Department of Geology and Center for Integrated Geological Studies, 1 Mihail Kogălniceanu Street, 400084 Cluj-Napoca, Romania; liana. sasaran @ ubbcluj. ro; * Corresponding author: emanoil. sasaran @ ubbcluj. ro; ioan. bucur @ ubbcluj. ro +liana.sasaran@ubbcluj.ro + + + +Author + +Bucur, Ioan I. +Babeş-Bolyai University, Department of Geology and Center for Integrated Geological Studies, 1 Mihail Kogălniceanu Street, 400084 Cluj-Napoca, Romania; liana. sasaran @ ubbcluj. ro; * Corresponding author: emanoil. sasaran @ ubbcluj. ro; ioan. bucur @ ubbcluj. ro +liana.sasaran@ubbcluj.ro + +text + + +Acta Palaeontologica Romaniae + + +2018 + +2018-05-06 + + +14 + + +1 + + +3 +20 + + + +journal article +10.5281/zenodo.13190185 +1842-371x +13190185 + + + + + + + +Radiolites nouleti +Bayle, 1857 + + + + + + + +Fig. 7 +h-i. + + +1908 + +Radiolites nouleti + +Bayle- Toucas, p. 72, pl.13, figs.18-19. + + +1967 + +Radiolites nouleti + +Bayle- Polšak, pp. 69, 180, pl.44, fig.4,4a, pl.45, figs.2-5 + + +1967 + +Radiolites nouleti + +Bayle- Lupu and Lupu, p. 308. + + +1982 + +Radiolites nouleti + +Bayle- Czabalay, p. 50, 85; pl.39, fig.11, pl.40, figs.3-4,7. + +Material: One RV specimen (BBU-MPS-24083). + +Description. Right valve conical, thick-shelled, having more than +50 mm +length and +78 mm +diameter antero-posterior and +55 mm +dorsoventral ( +Fig. 7h +). The ornamentation consists in fine and rounded longitudinal ribs, +2 mm +in thickness in the dorsal side. On the ventral side, dense, regularly folded growth lamellae can be seen, slightly ondulated in interband. The interband (Ib) is very wide, centrally depressed separating the radial bands Vb and Pb which are simple folds with almost the same amplitude ( +Fig. 7h +). In transversal section, the ligamental ridge (L) is triangular at base, with +11 mm +in length and its inner margin truncated. Anterior and posterior of the ligamental ridge are two small, oval cavities ( +Fig. 7i +). The outer shell layer varies between +13 to 15 mm +in thickness, having only +5 mm +in ventral side in interband area. Cells of the outer shell layer are irregular polygonal, predominantly penta- and hexagonal ( +Fig. 7i +). + + +Remarks: + +Radiolites nouleti + +is a large radiolitid easy identifiable by its thick-shelled, large interband and dense folded growth lamellae. + + +Age and distribution: Santonian-early Campanian in +Croatia +( +Polšak et al., 1982 +), +Romania +( +Lupu, 1976 +); early Campanian in +France +( +Bilotte, 1985 +), +Hungary +( +Czabalay, 1982 +), +Serbia +( +Milovanovic, 1935 +) and +Spain +( +Vicens, 1992 +); late Maastrichtian in +Spain +( +Bilotte, 1985 +). + + + + \ No newline at end of file diff --git a/data/03/EE/87/03EE87ECFFA9FFBF44DBD5D0BF2084D8.xml b/data/03/EE/87/03EE87ECFFA9FFBF44DBD5D0BF2084D8.xml new file mode 100644 index 00000000000..7d360d347dc --- /dev/null +++ b/data/03/EE/87/03EE87ECFFA9FFBF44DBD5D0BF2084D8.xml @@ -0,0 +1,173 @@ + + + +Upper Cretaceous Rudist-Bearing Mixed Siliciclastic-Carbonate And - Volcanoclastic Deposits From Strâmturii Valley, Borod Basin, Northern Apuseni Mountains: Description, Microfacies And Depositional Environments + + + +Author + +Săsăran, Liana +Babeş-Bolyai University, Department of Geology and Center for Integrated Geological Studies, 1 Mihail Kogălniceanu Street, 400084 Cluj-Napoca, Romania; liana. sasaran @ ubbcluj. ro; * Corresponding author: emanoil. sasaran @ ubbcluj. ro; ioan. bucur @ ubbcluj. ro +liana.sasaran@ubbcluj.ro + + + +Author + +Săsăran, Emanoil +Babeş-Bolyai University, Department of Geology and Center for Integrated Geological Studies, 1 Mihail Kogălniceanu Street, 400084 Cluj-Napoca, Romania; liana. sasaran @ ubbcluj. ro; * Corresponding author: emanoil. sasaran @ ubbcluj. ro; ioan. bucur @ ubbcluj. ro +liana.sasaran@ubbcluj.ro + + + +Author + +Bucur, Ioan I. +Babeş-Bolyai University, Department of Geology and Center for Integrated Geological Studies, 1 Mihail Kogălniceanu Street, 400084 Cluj-Napoca, Romania; liana. sasaran @ ubbcluj. ro; * Corresponding author: emanoil. sasaran @ ubbcluj. ro; ioan. bucur @ ubbcluj. ro +liana.sasaran@ubbcluj.ro + +text + + +Acta Palaeontologica Romaniae + + +2018 + +2018-05-06 + + +14 + + +1 + + +3 +20 + + + +journal article +10.5281/zenodo.13190185 +1842-371x +13190185 + + + + + + + +Radiolites squamosus +d'Orbigny, 1842 + + + + + + + +Fig. 7 +, f-g. + + +1842 + +Radiolites squamosa + +- d'Orbigny, pp. 185-186 1850 + +Radiolites squamosus + +d'Orbigny- d'Orbigny, p. 219, pl.561 + + +1908 + +Radiolites squamosus + +d'Orbigny- Toucas, p. 71, pl.13, figs.9-11 + + +1976 + +Radiolites squamosus + +d'Orbigny- Lupu, p. 124, pl.13, fig.5 + + +1993 + +Radiolites squamosus + +d'Orbigny- Swinburne and Noacco, text-fig.2 + + + +Material: +1 specimen +, both valves (no. 24082 +BBU-MPS +) + +. + + +Description: Small size shell, with right valve (RV) long conical, +40 mm +long and +20 mm +in diameter at the commissural plane ( +Fig. 7 +f-g). The ornamentation consists of dense growth lamellae ( +Fig. 7f +). The radial bands are folds curved towards the commissure separated by a narrow interband with one fold ( + +Fig. +7g + +). Left valve (LV) is highly convex, with central apex but much eroded ( +Fig. 7f +). + + +Discussion and remarks: Because we found only +one specimen +, the shell of + +Radiolites squamosus + +was not been cut for study in cross-section. This species is also mentioned by +Lupu (1976) +from RoȘia Basin (Northen Apuseni Mountains). + + +Age and distribution: early - middle Santonian in +France +( +Toucas, 1907 +); late Santonian- early Campanian in +Croatia +( +Polšak and Mamuzic, 1969 +), +Romania +( +Lupu, 1976 +), +Slovenia +( +Pleničar and Jurkovsek, 1999 +), middle-late Campanian in Spain ( +Floquet, 1991 +) and early Maastricthian in east +Serbia +( +Milovanovic, 1935 +). + + + + \ No newline at end of file diff --git a/data/03/EE/87/03EE87ECFFABFFBA477DD2BBBFEA81E5.xml b/data/03/EE/87/03EE87ECFFABFFBA477DD2BBBFEA81E5.xml new file mode 100644 index 00000000000..a5193030a76 --- /dev/null +++ b/data/03/EE/87/03EE87ECFFABFFBA477DD2BBBFEA81E5.xml @@ -0,0 +1,212 @@ + + + +Upper Cretaceous Rudist-Bearing Mixed Siliciclastic-Carbonate And - Volcanoclastic Deposits From Strâmturii Valley, Borod Basin, Northern Apuseni Mountains: Description, Microfacies And Depositional Environments + + + +Author + +Săsăran, Liana +Babeş-Bolyai University, Department of Geology and Center for Integrated Geological Studies, 1 Mihail Kogălniceanu Street, 400084 Cluj-Napoca, Romania; liana. sasaran @ ubbcluj. ro; * Corresponding author: emanoil. sasaran @ ubbcluj. ro; ioan. bucur @ ubbcluj. ro +liana.sasaran@ubbcluj.ro + + + +Author + +Săsăran, Emanoil +Babeş-Bolyai University, Department of Geology and Center for Integrated Geological Studies, 1 Mihail Kogălniceanu Street, 400084 Cluj-Napoca, Romania; liana. sasaran @ ubbcluj. ro; * Corresponding author: emanoil. sasaran @ ubbcluj. ro; ioan. bucur @ ubbcluj. ro +liana.sasaran@ubbcluj.ro + + + +Author + +Bucur, Ioan I. +Babeş-Bolyai University, Department of Geology and Center for Integrated Geological Studies, 1 Mihail Kogălniceanu Street, 400084 Cluj-Napoca, Romania; liana. sasaran @ ubbcluj. ro; * Corresponding author: emanoil. sasaran @ ubbcluj. ro; ioan. bucur @ ubbcluj. ro +liana.sasaran@ubbcluj.ro + +text + + +Acta Palaeontologica Romaniae + + +2018 + +2018-05-06 + + +14 + + +1 + + +3 +20 + + + +journal article +10.5281/zenodo.13190185 +1842-371x +13190185 + + + + + + + +Vaccinites gosaviensis +Douvillé, 1890 + + + + + + + +Fig. 8h, i +. + + +1891 + +Hippurites gosaviensis + +n. sp. +- Douvillé, p. 24, text-figs.9, 12-14 + + +1904 + +Vaccinites gosaviensis + +Douvillé- Toucas, p. 92, pl.13, fig.3, text-fig.146 + + +1966 + +Hippurites (Vaccinites) gosaviensis +Douvillé + +- Todiriță- Mihăilescu, p. 72, pl.17, fig.2, pls.18-20. + + +1960 + +Hippurites (Vaccinites) gosaviensis + +Douvillé- Lupu and Lupu, pp. 635-636, pl. 1, figs. 28-29, text-figs.3-4. + + +1969 + +Hippurites (Vaccinites) gosaviensis + +Douvillé- Polšak & Mamuzic, pp. 235, 239. + + +1976 + +Vaccinites gosaviensis + +Douvillé- Lupu, p. 110, pl.2, figs.1a-c,2, pl.35, figs.5,6. + + +2001 + +Vaccinites gosaviensis +(Douvillé) + +- Steuber, pp. 438, 441, tab.1. + + + +Material: +1 specimen +with both valves (no. 24089- +BBU-MPS +), one right valve (no. 23503- +BBU-MPS +) + +. + + +Description: The upper valve (LV) is very thin, slight convex but do not preserve any significant morphological characters due to erosion. The right valve (RV) has a conical shape, gently curved, +100 mm +in length and a diameter of 47/ +60 mm +at +5 mm +below to the commissural plane. The outer shell layer of the right valve is thin, +2 to 4 mm +in thickness, partly eroded ( +Fig. 8 +h-i). In the transversal section trough the RV, the ligamental ridge (L) appears straight, +8 mm +in length, with its inner termination truncated ( +Fig. 8i +). The first pillar (P1) is very pinched at the base and have a rounded-elliptic head, +9 mm +total length; the second pillar (P2) is more pedunculated having 12 + + +mm in length and an oval head which is curved towards to ligamental ridge ( +Fig. 8i +). The elements of the myocardinal apparatus are also visible: anterior tooth (at) in prolongation of L, posterior tooth (pt) located parallel and not surpassing the tip of ligamental ridge; posterior myophore (pm) rectangular outline, aligned sub-parallel to the first pillar (P1) and projecting interiorly +5 mm +over the tip of P1 ( +Fig. 8i +). + + +Discussion and remarks: From the area of Valea Neagră de Criş, southeastern part of Borod Basin, +Lupu & Lupu (1960) +, Lupu,(1976) described sub-species + +Vaccinites gosaviensis acicularis +( +Lupu & Lupu, 1960 +) + +that differs from + +Vaccinites gosaviensis + +by its ligamental ridges with sharp inner termination curved anteriorly and more wide and rounded furrows on the shell ornamentations. + + +Age and distribution: Santonian-early Campanian in +Austria +( +Steuber, 2001 +), +Croatia +( +Polšak and Mamuzic, 1969 +), +Greece +(Kollman et al., 1985), +Italy +( +Sirna, 1990 +), and +Romania +(Todiriță- +Mihăilescu, 1966 +; +Lupu, 1976 +); early Maastrichtian in +Turkey +( +Fenerci, 1999 +). + + + + \ No newline at end of file diff --git a/data/03/EE/87/03EE87ECFFABFFBD44DBD427BE1B8730.xml b/data/03/EE/87/03EE87ECFFABFFBD44DBD427BE1B8730.xml new file mode 100644 index 00000000000..843239bf8a7 --- /dev/null +++ b/data/03/EE/87/03EE87ECFFABFFBD44DBD427BE1B8730.xml @@ -0,0 +1,336 @@ + + + +Upper Cretaceous Rudist-Bearing Mixed Siliciclastic-Carbonate And - Volcanoclastic Deposits From Strâmturii Valley, Borod Basin, Northern Apuseni Mountains: Description, Microfacies And Depositional Environments + + + +Author + +Săsăran, Liana +Babeş-Bolyai University, Department of Geology and Center for Integrated Geological Studies, 1 Mihail Kogălniceanu Street, 400084 Cluj-Napoca, Romania; liana. sasaran @ ubbcluj. ro; * Corresponding author: emanoil. sasaran @ ubbcluj. ro; ioan. bucur @ ubbcluj. ro +liana.sasaran@ubbcluj.ro + + + +Author + +Săsăran, Emanoil +Babeş-Bolyai University, Department of Geology and Center for Integrated Geological Studies, 1 Mihail Kogălniceanu Street, 400084 Cluj-Napoca, Romania; liana. sasaran @ ubbcluj. ro; * Corresponding author: emanoil. sasaran @ ubbcluj. ro; ioan. bucur @ ubbcluj. ro +liana.sasaran@ubbcluj.ro + + + +Author + +Bucur, Ioan I. +Babeş-Bolyai University, Department of Geology and Center for Integrated Geological Studies, 1 Mihail Kogălniceanu Street, 400084 Cluj-Napoca, Romania; liana. sasaran @ ubbcluj. ro; * Corresponding author: emanoil. sasaran @ ubbcluj. ro; ioan. bucur @ ubbcluj. ro +liana.sasaran@ubbcluj.ro + +text + + +Acta Palaeontologica Romaniae + + +2018 + +2018-05-06 + + +14 + + +1 + + +3 +20 + + + +journal article +10.5281/zenodo.13190185 +1842-371x +13190185 + + + + + + + +Hippuritella lapeirousei +Goldfuss, 1840 + + + + + + + +Fig. 8 +a-g + + +1895 + +Hippurites (Orbignya) lapeirousei + +Goldfuss- Douvillé, p. 164, pl.24, figs.7-10. + + +1903 + +Orbignya lapeirousei + +Goldfuss- Toucas, p. 53, pl.6, figs.10-11. + + +1976 + +Hippurites lapeirousei + +Goldfuss- Lupu, p. 122, pl.12, fig.5. + + +1995 + +Hippuritella lapeirousei +(Goldfuss) + +- Caffau and Pleničar, p. 135, pl. 1, figs. 1-14. + + +1999 + +Hippuritella lapeirousei +(Goldfuss) + +- Steuber, p. 116, text-fig.46h, J-M. + + +2000 + +Hippuritella lapeirousei +(Goldfuss) + +- Steuber and Löser, p. 96. + + +2001 + +Hippuritella lapeirousei +(Goldfuss) + +- Götz, p. 64, pl.1, fig.4, pl.3, fig.2, pl.4, fig.6, pl.7, fig.16 + + +2005 + +Hippuritella lapeirousei +(Goldfuss) + +- Pleničar, p. 172, pl. 74, fig. 1. + + +2010 + +Hippuritella lapeirousei +(Goldfuss) + +- Moro et al., p. 626, 630, figs. 6, 9. + + +2014 + +Hippuritella lapeirousei +(Goldfuss) + +- Pons et al., p. 64, fig. 16.1-6. + + + +Material: +1 specimen +with both valves (24085 +BBU-MPS +) and 3 fragments of lower valves (24086, 24087, 24088 - +BBU-MPS +) + +. + + +Description: The specimen with both valves shows a very thin, flat left valve (LV) with a sub-central apex. The almost all surface of the LV is eroded and only on the edge the radial canals are visible ( +Fig. 8c +). All specimens have small, elongated-conical right valves (RV), without prominent longitudinal ribs, the surface of the shell is very eroded ( +Fig. 8b,d +). The length of right valves (RV) varies between +20 to 42 mm +and diameter measures +18 mm +to +25 mm +maximal. The position of the pillars (P1 and P2) is indicated externally on the outer shell layer by two shallow longitudinal furrow ( +Fig. 8b,d +). The internal characters observed in the transversal sections of right valves shows lack of ligament ridge and small pillars ( +Figs. 8a, e,f,g +). The pillars P1 and P2 are short and rounded and have same size ( +Figs. 8a,e,f +). Only in +one specimen +(BBU-MPS-24088) the first pillar P1 is slightly smaller than the second pillar (P2) and both pillars are broad and less prominent ( +Fig. 8-g +). The myocardinal apparatus is not visible in none of specimens. The outer shell layer shows variably thickness and seems to present radial ribbing ( +Fig. 8a, c +, e-g). + + +Discussion: Long time some authors placed + +Hipuritella +nabresinensis + +in synonymies with + +Hipuritella +lapeirousei + +( +Douville, 1895 +; +Parona, 1900 +; +1926 +; +Toucas, 1903 +- +1904 +). Others rudistologists (Sladić - +Trifunović, 1972 +, +1978 +; +Lupu, 1976 +; +Accordi et al., 1982 +; +Laviano, 1985 +; + + +Caffau and Pleničar, 1995 +) considered that the two species have distinctive characteristics as follows: in + +H. nabresinensis + +the right valve is cylindrical (Sladić - +Trifunović, 1978 +; +Laviano, 1985 +), have more pronounced rounded costae ( +Futterer, 1893 +; +Lupu, 1976 +; +Accordi et al., 1982 +) and their pillars are not of the same size ( +Laviano, 1985 +; +Caffau and Pleničar, 1995 +). In + +H. lapeirousei + +the right valve is small conical (Sladić - +Trifunović, 1978 +) without prominent longitudinal ribs ( +Steuber, 1999 +) and the pillars P1 and P2 are similar in size (Sladić - +Trifunović, 1972 +; +Lupu, 1976 +; +Caffau and Pleničar, 1995 +; +Moro et al., 2010 +) or P1 slightly smaller than P2 ( +Douville, 1895 +; +Moro et al., 2010 +). The ligamental ridge (L) is absent or reduced to a small inflexion in outer layer ( +Douville, 1895 +; +Vicens, 1992 +) in both species. +Steuber (1999) +considered as the thin outer shell layer and faintly projecting pillars as safe elements to recognition of + +H. lapeirousei +. + +Our specimens resembles more with those described from +Serbia +(Sladić- +Trifunović, 1972 +), +Italy +( +Laviano, 1985 +) and +Spain +( +Vicens et al., 2004 +) which have thick-shelled valves and same size pillars. + + +Age and distribution: late Santonian-early Campanian in +Croatia +( +Polšak and Mamuzic, 1969 +); middle Campanian in +Spain +( +Floquet, 1991 +); middle Campanian –early Maastrichtian in +Croatia +( +Polšak and Mamuzic, 1969 +), +Italy +( +Swinburne and Noacco, 1993 +), +Spain +( +Vicens, 1992 +); Maastrichtian in +Greece +( +Steuber, 1999 +), +France +( +Toucas, 1903 +; +Bilotte, 1985 +), +Italy +( +Pons and Sirna, 1994 +), +Spain +( +Astre, 1962 +), +Turkey +( +Özer, 1994 +; +Fenerci, 1999 +). + + + + \ No newline at end of file diff --git a/data/03/EE/87/03EE87ECFFACFFBA44DBD50BBEA881A0.xml b/data/03/EE/87/03EE87ECFFACFFBA44DBD50BBEA881A0.xml new file mode 100644 index 00000000000..978a2be20a6 --- /dev/null +++ b/data/03/EE/87/03EE87ECFFACFFBA44DBD50BBEA881A0.xml @@ -0,0 +1,224 @@ + + + +Upper Cretaceous Rudist-Bearing Mixed Siliciclastic-Carbonate And - Volcanoclastic Deposits From Strâmturii Valley, Borod Basin, Northern Apuseni Mountains: Description, Microfacies And Depositional Environments + + + +Author + +Săsăran, Liana +Babeş-Bolyai University, Department of Geology and Center for Integrated Geological Studies, 1 Mihail Kogălniceanu Street, 400084 Cluj-Napoca, Romania; liana. sasaran @ ubbcluj. ro; * Corresponding author: emanoil. sasaran @ ubbcluj. ro; ioan. bucur @ ubbcluj. ro +liana.sasaran@ubbcluj.ro + + + +Author + +Săsăran, Emanoil +Babeş-Bolyai University, Department of Geology and Center for Integrated Geological Studies, 1 Mihail Kogălniceanu Street, 400084 Cluj-Napoca, Romania; liana. sasaran @ ubbcluj. ro; * Corresponding author: emanoil. sasaran @ ubbcluj. ro; ioan. bucur @ ubbcluj. ro +liana.sasaran@ubbcluj.ro + + + +Author + +Bucur, Ioan I. +Babeş-Bolyai University, Department of Geology and Center for Integrated Geological Studies, 1 Mihail Kogălniceanu Street, 400084 Cluj-Napoca, Romania; liana. sasaran @ ubbcluj. ro; * Corresponding author: emanoil. sasaran @ ubbcluj. ro; ioan. bucur @ ubbcluj. ro +liana.sasaran@ubbcluj.ro + +text + + +Acta Palaeontologica Romaniae + + +2018 + +2018-05-06 + + +14 + + +1 + + +3 +20 + + + +journal article +10.5281/zenodo.13190185 +1842-371x +13190185 + + + + + + + +Vaccinites archiaci +Douvillé, 1892 + + + + + + + +Fig. 8j + + +1892 + +Hippurites archiaci +Munier + +Chalmas- Douvillé, p. 45, pl.5, figs.1-3, text-figs.30-33 + + +1904 + +Vaccinites archiaci + +Munier-Chalmas- Toucas, p. 103, pl.15, figs.4-5, text-figs.164, 165. + + +1966 + +Hippurites (Vaccinites) archiaci + +Munier- Chalmas- Todiriță- Mihăilescu, p. 72, pl. 21,22. + + +1968 + +Hippurites (Vaccinites) archiaci + +Munier- Chalmas- Lupu, p. 77, pl.1, fig.8, text-fig.5. + + +1969 + +Hippurites (Vaccinites) archiaci + +Munier- Chalmas- Polšak and Mamuzic, pp. 235, 239. + + +1976 + +Vaccinites archiaci + +Munier-Chalmas-Lupu, p. 114, pl.3, figs.12,12a-b,13, pl.36, fig.1. + + +1992 + +Vaccinites archiaci +(Douvillé) + +- Vicens, p. 120, pls.32-34, pl.45, figs.1-2. + + +1999 + +Vaccinites archiaci +(Douvillé) + +- Steuber, p. 125, pl.23, fig.1, text-fig.48a-c. + + +2016 + +Vaccinites archiaci +(Douvillé) + +- Moro et al., p.16,18, figs. 11d, 12c. + +Material: fragment of RV, embedded in rock (no. 24090- BBU-MPS). + +Description: Right valve is conical with umbo curved ventrally, having +70 mm +in length and 45/ +50 mm +in diameter. The thickness of the outer shell layer varies between +3 to 4 mm +. The ligamental ridge (L) is shorter, +7 mm +in length, wider and clearly truncated ( +Fig. 8j +). The first pillar (P1) is square and shorter than the second pillar (P2) which is slightly pedunculated at the base. In the specimen with right valve embedded in limestone the diameter in transverse section measure 35/ +45 mm +, showing a ligamental ridge (L) strongly developed, triangular at the base and lamelliform, +13 mm +in length, with inner termination truncated with V-shaped incision ( +Fig. 8j +). The first pillar (P1) is thick, rectangular in shape, with sub-parallel flanks; shorter than L and P2, having +10 mm +in length. The second pillar (P2) is slightly pinched at the base, +15 mm +in length with a head oval-elongated and curved anteriorly. The compact outer shell layer is thin, + + +2-3 mm +in thickness. No preserved myocardinal apparatus. + + +Observations: For many years species + +Vaccinites archiaci + +was assigned to Munier-Chalmas in the synonymy lists used by various authors. But, +Vicens (1992) +and +Steuber (1999) +draw attention that +Douvillé (1892) +described and illustrated this species for the first time based on the material from Munier-Chalmas which only mentioned ” + +Hippurites archiaci + +” in his work, without description. So, correct attribution is + +Vaccinites archiaci +Douvillé, 1892 + +. + + +Age and distribution: Santonian-early Campanian in +Croatia +( +Polšak and Mamuzic, 1969 +), +Greece +( +Steuber, 1999 +), +Romania +( +Lupu, 1976 +), early Campanian in +France +( +Astre, 1954 +; +Bilotte, 1985 +), middle Campanian in southern Pyrenees ( +Vicens, 1992 +); Campanian- Maastricthian in +Afghanistan +( +Vogel, 1971 +), BosniaHerzegovina (Sliskovic, 1984); +Slovenia +( +Pleničar and Sribar, 1992 +). + + + + \ No newline at end of file diff --git a/data/03/EE/87/03EE87ECFFACFFBA477DD4CCB81B84D8.xml b/data/03/EE/87/03EE87ECFFACFFBA477DD4CCB81B84D8.xml new file mode 100644 index 00000000000..52a377fd17d --- /dev/null +++ b/data/03/EE/87/03EE87ECFFACFFBA477DD4CCB81B84D8.xml @@ -0,0 +1,226 @@ + + + +Upper Cretaceous Rudist-Bearing Mixed Siliciclastic-Carbonate And - Volcanoclastic Deposits From Strâmturii Valley, Borod Basin, Northern Apuseni Mountains: Description, Microfacies And Depositional Environments + + + +Author + +Săsăran, Liana +Babeş-Bolyai University, Department of Geology and Center for Integrated Geological Studies, 1 Mihail Kogălniceanu Street, 400084 Cluj-Napoca, Romania; liana. sasaran @ ubbcluj. ro; * Corresponding author: emanoil. sasaran @ ubbcluj. ro; ioan. bucur @ ubbcluj. ro +liana.sasaran@ubbcluj.ro + + + +Author + +Săsăran, Emanoil +Babeş-Bolyai University, Department of Geology and Center for Integrated Geological Studies, 1 Mihail Kogălniceanu Street, 400084 Cluj-Napoca, Romania; liana. sasaran @ ubbcluj. ro; * Corresponding author: emanoil. sasaran @ ubbcluj. ro; ioan. bucur @ ubbcluj. ro +liana.sasaran@ubbcluj.ro + + + +Author + +Bucur, Ioan I. +Babeş-Bolyai University, Department of Geology and Center for Integrated Geological Studies, 1 Mihail Kogălniceanu Street, 400084 Cluj-Napoca, Romania; liana. sasaran @ ubbcluj. ro; * Corresponding author: emanoil. sasaran @ ubbcluj. ro; ioan. bucur @ ubbcluj. ro +liana.sasaran@ubbcluj.ro + +text + + +Acta Palaeontologica Romaniae + + +2018 + +2018-05-06 + + +14 + + +1 + + +3 +20 + + + +journal article +10.5281/zenodo.13190185 +1842-371x +13190185 + + + + + + + +Vaccinites sulcatus +Defrance, 1821 + + + + + + + +Fig. 8k +. + + +1821 + +Hippurites (Vaccinites) sulcatus + +-Defrance, p. 195, pl. LXXXIII, fig. 3. + + +1904 + +Vaccinites sulcatus +Defrance-Toucas + +, p. 102, pl.15, figs.1-3, text-figs.161-163. + + +1966 + +Hippurites (Vaccinites) sulcatus + +Defrance- Todiriță- Mihăilescu, p. 73, pl.26, figs.1,2. + + +1967 + +Hippurites (Vaccinites) sulcatus + +Defrance- Polšak, p. 124, 212, pl.79, fig.2. + + +1969 + +Hippurites (Vaccinites) sulcatus + +Defrance- Lupu, p. 208, pl.1, fig.20, text-fig.4. + + +1976 + +Vaccinites sulcatus + +Defrance- Lupu, p. 109, pl.1, figs.1a-b,2, pl.35, figs.1,2. + + +1992 + +Vaccinites sulcatus ( +Defrance +) + +- Vicens, p. 117, pl.31, figs.1-14. + + +1998 + +Vaccinites sulcatus ( +Defrance +) + +- Peza, p. 264, text-fig.14; fig. 4:5; figs.8:3-5; fig.10:2. + + +2004 + +Vaccinites sulcatus ( +Defrance +) + +- Caffau et al., p.160, pl. 2, fig.3. + + + +Material: +1 specimen +, only right valve (no. 23504- +BBU-MPS +) + +. + + +Description: Lower valve is conical, +50 mm +in length and with a diameter equal to +35 mm +. The triangular ligamental ridge (L) is wide and short, having its end clearly truncated ( +Fig. 8k +). The first pillar (P1) is wide and short, with the same length as ligamental ridge. The second pillar (P2) is longer than the first pillar (P1), and is slightly pinched at the base with a head oval-elongated, curved anteriorly ( +Fig. 8k +). + + +Remarks: + +Vaccinites sulcatus + +is very similar to + +Vaccinites archiaci + +but differs from the latter species by its wide and shorter ligamental ridge. In + +Vaccinites archiaci + +the ligamental ridge is thin and longer than first pillar (P1). + + +Age and distribution: Santonian-early Campanian in +Albania +( +Peza, 1992 +, +1998 +), +Austria +( +Steuber, 2001 +), +Croatia +( +Polšak and Mamuzic, 1969 +), +Italy +(Caffau et al., 2004), +France +( +Astre, 1962 +) +Romania +(Todiriță- +Mihăilescu, 1966 +; +Lupu, 1969 +, +1976 +), +Slovenia +( +Pleničar, 1961 +), and +Turkey +( +Özer, 1998 +); Campanian-Maastrichtian in +Croatia +( +Polšak and Mamuzic, 1969 +). + + + + \ No newline at end of file diff --git a/data/03/F4/07/03F40736FFE4FFFD1857FB7BFF2C5793.xml b/data/03/F4/07/03F40736FFE4FFFD1857FB7BFF2C5793.xml new file mode 100644 index 00000000000..406fde2b424 --- /dev/null +++ b/data/03/F4/07/03F40736FFE4FFFD1857FB7BFF2C5793.xml @@ -0,0 +1,93 @@ + + + +Dasycladales Algae From The Norian-Rhaetian Reef Carbonates Of Argolis Peninsula, Greece + + + +Author + +Senowbari-Daryan, Baba + +text + + +Acta Palaeontologica Romaniae + + +2014 + +2014-09-29 + + +10 + + +1 - 2 + + +1 +2 + + + +journal article +10.5281/zenodo.13189667 +1842-371x +13189667 + + + + + + +Probolocuspis +? +tenuiparia + +nov. sp. + + + + + +( +Fig. 5 +e-l) + +Derivatio nominis: Tenuis (latin) = thin, and paries (latin) = wall. Named from the thin thallus wall of the species. + +Holotype +: +Fig. 5h +. + + +Locus typicus: Norian-Rhaetian reef carbonates north of the nearby town Sarmeika ( +Fig. 1 +). + +Stratum typicum: Norian-Rhaetian reef carbonates. +Diagnosis: Cylindrical thallus with thin wall and wide axial cavity. Laterals, corresponding to the thin thallus wall, are short. Individual laterals are visible only as small spines on the outer surface of the thallus. +Material: Numerous species in several thin sections. + +Description: Similar to the preceding described species most specimens of this alga are cut in cross sections. The thallus walls of all specimens are recrystallized, the nature of laterals is visible only as small spines on the outer surface of the thallus. The arrangement of the laterals is not clear and therefore the attribution to the genus + +Probolocupsis + +is uncertain. + + +The specimen designated as +holotype +( +Fig. 5h +) is an oblique to longitudinal section exhibiting clearly the tip of the needle- or spine-like individual laterals on one side. Some specimens ( +Fig. 5 +e-f, j-k), cut in cross sections clearly show this character of the thallus. For the biometrical data and dimensions of the thallus see +Table 2 +. + + + + \ No newline at end of file diff --git a/data/03/F4/07/03F40736FFE6FFFD184EF9EBFD6E541D.xml b/data/03/F4/07/03F40736FFE6FFFD184EF9EBFD6E541D.xml new file mode 100644 index 00000000000..2adcbe37897 --- /dev/null +++ b/data/03/F4/07/03F40736FFE6FFFD184EF9EBFD6E541D.xml @@ -0,0 +1,481 @@ + + + +Dasycladales Algae From The Norian-Rhaetian Reef Carbonates Of Argolis Peninsula, Greece + + + +Author + +Senowbari-Daryan, Baba + +text + + +Acta Palaeontologica Romaniae + + +2014 + +2014-09-29 + + +10 + + +1 - 2 + + +1 +2 + + + +journal article +10.5281/zenodo.13189667 +1842-371x +13189667 + + + + + + +Probolocupsis sarmeikensis + +nov. sp. + + + + + +( +Fig. 2 +; +Fig. 4 +a-n) + +Derivatio nominis: Named from the town Sarmeika near the locality. + +Holotype +: +Fig. 4l +(magnification in +Fig. 2 +). + + +Paratypes +: +Fig. 4 +a-k, m-n. + + +Locus typicus: Norian-Rhaetian reef carbonates, north of the town of Sarmeika in the Mavrovouni Mountains ( +Fig. 1 +). + +Stratum typicum: Norian-Rhaetian reef carbonates. +Diagnosis: Cylindrical thallus with a narrow axial cavity. Trichophorous laterals of the first order are usually amalgamated at the base appearing as a thick wall around the axial cavity. Euspondyl arrangement of the laterals. + + +Fig. 2 + +Probolocupsis sarmeikensis + +nov. sp. +(Holotype). The magnification from Fig. 4l shows the spine-like extended individual laterals (some of the internal pores: see arrows). Laterals are perpendicular to the thallus axis. + + +Differential diagnosis: See comparison after the description of the species. +Material: Numerous specimens in several thin sections. + +Description: Almost all specimens of this cylindrical alga are cut in cross sections. +Two specimens +illustrated in +Fig. 4c +and the +holotype +Fig. 4l +(H) exhibit the most characteristics of the alga in longitudinal section. The thallus of the +holotype +reaches a length of almost +10 mm +with a diameter of +2.2 mm +. The axial cavity of the +holotype +has a diameter of about +0.4 mm +. Both longitudinal sections show that the laterals are arranged perpendicular to the axial cavity. The alga is characterized by a narrow axial cavity of +0.25-0.5 mm +and a thick thallus wall. Ratio of axial cavity/thallus diameter varies between 11 % and 25% (see +Tab. 1 +). Individual laterals appear spine-like on the thallus outside. + + +Marginal sections of the laterals may appear as points or small white circles ( +Fig. 4e, g, k +). Because of the recrystallization of the majority of specimens the base of laterals is not well recognizable. The well preserved specimen illustrated in +Fig. 4j +exhibits that the laterals are arisen as single from the axial cavity, but others show two or three laterals arisen from the common base ( +Fig. 4h +). Each spine-like lateral contains a very narrow tube ( +Fig. 2 +; + +Fig. +4m + +: arrows). Length of laterals is usually +1 mm +, their diameter about +0.08-0.15 mm +, their number in each is 22-40. In the +holotype +as well as in the majority of specimens the recrystallization amalgamated the base of laterals, appearing as a thick wall around the axial cavity. Some biometrical data of + +Probolocupsis sarmeikensis + +nov. sp. +are listed in +Table 1 +. + + + +Table 1. +Some biometrical data of the thallus of + +Probolocupsis sarmeikensis + +nov. sp. +D) diameter of the thallus, d) diameter of the axial cavity. “Specimen” indicates the number of the measured specimens of corresponding Plates and Figures. All measurements are in mm. + + + + + + + + + + + + + + + + + + + + + + + + + + + + + + + + + + + + + + + + + + + + + + + + + + + + + + + + + + + + + + + + + + + + + + + + + + + + + + + + + + + + + + + + + + + + + + + +
SpecimenDdd/DThin section
Pl. 1, Fig. 32.00.420 %G05C
Pl. 1, Fig. 82.40.3615 %G05C
Pl. 1, Fig. 82.50.3815 %G05C
Pl. 1, Fig. 12, H2.20.418 %G05C
Pl. 1, Fig. 122.20.418 %G05b
Pl. 1, Fig. 122.40.417 %G05b
Pl. 1, Fig. 52.60.3212 %G05b
Pl. 1, Fig. 13.20.3411 %G05b
Pl. 1, Fig. 22.40.4519 %G05b
Pl. 1, Fig. 22.00.420 %G05b
Pl. 1, Fig. 72.00.525 %G05b
Pl. 2, Fig. 41.00.2525 %G12
+ + + +Fig. 3 + +Diplopora obliqusipora + +nov. sp. +(Holotype). The magnification from Fig. 5c shows the relics of metaspondyle arrangement of the tufts (large arrows, also the cross sections of the laterals at the base of the thallus indicate the metaspondyle arrangement of the laterals). Small arrows indicate the tufts arising from the common base. The thin wall around the axial cavity is clearly recognizable. + + + +Comparison: The distinctly narrow axial cavity of + +Probolocuspis sarmeikensis + +nov. sp. +differs (without regard to the stratigraphic age) this species from the +type +species – + +Probolocupsis espahkensis +Brönnimann et al. + +– and from + +P. aculeata +Nittel + +clearly. Differences of the skeletal elements are additional criteria for distinguishing this species from the known species. + + + +Table 2. +Some biometrical data of the thallus of + +Probolocuspis +? +tenuiparia + +nov. sp. +All measurements are in mm. For abbreviations see Table 1. + + + +Schlagintweit et al. (2013) +illustrated in +Fig. 3a +some dasycladalean specimens (maybe recrystallized) from the “Lower Gosau Subgroup of +Austria +” as +Milanovicella + +hammudai +( +Radoičić 1975 +) + +, which are very similar to recrystallized specimens of + +P. sarmeikensis + +nov. sp. +According to the diagnosis of +Milanovicella +, given by +Granier & Berthou (1994) +and compared with illustrations of the +type +material of +Radoičić (1975) +, described as + +Likanella hammudai + +and revised by +Schlagintweit (1990) +the species of Sarmeika can not be attributed to this genus. + + + + + + + + + + + + + + + + + + + + + + + + + + + + + + + + + + + + + + + + + + + + + + + + + + + + + + + + + + + + + + + + + + + + + + + + + + + + + + + + + + + + + + + +
SpecimenDDd/DThin section
Pl. 2, Fig. 71.00.2525 %G08a
Pl. 2, Fig. 100.450.07517 %G08a
Pl. 2, Fig. 60.30.05.17 %G08a
Pl. 2, Fig. 90.40.0718 %G08a
Pl. 2, Fig. 90.40.1230 %G08a
Pl. 2, Fig. 90.80.1013 %G08a
Pl. 2, Fig. 80.30.0517 %G08a
Pl. 2, Fig. 50.40.0513 %G08b
Pl. 2, Fig. 50.50.0714 %G08b
Pl. 2, Fig. 50.450.0716 %G08b
Pl. 1, Fig. 50.360.0822 %G08b
+ + +There are some morphological similarities between the species + +Neogyroporella + +? +gawliki +described from the Upper Jurassic-Lower Cretaceous of the Northern Calcareous Alps by +Schlagintweit (2005 +, compare also +Schlagintweit 2011 +) and + +P. sarmeikensis +. + + + +The general appearance of + +P. sarmeikensis + +is similar to + +Teutloporella echinata + +, described by +Ott (1975) +from the Ladinian of the Lombardian Alps, northern +Italy +. The individual laterals in + +P. sarmeikensis + +are arranged perpendicular to the axial cavity, but they are orientated oblique in + +T. echinata + +. Laterals are risen as single from the axial cavity (later they can be branched: +Fig. 4d, h +) in + +P. sarmeikensis + +, but they may be doubled? in + +T. echinata + +. In addition the shape of laterals in + +P. sarmeikensis + +is always spine-like and their cross sections are always circular or oval, but the shapes of laterals (see + +Ott 1975 + +: fig. 3) and their cross sections in + +T. echinata + +are different. Advanced interpretations of these features deserve a comparing study of the material from Alps and Argolis. + + + + \ No newline at end of file diff --git a/data/26/3C/2D/263C2D4B2710FFA7F636FA017794F867.xml b/data/26/3C/2D/263C2D4B2710FFA7F636FA017794F867.xml new file mode 100644 index 00000000000..ef6a4e7f0f8 --- /dev/null +++ b/data/26/3C/2D/263C2D4B2710FFA7F636FA017794F867.xml @@ -0,0 +1,230 @@ + + + +Foraminiferal Assemblages And Facies Associations In The Upper Jurassic Carbonates From Ardeu Unit (Metaliferi Mountains, Romania) + + + +Author + +Pleş, George + + + +Author + +Bucur, Ioan I. + + + +Author + +Păcurariu, Adriana + +text + + +Acta Palaeontologica Romaniae + + +2015 + +2015-12-27 + + +11 + + +2 + + +43 +57 + + + +journal article +10.5281/zenodo.13190287 +1842-371x +13190287 + + + + + + + +Labyrinthina mirabilis +Weynschenk, 1951 + + + + + + + +( +Fig. 2 +a-h) + + +1956 – + +Labyrinthina mirabilis + +– Weynschenk, p. 283, pl. 1, fig. 8. + + +1896 – + +Labyrinthina mirabilis +– + +Mantea & Tomescu, pl 4, figs. 1-9. + + +1988 – + +Labyrinthina mirabilis +– + +Septfontaine, p. 243, pl. 1, figs. 10, 12. + + +2005a – + +Labyrinthina mirabilis + +– Bucur & Săsăran, p. 30, pl. 2, figs. 3, 4. + + +2005 – + +Labyrinthina mirabilis + +– Schlagintweit et al., p. 31, fig. 13 a, b. + + +2008 – + +Labyrinthina mirabilis + +– Omaña & Gonzalez- Arreola, p. 803, fig. 7a. + + + +Fig. 1 +Geological map of the BalȘa- Ardeu-Băcâia region (modified after +Mantea & Tomescu, 1986 +) +1 +Mesozoic ophiolites (CăpâlnaȘ- Techereu Nappe); +2 +Oxfordian limestones (Ardeu Unit); +3 +Kimmeridgian-Tithonian carbonates (Ardeu Unit); +4 +Barremian-Aptian limestones (Ardeu Unit); +5 +Aptian conglomerates and sandstones (CăpâlnaȘ- Techereu Nappe); +6 +Albian breccia and sandstones (CăpâlnaȘ- Techereu Nappe); +7 +Coniacian-Santonian siltites and sandstones; +8 +Santonian- Campanian marls; +9 +Santonian-Maastrichtian flysch deposits; +10 +?Maastrichtian-Paleogene continental deposits; +11 +Badenian limestones; +12 +Quaternary deposits; +13 +Faults; +14 +Nappe; +15 +Location of the studied sections. + + + +Description: +In early ontogenetic stage the test is planispirally coiled (up to 3 whorls), later becoming elongate, rectilinear up to +2.1 mm +in lenght. The diameter of the coiled part ranges between 0.49 and +0.91 mm +. Proloculus is globular. Chambers are separated by slightly convex septa. Vertical beams extend radially from the margins of the wall to the center, but not reaching it. Interseptal pillars are noticed in the adult uncoiled stage, mainly in the central part. They can be continuous from chamber to chamber (see +Fig. 2c +). Wall agglutinated. Aperture is simple and interiomarginal in the enrolled stage, becoming multiple in the adult rectilinear stage. + + + + +Remarks: +In our samples, + +Labyrinthina mirabilis + +specimens are very abundant and identified in all ontogenetic stages. An important structural feature of this species is represented by the presence of the interseptal pillars. In early ontogenetic stages pillars are less evolved or absent, accounting for the simple morphology of the chambers and aperture. In the adult uncoiled part of the test, interseptal pillars are well formed and may develop a continuous trend throughout the chambers. The labyrinthic architecture of + +L. mirabilis + +can be the result of a random fusing process between beams and pillars in the adult stage. All of the + +L. mirabilis + +specimens are found free, in contrast to some encrusting forms illustrated by +Weynschenk (1956) +. The non-encrusting feature of the species was documented soon after by several authors ( +Fourcade & Neumann, 1965 +; Gušić, 1968, +Schlagintweit et al. 2005 +). + + +Stratigraphic range: + +L. mirabilis + +is a widespread taxon in the Upper Jurassic carbonates of the Tethyan realm. It was first described by +Weynschenk (1951) +from the Upper Jurassic deposits of the Sonnwend Mountains ( +Austria +). Other occurrences are listed in +Table 1 +. +Loeblich & Tappan (1988) +included the foraminifer + +Lituosepta recoarensis +, + +described by +Cati (1959) +from Lower Jurassic limestones, into the synonymy list of + +L. mirabilis + +. Based on this fact, the authors extended the stratigraphic range of + +L. mirabilis + +from Lower to Upper Jurassic. +Septfontaine (1988) +in his evolutionary classification of Jurassic lituolids, clearly explains the main differences between the two taxa and restricts + +L. mirabilis + +to Upper Jurassic (as it was described) contrasting the Upper Sinemurian + +Lituosepta recoarensis +. + +Bassoullet (1997) +placed the stratigraphic position of this taxon between Uppermost Oxfordian and basal Tithonian. + + + + \ No newline at end of file diff --git a/data/26/3C/2D/263C2D4B2715FFA0F591F864708EF96E.xml b/data/26/3C/2D/263C2D4B2715FFA0F591F864708EF96E.xml new file mode 100644 index 00000000000..5a98e9bacd4 --- /dev/null +++ b/data/26/3C/2D/263C2D4B2715FFA0F591F864708EF96E.xml @@ -0,0 +1,188 @@ + + + +Foraminiferal Assemblages And Facies Associations In The Upper Jurassic Carbonates From Ardeu Unit (Metaliferi Mountains, Romania) + + + +Author + +Pleş, George + + + +Author + +Bucur, Ioan I. + + + +Author + +Păcurariu, Adriana + +text + + +Acta Palaeontologica Romaniae + + +2015 + +2015-12-27 + + +11 + + +2 + + +43 +57 + + + +journal article +10.5281/zenodo.13190287 +1842-371x +13190287 + + + + + + + +Bramkampella arabica +Redmond, 1964 + + + + + + + +( +Fig. 3 +a-c) + + +1964 – + +Bramkampella arabica + +– Redmond, p. 409-414, pl. 1, figs. 26-29; pl. 2, figs. 19-20. + + +1988 – + +Bramkampella arabica + +– Loeblich & Tappan., p. 101-102, pl. 100, figs. 14-18. + + +1991 – + +Bramkampella arabica + +– Banner & Whittaker, p. 45, pl. 2, figs. 1-7. + + +1997 – + +Bramkampella arabica + +– Gorbachik & Mohamad, p. 347, pl. 1, figs. 8, 9, 11. + + +2005a – + +Bramkampella arabica + +– Bucur & Sasaran, pl. 2, figs. 6, 7. + + +Description: +The test is subconical with a fine-grained imperforate agglutinated wall. In early ontogenetic stages, the test is planspirally-enrolled, involute. In the adult stage, the test begins to uncoil, finally becoming rectilinear, uniserial, up to +2.21 mm +in lenght. In transversal section the test is circular in shape with a diameter size between +1.1 – 1.56 mm +. The chambers are short and flattened, separated by strongly embowed septa. Beams and rafters are displayed as an interseptal alveolar network (septulae). The spetulae are elongated and radially developed inward up to the central part of the test. The aperture is terminal, multiple, represented as large pores on the central part of the septal surface. + + + + +Remarks: +In our samples, + +Bramkampella arabica + +is frequently associated with the species described before ( + +L. mirabilis + +, + +P. caelinensis + +and + +E. praekelleri + +). Several similarities with other cyclamminids, especially with + +Rectocyclammina chouberti +Hottinger + +can be noticed sometimes. They are restricted mainly to the internal morphology of the species. Even so, the multiple aperture, the presence of interseptal pillars or the highly arched septa, clearly differentiate + +Bramkampella arabica + +from + +Rectocyclammina chouberti +( +Gorbachik & Mohamad, 1997 +) + +. + + +Stratigraphic range: + +Bramkampella arabica + +was firstly described from Upper Jurassic-basal Cretaceous deposits from Arabia by +Redmond (1964) +. Several lowermost Cretaceous (Berriasian-Valanginian) records of the species were documented by +Gorbachik & Mohamad (1997) +and Nouajim +Clark & Boudagher-Fadel (2001) +. Due to these occurrences, mainly in lowermost Cretaceous carbonates, + +B. arabica + +was considered to be an index marker for the Berriasian-?Valanginian interval. However, +Bucur & Săsăran (2005a) +identified this species, besides the lowermost Cretaceous deposits, in Kimmeridgian-upper Tithonian limestones from Trascău Mountains. In the samples from Ardeu Unit, + +B. arabica + +is also found in association with typical Upper Jurasic foraminifera ( + +L. mirabilis + +or + +P. caelinensis + +). Summarizing, the stratigraphic position of + +Bramkampella arabica + +is Kimmeridgian-?lower Valanginian. + + + + \ No newline at end of file diff --git a/data/27/4E/B3/274EB30E4E3B9A25FF605D2FFC6F2F2E.xml b/data/27/4E/B3/274EB30E4E3B9A25FF605D2FFC6F2F2E.xml new file mode 100644 index 00000000000..1b633174db1 --- /dev/null +++ b/data/27/4E/B3/274EB30E4E3B9A25FF605D2FFC6F2F2E.xml @@ -0,0 +1,167 @@ + + + +Suraqalatia Brasieri Görmuş, Lawa & Nuaimy, 2017 (Larger Benthic Foraminifera; Suraqalatiidae N. Fam.) From The Late Maastrichtian Of The Tarbur Formation (Zagros Fold-Thrust-Belt) And Remarks On Dicyclina Munier-Chalmas, 1887 + + + +Author + +Schlagintweit, Felix +Lerchenauerstr. 167, 80935 Munich, Germany, * Corresponding author: felix. schlagintweit @ gmx. de +felix.schlagintweit@gmx.de + + + +Author + +Rashidi, Koorosh +Department of Geology, Payame Noor University, Po Box 19395 - 3697 Tehran, Iran, kooroshrashidi @ pnu. ac. ir +kooroshrashidi@pnu.ac.ir + +text + + +Acta Palaeontologica Romaniae + + +2018 + +2018-07-25 + + +14 + + +1 + + +21 +29 + + + +journal article +10.5281/zenodo.13190044 +1842-371x +13190044 + + + + + +Family +Suraqalatiidae Schlagintweit & Rashidi +n. fam. + + + + + +Diagnosis: +Test low-conical to almost flat with a reduced probably low trochospiral stage followed by an uncoiled main part with annular chambers. Marginal part of chambers with exoskeleton consisting of series of fine beams and rafters, covered externally by a thin epiderm. The exoskeleton forms a dense polygonal subepidermal network becoming coarser towards the chamber interior. The inner part of the chambers is undivided (no endoskeleton). Test wall agglutinating. Foramina multiple. + + + + +Remarks. +Discussing the suprageneric position, the genus + +Suraqalatia + +was placed in the family +Dicyclinidae Munier-Chalmas +by +Görmüş et al. (2017) +. The authors (p. 365) also state that "dicyclinid forms include a tiny proloculus" contrasting other forms such as + +Orbitopsella + +or + +Orbitolina + +. This statement is incorrect and does not take into account the results of +Cherchi & Schroeder (1990a +, b) as will be shown later in the text (see chapter on + +Dicyclina + +). +Loeblich and Tappan (1987) +and +Kaminski (2014) +separated two families, the +Cuneolinidae Saidova +(genera with conical, compressed or not, to flabelliform tests: + +Cuneolina + +, + +Palaeolituonella + +, + +Pseudotextulariella + +, + +Vercorsella + +) and the +Dicyclinidae Loeblich & Tappan +(genus with cyclic chambers: + +Dicyclina + +). According to the emendation of +Arriaga et al. (2016 +, p. 19), the +Cuneolinidae Saidova +are considered a synonym of +Dicyclinidae +, "because the differences in test shape of the adult forms are not considered a criterion sufficient to erect two separate families. The family is characterized by biserial arrangement of the chambers, reticular subepidermal network, and absence of an endoskeleton". The chamber arrangement in + +Suraqalatia + +is not biserial as in the +Dicyclinidae +and instead is cyclical-concentric, thereby excluding its belonging to the +Dicyclinidae +. Note that for genera that share the same +type +of exoskeleton covered by the epiderm (forming a polygonal subepidermal network), differences in the chamber arrangement are considered a suprageneric criterion: "planispiral to uncoiled, peneropliform or cyclical ( +Spirocyclinidae +); biserial ( +Dicyclinidae +); low trochospiral ( +Dictyopsellidae +)" ( +Albrich et al., 2015 +, p. 265). Representatives of the +Spirocyclinidae +with cyclic (ring-shaped) chambers have a discoidal flattened test; in the +Suraqalatiidae +test is low-conical with annular (ring-shaped) chambers. The early growth stage of the +Spirocyclinidae +displays planispirally arranged chambers. Concerning the exoskeleton, the comparably long (primary) beams protruding widely into the chamber lumen of + +Suraqalatia + +are worth mentioning. For the moment being the +Suraqalatiidae +only include the name-giving genus + +Suraqalatia +Görmüş, Lawa & Al Nuaimy, 2017 + +. The inadequate knowledge on the initial part of + +Suraqalatia + +respectively the megalospheric embryo, and the distributional pattern of the multiple foramina hinders a further specification in the family diagnosis for the time being. + + + + \ No newline at end of file diff --git a/data/2D/5F/87/2D5F8790FFFAFF90FCB1F812FB9BFA4F.xml b/data/2D/5F/87/2D5F8790FFFAFF90FCB1F812FB9BFA4F.xml new file mode 100644 index 00000000000..e76c96a9f98 --- /dev/null +++ b/data/2D/5F/87/2D5F8790FFFAFF90FCB1F812FB9BFA4F.xml @@ -0,0 +1,464 @@ + + + +Some New And Poorly Known Benthic Foraminifera From Late Maatrichtian Shallow-Water Carbonates Of The Zagros Zone, Sw Iran + + + +Author + +Schlagintweit, Felix +Lerchenauerstr. 167, 80935 Munich, Germany, felix. schlagintweit @ gmx. de +felix.schlagintweit@gmx.de + + + +Author + +Rashidi, Koorosh +Department of Geology, Payame Noor University, Po Box 19395 - 3697 Tehran, Iran, kooroshrashidi @ pnu. ac. ir +kooroshrashidi@pnu.ac.ir + +text + + +Acta Palaeontologica Romaniae + + +2016 + +2016-09-04 + + +12 + + +1 + + +53 +70 + + + +journal article +10.5281/zenodo.13189930 +1842-371x +13189930 + + + + + + +Pseudonumoloculina kalantarii + +n. sp. + + + + + + +Fig. +15 + +Holotype: +Slightly oblique axial section of a juvenile specimen (showing notched aperture) illustrated in +Figure 15k +(and detail in +Fig. 15n +). Thin-section NG 85. + + + +Fig. 9 + +Broeckinella arabica +Henson + +( +a–e +) and + +Dicyclina +cf. +schlumbergeri +Munier-Chalmas + +( +f +), Late Maastrichtian Tarbur Formation of Mandegan section, Zagros Zone, SW Iran. +a–d +Oblique equatorial sections, partly fragmentary, in some parts crossing the subepidermal network of beams and rafters (e.g., left side of +d +). +e +Oblique section of + +Broeckinella arabica + +, comparable to the section erroneously illustrated as “ + +Dicyclina schlumbergeri + +” by +Khosrow Tehrani et al., 2008 +in pl. 1, fig. 6. +f + +Dicyclina +cf. +schlumbergeri +Munier-Chalmas + +, subaxial section. Thin-sections: Rt 104 ( +a +), Rt 64 ( +b +), Rt 78 ( +c +), Rt 85 ( +d +), Rt 68 ( +e +), SNSB-BSPG 2016 III-4 ( +f +). Scale bars 0.5 mm. + + + +Origin of the name: +The species name is dedicated to Amir Kalantari, micropalaeontologist of the National Iranian Oil Company for his contributions to the micropalaeontology of +Iran +. + + + + + +Type +locality: + +Naghan section (see +Fig. 2 +) + + + +Type +level: + +Late Maastrichtian of the Tarbur Formation. + + + + +Diagnosis: +Representative of + +Pseudonummoloculina + +with egg-shaped, slightly biumbilicate test, and rounded margin. The test is streptospirally coiled initially (3 to 4 whorls) then oscillating to almost planispiral (up to 5 whorls). Chambers elongated along the coiling, low and only gradually increasing in height. + + + + +Description: +Test ovate, with slight biumbilical depression and broadly rounded periphery. First whorls streptospirally coiled, later planes of coiling become more and more regular to almost planispiral, resulting in an overall sigmoid arrangement when observed in axial sections ( +Fig. 15h +). +Septa +inclined and rather short delimiting chambers that are greatly elongated along the coiling direction and that only gradually increase in height. Number of chambers per whorl unclear. Wall calcareous imperforate, porcelaneous, possibly with some incorporated (agglutinated) grains (e.g., +Fig. 15j, g +). Foramina and aperture with numerous short notches, irregular in shape, protruding from the chamber roof and floor ( +Fig. 15l–n +) +Dimensions (in mm): + + + +Fig. 10 + +Fleuryana adriatica +De Castro, Drobne & Gušić, Late Maastrichtian Tarbur + + + +Formation of Mandegan section, Zagros Zone, SW Iran. +a, f +Equatorial sections. +b–c + + +Oblique sections. +d +Broken oblique section. +e +Axial section. Thin-sections: Rt 87 ( +a +), + + +SNSB-BSPG 2016 III-7 ( +b–c +), Rt 82 ( +d +), Rt 68 ( +e +), Rt 70 ( +f +). + + + + +Fig. 11 + +Broeckina +cf. +dufrenoyi +(d’Archiac) + +, Late Maastrichtian Tarbur Formation of Mandegan section, Zagros Zone, SW Iran. +a +Fragmentary equatorial section showing septules. +b–c +Oblique sections showing septula. +d +Subaxial section. Thin-sections: SNSB-BSPG 2016 III-16 ( +a–b +), SNSB-BSPG 2016 III-17 ( +c +), Rt 113-2 ( +d +). + + + + +Fig. 12 + +Cuvillierinella + +? sp., Late Maastrichtian Tarbur Formation of + + +Mandegan section, Zagros Zone, SW Iran. +a +Oblique section close to axial plane. +b–c +Subaxial sections. sl = septulum. Thin-sections: Rt + + +100 ( +a +), SNSB-BSPG 2016 III-10 ( +b +), SNSB-BSPG 2016 III-18 ( +c +). + + + + +Fig. 13 + +Spirolina +? +farsiana + +n. sp. +, Late Maastrichtian Tarbur Formation of Mandegan section, Zagros Zone, SW Iran. +a +Oblique equatorial section of specimen with uncoiled adult part. +b +Slightly oblique equatorial section with few uncoiling chambers; holotype specimen. +c +Subaxial section: Note changing growth direction of enrolled part. +d +Detail of +e +showing foramina with lip-like projections. +e, f +“Axial” section of the uncoiled part. +g–h +Subaxial sections. Note teeth-like projections in +g +(arrow). +i +, fragmentary oblique section. Thin-sections: Rt 67-3 ( +a, e–d +), Rt 67-2 ( +b, h +), SNSB-BSPG 2016 III-1 ( +c, g, i +), SNSB-BSPG 2016 III-8 ( +f +). + + + +Equatorial diameter (ed): up to +2 mm + + +Axial diameter (ad): up to +0.9 mm + +Ratio ad/ed: 0.6 to 0.7 + +Comparisons: +The differences to the other species of + +Pseudonummoloculina + +can be summarized as follows. + +Pseudonummoloculina aurigerica +Calvez, 1988 + +(Albian of Spain): The planispiral stage of the type-species is reduced with only 1 ½ to 2 ½ whorls compared to up to +5 in + +P. kalantarii + +. Also the size is reduced (ed up to +1.3 mm +, ad up to +0.73 mm +). + + + +Fig. 14 + +Spirolina +? +farsiana + +n. sp. +, Late Maastrichtian Tarbur Formation of Mandegan section, Zagros Zone, SW Iran. +a +Subaxial section. +b–c, f +Equatorial section, partly oblique. +d–e, g +Subaxial, slightly oblique sections. Thinsections: Rt 67-3 ( +a, e +), Rt 70 ( +b, f), +Rt 86 ( +c +), SNSB-BSPG 2016 III-3 ( +d +), Rt 84 ( +g +). + + + + +Pseudonumoloculina heimi +( +Bonet, 1956 +) + +(Cenomanian of +Mexico +): With its numerous whorls (up to 5), and size (ed up to +2.16 mm +), + +P. heimi + +is close to + +P. kalantarii + +. + +P. heimi + +is different from the former in its compressed discoidal test (ratio ad/ed 2.45 to 3.6, as measured from +Conkin and Conkin (1958 +, fig. 1-25). + + + +Pseudonummoloculina robusta +( +Torre, 1966 +) + +(Coniacian or Santonian of +Italy +): In + +P. robusta + +, wall thickness nearly equals the width of the chamber lumen, given rise to the species name. With maximum size of +1.025 mm +, + +P. robusta + +is much smaller than + +P. kalantarii + +. A further difference is the inclination of the axes of successive chamber within a whorl as discernible in equatorial sections ( +Torre, 1966 +, pl. 3, fig. 3) whereas in + +P. kalantarii + +they are more or less in line. + + + +Pseudonummoloculina sopadensis +Drobne, Premru & Ogorelec, 2005 + +, nom. nud. (Thanetian of +Slovenia +): In a congress abstract, +Drobne et al. (2005) +introduced the new species + +Pseudonummoloculina sopadensis + +(with test sizes of up to +1.5 mm +) from the Thanetian of +Slovenia +. So far no valid description and typification were provided and therefore currently the taxon fails to confirm to article 13 of the International Code of Zoological Nomenclature (= nomen nudem). Nonetheless, + +P. sopadensis + +was included in the list of the shallow benthic zones, respecttively SBZ 2 to 3 of +Serra-Kiel et al. (1998) +, noting a forthcoming description. In this connection reference was made to +Dieni et al. (1985 +, pl. 17, fig. 7). One illustration of this taxon can be found in +Drobne and Cosovic (2009 +, fig. 4, + +Pseudonummoloculina + +n. sp. +). A difference of + +P. sopadensis + +to + +P. kalantarii + +might be the reduced size, and test morphology indicated as spherical to slightly nautiloid in +Drobne et al. (2005) +. + + + + \ No newline at end of file diff --git a/data/2D/5F/87/2D5F8790FFFAFF94FCB1FC27FB0EF814.xml b/data/2D/5F/87/2D5F8790FFFAFF94FCB1FC27FB0EF814.xml new file mode 100644 index 00000000000..486a23e19cc --- /dev/null +++ b/data/2D/5F/87/2D5F8790FFFAFF94FCB1FC27FB0EF814.xml @@ -0,0 +1,148 @@ + + + +Some New And Poorly Known Benthic Foraminifera From Late Maatrichtian Shallow-Water Carbonates Of The Zagros Zone, Sw Iran + + + +Author + +Schlagintweit, Felix +Lerchenauerstr. 167, 80935 Munich, Germany, felix. schlagintweit @ gmx. de +felix.schlagintweit@gmx.de + + + +Author + +Rashidi, Koorosh +Department of Geology, Payame Noor University, Po Box 19395 - 3697 Tehran, Iran, kooroshrashidi @ pnu. ac. ir +kooroshrashidi@pnu.ac.ir + +text + + +Acta Palaeontologica Romaniae + + +2016 + +2016-09-04 + + +12 + + +1 + + +53 +70 + + + +journal article +10.5281/zenodo.13189930 +1842-371x +13189930 + + + + + +Genus + +Pseudonummoloculina +Calvez, 1988 + + + + + + +Remarks: +Calvez (1988) +established the genus + +Pseudonummoloculina + +(type-species + +Pseudonummoloculina aurigerica +, Albian + +of the Pyrenees) for “nummoloculinas” with a notched aperture (= an aperture bordered by a series of notches protruding from the floor and roof of the chambers). The widespread Cenomanian “nummoloculinas” were thereafter regarded as + +Pseudonummoloculina +sp. + +by +De Castro (1987) +since they show a “wavy margin” simulating a cribrate aperture. Likewise, the restudy of the Mexican material of + +Nummoloculina heimi +Bonet + +by +Hottinger et al. (1989) +did not substantiate the existence of an aperture with a tooth, in contrast to the emendation provided by +Conkin & Conkin (1958) +, but according to the former, the aperture “ +clearly show rows of notches in the distal margin +”. Owing to these structural differences, +Hottinger et al. (1989 +: p. 104) introduced the new combination + +Pseudonummoloculina heimi +(Bonet) + +concluding that “ +pseudonummoloculinid species exist from Albian to Senonian in at least three neighboring bioprovinces (Caribbean, Pyrenean and western Tethys) +”. In a contribution on Lower- Middle Cretaceous foraminifers from deep-sea drilling legs, +Arnaud-Vanneau & Sliter (1995) +state, “the genus + +Pseudonummoloculina + +is represented by three species: the type-species + +P. aurigerica +Calvez + +(Albian of Spain), + +P. heimi +(Bonet) + +(Cenomanian of Mexico) and + +P. robusta +(Torre) + +(Coniacian or Santonian of +Italy +)”. Excluded are + +Nummoloculina regularis +Philippson + +(late Cretaceous of +Austria +, see discussion in +Schlagintweit, 2008 +, for details) and + +Nummoloculina irregularis +Decrouez & Radoičić, 1977 + +. The latter possessing an ophthalmidid +type +of coiling different from + +Pseudonummoloculina + +. + + + + \ No newline at end of file diff --git a/data/59/37/26/59372626FFF7FFCEFC0771BF910FFB89.xml b/data/59/37/26/59372626FFF7FFCEFC0771BF910FFB89.xml new file mode 100644 index 00000000000..dd91ce028f9 --- /dev/null +++ b/data/59/37/26/59372626FFF7FFCEFC0771BF910FFB89.xml @@ -0,0 +1,126 @@ + + + +Oribatid Mite Fossils From Quaternary And Pre-Quaternary Sediments In Slovenian Caves I. Two New Genera And Two New Species Of The Family Oppiidae From The Early Pleistocene + + + +Author + +Miko, Ladislav +Institute for Environmental Studies, Charles University in Prague, Faculty of Science, Benátská 2, 12801 Prague 2, the Czech Republic; e-mail: ladislavmiko @ seznam. cz + + + +Author + +Mourek, Jan +Dept. of Teaching and Didactics of Biology, Charles University in Prague, Faculty of Science, Viničná 7, 128 44 Prague 2, the Czech Republic + + + +Author + +Meleg, Ioana N. +“ Emil Racoviţa “ Institute of Speleology, Romanian Academy, Clinicilor 5,400006 Cluj-Napoca, Romania + + + +Author + +Moldovan, Oana T. +“ Emil Racoviţa “ Institute of Speleology, Romanian Academy, Clinicilor 5,400006 Cluj-Napoca, Romania + +text + + +Acta Musei Nationalis Pragae Series B + + +2012 + +2012-07-31 + + +68 + + +1 - 2 + + +23 +34 + + + +journal article +2533-4069 + + + + + + + +Praoppiella +MIKO +et +MOUREK + +gen. nov. + + + + + + +Text-fig. 4 +, Pl. 3 + +D i a g n o s i s: Oppiid mites with large cup-like bothridia with indistinct postbothridial tubercles not fused with bothridial rim, with rounded rostrum, short lamellar costulae and well developed interbothridial tubercles. Two pairs of tubercles, larger postbothridial (humeral) and smaller central, present on anterior margin of notogaster. + +T y p e s p e c i e s: + +Praoppiella oanae +MIKO +et +MOUREK + +sp. nov. + + +R e m a r k s: General body form and development of prodorsum (interbothridial tubercles, lamellar costulae, position of setae) indicate similarity to recent species of + +Oppiella + +sensu lato +, e.g. + +Oppiella (Moritzoppia) + +SUBIAS + +et + +RODRIGUEZ + +, 1988 + +. However, large cup-like bothridia and presence of two pairs of tubercles on anterior border of notogaster broadly resemble characters of the suctobelbid group of oribatids. Some important characters (ie. subcapitulum and chelicerae, legs, genital plates etc.) are unfortunatelly lost from the single available specimen. Some characters resemble species of the family +Machuellidae +(eg. small body size, form of sensillus, epimeral setae +4a-c +inserted in one row on posterior border of epimeres etc.), but notogastral and interbothridial tubercles are unknown in +Machuellidae +. Therefore, including the genus in +Oppiidae +, in the vicinity of + +Oppiella +, + +seems to us the most appropriate, though it should be seen as provisional. + + + + \ No newline at end of file diff --git a/data/65/31/62/6531624615425261FE9DFC27FE79FAA3.xml b/data/65/31/62/6531624615425261FE9DFC27FE79FAA3.xml index 3eb7f90f008..2e6940585b5 100644 --- a/data/65/31/62/6531624615425261FE9DFC27FE79FAA3.xml +++ b/data/65/31/62/6531624615425261FE9DFC27FE79FAA3.xml @@ -1,61 +1,62 @@ - - - -Early Miocene Gastropods from the Felli Section (Proto-Mediterranean Sea NW Greece) + + + +Early Miocene Gastropods from the Felli Section (Proto-Mediterranean Sea NW Greece) - - -Author + + +Author -Thivaiou, Danae +Thivaiou, Danae - - -Author + + +Author -Harzhauser, Mathias +Harzhauser, Mathias - - -Author + + +Author -Koskeridou, Efterpi +Koskeridou, Efterpi -text - - -Geodiversitas +text + + +Geodiversitas - -2019 - -2019-04-15 + +2019 + +2019-04-15 - -41 + +41 - -8 + +8 - -323 -366 + +323 +366 -journal article -10.5252/geodiversitas2019v41a8 -2d9cc532-dbf4-46f5-b134-4d8fa2f93663 -1638-9395 -3700008 -urn:lsid:zoobank.org:pub:A2760279-BE3E-4730-9688-9AB777F3A357 +journal article +23659 +10.5252/geodiversitas2019v41a8 +2d9cc532-dbf4-46f5-b134-4d8fa2f93663 +1638-9395 +3700008 +urn:lsid:zoobank.org:pub:A2760279-BE3E-4730-9688-9AB777F3A357 Genus - + Odostomia J. Fleming, 1813 @@ -71,7 +72,7 @@ SPECIES . — Turbo plicatus Montagu, 1803 (= - + Odostomia plicata (Montagu, 1903)) @@ -83,7 +84,7 @@ Montagu, 1803 (= REMARK - + Odostomia has been used for including diff --git a/data/65/31/62/6531624615435260FC26FBA6FA7FFB31.xml b/data/65/31/62/6531624615435260FC26FBA6FA7FFB31.xml index 9935ac7592c..b6b2cde8745 100644 --- a/data/65/31/62/6531624615435260FC26FBA6FA7FFB31.xml +++ b/data/65/31/62/6531624615435260FC26FBA6FA7FFB31.xml @@ -1,61 +1,62 @@ - - - -Early Miocene Gastropods from the Felli Section (Proto-Mediterranean Sea NW Greece) + + + +Early Miocene Gastropods from the Felli Section (Proto-Mediterranean Sea NW Greece) - - -Author + + +Author -Thivaiou, Danae +Thivaiou, Danae - - -Author + + +Author -Harzhauser, Mathias +Harzhauser, Mathias - - -Author + + +Author -Koskeridou, Efterpi +Koskeridou, Efterpi -text - - -Geodiversitas +text + + +Geodiversitas - -2019 - -2019-04-15 + +2019 + +2019-04-15 - -41 + +41 - -8 + +8 - -323 -366 + +323 +366 -journal article -10.5252/geodiversitas2019v41a8 -2d9cc532-dbf4-46f5-b134-4d8fa2f93663 -1638-9395 -3700008 -urn:lsid:zoobank.org:pub:A2760279-BE3E-4730-9688-9AB777F3A357 +journal article +23659 +10.5252/geodiversitas2019v41a8 +2d9cc532-dbf4-46f5-b134-4d8fa2f93663 +1638-9395 +3700008 +urn:lsid:zoobank.org:pub:A2760279-BE3E-4730-9688-9AB777F3A357 Genus - + Pyramidella Lamarck, 1799 @@ -72,7 +73,7 @@ SPECIES — Trochus dolabratus Linnaeus, 1758 (= -Pyramidella +Pyramidella dolabrata (Linnaeus, 1758)), by monotypy. Recent, Caribbean. diff --git a/data/65/31/62/6531624615435261FC3FFB05FE8DFCA2.xml b/data/65/31/62/6531624615435261FC3FFB05FE8DFCA2.xml index 99d6da765f9..d761b58d82e 100644 --- a/data/65/31/62/6531624615435261FC3FFB05FE8DFCA2.xml +++ b/data/65/31/62/6531624615435261FC3FFB05FE8DFCA2.xml @@ -1,60 +1,61 @@ - - - -Early Miocene Gastropods from the Felli Section (Proto-Mediterranean Sea NW Greece) + + + +Early Miocene Gastropods from the Felli Section (Proto-Mediterranean Sea NW Greece) - - -Author + + +Author -Thivaiou, Danae +Thivaiou, Danae - - -Author + + +Author -Harzhauser, Mathias +Harzhauser, Mathias - - -Author + + +Author -Koskeridou, Efterpi +Koskeridou, Efterpi -text - - -Geodiversitas +text + + +Geodiversitas - -2019 - -2019-04-15 + +2019 + +2019-04-15 - -41 + +41 - -8 + +8 - -323 -366 + +323 +366 -journal article -10.5252/geodiversitas2019v41a8 -2d9cc532-dbf4-46f5-b134-4d8fa2f93663 -1638-9395 -3700008 -urn:lsid:zoobank.org:pub:A2760279-BE3E-4730-9688-9AB777F3A357 +journal article +23659 +10.5252/geodiversitas2019v41a8 +2d9cc532-dbf4-46f5-b134-4d8fa2f93663 +1638-9395 +3700008 +urn:lsid:zoobank.org:pub:A2760279-BE3E-4730-9688-9AB777F3A357 - + Pyramidella cf. plicosa @@ -71,7 +72,7 @@ G1-G3) cf. - + Pyramidella plicosa Bronn, 1838: 1026 @@ -79,7 +80,7 @@ cf. cf. - + Pyramidella plicosa – @@ -223,7 +224,7 @@ A and partially immersed, therefore no variability can be observed. There is a v The species differs from -Pyramidella +Pyramidella grateloupi (d’Orbigny, 1852) from the diff --git a/data/65/31/62/6531624615465265FC28FC47FB0FFBD2.xml b/data/65/31/62/6531624615465265FC28FC47FB0FFBD2.xml index 968f2b3c1c3..af2643eb41c 100644 --- a/data/65/31/62/6531624615465265FC28FC47FB0FFBD2.xml +++ b/data/65/31/62/6531624615465265FC28FC47FB0FFBD2.xml @@ -1,61 +1,62 @@ - - - -Early Miocene Gastropods from the Felli Section (Proto-Mediterranean Sea NW Greece) + + + +Early Miocene Gastropods from the Felli Section (Proto-Mediterranean Sea NW Greece) - - -Author + + +Author -Thivaiou, Danae +Thivaiou, Danae - - -Author + + +Author -Harzhauser, Mathias +Harzhauser, Mathias - - -Author + + +Author -Koskeridou, Efterpi +Koskeridou, Efterpi -text - - -Geodiversitas +text + + +Geodiversitas - -2019 - -2019-04-15 + +2019 + +2019-04-15 - -41 + +41 - -8 + +8 - -323 -366 + +323 +366 -journal article -10.5252/geodiversitas2019v41a8 -2d9cc532-dbf4-46f5-b134-4d8fa2f93663 -1638-9395 -3700008 -urn:lsid:zoobank.org:pub:A2760279-BE3E-4730-9688-9AB777F3A357 +journal article +23659 +10.5252/geodiversitas2019v41a8 +2d9cc532-dbf4-46f5-b134-4d8fa2f93663 +1638-9395 +3700008 +urn:lsid:zoobank.org:pub:A2760279-BE3E-4730-9688-9AB777F3A357 Genus - + Ringicula Deshayes, 1838 @@ -69,7 +70,7 @@ Deshayes, 1838 SPECIES . — - + Ringicula ringens (Lamarck, 1804) diff --git a/data/65/31/62/6531624615465265FE92FA05FA43FC82.xml b/data/65/31/62/6531624615465265FE92FA05FA43FC82.xml index 79542abe7bc..b7258396a99 100644 --- a/data/65/31/62/6531624615465265FE92FA05FA43FC82.xml +++ b/data/65/31/62/6531624615465265FE92FA05FA43FC82.xml @@ -1,60 +1,61 @@ - - - -Early Miocene Gastropods from the Felli Section (Proto-Mediterranean Sea NW Greece) + + + +Early Miocene Gastropods from the Felli Section (Proto-Mediterranean Sea NW Greece) - - -Author + + +Author -Thivaiou, Danae +Thivaiou, Danae - - -Author + + +Author -Harzhauser, Mathias +Harzhauser, Mathias - - -Author + + +Author -Koskeridou, Efterpi +Koskeridou, Efterpi -text - - -Geodiversitas +text + + +Geodiversitas - -2019 - -2019-04-15 + +2019 + +2019-04-15 - -41 + +41 - -8 + +8 - -323 -366 + +323 +366 -journal article -10.5252/geodiversitas2019v41a8 -2d9cc532-dbf4-46f5-b134-4d8fa2f93663 -1638-9395 -3700008 -urn:lsid:zoobank.org:pub:A2760279-BE3E-4730-9688-9AB777F3A357 +journal article +23659 +10.5252/geodiversitas2019v41a8 +2d9cc532-dbf4-46f5-b134-4d8fa2f93663 +1638-9395 +3700008 +urn:lsid:zoobank.org:pub:A2760279-BE3E-4730-9688-9AB777F3A357 - + Acteon cf. pinguis @@ -71,7 +72,7 @@ B1, B2) cf. - + Acteon pinguis d’Orbigny, 1852 @@ -158,22 +159,22 @@ Basin) ( A single species of ‘ -Acteon +Acteon ’ has been found, represented mainly by juveniles. The sculpture, apical angle coincide with those of - + A. pinguis but the juvenile and incomplete specimens does not allow a clear identification. Variation in sculpture consists of the grooves that bear less prominent pits and have a smoother aspect abapically. The last whorl of the specimens observed has slightly deeper grooves which could possibly be a feature dominating the sculpture of later whorls. The shape of the shell and the convexity of the whorls are reminiscent of - + Acteon semistriatus (Férussac, 1822) . The sculpture and overall morphology of the recovered specimens is most similar to - + A. pinguis d’Orbigny, 1852 diff --git a/data/65/31/62/6531624615465267FC3BFB25FCE4FDA1.xml b/data/65/31/62/6531624615465267FC3BFB25FCE4FDA1.xml index 4aeb379338d..22acacfad02 100644 --- a/data/65/31/62/6531624615465267FC3BFB25FCE4FDA1.xml +++ b/data/65/31/62/6531624615465267FC3BFB25FCE4FDA1.xml @@ -1,60 +1,61 @@ - - - -Early Miocene Gastropods from the Felli Section (Proto-Mediterranean Sea NW Greece) + + + +Early Miocene Gastropods from the Felli Section (Proto-Mediterranean Sea NW Greece) - - -Author + + +Author -Thivaiou, Danae +Thivaiou, Danae - - -Author + + +Author -Harzhauser, Mathias +Harzhauser, Mathias - - -Author + + +Author -Koskeridou, Efterpi +Koskeridou, Efterpi -text - - -Geodiversitas +text + + +Geodiversitas - -2019 - -2019-04-15 + +2019 + +2019-04-15 - -41 + +41 - -8 + +8 - -323 -366 + +323 +366 -journal article -10.5252/geodiversitas2019v41a8 -2d9cc532-dbf4-46f5-b134-4d8fa2f93663 -1638-9395 -3700008 -urn:lsid:zoobank.org:pub:A2760279-BE3E-4730-9688-9AB777F3A357 +journal article +23659 +10.5252/geodiversitas2019v41a8 +2d9cc532-dbf4-46f5-b134-4d8fa2f93663 +1638-9395 +3700008 +urn:lsid:zoobank.org:pub:A2760279-BE3E-4730-9688-9AB777F3A357 - + Ringicula minor ( Grateloup, 1838 @@ -72,7 +73,7 @@ C1, C2) Auricula ringens var. b. - + minor Grateloup, 1838: 286 @@ -83,7 +84,7 @@ var. b. - + Ringicula minor – @@ -191,7 +192,7 @@ Landau REMARKS In many specimens the outer lip and the parietal callus are not callous. This was also observed in French representatives of - + Ringicula minor from the @@ -207,7 +208,7 @@ Lozouet - + Ringicula minor is a widespread European species ( @@ -225,7 +226,7 @@ Landau FIG. 7. — A1-A3 , - + Mathilda sp., AMPG(IV) 2478; @@ -233,7 +234,7 @@ sp., AMPG(IV) 2478; , B2 , - + Acteon cf. pinguis @@ -248,7 +249,7 @@ d’Orbigny, 1852 , C2 , - + Ringicula minor ( Grateloup, 1838 @@ -291,7 +292,7 @@ sp., AMPG(IV) 2545; , AMPG(IV) 2547; G1-G3 , - + Pyramidella cf. plicosa @@ -306,7 +307,7 @@ cf. , AMPG(IV) 2555 (SEM image); H1-H3 , ‘ - + Odostomia ’ sp. 1, AMPG(IV) 2557; diff --git a/data/65/31/62/6531624615475264FE8AF8D2FE4AF85E.xml b/data/65/31/62/6531624615475264FE8AF8D2FE4AF85E.xml index fb47106e4d4..f24113d88bd 100644 --- a/data/65/31/62/6531624615475264FE8AF8D2FE4AF85E.xml +++ b/data/65/31/62/6531624615475264FE8AF8D2FE4AF85E.xml @@ -1,61 +1,62 @@ - - - -Early Miocene Gastropods from the Felli Section (Proto-Mediterranean Sea NW Greece) + + + +Early Miocene Gastropods from the Felli Section (Proto-Mediterranean Sea NW Greece) - - -Author + + +Author -Thivaiou, Danae +Thivaiou, Danae - - -Author + + +Author -Harzhauser, Mathias +Harzhauser, Mathias - - -Author + + +Author -Koskeridou, Efterpi +Koskeridou, Efterpi -text - - -Geodiversitas +text + + +Geodiversitas - -2019 - -2019-04-15 + +2019 + +2019-04-15 - -41 + +41 - -8 + +8 - -323 -366 + +323 +366 -journal article -10.5252/geodiversitas2019v41a8 -2d9cc532-dbf4-46f5-b134-4d8fa2f93663 -1638-9395 -3700008 -urn:lsid:zoobank.org:pub:A2760279-BE3E-4730-9688-9AB777F3A357 +journal article +23659 +10.5252/geodiversitas2019v41a8 +2d9cc532-dbf4-46f5-b134-4d8fa2f93663 +1638-9395 +3700008 +urn:lsid:zoobank.org:pub:A2760279-BE3E-4730-9688-9AB777F3A357 Genus - + Mathilda Semper, 1865 @@ -72,7 +73,7 @@ SPECIES Turbo quadricarinatus Brocchi, 1814 (= - + Mathilda quadricarinata ( Brocchi, 1814 diff --git a/data/65/31/62/6531624615505273FE9EFBE5FBE3FE40.xml b/data/65/31/62/6531624615505273FE9EFBE5FBE3FE40.xml index 56a42abf2d6..d6dd94577df 100644 --- a/data/65/31/62/6531624615505273FE9EFBE5FBE3FE40.xml +++ b/data/65/31/62/6531624615505273FE9EFBE5FBE3FE40.xml @@ -1,60 +1,61 @@ - - - -Early Miocene Gastropods from the Felli Section (Proto-Mediterranean Sea NW Greece) + + + +Early Miocene Gastropods from the Felli Section (Proto-Mediterranean Sea NW Greece) - - -Author + + +Author -Thivaiou, Danae +Thivaiou, Danae - - -Author + + +Author -Harzhauser, Mathias +Harzhauser, Mathias - - -Author + + +Author -Koskeridou, Efterpi +Koskeridou, Efterpi -text - - -Geodiversitas +text + + +Geodiversitas - -2019 - -2019-04-15 + +2019 + +2019-04-15 - -41 + +41 - -8 + +8 - -323 -366 + +323 +366 -journal article -10.5252/geodiversitas2019v41a8 -2d9cc532-dbf4-46f5-b134-4d8fa2f93663 -1638-9395 -3700008 -urn:lsid:zoobank.org:pub:A2760279-BE3E-4730-9688-9AB777F3A357 +journal article +23659 +10.5252/geodiversitas2019v41a8 +2d9cc532-dbf4-46f5-b134-4d8fa2f93663 +1638-9395 +3700008 +urn:lsid:zoobank.org:pub:A2760279-BE3E-4730-9688-9AB777F3A357 - + Turritella turris de Basterot, 1825 @@ -71,7 +72,7 @@ H1-H4) - + Turritella turris Basterot, 1825: 29 @@ -93,7 +94,7 @@ Lozouet - + Turritella ( Turritella @@ -202,7 +203,7 @@ in diameter.Transition to protoconch marked by the beginning of teleoconch sculp REMARKS The specimens are conspecific with - + Turritella turris of the type-region of the Aquitanian ( diff --git a/data/65/31/62/6531624615505273FF69FC07FE81FB91.xml b/data/65/31/62/6531624615505273FF69FC07FE81FB91.xml index e12c95e6daf..7bbf9cbc103 100644 --- a/data/65/31/62/6531624615505273FF69FC07FE81FB91.xml +++ b/data/65/31/62/6531624615505273FF69FC07FE81FB91.xml @@ -1,61 +1,62 @@ - - - -Early Miocene Gastropods from the Felli Section (Proto-Mediterranean Sea NW Greece) + + + +Early Miocene Gastropods from the Felli Section (Proto-Mediterranean Sea NW Greece) - - -Author + + +Author -Thivaiou, Danae +Thivaiou, Danae - - -Author + + +Author -Harzhauser, Mathias +Harzhauser, Mathias - - -Author + + +Author -Koskeridou, Efterpi +Koskeridou, Efterpi -text - - -Geodiversitas +text + + +Geodiversitas - -2019 - -2019-04-15 + +2019 + +2019-04-15 - -41 + +41 - -8 + +8 - -323 -366 + +323 +366 -journal article -10.5252/geodiversitas2019v41a8 -2d9cc532-dbf4-46f5-b134-4d8fa2f93663 -1638-9395 -3700008 -urn:lsid:zoobank.org:pub:A2760279-BE3E-4730-9688-9AB777F3A357 +journal article +23659 +10.5252/geodiversitas2019v41a8 +2d9cc532-dbf4-46f5-b134-4d8fa2f93663 +1638-9395 +3700008 +urn:lsid:zoobank.org:pub:A2760279-BE3E-4730-9688-9AB777F3A357 Genus - + Turritella ( s.l. diff --git a/data/65/31/62/6531624615525272FC00FA24FD24FCC1.xml b/data/65/31/62/6531624615525272FC00FA24FD24FCC1.xml index 12dfb8b9935..377736471df 100644 --- a/data/65/31/62/6531624615525272FC00FA24FD24FCC1.xml +++ b/data/65/31/62/6531624615525272FC00FA24FD24FCC1.xml @@ -1,54 +1,55 @@ - - - -Early Miocene Gastropods from the Felli Section (Proto-Mediterranean Sea NW Greece) + + + +Early Miocene Gastropods from the Felli Section (Proto-Mediterranean Sea NW Greece) - - -Author + + +Author -Thivaiou, Danae +Thivaiou, Danae - - -Author + + +Author -Harzhauser, Mathias +Harzhauser, Mathias - - -Author + + +Author -Koskeridou, Efterpi +Koskeridou, Efterpi -text - - -Geodiversitas +text + + +Geodiversitas - -2019 - -2019-04-15 + +2019 + +2019-04-15 - -41 + +41 - -8 + +8 - -323 -366 + +323 +366 -journal article -10.5252/geodiversitas2019v41a8 -2d9cc532-dbf4-46f5-b134-4d8fa2f93663 -1638-9395 -3700008 -urn:lsid:zoobank.org:pub:A2760279-BE3E-4730-9688-9AB777F3A357 +journal article +23659 +10.5252/geodiversitas2019v41a8 +2d9cc532-dbf4-46f5-b134-4d8fa2f93663 +1638-9395 +3700008 +urn:lsid:zoobank.org:pub:A2760279-BE3E-4730-9688-9AB777F3A357 @@ -70,7 +71,7 @@ E1-E3) - + Cerithium lignitarum Eichwald, 1830: 224 diff --git a/data/65/31/62/6531624615545271FBB7FB26FF12FC02.xml b/data/65/31/62/6531624615545271FBB7FB26FF12FC02.xml index 50e4d5da0f6..43be020f500 100644 --- a/data/65/31/62/6531624615545271FBB7FB26FF12FC02.xml +++ b/data/65/31/62/6531624615545271FBB7FB26FF12FC02.xml @@ -1,60 +1,61 @@ - - - -Early Miocene Gastropods from the Felli Section (Proto-Mediterranean Sea NW Greece) + + + +Early Miocene Gastropods from the Felli Section (Proto-Mediterranean Sea NW Greece) - - -Author + + +Author -Thivaiou, Danae +Thivaiou, Danae - - -Author + + +Author -Harzhauser, Mathias +Harzhauser, Mathias - - -Author + + +Author -Koskeridou, Efterpi +Koskeridou, Efterpi -text - - -Geodiversitas +text + + +Geodiversitas - -2019 - -2019-04-15 + +2019 + +2019-04-15 - -41 + +41 - -8 + +8 - -323 -366 + +323 +366 -journal article -10.5252/geodiversitas2019v41a8 -2d9cc532-dbf4-46f5-b134-4d8fa2f93663 -1638-9395 -3700008 -urn:lsid:zoobank.org:pub:A2760279-BE3E-4730-9688-9AB777F3A357 +journal article +23659 +10.5252/geodiversitas2019v41a8 +2d9cc532-dbf4-46f5-b134-4d8fa2f93663 +1638-9395 +3700008 +urn:lsid:zoobank.org:pub:A2760279-BE3E-4730-9688-9AB777F3A357 - + Melanopsis sp. @@ -114,11 +115,11 @@ DISTRIBUTION. — REMARKS A single species of - + Melanopsis was found in Felli, including a broken juvenile specimen. The specimens seem to represent an undescribed species, but the available material is not sufficient to formally describe it. All specimens are broken and the apical part is always missing. This species might already have been discussed from other Oligocene and lower Miocene sections in the Mesohellenic Basin as - + Melanopsis impressa Kraus, 1852 @@ -127,7 +128,7 @@ by and Harzhauser & Kowalke (2001) . Due to the poor preservation of these specimens a comparison with the specimens from Felli remains difficult. In any case, it is unlikely that the Greek records represent - + Melanopsis impressa , which is a species from the early Miocene of southern @@ -136,12 +137,12 @@ and et al. 2016) on -Melanopsis +Melanopsis hantkeni Hofmann, 1870). A separation of the species from Felli from -Melanopsis +Melanopsis hantkeni as described by Harzhauser @@ -154,7 +155,7 @@ as described by Harzhauser FIG. 4. — A1-A3 , - + Bittium larrieyense Vignal, 1911 @@ -239,7 +240,7 @@ d’Orbigny, 1852 , AMPG(IV) 2309, protoconch (SEM image); H1-H4 , - + Turritella turris de Basterot,1825 @@ -258,7 +259,7 @@ de Oligocene and early Miocene - + Melanopsis species are frequently found in brackish deposits but are assumed to have favoured freshwater envieronments ( @@ -286,7 +287,7 @@ Moissette 2016 ). Here, the presence of - + Melanopsis is considered to be an indicator of freshwater influx, which is in agreement with the preservation of the specimens. diff --git a/data/65/31/62/6531624615545277FC2EFC47FB71FBD2.xml b/data/65/31/62/6531624615545277FC2EFC47FB71FBD2.xml index d44aa43828e..fc1e56836bf 100644 --- a/data/65/31/62/6531624615545277FC2EFC47FB71FBD2.xml +++ b/data/65/31/62/6531624615545277FC2EFC47FB71FBD2.xml @@ -1,61 +1,62 @@ - - - -Early Miocene Gastropods from the Felli Section (Proto-Mediterranean Sea NW Greece) + + + +Early Miocene Gastropods from the Felli Section (Proto-Mediterranean Sea NW Greece) - - -Author + + +Author -Thivaiou, Danae +Thivaiou, Danae - - -Author + + +Author -Harzhauser, Mathias +Harzhauser, Mathias - - -Author + + +Author -Koskeridou, Efterpi +Koskeridou, Efterpi -text - - -Geodiversitas +text + + +Geodiversitas - -2019 - -2019-04-15 + +2019 + +2019-04-15 - -41 + +41 - -8 + +8 - -323 -366 + +323 +366 -journal article -10.5252/geodiversitas2019v41a8 -2d9cc532-dbf4-46f5-b134-4d8fa2f93663 -1638-9395 -3700008 -urn:lsid:zoobank.org:pub:A2760279-BE3E-4730-9688-9AB777F3A357 +journal article +23659 +10.5252/geodiversitas2019v41a8 +2d9cc532-dbf4-46f5-b134-4d8fa2f93663 +1638-9395 +3700008 +urn:lsid:zoobank.org:pub:A2760279-BE3E-4730-9688-9AB777F3A357 Genus - + Melanopsis Férussac, 1807 diff --git a/data/65/31/62/6531624615545277FE8FFA65FBD4FCC1.xml b/data/65/31/62/6531624615545277FE8FFA65FBD4FCC1.xml index 841bcb099ad..c2e7ab07de5 100644 --- a/data/65/31/62/6531624615545277FE8FFA65FBD4FCC1.xml +++ b/data/65/31/62/6531624615545277FE8FFA65FBD4FCC1.xml @@ -1,54 +1,55 @@ - - - -Early Miocene Gastropods from the Felli Section (Proto-Mediterranean Sea NW Greece) + + + +Early Miocene Gastropods from the Felli Section (Proto-Mediterranean Sea NW Greece) - - -Author + + +Author -Thivaiou, Danae +Thivaiou, Danae - - -Author + + +Author -Harzhauser, Mathias +Harzhauser, Mathias - - -Author + + +Author -Koskeridou, Efterpi +Koskeridou, Efterpi -text - - -Geodiversitas +text + + +Geodiversitas - -2019 - -2019-04-15 + +2019 + +2019-04-15 - -41 + +41 - -8 + +8 - -323 -366 + +323 +366 -journal article -10.5252/geodiversitas2019v41a8 -2d9cc532-dbf4-46f5-b134-4d8fa2f93663 -1638-9395 -3700008 -urn:lsid:zoobank.org:pub:A2760279-BE3E-4730-9688-9AB777F3A357 +journal article +23659 +10.5252/geodiversitas2019v41a8 +2d9cc532-dbf4-46f5-b134-4d8fa2f93663 +1638-9395 +3700008 +urn:lsid:zoobank.org:pub:A2760279-BE3E-4730-9688-9AB777F3A357 @@ -245,7 +246,7 @@ Lozouet . The Paratethyan subspecies -Alaba costellata +Alaba costellata anomala (Eichwald, 1850), as illustrated in diff --git a/data/65/31/62/6531624615555276FE81FB45FAB6FAFC.xml b/data/65/31/62/6531624615555276FE81FB45FAB6FAFC.xml index 1f386b1e3ee..554c20b84cb 100644 --- a/data/65/31/62/6531624615555276FE81FB45FAB6FAFC.xml +++ b/data/65/31/62/6531624615555276FE81FB45FAB6FAFC.xml @@ -1,60 +1,61 @@ - - - -Early Miocene Gastropods from the Felli Section (Proto-Mediterranean Sea NW Greece) + + + +Early Miocene Gastropods from the Felli Section (Proto-Mediterranean Sea NW Greece) - - -Author + + +Author -Thivaiou, Danae +Thivaiou, Danae - - -Author + + +Author -Harzhauser, Mathias +Harzhauser, Mathias - - -Author + + +Author -Koskeridou, Efterpi +Koskeridou, Efterpi -text - - -Geodiversitas +text + + +Geodiversitas - -2019 - -2019-04-15 + +2019 + +2019-04-15 - -41 + +41 - -8 + +8 - -323 -366 + +323 +366 -journal article -10.5252/geodiversitas2019v41a8 -2d9cc532-dbf4-46f5-b134-4d8fa2f93663 -1638-9395 -3700008 -urn:lsid:zoobank.org:pub:A2760279-BE3E-4730-9688-9AB777F3A357 +journal article +23659 +10.5252/geodiversitas2019v41a8 +2d9cc532-dbf4-46f5-b134-4d8fa2f93663 +1638-9395 +3700008 +urn:lsid:zoobank.org:pub:A2760279-BE3E-4730-9688-9AB777F3A357 - + Bittium larrieyense Vignal, 1911 @@ -70,7 +71,7 @@ A1-A3) - + Bittium vignali var. larrieyensis @@ -83,7 +84,7 @@ var. - + Bittium vignali – Vignal 1911: 158 @@ -99,7 +100,7 @@ var. - + Bittium reticulatum – Vignal 1911: 157 @@ -111,7 +112,7 @@ var. -Bittium +Bittium asperulatum – @@ -123,7 +124,7 @@ asperulatum - + Bittium larrieyense – @@ -236,18 +237,18 @@ The high variability of this species led to the description of several species a and Cossmann & Peyrot (1922) , such as - + B. vignali Dollfus, 1909 , -Bittium +Bittium subclathratum (d’Orbigny, 1852) and -Bittium +Bittium asperulum Cossmann & Peyrot, 1922 @@ -259,7 +260,7 @@ Lozouet these taxa seem to represent only morphotypes of -B. larrieyense +B. larrieyense . diff --git a/data/65/31/62/6531624615555276FEA0FB86FE9EFB08.xml b/data/65/31/62/6531624615555276FEA0FB86FE9EFB08.xml index d06095f3ba4..46932b102e7 100644 --- a/data/65/31/62/6531624615555276FEA0FB86FE9EFB08.xml +++ b/data/65/31/62/6531624615555276FEA0FB86FE9EFB08.xml @@ -1,61 +1,62 @@ - - - -Early Miocene Gastropods from the Felli Section (Proto-Mediterranean Sea NW Greece) + + + +Early Miocene Gastropods from the Felli Section (Proto-Mediterranean Sea NW Greece) - - -Author + + +Author -Thivaiou, Danae +Thivaiou, Danae - - -Author + + +Author -Harzhauser, Mathias +Harzhauser, Mathias - - -Author + + +Author -Koskeridou, Efterpi +Koskeridou, Efterpi -text - - -Geodiversitas +text + + +Geodiversitas - -2019 - -2019-04-15 + +2019 + +2019-04-15 - -41 + +41 - -8 + +8 - -323 -366 + +323 +366 -journal article -10.5252/geodiversitas2019v41a8 -2d9cc532-dbf4-46f5-b134-4d8fa2f93663 -1638-9395 -3700008 -urn:lsid:zoobank.org:pub:A2760279-BE3E-4730-9688-9AB777F3A357 +journal article +23659 +10.5252/geodiversitas2019v41a8 +2d9cc532-dbf4-46f5-b134-4d8fa2f93663 +1638-9395 +3700008 +urn:lsid:zoobank.org:pub:A2760279-BE3E-4730-9688-9AB777F3A357 Genus - + Bittium Gray, 1847 @@ -73,7 +74,7 @@ SPECIES da Costa , 1778 (= - + Bittium reticulatum (da diff --git a/data/65/31/62/6531624615555277FC02FA65FDDDFAE3.xml b/data/65/31/62/6531624615555277FC02FA65FDDDFAE3.xml index 21470b28b01..027ac4e8d8f 100644 --- a/data/65/31/62/6531624615555277FC02FA65FDDDFAE3.xml +++ b/data/65/31/62/6531624615555277FC02FA65FDDDFAE3.xml @@ -1,54 +1,55 @@ - - - -Early Miocene Gastropods from the Felli Section (Proto-Mediterranean Sea NW Greece) + + + +Early Miocene Gastropods from the Felli Section (Proto-Mediterranean Sea NW Greece) - - -Author + + +Author -Thivaiou, Danae +Thivaiou, Danae - - -Author + + +Author -Harzhauser, Mathias +Harzhauser, Mathias - - -Author + + +Author -Koskeridou, Efterpi +Koskeridou, Efterpi -text - - -Geodiversitas +text + + +Geodiversitas - -2019 - -2019-04-15 + +2019 + +2019-04-15 - -41 + +41 - -8 + +8 - -323 -366 + +323 +366 -journal article -10.5252/geodiversitas2019v41a8 -2d9cc532-dbf4-46f5-b134-4d8fa2f93663 -1638-9395 -3700008 -urn:lsid:zoobank.org:pub:A2760279-BE3E-4730-9688-9AB777F3A357 +journal article +23659 +10.5252/geodiversitas2019v41a8 +2d9cc532-dbf4-46f5-b134-4d8fa2f93663 +1638-9395 +3700008 +urn:lsid:zoobank.org:pub:A2760279-BE3E-4730-9688-9AB777F3A357 @@ -68,7 +69,7 @@ Cossmann, 1889 TYPE SPECIES . — - + Cerithium plicatum Bruguière, 1792 @@ -93,7 +94,7 @@ B1-B3) - + Cerithium plicatum Bruguière, 1792: 488 @@ -156,7 +157,7 @@ Cluzaud - + Cerithium ( Granulolabium diff --git a/data/65/31/62/6531624615565276FC0AF963FD6BFBA2.xml b/data/65/31/62/6531624615565276FC0AF963FD6BFBA2.xml index d0e3dc99415..72df9f9da17 100644 --- a/data/65/31/62/6531624615565276FC0AF963FD6BFBA2.xml +++ b/data/65/31/62/6531624615565276FC0AF963FD6BFBA2.xml @@ -1,54 +1,55 @@ - - - -Early Miocene Gastropods from the Felli Section (Proto-Mediterranean Sea NW Greece) + + + +Early Miocene Gastropods from the Felli Section (Proto-Mediterranean Sea NW Greece) - - -Author + + +Author -Thivaiou, Danae +Thivaiou, Danae - - -Author + + +Author -Harzhauser, Mathias +Harzhauser, Mathias - - -Author + + +Author -Koskeridou, Efterpi +Koskeridou, Efterpi -text - - -Geodiversitas +text + + +Geodiversitas - -2019 - -2019-04-15 + +2019 + +2019-04-15 - -41 + +41 - -8 + +8 - -323 -366 + +323 +366 -journal article -10.5252/geodiversitas2019v41a8 -2d9cc532-dbf4-46f5-b134-4d8fa2f93663 -1638-9395 -3700008 -urn:lsid:zoobank.org:pub:A2760279-BE3E-4730-9688-9AB777F3A357 +journal article +23659 +10.5252/geodiversitas2019v41a8 +2d9cc532-dbf4-46f5-b134-4d8fa2f93663 +1638-9395 +3700008 +urn:lsid:zoobank.org:pub:A2760279-BE3E-4730-9688-9AB777F3A357 @@ -70,7 +71,7 @@ E1, E2) - + Cerithium fallax Grateloup, 1832 diff --git a/data/65/31/62/65316246157C525FFEB6FE09FED9FABC.xml b/data/65/31/62/65316246157C525FFEB6FE09FED9FABC.xml index 011519673ff..25cf891fa58 100644 --- a/data/65/31/62/65316246157C525FFEB6FE09FED9FABC.xml +++ b/data/65/31/62/65316246157C525FFEB6FE09FED9FABC.xml @@ -1,61 +1,62 @@ - - - -Early Miocene Gastropods from the Felli Section (Proto-Mediterranean Sea NW Greece) + + + +Early Miocene Gastropods from the Felli Section (Proto-Mediterranean Sea NW Greece) - - -Author + + +Author -Thivaiou, Danae +Thivaiou, Danae - - -Author + + +Author -Harzhauser, Mathias +Harzhauser, Mathias - - -Author + + +Author -Koskeridou, Efterpi +Koskeridou, Efterpi -text - - -Geodiversitas +text + + +Geodiversitas - -2019 - -2019-04-15 + +2019 + +2019-04-15 - -41 + +41 - -8 + +8 - -323 -366 + +323 +366 -journal article -10.5252/geodiversitas2019v41a8 -2d9cc532-dbf4-46f5-b134-4d8fa2f93663 -1638-9395 -3700008 -urn:lsid:zoobank.org:pub:A2760279-BE3E-4730-9688-9AB777F3A357 +journal article +23659 +10.5252/geodiversitas2019v41a8 +2d9cc532-dbf4-46f5-b134-4d8fa2f93663 +1638-9395 +3700008 +urn:lsid:zoobank.org:pub:A2760279-BE3E-4730-9688-9AB777F3A357 Genus - + Turbonilla Risso, 1826 @@ -70,12 +71,12 @@ SPECIES . — - + Turbonilla costulata Risso, 1826 (= - + Turbonilla lactea (Linnaeus, 1758)) @@ -88,7 +89,7 @@ Risso, 1826 REMARK The genus - + Turbonilla is characterized by species with elongated and ornate shells, and @@ -104,7 +105,7 @@ Schander relationships within some major gastropod clades have still not been studied. The Pyramidellidae is one such group, comprising more than 6000 named species in more than 350 genera. We sequenced part of the mitochondrial 16S gene from 32 species in an attempt to clarify pyramidellid phylogeny and employed a successive alignment approach that allowed us to maximize the phylogenetic signal of the data. Neighbour-joining, maximum parsimony and likelihood analyses recovered two distinct clades. One clade consisted of Noemiamea which nested within -Odostomia +Odostomia (sensu stricto, the subfamily Turbonillinae Bronn, 1849 is polyphyletic. In the work by @@ -118,12 +119,12 @@ d’Orbigny 1840 and -Turbonilla +Turbonilla s.s. Risso, 1826. Herein, we use -Turbonilla +Turbonilla s.l. since the preservation of the shells does not allow a certain generic attribution or identification to the species level. diff --git a/data/97/37/87/9737878FFF8EFFD4FCF99C3878C0FAB5.xml b/data/97/37/87/9737878FFF8EFFD4FCF99C3878C0FAB5.xml new file mode 100644 index 00000000000..54134c9bc50 --- /dev/null +++ b/data/97/37/87/9737878FFF8EFFD4FCF99C3878C0FAB5.xml @@ -0,0 +1,333 @@ + + + +Contributions To The Study Of The Early Jurassic Petrified Forest Of Holbav And Cristian Areas (Brașov Region, South Carpathians, Romania). 1 Part + + + +Author + +Iamandei, Stănilă +Geological Institute of Romania, 1 st, Caransebeş Street, 012271 - Bucharest, Romania. * Corresponding author: iamandei @ gmail. com +iamandei@gmail.com + + + +Author + +Iamandei, Eugenia +Geological Institute of Romania, 1 st, Caransebeş Street, 012271 - Bucharest, Romania. * Corresponding author: iamandei @ gmail. com +iamandei@gmail.com + + + +Author + +Grădinaru, Eugen +University of Bucharest, Faculty of Geology and Geophysics, Department of Geology, 1 st, Bălcescu Nicolae Blvd., 010041, Romania. egradinaru @ gmail. com +egradinaru@gmail.com + +text + + +Acta Palaeontologica Romaniae + + +2018 + +2018-10-03 + + +14 + + +2 + + +3 +34 + + + +journal article +1842-371x + + + + + + +Brachyoxylon cristianicum + +sp. nov. + + + + + +Fig. 7 +a-i; +Fig. 8 +a-i. + + + + +The studied material + + +The studied material is represented by 8 pieces of silicified wood, four of them found in the Cristian area, on the Fabricii valley, and four in the Holbav area, on the Maiului brook, in the Lower Jurassic continental deposits with pyroclastic character considered of Sinemurian- Pliensbachian age, most probably Pliensbachian. All the studied samples are trunk or thick-branch fragments, having decimetric size, dark to black color and, by magnifying glass or even by naked eye, regular fibrous structure without vessels can be seen, clearly suggesting a conifer wood. The specimens having field-numbers: 1015, 1016Cr, 1018Cr, 1019Cr, 1020Cr, 1027, 1042, 1043 belong to "Grădinaru Collection", and are deposited now in the collections of the Geological Institute of +Romania +( +G +. +I +. +R +. Collections), under the inventory numbers: 27636 –27643 respectively, at the National Geological Museum, in +Bucharest +. + + +Microscopic description + +All the eight studied specimens present s e c o n d a r y w o o d with tracheidoxylic structure with quite distinct growth-rings boundary marked by the late wood which has smaller tracheids than the early wood. The structure is devoid of any normal or traumatic resin canals. + + +T +r a c h e i d s - in cross section viewed are polygonal with slightly rounded corners, sometimes determining intercellular spaces (specimens 1020, 1027), unequal in size, with quadrangular to rounded large lumina with radial/tangential diameters of 20-42(50-60)/20-35-(45-65) μm (smaller in the late wood), and with relatively not too thick walls: (4)6-9 μm the double wall in the early and in the transitional wood, up to 9-13 μm the double wall in the late wood. The interradial bundles have 1-10(12) radial regular rows of tracheids and density is 992- 1444(1518) tracheids per mm2. Tangentially seen the tracheids are usually unpitted, or rarely pitted (in specimen 1019) with small round pits (d=8-12 μm) with small apertures (d=4-5 μm), in a single row arranged, slightly irregular, locally as two opposite pits. The radial pitting is of mixed +type +, with almost abietinean pits, arranged either in a single vertical row as round pits, spaced, or contiguous separated by a horizontal line, with round or slightly elliptic apertures, or biseriate, round, alternate or opposite, contiguous on short rows often continued by uniseriate portions, not occupying all the length of the wall. In fact, generally, the pitted areas don't cover integrally the tracheidal wall. The pits have round borders of 18-22 often flattened when contiguous (d/D=0.65-0.88), and round or tilted to lying elliptic apertures of 7.5-10/2-3 μm (in specimen 1019). None crassulae or helical thickenings have been seen, but sometimes a brown content is present + +. + + + +Fig. 7 + +Brachyoxylon cristianicum + +sp. nov. +- holotype - inventory no. 27639 (field no. 1019cr). +a-c +Cross-section: distinct growthring boundary, thick-walled tracheids, polygonal with rounded corners, and linear rays. +d-f +Tangential section: unpitted tracheids, parenchyma with pits and crystals; uniseriate rays. +g-i +Radial section: uniseriate radial piting on tracheids of mixed type, cross fields with 1-2 rows of oculipores. + + + + +Fig. 8 + +Brachyoxylon cristianicum + +sp. nov. +- paratype - inventory no. 27640 (field no. 1020cr). +a-c +Cross-section: distinct growth-ring boundary, polygonal tracheids with rounded corners and thick walls; linear rays. +d-f +Tangential section: unpitted tracheids, parenchyma with pits and uniseriate rays. +g-i +Radial section: radial piting on tracheids of mixed type, uniseriate and biseriate, cross fields with 1-2 rows of oculipores. + + + +A +x i a l p a r e n c h y m a - in cross-section view is present, few, dispersed, often difficult to identify amongst the tracheids. It has relatively thin vertical walls relatively similar to those of the tracheids and sometimes with simple pits, irregularly arranged on 1-2 rows. The horizontal (terminal) walls are thin and smooth or slightly nodular and, inside the cells, resin content or plugs or granules, and sometimes small polygonal crystals are present (specimens 1015, 1019). + + + +M +e d u l l a r y r a y s - in cross section appear usually uniseriate, rectilinear, and with smooth horizontal cellular walls. In tangential view the rays have 1-20 (sometimes up to 25) cells in height, i.e. 30-570(650) μm high. The taller uniseriate rays have biseriations, sometimes giving aspect of fusiform rays (specimens 1015, 1016). The ray cells are polygonal rounded to oval sometimes having dark content and relatively thin walls. Ray density is 5-11 rays per horizontal tangential millimeter. Radially the rays are homocellular, cells all procumbent of 20-30 μm tall, moderately thin walled, of 4-5(7) μm the double wall. Within the marginal rows the cells are taller, of 25- 35(40) μm, and have corrugated outer wall. The crossfields of araucarioid +type +have 1-6 oculipores, hexagonal or slightly rounded to oval, of cupressoid +type +, tending to podocarpoid, with 15-19/8-12 μm in diameters, having circular or short elliptic tilted apertures of 10-14/5-7 μm. The pits arrangement is in 1-2 rows in the ray body fields, in the marginal fields on two horizontal rows, always alternate to slightly irregular when on two rows + +. + + +Affinities and discussions + + +After the microscopic study of each sample and the synthetic evaluation of their generic characters, a number of 8 samples of fossil wood were grouped all of them having tracheidoxylic structure, uniseriate rays, radial pitting of mixed +type +on the tracheids and araucarioid cross-fields, suggesting a + +Brachyoxylon + +type +of wood slightly differebt of the above described form (see +Table 1 +). + + +The discussion on the status of the genus + +Brachyoxylon +Hollick et Jeffrey + +, and of the species described under it along the time is presented in detail above. Even if the +type +species ( + +Brachyoxylon notabile +Hollick et Jeffrey, 1909 + +) has a very elliptic diagnosis, referring only to "a tracheidoxyl devoid of normal secretory ducts, with mixed radial pitting, araucarioid cross-fields and other ray walls integer" (see Philippe, 1993), it is interesting that traumatic canals were described, considered as a result of injury or freezing ( +Taylor & Taylor, 1993 +, p. 689; Philippe, 1995). Anyway, the specimens described here are devoid of any kind of canal. + + +In our studied specimens, apart from the known characters of the genus, there are some specific xylotomic details regarding the size of tracheids or their behavior insi- de the growth ring, their pitting +type +, aspect and size of the pits on the tracheids and in the cross fields. The accurate description of these very specific features of the studied material can be useful for the comparison with the already published and valid species (see +Table 1 +). + + +Anyway, it seems that the presence or the absence of the axial parenchyma and of the crassulae, and also the ray heights and the pits' number in the cross-fields, are important to separate the species of + +Brachyoxylon + +(Philippe, 1993, 1995). + + +- Two forms of + +Brachyoxylon + +preserving primary structure and pith were described from the Lower Cretaceous in southeastern of +Romania +as + +B.avramii + +and + +B. dobrogiacum +(Iamandei & Iamandei, 2005) + +as having a tracheidoxylic structure with few parenchyma and uniseriate low rays, with mixed radial pitting and araucarioid cross-fields (sensu Philippe, 1993), bearing cupressoid to podocarpoid pits in an araucarioid arrangement, but are slightly different of the here studied material which has high rays with biseriate stories, even with aspect of biseriate fusiform rays. + + +- Also, +Vera & Césari (2012) +have described an interesting material represented by +five specimens +of Aptian fossil woods from +Argentina +and identified as + +Brachyoxylon +sp. + +cf. + +Brachyoxylon boureaui +Serra, 1966 + +having radial pitting of a mixed +type +, predominantly uniseriate, with circular to polygonal bordered pits, sometimes biseriate and triseriate, even if less common, and numerous pits in the cross-fields (8 up to 26 small circular pits arranged in 2-4 rows, with slit-like pit apertures, obliquely oriented), details which are very different of our specimens. + + +- The Jurassic +new species +of + +Brachyoxylon currumilii + +described by Bodnar +et al +. (2013) from +Argentina +, has also some details which differ of our material. But in that paper there is a very well documented discussion on the status of + +Brachyoxylon + +genus and its already described species, and a comparative table of the valid species of + +Brachyoxylon + +in which we added, for comparison, the essential xylotomical characters of our studied material ( +Table 1 +). + + +- Interesting for comparison seems to us the more recently reidentification of Philippe +et al. +(2018) from "Lignier collection" of a sample initially identified as +Cedroxylon blevilense +by Lignier, as + +Brachyoxylon blevillense +(Lignier) Philippe +et al +., 2018 + +based on the mixed +type +of radial pitting and the araucarioid cross-fields. Also the identification of the “Échantillon n°150” from the same collection, which showed typical araucarioid cross-fields with up to six crowded oculipores and traumatic(?) resiniferous axial parenchyma is similar to + +Brachyoxylon liebermannii +Philippe, 1995 + +, a species previously described from the Liassic of northeastern +France +. + + +But, considering the xylotomic similarities and dissimilarities of our studied material with the already published species from this comparative table ( +Table 1 +) and the comparison with the original description of the species, and also, the discussions from above, it can be observed that our material is special. + +Thus, it presents a secondary wood structure without resin canals, with mixed radial pitting, uniseriate spaced or contiguous, or biseriate, alternate or opposite, contiguous, with round to elliptic apertures, with axial parenchyma, with uniseriate rays or even biseriate, relatively high, and cross fields with cupressoid oculipores in an araucarioid arrangement. + +These xylotomical details are slightly different of the other species of + +Brachyoxylon + +described in this paper and, based on this diference well exprimed in the +Table 1 +from above, we considered we have described here a new species that we named + +Brachyoxylon cristianicum + +sp. nov. +, after the name of the region from where it was fo- und (Romanian spelling for Christian is Cristian). From the studied material a +holotype +was designated the specimen with field number +1019 in +"Grădinaru Collection", (inventory number 27639), and a +paratype +the specimen with field number +1020 in +"Grădinaru Collection (inventory number 27640), from a population of +8 specimens +of fossil wood with similar to almost identical xylotomic, all material now deposited in GIR Collection, in the National Geological Museum, +Bucharest +, as we specified above. + + + + +Diagnosis of the new species + +Brachyoxylon cristianicum + +sp. nov. +: + + +Tracheidoxyl with distinct growth rings, devoid of any canal. Tangentially the tracheids are usually unpitted, rarely with small pits, uniseriate. Radial pitting of mixed +type +, of pits abietinean but with araucarian arrangement, uniseriate, spaced or contiguous, with round or slightly elliptic apertures, or biseriate, alternate or opposite, contiguous and flattened, in short rows often continued by uniseriate portions, not occupying all the length of the wall. Axial parenchyma present, dispersed, in longitudinal view presenting thin and smooth or slightly nodular horizontal walls and resin content or even crystals. Rays uniseriate, relatively tall, with biseriations, sometimes with fusiform aspect, homocellular, having typical araucarioid cross-fields with 1-6 oculipores alternate to slightly irregular on 1-2 rows, hexagonal ronded to oval, of cupressoid +type +tending to podocarpoid, with round or short elliptic tilted apertures. + + + + \ No newline at end of file diff --git a/data/A3/34/87/A33487E8FFAAA273FCD9F9C2FA898953.xml b/data/A3/34/87/A33487E8FFAAA273FCD9F9C2FA898953.xml new file mode 100644 index 00000000000..54161a8e6a5 --- /dev/null +++ b/data/A3/34/87/A33487E8FFAAA273FCD9F9C2FA898953.xml @@ -0,0 +1,78 @@ + + + +Dasycladalean Fossil Green Algae From The Maastrichtian-Paleocene Of Balkh Province (N Afghanistan) + + + +Author + +Barattolo, Filippo +Dipartimento di Scienze della Terra dell’Ambiente e delle Risorse - Università di Napoli Federico II - Largo S. Marcellino, + + + +Author + +Abad, Morteza Taherpour Khalil +Young Researchers and Elite Club, Mashhad Branch, Islamic Azad University, Mashhad, Iran, mortezataherpoor @ yahoo. com +mortezataherpoor@yahoo.com + + + +Author + +Introduction, Mehdi Ashrafi + +text + + +Acta Palaeontologica Romaniae + + +2014 + +2014-11-12 + + +10 + + +1 - 2 + + +1 +2 + + + +journal article +10.5281/zenodo.13190161 +1842-371x +13190161 + + + + + + +Orioporella malaviae +Pia 1936 + + + + + + +Fig. 10 d, g + + +This taxon is well recorded in the Paleocene, probably occurring in the SB1 (upper part) - SB3 interval ( +Barattolo, 1998 +). The alga is found as isolated discs. The oblique section of +Fig. 10 d +clearly shows the perforated upper and lower walls of the fertile disc, whereas the partitions between gametangia are imperforate. + + + + \ No newline at end of file diff --git a/data/A3/34/87/A33487E8FFAAA273FF7FFBF3FE8E8BDB.xml b/data/A3/34/87/A33487E8FFAAA273FF7FFBF3FE8E8BDB.xml new file mode 100644 index 00000000000..57ec086fbe6 --- /dev/null +++ b/data/A3/34/87/A33487E8FFAAA273FF7FFBF3FE8E8BDB.xml @@ -0,0 +1,90 @@ + + + +Dasycladalean Fossil Green Algae From The Maastrichtian-Paleocene Of Balkh Province (N Afghanistan) + + + +Author + +Barattolo, Filippo +Dipartimento di Scienze della Terra dell’Ambiente e delle Risorse - Università di Napoli Federico II - Largo S. Marcellino, + + + +Author + +Abad, Morteza Taherpour Khalil +Young Researchers and Elite Club, Mashhad Branch, Islamic Azad University, Mashhad, Iran, mortezataherpoor @ yahoo. com +mortezataherpoor@yahoo.com + + + +Author + +Introduction, Mehdi Ashrafi + +text + + +Acta Palaeontologica Romaniae + + +2014 + +2014-11-12 + + +10 + + +1 - 2 + + +1 +2 + + + +journal article +10.5281/zenodo.13190161 +1842-371x +13190161 + + + + + + +Jodotella +cf +sloveniaensis +Deloffre & Radoičić 1979 + + + + + + +Fig. 5 +s-t + + +A cylindrical alga with strong phloiophorous primary laterals occurs in the Paleocene (sample Sh 6 = BA. 4258). Large gametangia are set aside to primary laterals. The general shape of the alga is similar to + +Jodotella sloveniaensis +Deloffre & Radoičić. However + +, the size appears to be larger: D = +0.8 - 0.9 mm +vs. +0.4 - 0.65 mm +, d = +0.28 – 0.30 mm +vs. +0.2 – 0.275 mm +. Biometrical difference, the poor state of preservation and the paucity of material available do not allow confirmation of the attribution, therefore the taxon is given in open nomenclature. + + + + \ No newline at end of file diff --git a/data/B1/49/43/B149432292418E64FEF4C7879AA1FED0.xml b/data/B1/49/43/B149432292418E64FEF4C7879AA1FED0.xml new file mode 100644 index 00000000000..8c6e3881827 --- /dev/null +++ b/data/B1/49/43/B149432292418E64FEF4C7879AA1FED0.xml @@ -0,0 +1,90 @@ + + + +Taxonomic Record Of The Oligocene Benthic Foraminifera From The Vima Formation (Transylvanian Basin, Romania) + + + +Author + +Székely, Szabolcs-Flavius +BabeȘ-Bolyai University, Department of Geology, Str. Kogălniceanu 1, 400084, Cluj Napoca, Romania, szekelyflavius @ gmail. com, sorin. filipescu @ ubbcluj. ro +szekelyflavius@gmail.com + + + +Author + +Introduction, Sorin Filipescu + +text + + +Acta Palaeontologica Romaniae + + +2015 + +2015-08-26 + + +11 + + +1 + + +25 +62 + + + +journal article +10.5281/zenodo.13190119 +1842-371x +13190119 + + + + + + +Cycloforina ludwigi +( +Reuss, 1866 +) + + + + + + +Figs. 7.3, 7.5 +a-c + + + + + + + +Quinqueloculina ludwigi +Reuss, 1866 +, p. 126 + + +, pl. 1, fig. 12. + + + + +Cycloforina ludwigi +(Reuss) + +- Łuczkowska, 1972, p. 365. +Stratigraphical distribution in samples: +Rupelian- Chattian. + + + + \ No newline at end of file diff --git a/data/B1/49/43/B149432292458E60FEC1C2169AA0FA61.xml b/data/B1/49/43/B149432292458E60FEC1C2169AA0FA61.xml new file mode 100644 index 00000000000..8830107ccfa --- /dev/null +++ b/data/B1/49/43/B149432292458E60FEC1C2169AA0FA61.xml @@ -0,0 +1,94 @@ + + + +Taxonomic Record Of The Oligocene Benthic Foraminifera From The Vima Formation (Transylvanian Basin, Romania) + + + +Author + +Székely, Szabolcs-Flavius +BabeȘ-Bolyai University, Department of Geology, Str. Kogălniceanu 1, 400084, Cluj Napoca, Romania, szekelyflavius @ gmail. com, sorin. filipescu @ ubbcluj. ro +szekelyflavius@gmail.com + + + +Author + +Introduction, Sorin Filipescu + +text + + +Acta Palaeontologica Romaniae + + +2015 + +2015-08-26 + + +11 + + +1 + + +25 +62 + + + +journal article +10.5281/zenodo.13190119 +1842-371x +13190119 + + + + + + +Popovia plana +( +Bykova, 1939 +) + + + + + + +Fig. 5.9 +a-c + + + + + + + +Alveolophragmium planum +Bykova, 1939 +, p. 20 + + +, pl. 1, fig. 10, textfig. 1. (fide Ellis & Messina). + + + + +Popovia plana +(Bykova) + +- Suleymanov, 1965, p. 48. + + + + +Stratigraphical distribution in samples: +Rupelian- Chattian. + + + + \ No newline at end of file diff --git a/data/B1/49/43/B149432292478E62FC9EC1669F38F8B3.xml b/data/B1/49/43/B149432292478E62FC9EC1669F38F8B3.xml new file mode 100644 index 00000000000..673dde3131f --- /dev/null +++ b/data/B1/49/43/B149432292478E62FC9EC1669F38F8B3.xml @@ -0,0 +1,77 @@ + + + +Taxonomic Record Of The Oligocene Benthic Foraminifera From The Vima Formation (Transylvanian Basin, Romania) + + + +Author + +Székely, Szabolcs-Flavius +BabeȘ-Bolyai University, Department of Geology, Str. Kogălniceanu 1, 400084, Cluj Napoca, Romania, szekelyflavius @ gmail. com, sorin. filipescu @ ubbcluj. ro +szekelyflavius@gmail.com + + + +Author + +Introduction, Sorin Filipescu + +text + + +Acta Palaeontologica Romaniae + + +2015 + +2015-08-26 + + +11 + + +1 + + +25 +62 + + + +journal article +10.5281/zenodo.13190119 +1842-371x +13190119 + + + + + + +Spiroloculina canaliculata +d’Orbigny, 1846 + + + + + + +Fig. 7.2 + + + + + +Spiroloculina canaliculata +d’Orbigny, 1846, p. 269 + +, pl. 16, figs. 10-12. + + +Stratigraphical distribution in samples: +Rupelian. + + + + \ No newline at end of file diff --git a/data/B1/49/43/B149432292478E62FF16C43B9AA0FC6F.xml b/data/B1/49/43/B149432292478E62FF16C43B9AA0FC6F.xml new file mode 100644 index 00000000000..f517fa4b94f --- /dev/null +++ b/data/B1/49/43/B149432292478E62FF16C43B9AA0FC6F.xml @@ -0,0 +1,82 @@ + + + +Taxonomic Record Of The Oligocene Benthic Foraminifera From The Vima Formation (Transylvanian Basin, Romania) + + + +Author + +Székely, Szabolcs-Flavius +BabeȘ-Bolyai University, Department of Geology, Str. Kogălniceanu 1, 400084, Cluj Napoca, Romania, szekelyflavius @ gmail. com, sorin. filipescu @ ubbcluj. ro +szekelyflavius@gmail.com + + + +Author + +Introduction, Sorin Filipescu + +text + + +Acta Palaeontologica Romaniae + + +2015 + +2015-08-26 + + +11 + + +1 + + +25 +62 + + + +journal article +10.5281/zenodo.13190119 +1842-371x +13190119 + + + + + + +Karreriella hantkeniana +Cushman, 1936 + + + + + + +Fig. 6.6 + + + + + + + +Karreriella hantkeniana +Cushman, 1936 +, p. 36 + + +, pl. 5, fig. 19. + + + +Stratigraphical distribution in samples: +Rupelian- Chattian. + + + + \ No newline at end of file diff --git a/data/B1/49/43/B149432292498E6CFC27C64F99CAFE55.xml b/data/B1/49/43/B149432292498E6CFC27C64F99CAFE55.xml new file mode 100644 index 00000000000..1fe55b097e5 --- /dev/null +++ b/data/B1/49/43/B149432292498E6CFC27C64F99CAFE55.xml @@ -0,0 +1,80 @@ + + + +Taxonomic Record Of The Oligocene Benthic Foraminifera From The Vima Formation (Transylvanian Basin, Romania) + + + +Author + +Székely, Szabolcs-Flavius +BabeȘ-Bolyai University, Department of Geology, Str. Kogălniceanu 1, 400084, Cluj Napoca, Romania, szekelyflavius @ gmail. com, sorin. filipescu @ ubbcluj. ro +szekelyflavius@gmail.com + + + +Author + +Introduction, Sorin Filipescu + +text + + +Acta Palaeontologica Romaniae + + +2015 + +2015-08-26 + + +11 + + +1 + + +25 +62 + + + +journal article +10.5281/zenodo.13190119 +1842-371x +13190119 + + + + + + +Reophax pilulifer +Brady, 1884 + + + + + + +Fig. 4.2 + + + + + + + +Reophax pilulifer +Brady, 1884 +, p. 292 + + +, pl. 30, figs. 18-20. +Stratigraphical distribution in samples: +Rupelian- Chattian. + + + + + \ No newline at end of file diff --git a/data/B1/49/43/B149432292498E6CFC75C51799CAFD03.xml b/data/B1/49/43/B149432292498E6CFC75C51799CAFD03.xml new file mode 100644 index 00000000000..d3cef4f2769 --- /dev/null +++ b/data/B1/49/43/B149432292498E6CFC75C51799CAFD03.xml @@ -0,0 +1,84 @@ + + + +Taxonomic Record Of The Oligocene Benthic Foraminifera From The Vima Formation (Transylvanian Basin, Romania) + + + +Author + +Székely, Szabolcs-Flavius +BabeȘ-Bolyai University, Department of Geology, Str. Kogălniceanu 1, 400084, Cluj Napoca, Romania, szekelyflavius @ gmail. com, sorin. filipescu @ ubbcluj. ro +szekelyflavius@gmail.com + + + +Author + +Introduction, Sorin Filipescu + +text + + +Acta Palaeontologica Romaniae + + +2015 + +2015-08-26 + + +11 + + +1 + + +25 +62 + + + +journal article +10.5281/zenodo.13190119 +1842-371x +13190119 + + + + + + +Reophax scorpiurus +de +Montfort, 1808 + + + + + + +Fig. 4.1 + + + + + + + +Reophax scorpiurus +de +Montfort, 1808 +, p. 331 + + +, fig. p. 330 (fide Ellis & Messina). + + + +Stratigraphical distribution in samples: +Rupelian- Chattian. + + + + \ No newline at end of file diff --git a/data/B1/49/43/B149432292498E6CFCDFC5FE99CAFBAD.xml b/data/B1/49/43/B149432292498E6CFCDFC5FE99CAFBAD.xml new file mode 100644 index 00000000000..6609d59bb7e --- /dev/null +++ b/data/B1/49/43/B149432292498E6CFCDFC5FE99CAFBAD.xml @@ -0,0 +1,98 @@ + + + +Taxonomic Record Of The Oligocene Benthic Foraminifera From The Vima Formation (Transylvanian Basin, Romania) + + + +Author + +Székely, Szabolcs-Flavius +BabeȘ-Bolyai University, Department of Geology, Str. Kogălniceanu 1, 400084, Cluj Napoca, Romania, szekelyflavius @ gmail. com, sorin. filipescu @ ubbcluj. ro +szekelyflavius@gmail.com + + + +Author + +Introduction, Sorin Filipescu + +text + + +Acta Palaeontologica Romaniae + + +2015 + +2015-08-26 + + +11 + + +1 + + +25 +62 + + + +journal article +10.5281/zenodo.13190119 +1842-371x +13190119 + + + + + + +Reophax subfusiformis +Earland, 1933 +emend. +Höglund, + + + +1947 + + + +Fig. 3.15 + + + + + + + +Reophax subfusiformis +Earland, 1933 +, p. 74 + + +, pl. 2, figs. 16-19 (fide Ellis & Messina). + + + + + + +Reophax subfusiformis +Earland emend. +Höglund, 1947 +, p. 82 + + +, pl. 9, figs. 1-4, pl. 26, figs. 1-36, pl. 27, figs. 1-19, textfigs. 43-50. + + + +Stratigraphical distribution in samples: +Rupelian- Chattian. + + + + \ No newline at end of file diff --git a/data/B1/49/43/B149432292498E6CFEE5C049982BF79F.xml b/data/B1/49/43/B149432292498E6CFEE5C049982BF79F.xml new file mode 100644 index 00000000000..7929e19e3a4 --- /dev/null +++ b/data/B1/49/43/B149432292498E6CFEE5C049982BF79F.xml @@ -0,0 +1,80 @@ + + + +Taxonomic Record Of The Oligocene Benthic Foraminifera From The Vima Formation (Transylvanian Basin, Romania) + + + +Author + +Székely, Szabolcs-Flavius +BabeȘ-Bolyai University, Department of Geology, Str. Kogălniceanu 1, 400084, Cluj Napoca, Romania, szekelyflavius @ gmail. com, sorin. filipescu @ ubbcluj. ro +szekelyflavius@gmail.com + + + +Author + +Introduction, Sorin Filipescu + +text + + +Acta Palaeontologica Romaniae + + +2015 + +2015-08-26 + + +11 + + +1 + + +25 +62 + + + +journal article +10.5281/zenodo.13190119 +1842-371x +13190119 + + + + + + +Reophax excentricus +Cushman, 1910 + + + + + + +Fig. 3.16 + +Reophax excentricus +Cushman, 1910 +, p. 92 + +, textfig. 134 (fide Ellis & Messina). +Stratigraphical distribution in samples: +Rupelian- Chattian. + + + + + +Reophax globosus +Sliter, 1968 + + + + + \ No newline at end of file diff --git a/data/B1/49/43/B149432292498E6CFEE8C1259AA0F890.xml b/data/B1/49/43/B149432292498E6CFEE8C1259AA0F890.xml new file mode 100644 index 00000000000..69ccbf745d8 --- /dev/null +++ b/data/B1/49/43/B149432292498E6CFEE8C1259AA0F890.xml @@ -0,0 +1,89 @@ + + + +Taxonomic Record Of The Oligocene Benthic Foraminifera From The Vima Formation (Transylvanian Basin, Romania) + + + +Author + +Székely, Szabolcs-Flavius +BabeȘ-Bolyai University, Department of Geology, Str. Kogălniceanu 1, 400084, Cluj Napoca, Romania, szekelyflavius @ gmail. com, sorin. filipescu @ ubbcluj. ro +szekelyflavius@gmail.com + + + +Author + +Introduction, Sorin Filipescu + +text + + +Acta Palaeontologica Romaniae + + +2015 + +2015-08-26 + + +11 + + +1 + + +25 +62 + + + +journal article +10.5281/zenodo.13190119 +1842-371x +13190119 + + + + + + +Reophax duplex +Grzybowski, 1896 + + + + + + +Fig. 3.12 + + + + + + + +Reophax duplex +Grzybowski, 1896 +, p. 276 + + +, pl. 8, figs. 23- 24 (fide Ellis & Messina). + + + + +Reophax paraduplex +Mjatliuk, 1970, p. 65 + +, pl. 9, figs. 1a- 3, pl. 10, fig. 2. + + +Stratigraphical distribution in samples: +Rupelian- Chattian. + + + + \ No newline at end of file diff --git a/data/B1/49/43/B1494322924B8E6EFC6BC2169F38F8B3.xml b/data/B1/49/43/B1494322924B8E6EFC6BC2169F38F8B3.xml new file mode 100644 index 00000000000..4a5c987759d --- /dev/null +++ b/data/B1/49/43/B1494322924B8E6EFC6BC2169F38F8B3.xml @@ -0,0 +1,147 @@ + + + +Taxonomic Record Of The Oligocene Benthic Foraminifera From The Vima Formation (Transylvanian Basin, Romania) + + + +Author + +Székely, Szabolcs-Flavius +BabeȘ-Bolyai University, Department of Geology, Str. Kogălniceanu 1, 400084, Cluj Napoca, Romania, szekelyflavius @ gmail. com, sorin. filipescu @ ubbcluj. ro +szekelyflavius@gmail.com + + + +Author + +Introduction, Sorin Filipescu + +text + + +Acta Palaeontologica Romaniae + + +2015 + +2015-08-26 + + +11 + + +1 + + +25 +62 + + + +journal article +10.5281/zenodo.13190119 +1842-371x +13190119 + + + + + + +Vulvulina haeringensis +( +Gümbel, 1868 +) + + + + + + +Fig. 5.4 + + + + + + + +Venilina haeringensis +Gümbel, 1868 +, p. 649 + + +, pl. 2, fig. 84. + + + + + +Schizophora haeringensis +(Gümbel) + +- + +Hantken, 1875 +, p. 68 + +, pl. 3, fig. 3. + + + + +Vulvulina haeringensis +(Gümbel) + +- Hagn, 1956, p. 115, pl. 9, figs. 7-8. + + + + +Stratigraphical distribution in samples: +Rupelian- Chattian. + + + + + +Vulvulina spinosa +Cushman, 1927a + + + +Figs. 5.3 +a-b, 5.6 + + + +Vulvulina spinosa +Cushman, 1927a + +, pl. 23, fig. 1. + + +? + +Vulvulina jarvisi +Cushman, 1932, p. 84 + +, pl. 10, fig. 20. + + + +Spiroplectammina spinosa +(Cushman) + +- Parisi & Coccioni, 1988, p. 105, pl. 1, fig. 7. + + + + +Stratigraphical distribution in samples: +Rupelian. + + + + \ No newline at end of file diff --git a/data/B1/49/43/B1494322924B8E6EFF10C1A3989FF8F1.xml b/data/B1/49/43/B1494322924B8E6EFF10C1A3989FF8F1.xml new file mode 100644 index 00000000000..86c8a1138d0 --- /dev/null +++ b/data/B1/49/43/B1494322924B8E6EFF10C1A3989FF8F1.xml @@ -0,0 +1,82 @@ + + + +Taxonomic Record Of The Oligocene Benthic Foraminifera From The Vima Formation (Transylvanian Basin, Romania) + + + +Author + +Székely, Szabolcs-Flavius +BabeȘ-Bolyai University, Department of Geology, Str. Kogălniceanu 1, 400084, Cluj Napoca, Romania, szekelyflavius @ gmail. com, sorin. filipescu @ ubbcluj. ro +szekelyflavius@gmail.com + + + +Author + +Introduction, Sorin Filipescu + +text + + +Acta Palaeontologica Romaniae + + +2015 + +2015-08-26 + + +11 + + +1 + + +25 +62 + + + +journal article +10.5281/zenodo.13190119 +1842-371x +13190119 + + + + + + +Sculptobaculites barri +Beckmann, 1991 + + + + + + +Fig. 4.12 + + + + + + + +Sculptobaculites barri +Beckmann, 1991 +, p. 823 + + +, pl. 1, figs. 6-9. + + + +Stratigraphical distribution in samples: +Rupelian. + + + + \ No newline at end of file diff --git a/data/B1/49/43/B1494322924B8E6EFF4FC7E398A0FE55.xml b/data/B1/49/43/B1494322924B8E6EFF4FC7E398A0FE55.xml new file mode 100644 index 00000000000..67afcae7375 --- /dev/null +++ b/data/B1/49/43/B1494322924B8E6EFF4FC7E398A0FE55.xml @@ -0,0 +1,84 @@ + + + +Taxonomic Record Of The Oligocene Benthic Foraminifera From The Vima Formation (Transylvanian Basin, Romania) + + + +Author + +Székely, Szabolcs-Flavius +BabeȘ-Bolyai University, Department of Geology, Str. Kogălniceanu 1, 400084, Cluj Napoca, Romania, szekelyflavius @ gmail. com, sorin. filipescu @ ubbcluj. ro +szekelyflavius@gmail.com + + + +Author + +Introduction, Sorin Filipescu + +text + + +Acta Palaeontologica Romaniae + + +2015 + +2015-08-26 + + +11 + + +1 + + +25 +62 + + + +journal article +10.5281/zenodo.13190119 +1842-371x +13190119 + + + + + + +Haplophragmoides carinatus +Cushman & Renz, 1941 + + + + + + +Figs. 4.5, 4.6 +a-b, 4.7-4.9 + +Haplophragmoides carinatus +Cushman & Renz, 1941 + +, pl. 1, fig. 1. + + +Stratigraphical distribution in samples: +Rupelian- Chattian. + + + + + +Haplophragmoides suborbicularis +( +Grzybowski, 1896 +) + + + + + \ No newline at end of file diff --git a/data/B1/49/43/B1494322924F8E6AFEE0C2319AA0FA61.xml b/data/B1/49/43/B1494322924F8E6AFEE0C2319AA0FA61.xml new file mode 100644 index 00000000000..a1d34c5a92e --- /dev/null +++ b/data/B1/49/43/B1494322924F8E6AFEE0C2319AA0FA61.xml @@ -0,0 +1,82 @@ + + + +Taxonomic Record Of The Oligocene Benthic Foraminifera From The Vima Formation (Transylvanian Basin, Romania) + + + +Author + +Székely, Szabolcs-Flavius +BabeȘ-Bolyai University, Department of Geology, Str. Kogălniceanu 1, 400084, Cluj Napoca, Romania, szekelyflavius @ gmail. com, sorin. filipescu @ ubbcluj. ro +szekelyflavius@gmail.com + + + +Author + +Introduction, Sorin Filipescu + +text + + +Acta Palaeontologica Romaniae + + +2015 + +2015-08-26 + + +11 + + +1 + + +25 +62 + + + +journal article +10.5281/zenodo.13190119 +1842-371x +13190119 + + + + + + +Hyperammina elongata +Brady, 1878 + + + + + + +Fig. 3.7 + + + + + + + +Hyperammina elongata +Brady, 1878 +, p. 433 + + +, pl. 1, figs. 16, 18-19. + + + +Stratigraphical distribution in samples: +Rupelian- Chattian. + + + + \ No newline at end of file diff --git a/data/B1/49/43/B1494322924F8E6AFEE4C7C09AA0FE74.xml b/data/B1/49/43/B1494322924F8E6AFEE4C7C09AA0FE74.xml new file mode 100644 index 00000000000..0be1c30c22a --- /dev/null +++ b/data/B1/49/43/B1494322924F8E6AFEE4C7C09AA0FE74.xml @@ -0,0 +1,101 @@ + + + +Taxonomic Record Of The Oligocene Benthic Foraminifera From The Vima Formation (Transylvanian Basin, Romania) + + + +Author + +Székely, Szabolcs-Flavius +BabeȘ-Bolyai University, Department of Geology, Str. Kogălniceanu 1, 400084, Cluj Napoca, Romania, szekelyflavius @ gmail. com, sorin. filipescu @ ubbcluj. ro +szekelyflavius@gmail.com + + + +Author + +Introduction, Sorin Filipescu + +text + + +Acta Palaeontologica Romaniae + + +2015 + +2015-08-26 + + +11 + + +1 + + +25 +62 + + + +journal article +10.5281/zenodo.13190119 +1842-371x +13190119 + + + + + + +Bathysiphon taurinensis +Sacco, 1893 + + + + + + +Fig. 3.1 +a-b + + + +Stratigraphical distribution in samples: +Rupelian. + + + + + + +Bathysiphon taurinensis +Sacco, 1893 +, p. 168 + + +, pl. 11, fig. 2 (fide Ellis & Messina). + + + + + +Bathysiphon taurinense +Sacco + +- + +Popescu, 1975 +, p. 32 + +, pl. 1, fig. 2. + + + +Stratigraphical distribution in samples: +Rupelian- Chattian. + + + + \ No newline at end of file diff --git a/data/B1/49/43/B1494322924F8E6AFF52C11B9AA0F90E.xml b/data/B1/49/43/B1494322924F8E6AFF52C11B9AA0F90E.xml new file mode 100644 index 00000000000..fd14c7eb5d0 --- /dev/null +++ b/data/B1/49/43/B1494322924F8E6AFF52C11B9AA0F90E.xml @@ -0,0 +1,83 @@ + + + +Taxonomic Record Of The Oligocene Benthic Foraminifera From The Vima Formation (Transylvanian Basin, Romania) + + + +Author + +Székely, Szabolcs-Flavius +BabeȘ-Bolyai University, Department of Geology, Str. Kogălniceanu 1, 400084, Cluj Napoca, Romania, szekelyflavius @ gmail. com, sorin. filipescu @ ubbcluj. ro +szekelyflavius@gmail.com + + + +Author + +Introduction, Sorin Filipescu + +text + + +Acta Palaeontologica Romaniae + + +2015 + +2015-08-26 + + +11 + + +1 + + +25 +62 + + + +journal article +10.5281/zenodo.13190119 +1842-371x +13190119 + + + + + + +Hyperammina rugosa +Verdenius & van Hinte, 1983 + + + + + + +Fig. 3.6 +a-b + + + + + + + +Hyperammina rugosa +Verdenius & van Hinte, 1983 +, p. 187 + + +, pl. 1, figs. 12-14. + + + +Stratigraphical distribution in samples: +Rupelian- Chattian. + + + + \ No newline at end of file diff --git a/data/B1/49/43/B149432292518E74FC4DC2DE99CAF929.xml b/data/B1/49/43/B149432292518E74FC4DC2DE99CAF929.xml new file mode 100644 index 00000000000..b2ef9df96a5 --- /dev/null +++ b/data/B1/49/43/B149432292518E74FC4DC2DE99CAF929.xml @@ -0,0 +1,94 @@ + + + +Taxonomic Record Of The Oligocene Benthic Foraminifera From The Vima Formation (Transylvanian Basin, Romania) + + + +Author + +Székely, Szabolcs-Flavius +BabeȘ-Bolyai University, Department of Geology, Str. Kogălniceanu 1, 400084, Cluj Napoca, Romania, szekelyflavius @ gmail. com, sorin. filipescu @ ubbcluj. ro +szekelyflavius@gmail.com + + + +Author + +Introduction, Sorin Filipescu + +text + + +Acta Palaeontologica Romaniae + + +2015 + +2015-08-26 + + +11 + + +1 + + +25 +62 + + + +journal article +10.5281/zenodo.13190119 +1842-371x +13190119 + + + + + + +Planulina costata +( +Hantken, 1875 +) + + + + + + +Fig. 16.2 +a-b + + + + + + + +Truncatulina costata +Hantken, 1875 +, p. 63 + + +, pl. 9, fig. 2. + + + + +Planulina costata +(Hantken) + +- Hagn, 1956, p. 178, pl. 17, figs. 3a-b, 4a-b. + + + + +Stratigraphical distribution in samples: +Rupelian- Chattian. + + + + \ No newline at end of file diff --git a/data/B1/49/43/B149432292518E74FC7EC3AA99CAFA23.xml b/data/B1/49/43/B149432292518E74FC7EC3AA99CAFA23.xml new file mode 100644 index 00000000000..cc7b9dc43ec --- /dev/null +++ b/data/B1/49/43/B149432292518E74FC7EC3AA99CAFA23.xml @@ -0,0 +1,94 @@ + + + +Taxonomic Record Of The Oligocene Benthic Foraminifera From The Vima Formation (Transylvanian Basin, Romania) + + + +Author + +Székely, Szabolcs-Flavius +BabeȘ-Bolyai University, Department of Geology, Str. Kogălniceanu 1, 400084, Cluj Napoca, Romania, szekelyflavius @ gmail. com, sorin. filipescu @ ubbcluj. ro +szekelyflavius@gmail.com + + + +Author + +Introduction, Sorin Filipescu + +text + + +Acta Palaeontologica Romaniae + + +2015 + +2015-08-26 + + +11 + + +1 + + +25 +62 + + + +journal article +10.5281/zenodo.13190119 +1842-371x +13190119 + + + + + + +Planulina compressa +( +Hantken, 1875 +) + + + + + + +Fig. 16.1 +a-c + + + + + + + +Truncatulina compressa +Hantken, 1875 +, p. 62 + + +, pl. 8, fig. 8. + + + + +Planulina compressa +(Hantken) + +- Hagn, 1956, p. 179, pl. 17, fig. 5a-b. + + + + +Stratigraphical distribution in samples: +Rupelian- Chattian. + + + + \ No newline at end of file diff --git a/data/B1/49/43/B149432292518E74FF1EC34E989FFA99.xml b/data/B1/49/43/B149432292518E74FF1EC34E989FFA99.xml new file mode 100644 index 00000000000..1bfa0bc8f1e --- /dev/null +++ b/data/B1/49/43/B149432292518E74FF1EC34E989FFA99.xml @@ -0,0 +1,98 @@ + + + +Taxonomic Record Of The Oligocene Benthic Foraminifera From The Vima Formation (Transylvanian Basin, Romania) + + + +Author + +Székely, Szabolcs-Flavius +BabeȘ-Bolyai University, Department of Geology, Str. Kogălniceanu 1, 400084, Cluj Napoca, Romania, szekelyflavius @ gmail. com, sorin. filipescu @ ubbcluj. ro +szekelyflavius@gmail.com + + + +Author + +Introduction, Sorin Filipescu + +text + + +Acta Palaeontologica Romaniae + + +2015 + +2015-08-26 + + +11 + + +1 + + +25 +62 + + + +journal article +10.5281/zenodo.13190119 +1842-371x +13190119 + + + + + + +Cibicidoides acutus +( +Samoylova, 1947 +) + + + + + + +Fig. 15.4 + + + + + + + +Cibicides acutus +Samoylova, 1947 +, p. 97 + + +, textfigs. 40-42 (fide Ellis & Messina). + + + + + +Cibicidoides acutus +(Samoylova) + +- + +Popescu & Iva, 1971 +, p. 48 + +, pl. 9, fig. 1. + + + +Stratigraphical distribution in samples: +Rupelian. + + + + \ No newline at end of file diff --git a/data/B1/49/43/B149432292518E74FF28C1669AA0F81A.xml b/data/B1/49/43/B149432292518E74FF28C1669AA0F81A.xml new file mode 100644 index 00000000000..7ae077bfdc3 --- /dev/null +++ b/data/B1/49/43/B149432292518E74FF28C1669AA0F81A.xml @@ -0,0 +1,108 @@ + + + +Taxonomic Record Of The Oligocene Benthic Foraminifera From The Vima Formation (Transylvanian Basin, Romania) + + + +Author + +Székely, Szabolcs-Flavius +BabeȘ-Bolyai University, Department of Geology, Str. Kogălniceanu 1, 400084, Cluj Napoca, Romania, szekelyflavius @ gmail. com, sorin. filipescu @ ubbcluj. ro +szekelyflavius@gmail.com + + + +Author + +Introduction, Sorin Filipescu + +text + + +Acta Palaeontologica Romaniae + + +2015 + +2015-08-26 + + +11 + + +1 + + +25 +62 + + + +journal article +10.5281/zenodo.13190119 +1842-371x +13190119 + + + + + + +Cibicidoides ungerianus filicosta +( +Hagn, 1952 +) + + + + + + +Fig. 15.3 +a-c + + + + + + + +Cibicides ungerianus +(d’Orbigny) var. +filicosta +Hagn, 1952 +, p. 186 + + +, pl. 1, fig. 4. + + + + +Cibicides ungerianus filicosta +Hagn + +- Hagn, 1960, pl. 7, fig. 9. + + + + +Cibicidoides ungerianus filicosta +(Hagn) + +- + +Reiser, 1987 +, p. 117 + +, pl. 19, figs. 4, 7-8. + + + +Stratigraphical distribution in samples: +Rupelian- Chattian. + + + + \ No newline at end of file diff --git a/data/B1/49/43/B149432292518E74FF3EC253989FF9EB.xml b/data/B1/49/43/B149432292518E74FF3EC253989FF9EB.xml new file mode 100644 index 00000000000..5a516df2b0e --- /dev/null +++ b/data/B1/49/43/B149432292518E74FF3EC253989FF9EB.xml @@ -0,0 +1,108 @@ + + + +Taxonomic Record Of The Oligocene Benthic Foraminifera From The Vima Formation (Transylvanian Basin, Romania) + + + +Author + +Székely, Szabolcs-Flavius +BabeȘ-Bolyai University, Department of Geology, Str. Kogălniceanu 1, 400084, Cluj Napoca, Romania, szekelyflavius @ gmail. com, sorin. filipescu @ ubbcluj. ro +szekelyflavius@gmail.com + + + +Author + +Introduction, Sorin Filipescu + +text + + +Acta Palaeontologica Romaniae + + +2015 + +2015-08-26 + + +11 + + +1 + + +25 +62 + + + +journal article +10.5281/zenodo.13190119 +1842-371x +13190119 + + + + + + +Cibicidoides oligocenicus +( +Samoylova, 1947 +) + + + + + + +Fig. 15.6 +a-c + + + + + + + +Cibicides dutemplei +(d’Orbigny) var. +oligocenica +Samoylova, 1947 +, p. 96 + + +, figs. 34-36. + + + + +Cibicides oligocenicus +(Samoylova) + +- Pozaryska, 1977 p. 39, pl. 6. figs. 1–6; pl. 7, fig. 3a–c; pl. 13, figs. 8–9. + + + + +Cibicidoides oligocenicus +(Samoylova) + +- + +Cicha et al., 1998 +, p. 90 + +, pl. 62, figs. 1-3. + + + +Stratigraphical distribution in samples: +Rupelian. + + + + \ No newline at end of file diff --git a/data/B1/49/43/B149432292518E77FC63C02E9FC4F7FC.xml b/data/B1/49/43/B149432292518E77FC63C02E9FC4F7FC.xml new file mode 100644 index 00000000000..e3bcba6df54 --- /dev/null +++ b/data/B1/49/43/B149432292518E77FC63C02E9FC4F7FC.xml @@ -0,0 +1,153 @@ + + + +Taxonomic Record Of The Oligocene Benthic Foraminifera From The Vima Formation (Transylvanian Basin, Romania) + + + +Author + +Székely, Szabolcs-Flavius +BabeȘ-Bolyai University, Department of Geology, Str. Kogălniceanu 1, 400084, Cluj Napoca, Romania, szekelyflavius @ gmail. com, sorin. filipescu @ ubbcluj. ro +szekelyflavius@gmail.com + + + +Author + +Introduction, Sorin Filipescu + +text + + +Acta Palaeontologica Romaniae + + +2015 + +2015-08-26 + + +11 + + +1 + + +25 +62 + + + +journal article +10.5281/zenodo.13190119 +1842-371x +13190119 + + + + + + +Cibicides amphysiliensis +( +Andreae, 1884 +) + + + + + + +Fig. 15.5 +a-c + + + + + + + +Truncatulina amphysiliensis +Andreae, 1884 +, p. 255 + + +, pl. 10, fig. 30. + + + + + +Cibicides amphysiliensis +(Andreae) + +- + +Cicha et al., 1998 +, p. 90 + +, pl. 72, figs. 14-17. + + + +Stratigraphical distribution in samples: +Rupelian- Chattian. + + + + +Fig. 16 +All scales represent 100 μm. 1. + +Planulina compressa +(Hantken) + +. Same specimen, a. umbilical view, b. peripherial view, c. spiral view, same scale, sample FB20, Chattian. 2. + +Planulina costata +(Hantken) + +. Same specimen, a. umbilical view, b. spiral view, same scale, sample F12, Rupelian. 3. + +Asterigerinoides guerichi +(Franke) + +. Same specimen, a. umbilical view, b. spiral view, same scale, sample F18, Rupelian. 4. + +Nonion commune +(d’Orbigny) + +. Same specimen, a. lateral view, b. peripherial view, same scale, sample F4, Rupelian. 5. + +Pullenia salisburyii +Stewart & Stewart. Same + +specimen, a. lateral view, b. peripherial view, same scale, sample F10, Rupelian. 6. + +Chilostomella cylindroides +Reuss. Sample F + +34, Rupelian/Chattian. 7. + +Quadrimorphina petrolei +(Andreae) + +. Same specimen, a. umbilical view, b. spiral view, same scale, sample F18, Rupelian. 8-9. + +Alabamina tangentialis +(Clodius) + +. 8a-b. same specimen, a. umbilical view, b. spiral view, same scale, sample FB01, Chattian; 9a-b. same specimen, a. umbilical view, b. spiral view, same scale, sample FB21, Chattian. 10. + +Anomalinoides granosus +(Hantken) + +. Same specimen, a. + + + +umbilical view, b. spiral view, same scale, sample F15, Rupelian 55 + + + \ No newline at end of file diff --git a/data/B1/49/43/B149432292538E76FC76C55199CAFD46.xml b/data/B1/49/43/B149432292538E76FC76C55199CAFD46.xml new file mode 100644 index 00000000000..38c02160d3c --- /dev/null +++ b/data/B1/49/43/B149432292538E76FC76C55199CAFD46.xml @@ -0,0 +1,82 @@ + + + +Taxonomic Record Of The Oligocene Benthic Foraminifera From The Vima Formation (Transylvanian Basin, Romania) + + + +Author + +Székely, Szabolcs-Flavius +BabeȘ-Bolyai University, Department of Geology, Str. Kogălniceanu 1, 400084, Cluj Napoca, Romania, szekelyflavius @ gmail. com, sorin. filipescu @ ubbcluj. ro +szekelyflavius@gmail.com + + + +Author + +Introduction, Sorin Filipescu + +text + + +Acta Palaeontologica Romaniae + + +2015 + +2015-08-26 + + +11 + + +1 + + +25 +62 + + + +journal article +10.5281/zenodo.13190119 +1842-371x +13190119 + + + + + + +Chilostomella cylindroides +Reuss, 1851 + + + + + + +Fig. 16.6 + + + + + + + +Chilostomella cylindroides +Reuss, 1851 +, p. 80 + + +, pl. 6, fig. 43. + + + +Stratigraphical distribution in samples: +Rupelian- Chattian. + + + + \ No newline at end of file diff --git a/data/B1/49/43/B149432292538E76FC92C7C099CAFE36.xml b/data/B1/49/43/B149432292538E76FC92C7C099CAFE36.xml new file mode 100644 index 00000000000..210d91076e8 --- /dev/null +++ b/data/B1/49/43/B149432292538E76FC92C7C099CAFE36.xml @@ -0,0 +1,84 @@ + + + +Taxonomic Record Of The Oligocene Benthic Foraminifera From The Vima Formation (Transylvanian Basin, Romania) + + + +Author + +Székely, Szabolcs-Flavius +BabeȘ-Bolyai University, Department of Geology, Str. Kogălniceanu 1, 400084, Cluj Napoca, Romania, szekelyflavius @ gmail. com, sorin. filipescu @ ubbcluj. ro +szekelyflavius@gmail.com + + + +Author + +Introduction, Sorin Filipescu + +text + + +Acta Palaeontologica Romaniae + + +2015 + +2015-08-26 + + +11 + + +1 + + +25 +62 + + + +journal article +10.5281/zenodo.13190119 +1842-371x +13190119 + + + + + + +Pullenia salisburyii +Stewart & Stewart, 1930 + + + + + + +Fig. 16.5 +a-b + + + + + + +Pullenia salisburyii + +R. E & K. C. + +Stewart, 1930 +, p. 72 + +, pl. 8, fig. 2 (fide Ellis & Messina). + + + +Stratigraphical distribution in samples: +Rupelian- Chattian. + + + + \ No newline at end of file diff --git a/data/B1/49/43/B149432292558E70FC46C21699CAF98A.xml b/data/B1/49/43/B149432292558E70FC46C21699CAF98A.xml new file mode 100644 index 00000000000..e62198e73e7 --- /dev/null +++ b/data/B1/49/43/B149432292558E70FC46C21699CAF98A.xml @@ -0,0 +1,110 @@ + + + +Taxonomic Record Of The Oligocene Benthic Foraminifera From The Vima Formation (Transylvanian Basin, Romania) + + + +Author + +Székely, Szabolcs-Flavius +BabeȘ-Bolyai University, Department of Geology, Str. Kogălniceanu 1, 400084, Cluj Napoca, Romania, szekelyflavius @ gmail. com, sorin. filipescu @ ubbcluj. ro +szekelyflavius@gmail.com + + + +Author + +Introduction, Sorin Filipescu + +text + + +Acta Palaeontologica Romaniae + + +2015 + +2015-08-26 + + +11 + + +1 + + +25 +62 + + + +journal article +10.5281/zenodo.13190119 +1842-371x +13190119 + + + + + + +Angulogerina globosa +( +Stoltz, 1925 +) + + + + + + +Fig. 13.9 +a-b + + + + + + + +Uvigerina tenuistriata +d’Orbigny var. +globosa +Stoltz, 1925 +, p. 130 + + +, fig. 2 (fide Ellis & Messina). + + + + + +Trifarina globosa +(Stoltz) + +- + +Sztrákos, 1979 +, p. 67 + +, pl. 20, figs. 13-14. + + + + +Angulogerina globosa +(Stoltz) + +- Mathelin & Sztrákos, 1993, p. 48, pl. 34, fig. 20. + + + + +Stratigraphical distribution in samples: +Rupelian- Chattian. + + + + \ No newline at end of file diff --git a/data/B1/49/43/B149432292558E70FC9FC4869F38FB5B.xml b/data/B1/49/43/B149432292558E70FC9FC4869F38FB5B.xml new file mode 100644 index 00000000000..6ce90c854ec --- /dev/null +++ b/data/B1/49/43/B149432292558E70FC9FC4869F38FB5B.xml @@ -0,0 +1,108 @@ + + + +Taxonomic Record Of The Oligocene Benthic Foraminifera From The Vima Formation (Transylvanian Basin, Romania) + + + +Author + +Székely, Szabolcs-Flavius +BabeȘ-Bolyai University, Department of Geology, Str. Kogălniceanu 1, 400084, Cluj Napoca, Romania, szekelyflavius @ gmail. com, sorin. filipescu @ ubbcluj. ro +szekelyflavius@gmail.com + + + +Author + +Introduction, Sorin Filipescu + +text + + +Acta Palaeontologica Romaniae + + +2015 + +2015-08-26 + + +11 + + +1 + + +25 +62 + + + +journal article +10.5281/zenodo.13190119 +1842-371x +13190119 + + + + + + +Angulogerina angulosa +( +Williamson, 1858 +) + + + + + + +Figs. 13.10 +a-b, 13.13a-b + + + + + + + +Uvigerina angulosa +Williamson, 1858 +, p. 67 + + +, pl. 5, fig. 140. + + + + +Angulogerina angulosa +(Williamson) + +- Cushman, 1949, p. 111, pl. 6, figs. 9-10. + + + + + +Trifarina angulosa +(Williamson) + +- Popescu, 1979, p. 36, pl. 21, fig. 6. + + + +Angulogerina angulosa +(Williamson) + +- Loeblich & Tappan, 1987, pl. 574, figs. 5-9. + + +Stratigraphical distribution in samples: +Rupelian. + + + + \ No newline at end of file diff --git a/data/B1/49/43/B149432292558E70FCD7C6889FD5FD3C.xml b/data/B1/49/43/B149432292558E70FCD7C6889FD5FD3C.xml new file mode 100644 index 00000000000..9c49d84af8b --- /dev/null +++ b/data/B1/49/43/B149432292558E70FCD7C6889FD5FD3C.xml @@ -0,0 +1,89 @@ + + + +Taxonomic Record Of The Oligocene Benthic Foraminifera From The Vima Formation (Transylvanian Basin, Romania) + + + +Author + +Székely, Szabolcs-Flavius +BabeȘ-Bolyai University, Department of Geology, Str. Kogălniceanu 1, 400084, Cluj Napoca, Romania, szekelyflavius @ gmail. com, sorin. filipescu @ ubbcluj. ro +szekelyflavius@gmail.com + + + +Author + +Introduction, Sorin Filipescu + +text + + +Acta Palaeontologica Romaniae + + +2015 + +2015-08-26 + + +11 + + +1 + + +25 +62 + + + +journal article +10.5281/zenodo.13190119 +1842-371x +13190119 + + + + + + +Angulogerina oligocaenica +(Andreae) + +- Cushman & + +Edwards, 1938, p. 86, pl. 15, figs. 8-11. + + + + + + +Uvigerina gracilis +(Reuss) var. +oligocaenica +(Andreae) + +- + +Batjes, 1958 +, p. 135 + +, pl. 6, fig. 3. + + + +Stratigraphical distribution in samples: +Rupelian- Chattian. + + + +Uvigerina tenuistriata schlichti +Schudack & Nuglisch, + + + + + \ No newline at end of file diff --git a/data/B1/49/43/B149432292558E70FEC2C2169AA1FA23.xml b/data/B1/49/43/B149432292558E70FEC2C2169AA1FA23.xml new file mode 100644 index 00000000000..b8751c8c50d --- /dev/null +++ b/data/B1/49/43/B149432292558E70FEC2C2169AA1FA23.xml @@ -0,0 +1,74 @@ + + + +Taxonomic Record Of The Oligocene Benthic Foraminifera From The Vima Formation (Transylvanian Basin, Romania) + + + +Author + +Székely, Szabolcs-Flavius +BabeȘ-Bolyai University, Department of Geology, Str. Kogălniceanu 1, 400084, Cluj Napoca, Romania, szekelyflavius @ gmail. com, sorin. filipescu @ ubbcluj. ro +szekelyflavius@gmail.com + + + +Author + +Introduction, Sorin Filipescu + +text + + +Acta Palaeontologica Romaniae + + +2015 + +2015-08-26 + + +11 + + +1 + + +25 +62 + + + +journal article +10.5281/zenodo.13190119 +1842-371x +13190119 + + + + + + +Uvigerina popescui +Rögl, 1998 + + + + + + +Figs. 13.2 +a-b, 13.3a-b, 13.4a-b, 13.5a-b + +Uvigerina popescui +Rögl, 1998, p. 74 + +, pl. 52, figs. 1-3. + + +Stratigraphical distribution in samples: +Rupelian- Chattian. + + + + \ No newline at end of file diff --git a/data/B1/49/43/B149432292558E70FEF7C32F9AA0FB5B.xml b/data/B1/49/43/B149432292558E70FEF7C32F9AA0FB5B.xml new file mode 100644 index 00000000000..71fef8eed38 --- /dev/null +++ b/data/B1/49/43/B149432292558E70FEF7C32F9AA0FB5B.xml @@ -0,0 +1,83 @@ + + + +Taxonomic Record Of The Oligocene Benthic Foraminifera From The Vima Formation (Transylvanian Basin, Romania) + + + +Author + +Székely, Szabolcs-Flavius +BabeȘ-Bolyai University, Department of Geology, Str. Kogălniceanu 1, 400084, Cluj Napoca, Romania, szekelyflavius @ gmail. com, sorin. filipescu @ ubbcluj. ro +szekelyflavius@gmail.com + + + +Author + +Introduction, Sorin Filipescu + +text + + +Acta Palaeontologica Romaniae + + +2015 + +2015-08-26 + + +11 + + +1 + + +25 +62 + + + +journal article +10.5281/zenodo.13190119 +1842-371x +13190119 + + + + + + +Uvigerina moravia +Boersma, 1984 + + + + + + +Fig. 13.1 +a-b + + + + + + + +Uvigerina moravia +Boersma, 1984 +, p. 114 + + +, textfig. p. 114, figs. 1-4. + + + +Stratigraphical distribution in samples: +Rupelian- Chattian. + + + + \ No newline at end of file diff --git a/data/B1/49/43/B149432292558E70FF2CC5739AA0FC28.xml b/data/B1/49/43/B149432292558E70FF2CC5739AA0FC28.xml new file mode 100644 index 00000000000..d7b020a152c --- /dev/null +++ b/data/B1/49/43/B149432292558E70FF2CC5739AA0FC28.xml @@ -0,0 +1,98 @@ + + + +Taxonomic Record Of The Oligocene Benthic Foraminifera From The Vima Formation (Transylvanian Basin, Romania) + + + +Author + +Székely, Szabolcs-Flavius +BabeȘ-Bolyai University, Department of Geology, Str. Kogălniceanu 1, 400084, Cluj Napoca, Romania, szekelyflavius @ gmail. com, sorin. filipescu @ ubbcluj. ro +szekelyflavius@gmail.com + + + +Author + +Introduction, Sorin Filipescu + +text + + +Acta Palaeontologica Romaniae + + +2015 + +2015-08-26 + + +11 + + +1 + + +25 +62 + + + +journal article +10.5281/zenodo.13190119 +1842-371x +13190119 + + + + + + +Praeglobobulimina pupoides +(d’Orbigny, 1846) + + + + + + +Fig. 12.13 + + + + + +Bulimina pupoides +d’Orbigny, 1846, p. 185 + +, pl. 11, figs. 11-12. + + + +Praeglobobulimina pupoides +(d’Orbigny) + +- Foraminiferi Padani, AGIP, 1982, p. 122, pl. 6, fig. 12. + + + + +Protoglobobulimina pupoides +(d’Orbigny) + +- + +Loeblich & Tappan, 1988 +, p. 522 + +, pl. 572, figs. 1-6. + + + +Stratigraphical distribution in samples: +Rupelian- Chattian. + + + + \ No newline at end of file diff --git a/data/B1/49/43/B149432292558E70FF71C1ED989FF8F1.xml b/data/B1/49/43/B149432292558E70FF71C1ED989FF8F1.xml new file mode 100644 index 00000000000..276d9ab0113 --- /dev/null +++ b/data/B1/49/43/B149432292558E70FF71C1ED989FF8F1.xml @@ -0,0 +1,67 @@ + + + +Taxonomic Record Of The Oligocene Benthic Foraminifera From The Vima Formation (Transylvanian Basin, Romania) + + + +Author + +Székely, Szabolcs-Flavius +BabeȘ-Bolyai University, Department of Geology, Str. Kogălniceanu 1, 400084, Cluj Napoca, Romania, szekelyflavius @ gmail. com, sorin. filipescu @ ubbcluj. ro +szekelyflavius@gmail.com + + + +Author + +Introduction, Sorin Filipescu + +text + + +Acta Palaeontologica Romaniae + + +2015 + +2015-08-26 + + +11 + + +1 + + +25 +62 + + + +journal article +10.5281/zenodo.13190119 +1842-371x +13190119 + + + + + + +Uvigerina vicksburgensis +Cushman & Ellisor, 1931 + +, p. + + +54, pl. 7, fig. 7. + + + +Stratigraphical distribution in samples: +Rupelian. + + + + \ No newline at end of file diff --git a/data/B1/49/43/B149432292578E72FF0BC2BF989FF952.xml b/data/B1/49/43/B149432292578E72FF0BC2BF989FF952.xml new file mode 100644 index 00000000000..8bd43f0aa7e --- /dev/null +++ b/data/B1/49/43/B149432292578E72FF0BC2BF989FF952.xml @@ -0,0 +1,106 @@ + + + +Taxonomic Record Of The Oligocene Benthic Foraminifera From The Vima Formation (Transylvanian Basin, Romania) + + + +Author + +Székely, Szabolcs-Flavius +BabeȘ-Bolyai University, Department of Geology, Str. Kogălniceanu 1, 400084, Cluj Napoca, Romania, szekelyflavius @ gmail. com, sorin. filipescu @ ubbcluj. ro +szekelyflavius@gmail.com + + + +Author + +Introduction, Sorin Filipescu + +text + + +Acta Palaeontologica Romaniae + + +2015 + +2015-08-26 + + +11 + + +1 + + +25 +62 + + + +journal article +10.5281/zenodo.13190119 +1842-371x +13190119 + + + + + + +Pleurostomella incrassata +Hantken, 1883 + + + + + + +Fig. 14.11 +a-b + + + + + + + +Pleurostomella incrassata +Hantken, 1883 +, p. 25 + + +, pl. 1, figs. 4, 7. + + + + +Pleurostomella alternans +Schwager var. +moravica +Schubert, 1900, p. 157 + +, pl. 2, figs. 5a-c. + + + +Pleurostomella velascoensis +Cushman, 1926, p. 590 + +, pl. 16, fig. 4. + + + +Pleurostomella paleocenica +Cushman, 1947, p. 86 + +, pl. 18, figs. 14-15. + + +Stratigraphical distribution in samples: +Rupelian. + + + + \ No newline at end of file diff --git a/data/B1/49/43/B149432292578E72FF10C4E29AA0FB5B.xml b/data/B1/49/43/B149432292578E72FF10C4E29AA0FB5B.xml new file mode 100644 index 00000000000..2754acfb486 --- /dev/null +++ b/data/B1/49/43/B149432292578E72FF10C4E29AA0FB5B.xml @@ -0,0 +1,97 @@ + + + +Taxonomic Record Of The Oligocene Benthic Foraminifera From The Vima Formation (Transylvanian Basin, Romania) + + + +Author + +Székely, Szabolcs-Flavius +BabeȘ-Bolyai University, Department of Geology, Str. Kogălniceanu 1, 400084, Cluj Napoca, Romania, szekelyflavius @ gmail. com, sorin. filipescu @ ubbcluj. ro +szekelyflavius@gmail.com + + + +Author + +Introduction, Sorin Filipescu + +text + + +Acta Palaeontologica Romaniae + + +2015 + +2015-08-26 + + +11 + + +1 + + +25 +62 + + + +journal article +10.5281/zenodo.13190119 +1842-371x +13190119 + + + + + + +Caucasina oligocaenica +Khalilov, 1951 + + + + + + +Figs. 12.3 +a-b, 12.4-12.5 + + + + + + + +Caucasina oligocaenica +Khalilov, 1951 +, p. 58 + + +, pl. 4, fig. 4 (fide Ellis & Messina). + + + + + +Baggatella oligocaenica +(Khalilov) + +- + +Popescu & Iva, 1971 +, p. 43 + +, pl. 10, figs. 2-7. + + + +Stratigraphical distribution in samples: +Rupelian- Chattian. + + + + \ No newline at end of file diff --git a/data/B1/49/43/B149432292598E7CFC4DC3AA9F03FA99.xml b/data/B1/49/43/B149432292598E7CFC4DC3AA9F03FA99.xml new file mode 100644 index 00000000000..3d71c07929f --- /dev/null +++ b/data/B1/49/43/B149432292598E7CFC4DC3AA9F03FA99.xml @@ -0,0 +1,80 @@ + + + +Taxonomic Record Of The Oligocene Benthic Foraminifera From The Vima Formation (Transylvanian Basin, Romania) + + + +Author + +Székely, Szabolcs-Flavius +BabeȘ-Bolyai University, Department of Geology, Str. Kogălniceanu 1, 400084, Cluj Napoca, Romania, szekelyflavius @ gmail. com, sorin. filipescu @ ubbcluj. ro +szekelyflavius@gmail.com + + + +Author + +Introduction, Sorin Filipescu + +text + + +Acta Palaeontologica Romaniae + + +2015 + +2015-08-26 + + +11 + + +1 + + +25 +62 + + + +journal article +10.5281/zenodo.13190119 +1842-371x +13190119 + + + + + + +Bolivina plicatella +Cushman, 1930 + + + + + + +Fig. 10.9 + + + + + + + +Bolivina plicatella +Cushman, 1930 +, p. 46 + + +, pl. 8, fig. 10. +Stratigraphical distribution in samples: +Chattian. + + + + + \ No newline at end of file diff --git a/data/B1/49/43/B149432292598E7CFC53C43B99CAFB37.xml b/data/B1/49/43/B149432292598E7CFC53C43B99CAFB37.xml new file mode 100644 index 00000000000..32592220f42 --- /dev/null +++ b/data/B1/49/43/B149432292598E7CFC53C43B99CAFB37.xml @@ -0,0 +1,109 @@ + + + +Taxonomic Record Of The Oligocene Benthic Foraminifera From The Vima Formation (Transylvanian Basin, Romania) + + + +Author + +Székely, Szabolcs-Flavius +BabeȘ-Bolyai University, Department of Geology, Str. Kogălniceanu 1, 400084, Cluj Napoca, Romania, szekelyflavius @ gmail. com, sorin. filipescu @ ubbcluj. ro +szekelyflavius@gmail.com + + + +Author + +Introduction, Sorin Filipescu + +text + + +Acta Palaeontologica Romaniae + + +2015 + +2015-08-26 + + +11 + + +1 + + +25 +62 + + + +journal article +10.5281/zenodo.13190119 +1842-371x +13190119 + + + + + + +Bolivina fastigia +Cushman, 1936 + + + + + + +Fig. 11.2 +a-b + + + + + + + +Bolivina fastigia +Cushman, 1936 +, p. 51 + + +, pl. 7, fig. 17 (fide Ellis & Messina). + + + +Stratigraphical distribution in samples: +Rupelian- Chattian. + + + +Bolivina molassica +Hofmann, 1967 + + + +Fig. 11.10 +a-b + + + + + +Bolivina molassica +Hofmann, 1967 +, p. 158 + + +, pl. 4, figs. 9- 11. + + + +Stratigraphical distribution in samples: +Rupelian- Chattian. + + + + \ No newline at end of file diff --git a/data/B1/49/43/B149432292598E7CFC61C6899FDEFD3C.xml b/data/B1/49/43/B149432292598E7CFC61C6899FDEFD3C.xml new file mode 100644 index 00000000000..99d88f468de --- /dev/null +++ b/data/B1/49/43/B149432292598E7CFC61C6899FDEFD3C.xml @@ -0,0 +1,89 @@ + + + +Taxonomic Record Of The Oligocene Benthic Foraminifera From The Vima Formation (Transylvanian Basin, Romania) + + + +Author + +Székely, Szabolcs-Flavius +BabeȘ-Bolyai University, Department of Geology, Str. Kogălniceanu 1, 400084, Cluj Napoca, Romania, szekelyflavius @ gmail. com, sorin. filipescu @ ubbcluj. ro +szekelyflavius@gmail.com + + + +Author + +Introduction, Sorin Filipescu + +text + + +Acta Palaeontologica Romaniae + + +2015 + +2015-08-26 + + +11 + + +1 + + +25 +62 + + + +journal article +10.5281/zenodo.13190119 +1842-371x +13190119 + + + + + + +Bolivina dilatata hyalina +Hofmann, 1967 + + + + + + +Fig. 11.4 +a-b + + + + + + + +Bolivina dilatata hyalina +Hofmann, 1967 +, p. 156 + + +, pl. 1, figs. 7-9. + + + +Stratigraphical distribution in samples: +Rupelian- Chattian. + + + +Bolivina dilatata maxima +Cicha & Zapletalová, 1963 + + + + + \ No newline at end of file diff --git a/data/B1/49/43/B149432292598E7CFC81C1C299CAF81A.xml b/data/B1/49/43/B149432292598E7CFC81C1C299CAF81A.xml new file mode 100644 index 00000000000..8ac52c93771 --- /dev/null +++ b/data/B1/49/43/B149432292598E7CFC81C1C299CAF81A.xml @@ -0,0 +1,97 @@ + + + +Taxonomic Record Of The Oligocene Benthic Foraminifera From The Vima Formation (Transylvanian Basin, Romania) + + + +Author + +Székely, Szabolcs-Flavius +BabeȘ-Bolyai University, Department of Geology, Str. Kogălniceanu 1, 400084, Cluj Napoca, Romania, szekelyflavius @ gmail. com, sorin. filipescu @ ubbcluj. ro +szekelyflavius@gmail.com + + + +Author + +Introduction, Sorin Filipescu + +text + + +Acta Palaeontologica Romaniae + + +2015 + +2015-08-26 + + +11 + + +1 + + +25 +62 + + + +journal article +10.5281/zenodo.13190119 +1842-371x +13190119 + + + + + + +Bolivina semistriata semistriata +Hantken, 1875 + + + + + + +Fig. 11.9 +a-b + + + + + + + +Bolivina semistriata +Hantken, 1875 +, p. 95 + + +, pl. 15, fig. 4. + + + + + +Bolivina semistriata semistriata +Hantken + +- + +Cicha et al., 1998 +, p. 85 + +, pl. 44, fig. 6. + + + +Stratigraphical distribution in samples: +Rupelian- Chattian. + + + + \ No newline at end of file diff --git a/data/B1/49/43/B149432292598E7CFC97C13A9F38F90F.xml b/data/B1/49/43/B149432292598E7CFC97C13A9F38F90F.xml new file mode 100644 index 00000000000..e217b249c20 --- /dev/null +++ b/data/B1/49/43/B149432292598E7CFC97C13A9F38F90F.xml @@ -0,0 +1,85 @@ + + + +Taxonomic Record Of The Oligocene Benthic Foraminifera From The Vima Formation (Transylvanian Basin, Romania) + + + +Author + +Székely, Szabolcs-Flavius +BabeȘ-Bolyai University, Department of Geology, Str. Kogălniceanu 1, 400084, Cluj Napoca, Romania, szekelyflavius @ gmail. com, sorin. filipescu @ ubbcluj. ro +szekelyflavius@gmail.com + + + +Author + +Introduction, Sorin Filipescu + +text + + +Acta Palaeontologica Romaniae + + +2015 + +2015-08-26 + + +11 + + +1 + + +25 +62 + + + +journal article +10.5281/zenodo.13190119 +1842-371x +13190119 + + + + + + +Bolivina scalprata retiformis +Cushman, 1936 + + + + + + +Fig. 11.1 +a-b + + + + + + + +Bolivina scalprata +Schwager var. +retiformis +Cushman, 1936 +, p. 53 + + +, pl. 7, fig. 19. + + + +Stratigraphical distribution in samples: +Rupelian. + + + + \ No newline at end of file diff --git a/data/B1/49/43/B149432292598E7CFCA0C25399CAFA47.xml b/data/B1/49/43/B149432292598E7CFCA0C25399CAFA47.xml new file mode 100644 index 00000000000..255dc1e2d33 --- /dev/null +++ b/data/B1/49/43/B149432292598E7CFCA0C25399CAFA47.xml @@ -0,0 +1,83 @@ + + + +Taxonomic Record Of The Oligocene Benthic Foraminifera From The Vima Formation (Transylvanian Basin, Romania) + + + +Author + +Székely, Szabolcs-Flavius +BabeȘ-Bolyai University, Department of Geology, Str. Kogălniceanu 1, 400084, Cluj Napoca, Romania, szekelyflavius @ gmail. com, sorin. filipescu @ ubbcluj. ro +szekelyflavius@gmail.com + + + +Author + +Introduction, Sorin Filipescu + +text + + +Acta Palaeontologica Romaniae + + +2015 + +2015-08-26 + + +11 + + +1 + + +25 +62 + + + +journal article +10.5281/zenodo.13190119 +1842-371x +13190119 + + + + + + +Bolivina pokornyi serrata +Cicha & Zapletalová, 1963 + + + + + + +Fig. 11.12 +a-b + + + + + + + +Bolivina pokornyi serrata +Cicha & Zapletalová, 1963 +, p. 144 + + +, textfig. 19. + + + +Stratigraphical distribution in samples: +Rupelian- Chattian. + + + + \ No newline at end of file diff --git a/data/B1/49/43/B149432292598E7CFCD7C5BC9F03FD46.xml b/data/B1/49/43/B149432292598E7CFCD7C5BC9F03FD46.xml new file mode 100644 index 00000000000..c99dbce207f --- /dev/null +++ b/data/B1/49/43/B149432292598E7CFCD7C5BC9F03FD46.xml @@ -0,0 +1,67 @@ + + + +Taxonomic Record Of The Oligocene Benthic Foraminifera From The Vima Formation (Transylvanian Basin, Romania) + + + +Author + +Székely, Szabolcs-Flavius +BabeȘ-Bolyai University, Department of Geology, Str. Kogălniceanu 1, 400084, Cluj Napoca, Romania, szekelyflavius @ gmail. com, sorin. filipescu @ ubbcluj. ro +szekelyflavius@gmail.com + + + +Author + +Introduction, Sorin Filipescu + +text + + +Acta Palaeontologica Romaniae + + +2015 + +2015-08-26 + + +11 + + +1 + + +25 +62 + + + +journal article +10.5281/zenodo.13190119 +1842-371x +13190119 + + + + + + +Bolivina dilatata maxima +Cicha & Zapletalová, 1963 + +, p. + + +136, textfig. 15. + + + +Stratigraphical distribution in samples: +Chattian. + + + + \ No newline at end of file diff --git a/data/B1/49/43/B149432292598E7CFEE9C1ED9AA0F858.xml b/data/B1/49/43/B149432292598E7CFEE9C1ED9AA0F858.xml new file mode 100644 index 00000000000..34cfb7a9c1b --- /dev/null +++ b/data/B1/49/43/B149432292598E7CFEE9C1ED9AA0F858.xml @@ -0,0 +1,97 @@ + + + +Taxonomic Record Of The Oligocene Benthic Foraminifera From The Vima Formation (Transylvanian Basin, Romania) + + + +Author + +Székely, Szabolcs-Flavius +BabeȘ-Bolyai University, Department of Geology, Str. Kogălniceanu 1, 400084, Cluj Napoca, Romania, szekelyflavius @ gmail. com, sorin. filipescu @ ubbcluj. ro +szekelyflavius@gmail.com + + + +Author + +Introduction, Sorin Filipescu + +text + + +Acta Palaeontologica Romaniae + + +2015 + +2015-08-26 + + +11 + + +1 + + +25 +62 + + + +journal article +10.5281/zenodo.13190119 +1842-371x +13190119 + + + + + + +Bolivina crenulata +Cushman, 1936 + + + + + + +Figs. 10.10, 10.11 +a-b + + + + + + + +Bolivina crenulata +Cushman, 1936 +, p. 50 + + +, pl. 7, fig. 13ab. + + + + + +Bolivina crenulata crenulata +Cushman + +- + +Hofmann, 1967 +, p. 146 + +, pl. 1, figs. 4-6. + + + +Stratigraphical distribution in samples: +Rupelian- Chattian. + + + + \ No newline at end of file diff --git a/data/B1/49/43/B149432292598E7CFEF3C4679AA0FB93.xml b/data/B1/49/43/B149432292598E7CFEF3C4679AA0FB93.xml new file mode 100644 index 00000000000..b52a5864c25 --- /dev/null +++ b/data/B1/49/43/B149432292598E7CFEF3C4679AA0FB93.xml @@ -0,0 +1,77 @@ + + + +Taxonomic Record Of The Oligocene Benthic Foraminifera From The Vima Formation (Transylvanian Basin, Romania) + + + +Author + +Székely, Szabolcs-Flavius +BabeȘ-Bolyai University, Department of Geology, Str. Kogălniceanu 1, 400084, Cluj Napoca, Romania, szekelyflavius @ gmail. com, sorin. filipescu @ ubbcluj. ro +szekelyflavius@gmail.com + + + +Author + +Introduction, Sorin Filipescu + +text + + +Acta Palaeontologica Romaniae + + +2015 + +2015-08-26 + + +11 + + +1 + + +25 +62 + + + +journal article +10.5281/zenodo.13190119 +1842-371x +13190119 + + + + + + +Bolivina antiqua +d’Orbigny, 1846 + + + + + + +Fig. 11.7 + + + + + +Bolivina antiqua +d’Orbigny, 1846, p. 240 + +, pl. 14, figs. 11- 13. + + +Stratigraphical distribution in samples: +Rupelian- Chattian. + + + + \ No newline at end of file diff --git a/data/B1/49/43/B149432292598E7CFEF6C6F59899FD1D.xml b/data/B1/49/43/B149432292598E7CFEF6C6F59899FD1D.xml new file mode 100644 index 00000000000..e2c78f934f1 --- /dev/null +++ b/data/B1/49/43/B149432292598E7CFEF6C6F59899FD1D.xml @@ -0,0 +1,80 @@ + + + +Taxonomic Record Of The Oligocene Benthic Foraminifera From The Vima Formation (Transylvanian Basin, Romania) + + + +Author + +Székely, Szabolcs-Flavius +BabeȘ-Bolyai University, Department of Geology, Str. Kogălniceanu 1, 400084, Cluj Napoca, Romania, szekelyflavius @ gmail. com, sorin. filipescu @ ubbcluj. ro +szekelyflavius@gmail.com + + + +Author + +Introduction, Sorin Filipescu + +text + + +Acta Palaeontologica Romaniae + + +2015 + +2015-08-26 + + +11 + + +1 + + +25 +62 + + + +journal article +10.5281/zenodo.13190119 +1842-371x +13190119 + + + + + + +Glandulina ovula +d’Orbigny, 1846 + + + + + + +Fig. 10.6 + + + +Glandulina ovula +d’Orbigny, 1846, p. 29 + +, pl. 1, figs. 6-7. + +Glandulina ovula +d’Orbigny + +- Papp & Schmid, 1985, p. 21, pl. 2, figs. 1-9. + + +Stratigraphical distribution in samples: +Chattian. + + + + \ No newline at end of file diff --git a/data/B1/49/43/B149432292598E7CFF0DC2BF9AA0F96C.xml b/data/B1/49/43/B149432292598E7CFF0DC2BF9AA0F96C.xml new file mode 100644 index 00000000000..e47a6e58119 --- /dev/null +++ b/data/B1/49/43/B149432292598E7CFF0DC2BF9AA0F96C.xml @@ -0,0 +1,101 @@ + + + +Taxonomic Record Of The Oligocene Benthic Foraminifera From The Vima Formation (Transylvanian Basin, Romania) + + + +Author + +Székely, Szabolcs-Flavius +BabeȘ-Bolyai University, Department of Geology, Str. Kogălniceanu 1, 400084, Cluj Napoca, Romania, szekelyflavius @ gmail. com, sorin. filipescu @ ubbcluj. ro +szekelyflavius@gmail.com + + + +Author + +Introduction, Sorin Filipescu + +text + + +Acta Palaeontologica Romaniae + + +2015 + +2015-08-26 + + +11 + + +1 + + +25 +62 + + + +journal article +10.5281/zenodo.13190119 +1842-371x +13190119 + + + + + + +Bolivina beyrichi carinata +Hantken, 1875 + + + + + + +Fig. 10.7 +a-b + + + + + +Bolivina beyrichi +Reuss var. +carinata +Hantken, 1875 + +, pl. 7, fig. 12. + + + +Bolivina beyrichi carinata +Hantken + +- Lindenberg, 1966, p. 96, abb. 4/4. + + + + +Bolivina beyrichi carinata +Hantken + +- + +Cicha et al., 1998 +, p. 83 + +, pl. 44, fig. 3. + + + +Stratigraphical distribution in samples: +Rupelian- Chattian. + + + + \ No newline at end of file diff --git a/data/B1/49/43/B149432292598E7CFF1CC34E9AA0FA3D.xml b/data/B1/49/43/B149432292598E7CFF1CC34E9AA0FA3D.xml new file mode 100644 index 00000000000..158811f708e --- /dev/null +++ b/data/B1/49/43/B149432292598E7CFF1CC34E9AA0FA3D.xml @@ -0,0 +1,110 @@ + + + +Taxonomic Record Of The Oligocene Benthic Foraminifera From The Vima Formation (Transylvanian Basin, Romania) + + + +Author + +Székely, Szabolcs-Flavius +BabeȘ-Bolyai University, Department of Geology, Str. Kogălniceanu 1, 400084, Cluj Napoca, Romania, szekelyflavius @ gmail. com, sorin. filipescu @ ubbcluj. ro +szekelyflavius@gmail.com + + + +Author + +Introduction, Sorin Filipescu + +text + + +Acta Palaeontologica Romaniae + + +2015 + +2015-08-26 + + +11 + + +1 + + +25 +62 + + + +journal article +10.5281/zenodo.13190119 +1842-371x +13190119 + + + + + + +Bolivina beyrichi beyrichi +Reuss, 1851 + + + + + + +Fig. 10.8 + + + + + + + +Bolivina beyrichi +Reuss, 1851 +, p. 83 + + +, pl. 6, fig. 51 (fide Ellis & Messina). + + + + + +Bolivina beyrichi beyrichi +Reuss + +- + +Hofmann, 1967 +, p. 137 + +, pl. 3, figs. 1-4. + + + + + +Bolivina beyrichi +Reuss + +- + +Popescu, 1975 +, p. 73 + +, pl. 43, figs. 1-2. + + + +Stratigraphical distribution in samples: +Rupelian- Chattian. + + + + \ No newline at end of file diff --git a/data/B1/49/43/B149432292598E7EFC98C0D79AA0FEAC.xml b/data/B1/49/43/B149432292598E7EFC98C0D79AA0FEAC.xml new file mode 100644 index 00000000000..4b0d336ae25 --- /dev/null +++ b/data/B1/49/43/B149432292598E7EFC98C0D79AA0FEAC.xml @@ -0,0 +1,148 @@ + + + +Taxonomic Record Of The Oligocene Benthic Foraminifera From The Vima Formation (Transylvanian Basin, Romania) + + + +Author + +Székely, Szabolcs-Flavius +BabeȘ-Bolyai University, Department of Geology, Str. Kogălniceanu 1, 400084, Cluj Napoca, Romania, szekelyflavius @ gmail. com, sorin. filipescu @ ubbcluj. ro +szekelyflavius@gmail.com + + + +Author + +Introduction, Sorin Filipescu + +text + + +Acta Palaeontologica Romaniae + + +2015 + +2015-08-26 + + +11 + + +1 + + +25 +62 + + + +journal article +10.5281/zenodo.13190119 +1842-371x +13190119 + + + + + + +Bolivina semistriata nobilis +Hantken, 1875 + + + + + + +Fig. 11.11 +a-b + + + + + + + +Bolivina nobilis +Hantken, 1875 +, p. 65 + + +, pl. 14, fig. 4. + + + + +Fig. 12 +All scales represent 100 μm. 1,8. + +Bulimina coprolithoides +Andreae. + +1a-b. same specimen, a. apertural view, b. lateral view, same scale, sample F14, Rupelian; 8. sample F33, Rupelian/Chattian. 2. + +Bulimina elongata +d’Orbigny. Same + +specimen, a. apertural view, b. lateral view, same scale, sample F17, Rupelian. 3-5. + +Caucasina oligocaenica +Khalilov. + +3a-b. same specimen, a. apertural view, b. lateral view, same scale, sample F14, Rupelian; 4. sample F3, Rupelian; 5. sample F12, Rupelian. 6-7. + +Bulimina alsatica +Cushman & Parker. + +6a-b. same specimen, a. apertural view, b. lateral view, same scale, sample F7, Rupelian; 7. sample F5, Rupelian. 9. + +Bulimina schischkinskayae +Samoylova. Sample F + +27, Rupelian. 10. + +Bulimina alazanensis +Cushman. Sample F + +18, Rupelian. 11. + +Bulimina striata striata +d’Orbigny. Same + +specimen, a. apertural view, b. lateral view, same scale, sample F7, Rupelian. 12. + +Bulimina arndti +Hagn. Same + +specimen, a. apertural view, b. lateral view, same scale, FB19, Chattian. 13. + +Praeglobobulimina pupoides +(d’Orbigny) + +. Sample F25, Rupelian. + + + + + +Bolivina semistriata nobilis +Hantken + +- + +Cicha et al., 1998 +, p. 85 + +, pl. 44, fig. 7. + + + +Stratigraphical distribution in samples: +Rupelian- Chattian. + + + + \ No newline at end of file diff --git a/data/B1/49/43/B1494322925B8E7EFC2AC59299CAFCA7.xml b/data/B1/49/43/B1494322925B8E7EFC2AC59299CAFCA7.xml new file mode 100644 index 00000000000..9067f7ed604 --- /dev/null +++ b/data/B1/49/43/B1494322925B8E7EFC2AC59299CAFCA7.xml @@ -0,0 +1,83 @@ + + + +Taxonomic Record Of The Oligocene Benthic Foraminifera From The Vima Formation (Transylvanian Basin, Romania) + + + +Author + +Székely, Szabolcs-Flavius +BabeȘ-Bolyai University, Department of Geology, Str. Kogălniceanu 1, 400084, Cluj Napoca, Romania, szekelyflavius @ gmail. com, sorin. filipescu @ ubbcluj. ro +szekelyflavius@gmail.com + + + +Author + +Introduction, Sorin Filipescu + +text + + +Acta Palaeontologica Romaniae + + +2015 + +2015-08-26 + + +11 + + +1 + + +25 +62 + + + +journal article +10.5281/zenodo.13190119 +1842-371x +13190119 + + + + + + +Bulimina arndti +Hagn, 1952 + + + + + + +Fig. 12.12 +a-b + + + + + + + +Bulimina arndti +Hagn, 1952 +, p. 168 + + +, pl. 2, fig. 15. + + + +Stratigraphical distribution in samples: +Rupelian- Chattian. + + + + \ No newline at end of file diff --git a/data/B1/49/43/B1494322925B8E7EFC42C38B99CAFA47.xml b/data/B1/49/43/B1494322925B8E7EFC42C38B99CAFA47.xml new file mode 100644 index 00000000000..11759fc0e5a --- /dev/null +++ b/data/B1/49/43/B1494322925B8E7EFC42C38B99CAFA47.xml @@ -0,0 +1,110 @@ + + + +Taxonomic Record Of The Oligocene Benthic Foraminifera From The Vima Formation (Transylvanian Basin, Romania) + + + +Author + +Székely, Szabolcs-Flavius +BabeȘ-Bolyai University, Department of Geology, Str. Kogălniceanu 1, 400084, Cluj Napoca, Romania, szekelyflavius @ gmail. com, sorin. filipescu @ ubbcluj. ro +szekelyflavius@gmail.com + + + +Author + +Introduction, Sorin Filipescu + +text + + +Acta Palaeontologica Romaniae + + +2015 + +2015-08-26 + + +11 + + +1 + + +25 +62 + + + +journal article +10.5281/zenodo.13190119 +1842-371x +13190119 + + + + + + +Bulimina elongata +d’Orbigny, 1846 + + + + + + +Fig. 12.2 +a-b + + + + + +Bulimina elongata +d’Orbigny, 1846, p. 187 + +, pl. 11, figs. 19-20. + + + +Caucasina elongata +(d’Orbigny) + +- Loeblich & Tappan, 1964, p. 82, pl. 2, figs. 14-15. + + + + + +Bulimina elongata elongata +d’Orbigny + +- Didkowski & Satanovskaja, 1970, p. 129, pl. 77, fig. 2. + + + + + + +Baggatella elongata +(d’Orbigny) + +- + +Popescu, 1975 +, p. 71 + +, pl. 49, fig. 1. + + + +Stratigraphical distribution in samples: +Rupelian- Chattian. + + + + \ No newline at end of file diff --git a/data/B1/49/43/B1494322925B8E7EFC74C7E39F38FE36.xml b/data/B1/49/43/B1494322925B8E7EFC74C7E39F38FE36.xml new file mode 100644 index 00000000000..ef03f7ba0ee --- /dev/null +++ b/data/B1/49/43/B1494322925B8E7EFC74C7E39F38FE36.xml @@ -0,0 +1,82 @@ + + + +Taxonomic Record Of The Oligocene Benthic Foraminifera From The Vima Formation (Transylvanian Basin, Romania) + + + +Author + +Székely, Szabolcs-Flavius +BabeȘ-Bolyai University, Department of Geology, Str. Kogălniceanu 1, 400084, Cluj Napoca, Romania, szekelyflavius @ gmail. com, sorin. filipescu @ ubbcluj. ro +szekelyflavius@gmail.com + + + +Author + +Introduction, Sorin Filipescu + +text + + +Acta Palaeontologica Romaniae + + +2015 + +2015-08-26 + + +11 + + +1 + + +25 +62 + + + +journal article +10.5281/zenodo.13190119 +1842-371x +13190119 + + + + + + +Bulimina alazanensis +Cushman, 1927b + + + + + + +Fig. 12.10 + + + + + + + +Bulimina alazanensis +Cushman, 1927b +, p. 161 + + +, pl. 25, fig. 4 + + + +Stratigraphical distribution in samples: +Rupelian. + + + + \ No newline at end of file diff --git a/data/B1/49/43/B1494322925B8E7EFC76C45A99CAFBD6.xml b/data/B1/49/43/B1494322925B8E7EFC76C45A99CAFBD6.xml new file mode 100644 index 00000000000..a1f0f7b177e --- /dev/null +++ b/data/B1/49/43/B1494322925B8E7EFC76C45A99CAFBD6.xml @@ -0,0 +1,104 @@ + + + +Taxonomic Record Of The Oligocene Benthic Foraminifera From The Vima Formation (Transylvanian Basin, Romania) + + + +Author + +Székely, Szabolcs-Flavius +BabeȘ-Bolyai University, Department of Geology, Str. Kogălniceanu 1, 400084, Cluj Napoca, Romania, szekelyflavius @ gmail. com, sorin. filipescu @ ubbcluj. ro +szekelyflavius@gmail.com + + + +Author + +Introduction, Sorin Filipescu + +text + + +Acta Palaeontologica Romaniae + + +2015 + +2015-08-26 + + +11 + + +1 + + +25 +62 + + + +journal article +10.5281/zenodo.13190119 +1842-371x +13190119 + + + + + + +Bulimina coprolithoides +Andreae, 1884 + + + + + + +Figs. 12.1 +a-b, 12.8 + + + + + + + +Bulimina coprolithoides +Andreae, 1884 +, p. 305 + + +, pl. 6, fig. 4. + + + + +Caucasina coprolithoides +(Andreae) + +- Le Calvez, 1966, p. 408, pl. 1, figs. 7-8. + + + + +Bulimina coprolithoides +Andreae + +- + +Cicha et al., 1998 +, p. 86 + +, pl. 47, fig. 1. + + + +Stratigraphical distribution in samples: +Rupelian- Chattian. + + + + \ No newline at end of file diff --git a/data/B1/49/43/B1494322925B8E7EFC89C13A99CAF834.xml b/data/B1/49/43/B1494322925B8E7EFC89C13A99CAF834.xml new file mode 100644 index 00000000000..938060feed1 --- /dev/null +++ b/data/B1/49/43/B1494322925B8E7EFC89C13A99CAF834.xml @@ -0,0 +1,117 @@ + + + +Taxonomic Record Of The Oligocene Benthic Foraminifera From The Vima Formation (Transylvanian Basin, Romania) + + + +Author + +Székely, Szabolcs-Flavius +BabeȘ-Bolyai University, Department of Geology, Str. Kogălniceanu 1, 400084, Cluj Napoca, Romania, szekelyflavius @ gmail. com, sorin. filipescu @ ubbcluj. ro +szekelyflavius@gmail.com + + + +Author + +Introduction, Sorin Filipescu + +text + + +Acta Palaeontologica Romaniae + + +2015 + +2015-08-26 + + +11 + + +1 + + +25 +62 + + + +journal article +10.5281/zenodo.13190119 +1842-371x +13190119 + + + + + + +Bulimina schischkinskayae +Samoylova, 1947 + + + + + + +Fig. 12.9 + + + + + + + +Bulimina schischkinskye +Samoylova, 1947 +, p. 82 + + +, pl. 10 (fide Ellis & Messina). + + + + +Caucasina schischkinskayae +(Samoylova) + +- Khalilov, 1958, p. 4. + + + + +Baggatella schischkinskayae +(Samoylova) + +- + +Popescu & Iva, 1971 +, p. 43 + +, pl. 11, figs. 1-5. + + + + + +Bulimina schischkinskayae +Samoylova + +- + +Cicha et al., 1998 +, p. 87 + +, pl. 47, figs. 2-4. + + + +Stratigraphical distribution in samples: +Rupelian- Chattian. + + + + \ No newline at end of file diff --git a/data/B1/49/43/B1494322925B8E7EFC9CC6AB99CAFDDF.xml b/data/B1/49/43/B1494322925B8E7EFC9CC6AB99CAFDDF.xml new file mode 100644 index 00000000000..d1397c44967 --- /dev/null +++ b/data/B1/49/43/B1494322925B8E7EFC9CC6AB99CAFDDF.xml @@ -0,0 +1,83 @@ + + + +Taxonomic Record Of The Oligocene Benthic Foraminifera From The Vima Formation (Transylvanian Basin, Romania) + + + +Author + +Székely, Szabolcs-Flavius +BabeȘ-Bolyai University, Department of Geology, Str. Kogălniceanu 1, 400084, Cluj Napoca, Romania, szekelyflavius @ gmail. com, sorin. filipescu @ ubbcluj. ro +szekelyflavius@gmail.com + + + +Author + +Introduction, Sorin Filipescu + +text + + +Acta Palaeontologica Romaniae + + +2015 + +2015-08-26 + + +11 + + +1 + + +25 +62 + + + +journal article +10.5281/zenodo.13190119 +1842-371x +13190119 + + + + + + +Bulimina alsatica +Cushman & Parker, 1937 + + + + + + +Figs. 12.6 +a-b, 12.7 + + + + + + + +Bulimina alsatica +Cushman & Parker, 1937 +, p. 39 + + +, pl. 4, figs. 6-7. + + + +Stratigraphical distribution in samples: +Rupelian- Chattian. + + + + \ No newline at end of file diff --git a/data/B1/49/43/B1494322925B8E7EFEEAC3D59AA0FADC.xml b/data/B1/49/43/B1494322925B8E7EFEEAC3D59AA0FADC.xml new file mode 100644 index 00000000000..146bc338348 --- /dev/null +++ b/data/B1/49/43/B1494322925B8E7EFEEAC3D59AA0FADC.xml @@ -0,0 +1,81 @@ + + + +Taxonomic Record Of The Oligocene Benthic Foraminifera From The Vima Formation (Transylvanian Basin, Romania) + + + +Author + +Székely, Szabolcs-Flavius +BabeȘ-Bolyai University, Department of Geology, Str. Kogălniceanu 1, 400084, Cluj Napoca, Romania, szekelyflavius @ gmail. com, sorin. filipescu @ ubbcluj. ro +szekelyflavius@gmail.com + + + +Author + +Introduction, Sorin Filipescu + +text + + +Acta Palaeontologica Romaniae + + +2015 + +2015-08-26 + + +11 + + +1 + + +25 +62 + + + +journal article +10.5281/zenodo.13190119 +1842-371x +13190119 + + + + + + +Cassidulinoides bodeni +Hagn, 1952 + + + + + + +Fig. 11.13 +a-b + + + + + + + +Cassidulinoides bodeni +Hagn, 1952 +, p. 181 + + +, pl. 2, fig. 12. +Stratigraphical distribution in samples: +Rupelian- Chattian. + + + + + \ No newline at end of file diff --git a/data/B1/49/43/B1494322925B8E7EFF03C2DE9AA0F96C.xml b/data/B1/49/43/B1494322925B8E7EFF03C2DE9AA0F96C.xml new file mode 100644 index 00000000000..e279ad78e69 --- /dev/null +++ b/data/B1/49/43/B1494322925B8E7EFF03C2DE9AA0F96C.xml @@ -0,0 +1,112 @@ + + + +Taxonomic Record Of The Oligocene Benthic Foraminifera From The Vima Formation (Transylvanian Basin, Romania) + + + +Author + +Székely, Szabolcs-Flavius +BabeȘ-Bolyai University, Department of Geology, Str. Kogălniceanu 1, 400084, Cluj Napoca, Romania, szekelyflavius @ gmail. com, sorin. filipescu @ ubbcluj. ro +szekelyflavius@gmail.com + + + +Author + +Introduction, Sorin Filipescu + +text + + +Acta Palaeontologica Romaniae + + +2015 + +2015-08-26 + + +11 + + +1 + + +25 +62 + + + +journal article +10.5281/zenodo.13190119 +1842-371x +13190119 + + + + + + +Globocassidulina globosa +( +Hantken, 1875 +) + + + + + + +Fig. 11.16 + + + + + + + +Cassidulina globosa +Hantken, 1875 +, p. 54 + + +, pl. 16, fig. 2. + + + + + +Globocassidulina globosa +(Hantken) + +- + +Popescu & Iva, 1971 +, p. 12 + +, pl. 7, figs. 2-3. + + + + + +Globocassidulina globosa +(Hantken) + +- + +Cicha et al., 1998 +, p. 102 + +, pl. 45, figs. 12-14. + + + +Stratigraphical distribution in samples: +Rupelian- Chattian. + + + + \ No newline at end of file diff --git a/data/B1/49/43/B1494322925B8E7EFF38C1ED9AA0F858.xml b/data/B1/49/43/B1494322925B8E7EFF38C1ED9AA0F858.xml new file mode 100644 index 00000000000..d8998d6c1d3 --- /dev/null +++ b/data/B1/49/43/B1494322925B8E7EFF38C1ED9AA0F858.xml @@ -0,0 +1,95 @@ + + + +Taxonomic Record Of The Oligocene Benthic Foraminifera From The Vima Formation (Transylvanian Basin, Romania) + + + +Author + +Székely, Szabolcs-Flavius +BabeȘ-Bolyai University, Department of Geology, Str. Kogălniceanu 1, 400084, Cluj Napoca, Romania, szekelyflavius @ gmail. com, sorin. filipescu @ ubbcluj. ro +szekelyflavius@gmail.com + + + +Author + +Introduction, Sorin Filipescu + +text + + +Acta Palaeontologica Romaniae + + +2015 + +2015-08-26 + + +11 + + +1 + + +25 +62 + + + +journal article +10.5281/zenodo.13190119 +1842-371x +13190119 + + + + + + +Globocassidulina subglobosa +( +Brady, 1881 +) + + + + + + +Fig. 11.14 + + + + + + + +Cassidulina subglobosa +Brady, 1881 +, p. 60 + + +, pl. 54, fig. 17a-c. + + + + +Globocassidulina subglobosa +(Brady) + +- +Sztrákos, 1979 +, pl. 27, fig. 16. + + + + +Stratigraphical distribution in samples: +Rupelian- Chattian. + + + + \ No newline at end of file diff --git a/data/B1/49/43/B1494322925D8E78FC49C2F999CAF929.xml b/data/B1/49/43/B1494322925D8E78FC49C2F999CAF929.xml new file mode 100644 index 00000000000..9f54a661825 --- /dev/null +++ b/data/B1/49/43/B1494322925D8E78FC49C2F999CAF929.xml @@ -0,0 +1,83 @@ + + + +Taxonomic Record Of The Oligocene Benthic Foraminifera From The Vima Formation (Transylvanian Basin, Romania) + + + +Author + +Székely, Szabolcs-Flavius +BabeȘ-Bolyai University, Department of Geology, Str. Kogălniceanu 1, 400084, Cluj Napoca, Romania, szekelyflavius @ gmail. com, sorin. filipescu @ ubbcluj. ro +szekelyflavius@gmail.com + + + +Author + +Introduction, Sorin Filipescu + +text + + +Acta Palaeontologica Romaniae + + +2015 + +2015-08-26 + + +11 + + +1 + + +25 +62 + + + +journal article +10.5281/zenodo.13190119 +1842-371x +13190119 + + + + + + +Saracenaria senni +Hedberg, 1937 + + + + + + +Fig. 8.12 +a-b + + + + + + + +Saracenaria senni +Hedberg, 1937 +, p. 674 + + +, pl. 90, fig. 18ab. + + + +Stratigraphical distribution in samples: +Rupelian- Chattian. + + + + \ No newline at end of file diff --git a/data/B1/49/43/B1494322925F8E7AFC4AC3AA99CAFA3D.xml b/data/B1/49/43/B1494322925F8E7AFC4AC3AA99CAFA3D.xml new file mode 100644 index 00000000000..d211ff16d87 --- /dev/null +++ b/data/B1/49/43/B1494322925F8E7AFC4AC3AA99CAFA3D.xml @@ -0,0 +1,93 @@ + + + +Taxonomic Record Of The Oligocene Benthic Foraminifera From The Vima Formation (Transylvanian Basin, Romania) + + + +Author + +Székely, Szabolcs-Flavius +BabeȘ-Bolyai University, Department of Geology, Str. Kogălniceanu 1, 400084, Cluj Napoca, Romania, szekelyflavius @ gmail. com, sorin. filipescu @ ubbcluj. ro +szekelyflavius@gmail.com + + + +Author + +Introduction, Sorin Filipescu + +text + + +Acta Palaeontologica Romaniae + + +2015 + +2015-08-26 + + +11 + + +1 + + +25 +62 + + + +journal article +10.5281/zenodo.13190119 +1842-371x +13190119 + + + + + + +Lagena tenuis +( +Bornemann, 1855 +) + + + + + + +Fig. 10.3 + + + + + + + +Ovulina tenuis +Bornemann, 1855 +, p. 317 + + +, pl. 12, fig. 3. + + + + +Lagena tenuis +(Bornemann) + +- Reuss, 1862, p. 325, pl. 3, figs. 30-39. + + + + +Stratigraphical distribution in samples: +Rupelian- Chattian. + + + + \ No newline at end of file diff --git a/data/B1/49/43/B1494322925F8E7AFF1DC2319AA1F9EB.xml b/data/B1/49/43/B1494322925F8E7AFF1DC2319AA1F9EB.xml new file mode 100644 index 00000000000..fe1b16d67eb --- /dev/null +++ b/data/B1/49/43/B1494322925F8E7AFF1DC2319AA1F9EB.xml @@ -0,0 +1,111 @@ + + + +Taxonomic Record Of The Oligocene Benthic Foraminifera From The Vima Formation (Transylvanian Basin, Romania) + + + +Author + +Székely, Szabolcs-Flavius +BabeȘ-Bolyai University, Department of Geology, Str. Kogălniceanu 1, 400084, Cluj Napoca, Romania, szekelyflavius @ gmail. com, sorin. filipescu @ ubbcluj. ro +szekelyflavius@gmail.com + + + +Author + +Introduction, Sorin Filipescu + +text + + +Acta Palaeontologica Romaniae + + +2015 + +2015-08-26 + + +11 + + +1 + + +25 +62 + + + +journal article +10.5281/zenodo.13190119 +1842-371x +13190119 + + + + + + +Hemirobulina hantkeni +( +Bandy, 1949 +) + + + + + + +Fig. 9.11 +a-b + + + + + + + +Marginulina subbullata +Hantken, 1875 +, p. 46 + + +, pl. 4, figs. 9-10, pl. 5, fig. 9. + + + + + + +Marginulina hantkeni +Bandy, 1949 +, p. 46 + + +, pl. 6, fig. 9 (fide Ellis & Messina). + + + + + +Hemirobulina hantkeni +(Bandy) + +- + +Cicha et al., 1998 +, p. 107 + +, pl. 25, figs. 9-10. + + + +Stratigraphical distribution in samples: +Rupelian- Chattian. + + + + \ No newline at end of file diff --git a/data/D6/47/B8/D647B8442F004401FCECC6FCFDA0FF48.xml b/data/D6/47/B8/D647B8442F004401FCECC6FCFDA0FF48.xml new file mode 100644 index 00000000000..5abeb148544 --- /dev/null +++ b/data/D6/47/B8/D647B8442F004401FCECC6FCFDA0FF48.xml @@ -0,0 +1,220 @@ + + + +Micropaleontological Study Of The Gura Beliei Red Marls Formation From The Pietroșița Area (Turonian - Maastrichtian). Part Iii Campanian-Maastrichtian Planktonic Foraminifera + + + +Author + +Neagu, Theodor + +text + + +Acta Palaeontologica Romaniae + + +2016 + +2016-12-27 + + +12 + + +2 + + +67 +91 + + + +journal article +1842-371x + + + + + + +Rugoglobigerina subbotinae +Maslakova 1978 + + + + + + +Figs. 1 +: 1-3, 7-15; +Figs. 2 +: 4-9; +Figs. 4 +: 1-9 + + +1953 + +Rotundina ordinaria +Subbotina + +, p.116, pl.3, fig.6 1978 + +Rugoglobigerina subbontinae +Maslakova + +, p.110, pl.26, fig.2 + + +Dimensions: D = 0,36- +0,29 mm +; d = 0,31- +0,24 mm +; g = 0,17- +0,15 mm + +Remarks: By the globular chambers well compressed with a low trochospire, the shell come out planspiral; by this aspect the species is well delimited as Maslakova show in the pl. 26, fig.2. + + +Fig. 12: 1-3 + +Gansserina gansseri +( +Bolli 1951 +) + +, Maastrichtian, Țâța Valley, PietroȘița, LPB. IV. 12442; +4-6 + +Gansserina wiedenmayeri +( +Gandolfi 1955 +) + +, Maastrichtian, Țâța Valley, PietroȘița, LPB. IV. 12431; +7-9 + +Rugotruncana subglaessneri +( +Gandolfi 1955 +) + +, Maastrichtian, Țâța Valley, PietroȘița, LPB. IV. 12421; +10-16 + +Abatomphalus mayaroensis +( +Bolli 1951 +) + +, Maastrichtian, Țâța Valley, PietroȘița, LPB. IV. 12433; +17-19 + +Globotruncanella havanensis +(VOORWJIK 1937) emend. Brönnimann & Brown 1955 + +, Maastrichtian, Țâța Valley, PietroȘița, L.P.B. VI. 12429 (All specimens x 90). + + + + +Fig. 13: 1-3 + +Rugotruncana subpennyi +( +Gandolfi 1955 +) + +, Maastrichtian, Țâța Valley, PietroȘița, LPB.IV.12426; +4-6 + +Rugotruncana subhexacamerata +( +Gandolfi 1955 +) + +, Maastrichtian, Țâța Valley, PietroȘița, LPB.IV.12422; +7-12 + +Archaeoglobigerina blowi +Pessagno 1967 + +, Maastrichtian, Țâța Valley, PietroȘița, LPB.IV.12441; 13-15 + +Globotruncanella pshadae +(KELLER 1946) + +, Maastrichtian, Țâța Valley, PietroȘița, LPB.IV.12427; +16-18 + +Rugoglobigerina kelleri +( +Subbotina 1953 +) + +, Maastrichtian, Țâța Valley, PietroȘița, LPB.IV.12451; +19-26 + +Globotruncanella sarmientoi +( +Gandolfi 1955 +) + +, Maastrichtian, Țâța Valley, PietroȘița, LPB.IV.12448 + +(All specimens x 90). + + + +Fig. 14: 1-3 + +Globotruncanella sarmientoi +( +Gandolfi 1955 +) + +, Maastrichtian, Țâța Valley, PietroȘița, LPB.IV.12448; +4-12 + +Archaeoglobigerina blowi +( +Pessagno 1967 +) + +, Maastrichtian, Țâța Valley, PietroȘița, LPB.IV.12449; +13-15 + +Rugoglobigerina pustulata +Brönnimann 1952 + +, Maastrichtian, Țâța Valley, PietroȘița, LPB.IV.12415; +16-24 + +Rugoglobigerina ordinaria +( +Subbotina 1953 +) + +, Maastrichtian, Țâța Valley, PietroȘița, LPB.IV.12446; +25-29 + +Rugoglobigrerina kelleri + +( +Subbotina 1953 +Maastrichtian, Țâța Valley, PietroȘița, LPB.IV.12451; +30-31 + +Rugoglobigerina rotundata +Brönnimann 1952 +Maastrichtian + +, Țâța Valley, PietroȘița, LPB.IV.12416 (All specimens x 90). + + +Occurrences: Țâța Valley, Pietrosița- Fieni area Stratigraphic distribution: Upper Maastrichtian Specimens: LPB.IV. 12446, 12419, 12411 + + + \ No newline at end of file diff --git a/data/D6/47/B8/D647B8442F00441DFC18C2E3FBB2FB13.xml b/data/D6/47/B8/D647B8442F00441DFC18C2E3FBB2FB13.xml new file mode 100644 index 00000000000..22426ceb704 --- /dev/null +++ b/data/D6/47/B8/D647B8442F00441DFC18C2E3FBB2FB13.xml @@ -0,0 +1,97 @@ + + + +Micropaleontological Study Of The Gura Beliei Red Marls Formation From The Pietroșița Area (Turonian - Maastrichtian). Part Iii Campanian-Maastrichtian Planktonic Foraminifera + + + +Author + +Neagu, Theodor + +text + + +Acta Palaeontologica Romaniae + + +2016 + +2016-12-27 + + +12 + + +2 + + +67 +91 + + + +journal article +1842-371x + + + + + + +Rugoglobigerina kelleri +( +Subbotina 1953 +) + + + + + + +Figs. 5 +: 7-9; +Figs. 6 +: 22-24; +Figs. 8 +:13-18; +Figs. 13 +:16-18; + + +Figs. 14 +: 25-29 + + +1953 + +Globigerina kelleri +Subbotina + +, p.54, pl.1, fig.16 1978 + +Rugoglobigerina kelleri +(Subbotina) Maslakova + +, p.112, pl.26, fig.5 + + +Dimensions: D = +0,26-0,42 mm +; d = +0,24-0,36 mm +; g = +0,16-0,28 mm + + +Remarks: The high trochospiral side with globular 5 to 6 chambers, a large umbilical-axial area and the typical ornamentation-especial radial costellae - this species differs from + +Rugoglobigerina rugosa rugossa +Brönnimann + +text-figs.12-13. + +Occurrences: Țâța Valley, Pietrosița- Fieni area Stratigraphic distribution: Upper Maastrichtian Specimens: LPB.IV.12451 + + + \ No newline at end of file diff --git a/data/D6/47/B8/D647B8442F00441DFC3AC0D8FBABFD3B.xml b/data/D6/47/B8/D647B8442F00441DFC3AC0D8FBABFD3B.xml new file mode 100644 index 00000000000..9b845e38194 --- /dev/null +++ b/data/D6/47/B8/D647B8442F00441DFC3AC0D8FBABFD3B.xml @@ -0,0 +1,75 @@ + + + +Micropaleontological Study Of The Gura Beliei Red Marls Formation From The Pietroșița Area (Turonian - Maastrichtian). Part Iii Campanian-Maastrichtian Planktonic Foraminifera + + + +Author + +Neagu, Theodor + +text + + +Acta Palaeontologica Romaniae + + +2016 + +2016-12-27 + + +12 + + +2 + + +67 +91 + + + +journal article +1842-371x + + + + + + +Rugoglobigerina kingi +Trujillo 1960 + + + + + + +Figs. 2 +: 10-12; +Figs. 15 +: 25-27 + + +1978 + +Rugoglobigerina kingi +Trujillo, Maslakova + +, p.111, pl.26, fig. 3 + + +Dimensions: D = +0,34-0,38 mm +; d = +0,31-0,36 mm +; g = +0,20-0,21mm + +Remarks: Specimens from the Țâța Valley with very low trochospiral aspect close to planispiral of the spiral side, by the globular chambers with a radial disposition of the costellae, differs from Maslakova's specimens; from the Marianos & Zingula specimens pl.38, fig.6 differs also by the ornamentation. +Occurrences: Țâța Valley, Pietrosița- Fieni area Stratigraphic distribution: Upper Maastrichtian Specimens: LPB.IV. 12450 + + + \ No newline at end of file diff --git a/data/D6/47/B8/D647B8442F00441DFCEBC48AFBB2F92E.xml b/data/D6/47/B8/D647B8442F00441DFCEBC48AFBB2F92E.xml new file mode 100644 index 00000000000..2c2b63a911d --- /dev/null +++ b/data/D6/47/B8/D647B8442F00441DFCEBC48AFBB2F92E.xml @@ -0,0 +1,93 @@ + + + +Micropaleontological Study Of The Gura Beliei Red Marls Formation From The Pietroșița Area (Turonian - Maastrichtian). Part Iii Campanian-Maastrichtian Planktonic Foraminifera + + + +Author + +Neagu, Theodor + +text + + +Acta Palaeontologica Romaniae + + +2016 + +2016-12-27 + + +12 + + +2 + + +67 +91 + + + +journal article +1842-371x + + + + + + +Rugoglobigerina ordinaria +( +Subbotina 1953 +) + + + + + + +Figs. 2 +: 13-15; +Figs. 6 +: 1-3; +Figs. 14 +: 16-24 + + +1953 + +Rotundina ordinaria +Subbotina + +, p.166, pl.3, fig.3, pl.4, figs. 1, 6 + + +1978 + +Rugoglobigerina ordinaria +(Subbotina) Maslakova + +, p.111, pl.26, fig.4 + + +Dimensions: D = +0,36-0,42 mm +; d = +0,24-0,38 mm +; g = +0,19-0,21mm + + +Remarks: With a moderate to low trochospiral side, with globular chambers, 4 to 5 on the last whorl this species differs from + +R. kelleri + +. + +Occurrences: Țâța Valley, Pietrosița- Fieni area Stratigraphic distribution: Upper Maastrichtian Specimens: LPB.IV.12446 + + + \ No newline at end of file diff --git a/data/D6/47/B8/D647B8442F00441DFF21C0D8FE40FD1A.xml b/data/D6/47/B8/D647B8442F00441DFF21C0D8FE40FD1A.xml new file mode 100644 index 00000000000..78859942cc9 --- /dev/null +++ b/data/D6/47/B8/D647B8442F00441DFF21C0D8FE40FD1A.xml @@ -0,0 +1,81 @@ + + + +Micropaleontological Study Of The Gura Beliei Red Marls Formation From The Pietroșița Area (Turonian - Maastrichtian). Part Iii Campanian-Maastrichtian Planktonic Foraminifera + + + +Author + +Neagu, Theodor + +text + + +Acta Palaeontologica Romaniae + + +2016 + +2016-12-27 + + +12 + + +2 + + +67 +91 + + + +journal article +1842-371x + + + + + + +Rugoglobigerina macrocephala +Brönnimann 1952 + + + + + + +Fig. 1 +: 4; +Figs. 5 +: 10-12, 27-29 + + +1952 + +Rugoglobigerina macrocephala macrocephala + + + +Brönnimann, p. 25, text-fig.9, pl.2, figs. +1-3 1955 + +Globotruncana (Rugoglobigerina) macrocephala macrocephala +(Brönnimann) Gandolfi + +, p.45, pl.2, + + +fig.12 Dimensions: D = 0,31- +0,26 mm +; d = 0,4- +0,26 mm +; g = +0,17 mm +. Remarks: The 4-5 globular chambers in the last whorl ornate by delicate rugositis or numerous fine continuous and discontinuous ridges or costellae, this species are well characterized. Occurrences: Țâța Valley, Pietrosița- Fieni area Stratigraphic distribution: Maastrichtian Specimens: LPB.IV. 12413 + + + + \ No newline at end of file diff --git a/data/D6/47/B8/D647B8442F00441DFF44C280FE40FC4B.xml b/data/D6/47/B8/D647B8442F00441DFF44C280FE40FC4B.xml new file mode 100644 index 00000000000..3a215f3d23b --- /dev/null +++ b/data/D6/47/B8/D647B8442F00441DFF44C280FE40FC4B.xml @@ -0,0 +1,78 @@ + + + +Micropaleontological Study Of The Gura Beliei Red Marls Formation From The Pietroșița Area (Turonian - Maastrichtian). Part Iii Campanian-Maastrichtian Planktonic Foraminifera + + + +Author + +Neagu, Theodor + +text + + +Acta Palaeontologica Romaniae + + +2016 + +2016-12-27 + + +12 + + +2 + + +67 +91 + + + +journal article +1842-371x + + + + + + +Rugoglobigerina pustulata +Brönnimann 1952 + + + + + + +Figs.5 +: 4-6; +Figs. 14 +: 13-15 + + +1952 + +Rugoglobigerina reicheli pustulata +Brönnimann + +, p.20, text-figs.6, 7, pl.2, figs.7-9 + + +Dimensions: D = 0,34- +0,31mm +; d = 0,26- +0,21 mm +; g = + + +0,19 mm + +Occurrences: Țâța Valley, Pietrosița- Fieni area +Stratigraphic distribution: Maastrichtian +Specimens: LPB.IV. 12415 + + + \ No newline at end of file diff --git a/data/D6/47/B8/D647B8442F00441DFF64C618FE40F7BE.xml b/data/D6/47/B8/D647B8442F00441DFF64C618FE40F7BE.xml new file mode 100644 index 00000000000..a24b5432ad1 --- /dev/null +++ b/data/D6/47/B8/D647B8442F00441DFF64C618FE40F7BE.xml @@ -0,0 +1,78 @@ + + + +Micropaleontological Study Of The Gura Beliei Red Marls Formation From The Pietroșița Area (Turonian - Maastrichtian). Part Iii Campanian-Maastrichtian Planktonic Foraminifera + + + +Author + +Neagu, Theodor + +text + + +Acta Palaeontologica Romaniae + + +2016 + +2016-12-27 + + +12 + + +2 + + +67 +91 + + + +journal article +1842-371x + + + + + + +Rugoglobigerina loetterli +( +Nauss 1947 +) + + + + + + +Figs. 5 +: 16-18 + + +1947 + +Globigerina loetterli +Nauss + +, p.336, pl.49, fig.11 1955 + +Globotruncana (Rugoglobigerina) loetterli loetterli +(Nauss) Gandolfi + +, p.35, pl.1, figs.15 a-c Dimensions: D = +0,31mm +; d = +0,24 mm +; g = +0,12 mm +Remarks: Specimens from Țâța Valley differs from Nauss's species by the ornamentations of the shell, represented by fine discontinuous costellae or trace of those and the absence of the peripheral keel. + +Occurrences: Țâța Valley, Pietrosița- Fieni area Stratigraphic distribution: Maastrichtian +Specimens: LPB.IV. 12443 + + + \ No newline at end of file diff --git a/data/D6/47/B8/D647B8442F00441DFF6DC453FE40F982.xml b/data/D6/47/B8/D647B8442F00441DFF6DC453FE40F982.xml new file mode 100644 index 00000000000..596e3cd9564 --- /dev/null +++ b/data/D6/47/B8/D647B8442F00441DFF6DC453FE40F982.xml @@ -0,0 +1,75 @@ + + + +Micropaleontological Study Of The Gura Beliei Red Marls Formation From The Pietroșița Area (Turonian - Maastrichtian). Part Iii Campanian-Maastrichtian Planktonic Foraminifera + + + +Author + +Neagu, Theodor + +text + + +Acta Palaeontologica Romaniae + + +2016 + +2016-12-27 + + +12 + + +2 + + +67 +91 + + + +journal article +1842-371x + + + + + + +Rugoglobigerina beldingi +Gandolfi 1955 + + + + + + +Figs. 6 +: 10-12 + + +1955 + +Globotruncana (Rugoglobigerina) beldingi +Gandolfi + +, p.31, text-fig. 4 a-c, pl.l, fig.8 Dimensions: D = +0,24-0,31mm +; d = +0,22-0,31mm +; g = +0,14 mm + + +Remarks: Gandolfi's description of this taxon is clear: " +Test nearly plan spiral, become somewhat involute on the dorsal (spiral) side.......five to six chambers in the last whorl, inflated......test smooth somewhat rough by tubercles, papillae are more frequent along the margin of the shell, on the early chambers along appear in two approximately parallel lines +" Our specimens corresponds to the Ganbdolfi's description. + +Occurrences: Țâța Valley, Pietrosița- Fieni area Stratigraphic distribution: Maastrichtian +Specimens: LPB.IV. 12419 + + + \ No newline at end of file diff --git a/data/D6/47/B8/D647B8442F044419FC1FC20FFBDAFC4B.xml b/data/D6/47/B8/D647B8442F044419FC1FC20FFBDAFC4B.xml new file mode 100644 index 00000000000..32493d7e849 --- /dev/null +++ b/data/D6/47/B8/D647B8442F044419FC1FC20FFBDAFC4B.xml @@ -0,0 +1,81 @@ + + + +Micropaleontological Study Of The Gura Beliei Red Marls Formation From The Pietroșița Area (Turonian - Maastrichtian). Part Iii Campanian-Maastrichtian Planktonic Foraminifera + + + +Author + +Neagu, Theodor + +text + + +Acta Palaeontologica Romaniae + + +2016 + +2016-12-27 + + +12 + + +2 + + +67 +91 + + + +journal article +1842-371x + + + + + + +Rugoglobigerina pennyi +Brönnimann 1952 + + + + + + +Figs. 2 +: 1-3; +Figs. 5 +:1-3 + + +1952 + +Rugoglobigerina rugosa pennyi +Brönnimann + +, p. 34, pl. 4, figs.1-3, text-fig. 16 + + +1955 + +Globotruncana (Rugoglobigerina) pennyi pennyi +(Brönnimann) Gandolfi + +, p. 73, pl. 7, fig.8 Dimensions: D = +0,34 mm +; d = +0,19 mm +; g = +0,12 mm +Remarks: By the typical ornamentation with radial costellae and a low trochospiral test, this species is well delimited. + +Occurrences: Țâța Valley, Pietrosița- Fieni area Stratigraphic distribution: Maastrichtian +Specimens: LPB.IV.12 + + + \ No newline at end of file diff --git a/data/D6/47/B8/D647B8442F044419FCEEC644FBB2F812.xml b/data/D6/47/B8/D647B8442F044419FCEEC644FBB2F812.xml new file mode 100644 index 00000000000..9b213670e3f --- /dev/null +++ b/data/D6/47/B8/D647B8442F044419FCEEC644FBB2F812.xml @@ -0,0 +1,81 @@ + + + +Micropaleontological Study Of The Gura Beliei Red Marls Formation From The Pietroșița Area (Turonian - Maastrichtian). Part Iii Campanian-Maastrichtian Planktonic Foraminifera + + + +Author + +Neagu, Theodor + +text + + +Acta Palaeontologica Romaniae + + +2016 + +2016-12-27 + + +12 + + +2 + + +67 +91 + + + +journal article +1842-371x + + + + + + +Rugoglobigerina rotundata +Brönnimann 1952 + + + + + + +Figs. 1 +: 5-6; +Figs. 14 +: 30-31 + + +1952 + +Rugoglobigerina rugosa rotundata +Brönnimann + +, p.34, text-figs.15-16, pl.4, fig.7 + + +1955 + +Globotruncana (Rugoglobigerina) rotundata rotundata +(Brönnimann) Gandolfi + +, p.70, pl.7, fig. 2 Dimensions: D = +0,26 mm +; d = +0,21mm +; g = +0,20 mm +Remarks: By the ball aspect of the test with globular chambers, ornate by radial costellae, this species is obvious delimited. + +Occurrences: Țâța Valley, Pietrosița- Fieni area Stratigraphic distribution: Maastrichtian +Specimens: LPB.IV.12416 + + + \ No newline at end of file diff --git a/data/D6/47/B8/D647B8442F044419FF70C31BFE37FA66.xml b/data/D6/47/B8/D647B8442F044419FF70C31BFE37FA66.xml new file mode 100644 index 00000000000..ee84e0b7695 --- /dev/null +++ b/data/D6/47/B8/D647B8442F044419FF70C31BFE37FA66.xml @@ -0,0 +1,94 @@ + + + +Micropaleontological Study Of The Gura Beliei Red Marls Formation From The Pietroșița Area (Turonian - Maastrichtian). Part Iii Campanian-Maastrichtian Planktonic Foraminifera + + + +Author + +Neagu, Theodor + +text + + +Acta Palaeontologica Romaniae + + +2016 + +2016-12-27 + + +12 + + +2 + + +67 +91 + + + +journal article +1842-371x + + + + + + +Archaeoglobigerina blowi +Pessagno 1967 + + + + + + +Figs. 4 +: 25-30; +Figs. 8 +: 7-9: +Figs. 13 +: 7-12; +Figs. 14 +: 4-12 + + +1967 + +Archaeoglobigerina blowi +Pessagno + +, pl. 316, pl. 59, figs. 1-10 + + +Dimensions: D = 0,39- +0,34 mm +; d = 0,29- +0,24 mm +; g = 0,17- +0,14 mm + + +Remarks: Specimens from the Maastrichtian of Țâța Valley correspond with Pesanno's species: " + +Test trochoid, lobulat periphrerally; chambers spheroidal.....umbilicus medium sized....periphery occasionally with weakly double keel....the surface smooth through or somewhat rugose on the early chambers.... +A.blowi +is closely relat- ed to +A. cretacea (d'Orbigny) +. It differs from the latter species by possessing a more spherical and inflated chambers and by having a markedly lobulated periphery...."\ + +in the Pessagno's opinion this taxon gave rise to + +Rugoglobigerina rugosa + +. + +Occurrences: Țâța Valley, Pietrosița- Fieni area Stratigraphic distribution: Maastrichtian +Specimens: L.P.B.IV. 12449 + + + \ No newline at end of file diff --git a/data/D6/47/B8/D647B8442F044419FF71C665FE4BF7BE.xml b/data/D6/47/B8/D647B8442F044419FF71C665FE4BF7BE.xml new file mode 100644 index 00000000000..bcd7edadd21 --- /dev/null +++ b/data/D6/47/B8/D647B8442F044419FF71C665FE4BF7BE.xml @@ -0,0 +1,88 @@ + + + +Micropaleontological Study Of The Gura Beliei Red Marls Formation From The Pietroșița Area (Turonian - Maastrichtian). Part Iii Campanian-Maastrichtian Planktonic Foraminifera + + + +Author + +Neagu, Theodor + +text + + +Acta Palaeontologica Romaniae + + +2016 + +2016-12-27 + + +12 + + +2 + + +67 +91 + + + +journal article +1842-371x + + + + + + +Rugoglobigerina rugosa +( +Plummer 1926 +) + + + + + + +Figs. 7 +: 7-9 + + +1926 + +Globigrerina rugosa +Plummer + +, p.38, pl.12, fig.10 1952 + +Rugoglobigerina rugosa rugosa +(Plumer) Brönnimann + +, p. 28, text-figs.11, 12, 13 + + +1955 + +Globotruncana (Rugoglobigerina) rugosa rugosa +(Plammer) Gandolfi + +, p. 72, +Fig.6 +, text-fig.11c Dimensions: D = 0,43-0,39- +0,31 mm +; d = 0,40-0,31- +0,29 mm +; g = 0,24-0,21- +0,09 mm + +Remarks: By theirs features our specimens correspond very well with the Broniman’s specimens. +Occurrences: Țâța Valley, Pietrosița- Fieni area Stratigraphic distribution: Upper Campanian (calcarata biozone) - Maastrichtian +Specimens: LPB.IV.12411 + + + \ No newline at end of file diff --git a/data/D6/47/B8/D647B8442F084415FC1FC347FBABFA3A.xml b/data/D6/47/B8/D647B8442F084415FC1FC347FBABFA3A.xml new file mode 100644 index 00000000000..abf316316cf --- /dev/null +++ b/data/D6/47/B8/D647B8442F084415FC1FC347FBABFA3A.xml @@ -0,0 +1,107 @@ + + + +Micropaleontological Study Of The Gura Beliei Red Marls Formation From The Pietroșița Area (Turonian - Maastrichtian). Part Iii Campanian-Maastrichtian Planktonic Foraminifera + + + +Author + +Neagu, Theodor + +text + + +Acta Palaeontologica Romaniae + + +2016 + +2016-12-27 + + +12 + + +2 + + +67 +91 + + + +journal article +1842-371x + + + + + + +Abatomphalus mayaroensis +(BOLLI) 1951 + + + + + + +Figs. 12 +: 10-16 + + +1951 + +Globotruncana mayaroensis +Bolli + +, p.198, pl.35, figs.10-12 + + +1955 + +Rugotruncana mayaroensis +(Bolli) Brönnimann & Brown + +, p.553, pl.22, figs.10-12 + + +1957 + +Abatomphalus mayaroensis +(Bolli) Bolli + +, p.53, pl.1, fig.1 + + +Dimensions: D = 0,62- +0,53 mm +; d = 0,60- +0,43 mm +; g = + + +0,21- +0,14 mm + +Remarks: By its particularly features of the test, this species (among the last planktonic species before the biggest biologic crisis between the Mesozoic and Neozoic times, +represented in Oceanic Seas life in parallel of the Land. + +After the biozone with + +A. mayaroensis + +start the new life of the Neozoic planktonic foraminifera with the smallest + + +" +Glogiberina +". + +Occurrences: Țâța Valley, Pietrosița- Fieni area +Stratigraphic distribution: Upper Maastrichtian +Specimens: LPB.IV. 12433 + + + \ No newline at end of file diff --git a/data/D6/47/B8/D647B8442F084415FF46C364FE40F9CF.xml b/data/D6/47/B8/D647B8442F084415FF46C364FE40F9CF.xml new file mode 100644 index 00000000000..05b101bfea7 --- /dev/null +++ b/data/D6/47/B8/D647B8442F084415FF46C364FE40F9CF.xml @@ -0,0 +1,110 @@ + + + +Micropaleontological Study Of The Gura Beliei Red Marls Formation From The Pietroșița Area (Turonian - Maastrichtian). Part Iii Campanian-Maastrichtian Planktonic Foraminifera + + + +Author + +Neagu, Theodor + +text + + +Acta Palaeontologica Romaniae + + +2016 + +2016-12-27 + + +12 + + +2 + + +67 +91 + + + +journal article +1842-371x + + + + + + +Globotruncanella saratogensis +(Applin 1920) + + + + + + +Figs 3 +: 25-27; +Figs. 7 +: 16-18 + + +1920 + +Globigerina cretacea +d'Orbigny var. +saratogensis +Applin + +, p. 98, pl.3, fig.8. + + +Dimensions: D = +0,43-0,46 mm +; d = 0,36- +0,36 mm +; g = +0,19 mm + + +Remarks: In the paper of +Applin et al. (1925) +in the last part of this article were described few species of foraminifera. Some of these species belong to the Paleogen, but there are also two species from the Upper Cretaceous: + +Globigerina marginata +d'Orbigny + +and a new taxon + +Globigerina cretacea +var. +saratogensis + +( +Fig. 17 +: +1-6 in +the present paper). In the description of this new subspecies, +Applin et al. (1925 +, p. 98) pointed out the following features: " +chambers increasing gradually in size, sometime slightly carinated at the periphery (which is frail represented on the figure) wall smoothing. The regularity of coiling and the tendency for the form to develop a carinared rim +.".......Taking in consideration all the presented features, our specimens ( +Fig. 3 +: 25-27) corresponds with the Applin taxon. + + +By the inflated character of the chambers, spiral and umbilical, this species differs from Bolli's + +Praeglobotruncana coarctata + +1957. + +Occurrences: Țâța Valley, Pietrosița- Fieni area Stratigraphic distribution: Upper Maastrichtian. +Specimens: LPB.IV. 12441 + + + \ No newline at end of file diff --git a/data/D6/47/B8/D647B8442F084415FF46C6DEFBB2FD1A.xml b/data/D6/47/B8/D647B8442F084415FF46C6DEFBB2FD1A.xml new file mode 100644 index 00000000000..bf17d2e00a4 --- /dev/null +++ b/data/D6/47/B8/D647B8442F084415FF46C6DEFBB2FD1A.xml @@ -0,0 +1,102 @@ + + + +Micropaleontological Study Of The Gura Beliei Red Marls Formation From The Pietroșița Area (Turonian - Maastrichtian). Part Iii Campanian-Maastrichtian Planktonic Foraminifera + + + +Author + +Neagu, Theodor + +text + + +Acta Palaeontologica Romaniae + + +2016 + +2016-12-27 + + +12 + + +2 + + +67 +91 + + + +journal article +1842-371x + + + + + + +Globotruncanella sarmientoi +( +Gandolfi 1955 +) + + + + + + +Figs. 5 +: 15-27; +Figs. 13 +: 19-26; +Figs. 14 +: 1-3; +Figs. 15 +: 13-24 + + +1955 + +Globotruncana caliciformis ssp. sarmientoi +Gandolfi + +, p.47, pl.3, fig.3 a-c + + +Dimensions: D = 0,53- +0,43 mm +; d = 0,40- +0,36 mm +; g = 0,19- +0,17 mm + + +Remarks: The general aspect of the shell is specific to the genus + +Globotruncanella + +. +Gandolfi (1955 +, p. 48) mention: " + +This species is morphologically related to +Globorotalia pshadae Keller 1946 + +". In contrast with Kellerr's species, + +G. sarmientoi + +differs by the large size; the presence of a double keel from the peripheral margins of the early chambers (the peripheral keel) is represented by a row of muricae. The last chamber or the last two chambers present only one keel smooth not rugose as there are on the early chambers. Ordinary on the umbilical side the early chambers a strong to weak rouged aspect. From the Gandolfi's species ours specimens differs by the aspect of the spiral side, where the chambers have a moderate inflated and smooth aspect. From + +Globotruncanella havanensis + +(Vootwjik l937) emend. Brönnimann & Brown 1955, ours specimens differs by the presence of a double peripheral keel on the early chambers, the presence of a single smooth keel on the last two chambers and the moderate convex but not flat aspect of the spiral size. + +Occurrences: Țâța Valley, Pietrosița- Fieni area Stratigraphic distribution: Upper Maastrichtian Specimens: LPB.IV.12448 + + + \ No newline at end of file diff --git a/data/D6/47/B8/D647B8442F084415FF6DC15DFE40FD46.xml b/data/D6/47/B8/D647B8442F084415FF6DC15DFE40FD46.xml new file mode 100644 index 00000000000..26a9763e7b9 --- /dev/null +++ b/data/D6/47/B8/D647B8442F084415FF6DC15DFE40FD46.xml @@ -0,0 +1,88 @@ + + + +Micropaleontological Study Of The Gura Beliei Red Marls Formation From The Pietroșița Area (Turonian - Maastrichtian). Part Iii Campanian-Maastrichtian Planktonic Foraminifera + + + +Author + +Neagu, Theodor + +text + + +Acta Palaeontologica Romaniae + + +2016 + +2016-12-27 + + +12 + + +2 + + +67 +91 + + + +journal article +1842-371x + + + + + + +Globotruncanella coarctata +(Bolli 1957) + + + + + + +Figs. 3 +:1-9; +Figs. 8 +:1-3 + + +1957 + +Praeglobotruncana coarctata +Bolli + +, p.53, pl.12, fig. 2-3. + + +1978 + +Globotruncanella coarctata +(Bolli) Maslakova + +, p.106, pl.24, fig.4 + + +Dimensions: D = 0,36 - +0,29 mm +; d = 0,31- +0,26 mm +Remarks: Ours specimens differs from the Bolli's 1957 species by the more inflated chambers on the spiral side. The very faint keel and the minute spines of the umbilical chambers are tipical to the Bolli's species. + + +Occurrence: Țâța Valley, Pietrosița- Fieni area Stratigraphic distribution: Maastrichtian ( + +Abatomphalus mayaroensis + +biozone) + +Specimens: LPB.IV. 12437 + + + \ No newline at end of file diff --git a/data/D6/47/B8/D647B8442F0B4415FCFEC6FCFE37FF48.xml b/data/D6/47/B8/D647B8442F0B4415FCFEC6FCFE37FF48.xml new file mode 100644 index 00000000000..a233a5b68b4 --- /dev/null +++ b/data/D6/47/B8/D647B8442F0B4415FCFEC6FCFE37FF48.xml @@ -0,0 +1,175 @@ + + + +Micropaleontological Study Of The Gura Beliei Red Marls Formation From The Pietroșița Area (Turonian - Maastrichtian). Part Iii Campanian-Maastrichtian Planktonic Foraminifera + + + +Author + +Neagu, Theodor + +text + + +Acta Palaeontologica Romaniae + + +2016 + +2016-12-27 + + +12 + + +2 + + +67 +91 + + + +journal article +1842-371x + + + + + + +Globotruncanella subpetaloidea +( +Gandolfi 1955 +) + + + + + + +Figs. 1 +: 28-33 + + +1955 + +Globotruncana (Rugoglobigerina) petaloidea subpetaloidea +Gandolfi + +, p.52, text-fig. 8, pl.3, fig.12 a-c + + +Dimensions: D = +0,24-0,26 mm +; d= +0,21mm +. + + +Remarks: By its aspect of the chambers on spiral side and umbilical sides and by evident rough or spinose test on the umbilical and spiral sides of chambers thus species differs from + +Globotruncanella pshadae +Keller. + + + + +Fig. 4: 1-9 + +Rugoglobigerina subbotinae +Maslakova 1978 + +, Maastrichtian, Țâța Valley, PietroȘița, LPB.IV. 12446; +10-15 + +Globotruncanella havanensis +(Voorwjik 1937) + +, Maastrichtian, Țâța Valley, PietroȘița, LPB.IV. 12429; +16-21 + +Globotruncanella pshadae +(Keller 1946) + +, Maastrichtian, Țâța Valley, PietroȘița, L.P.B.IV.12427; +22-24 +, +31-36 + +Globotruncanella petaloidea +( +Gandolfi 1955 +) + +, Maastrichtian, Țâța Valley, PietroȘița, LPB.IV.12428; +25-30 + +Archaeoglobigerina blowi +Pessagno 1967 + +, Maastrichtian, Țâța Valley, PietroȘița, LPB.IV.12449 (All specimens x 90). + + + + +Fig. 5: 1-3 + +Rugoglobigerina pennyi +Brönnimann 1952 + +, Maastrichtian, Țâța Valley, PietroȘița, LPB.IV.12417; +4-6 + +Rugoglobigerina pustulata +Brönnimann 1952 + +, Maastrichtian, Țâța Valley, PietroȘița, L.P.B.IV.12415; +7-9 + +Rugoglobigerins kelleri +( +Subbotina 1953 +) + +, Maastrichtian, Țâța Valley, PietroȘița, L.P.B.IV.12451; +10-12 +, +27-29 + +Rugoglobigerina macrocephala +Brönnimann, Maastrichtian + +, Țâța Valley, PietroȘița, L.P.B.IV.12413; +13-15 +, +19-24 + +Rugotruncana ellissi +Brönnimann & Brown 1955 + +, Maastrichtian, Țâța Valley, PietroȘița, L.P.B.IV 12426; +16-18 + +Rugoglobigerina loetterli +( +Nauss 1947 +) + +, Maestrichtian, Maastrichtian, Țâța Valley, PietroȘița, L.P.B.IV.12443; +15-27 + +Globotruncanella sarmientoi +( +Gandolfi 1955 +) + +, Maastrichtian, Țâța Valley, PietroȘița LPB.12448 (All specimens x 90). + + +Occurrence: Țâța Valley, Pietrosița- Fieni area Stratigraphic distribution: Maastrichtian +Specimens: LPB.IV. 124542 + + + \ No newline at end of file diff --git a/data/D6/47/B8/D647B8442F0B4416FC12C4D4FBABF92E.xml b/data/D6/47/B8/D647B8442F0B4416FC12C4D4FBABF92E.xml new file mode 100644 index 00000000000..6cb473243a3 --- /dev/null +++ b/data/D6/47/B8/D647B8442F0B4416FC12C4D4FBABF92E.xml @@ -0,0 +1,87 @@ + + + +Micropaleontological Study Of The Gura Beliei Red Marls Formation From The Pietroșița Area (Turonian - Maastrichtian). Part Iii Campanian-Maastrichtian Planktonic Foraminifera + + + +Author + +Neagu, Theodor + +text + + +Acta Palaeontologica Romaniae + + +2016 + +2016-12-27 + + +12 + + +2 + + +67 +91 + + + +journal article +1842-371x + + + + + + +Globotruncanella pshadae +(Keller 1946) + + + + + + +Figs. 3 +: 10-17, +Figs 4 +: 16-21; +Figs. 9 +: 10-12; +Figs. 13 +: 13- 15 + + +1946 + +Globorotalia pshadae +Keller + +(from Subbotina l953) p. 204, pl.16, fig.1-6 (fig.2a-c hollotype) Dimensions: D = +0,31-0,34 mm +; d = +0,29-0,31mm +; g = +0,34 mm +- +0,29 mm + + +Remarks: The Keller's original specimens are restudied and figured by Subbotina l953, p.204, pl.16, fig.1-6; fig.1=hyolotype; fig.2 = +paratype +of Keller 1946. In the requirement of the ICZN Keller's species has priority and Bolli's + +Globotruncana citae + +1951 plate 35, fig.4-6 become junior synonymous. + +Occurrence: Țâța Valley, Pietrosița- Fieni area Stratigraphic distribution: Maastrichtian +Specimens: LPB.IV. 12427 + + + \ No newline at end of file diff --git a/data/D6/47/B8/D647B8442F0B4416FCE8C248FBABFBD6.xml b/data/D6/47/B8/D647B8442F0B4416FCE8C248FBABFBD6.xml new file mode 100644 index 00000000000..1f6afc3a4a6 --- /dev/null +++ b/data/D6/47/B8/D647B8442F0B4416FCE8C248FBABFBD6.xml @@ -0,0 +1,97 @@ + + + +Micropaleontological Study Of The Gura Beliei Red Marls Formation From The Pietroșița Area (Turonian - Maastrichtian). Part Iii Campanian-Maastrichtian Planktonic Foraminifera + + + +Author + +Neagu, Theodor + +text + + +Acta Palaeontologica Romaniae + + +2016 + +2016-12-27 + + +12 + + +2 + + +67 +91 + + + +journal article +1842-371x + + + + + + +Globotruncanella petaloidea +( +Gandolfi1955 +) + + + + + + +Figs. 3 +: 18-20; +Figs. 4 +: 22-24, 31-36; +Figs. 9 +: 7-9 + + +1955 + +Globotruncana (Rugoglobigerina) petaloidea +ssp. + + + + + + +petaloidea +Gandolfi + +, p.52, pl.3, fig.13 a-c 1985 + +Globotruncanella petaloidea +( +Gandolfi 1955 +) Caron + +, p.51, pl.21, fig.5-6 Dimensions: D = 0,36- +0,29 mm +; d = 0,21- +0,14mm +. Remarks: The distinctive features of this species are (after Gandolfi's +specially +) 1955, p.52: " +the pronounce petaloid periphery (out-line). Chambers subpetaloid.... where presents frequent tubercles +". The subglobular aspect spiral and umbilical of chambers make the differences from + +Globotruncanella citae +Bolli 1951 + +.The presence of the tubercles along the margins of the chambers or finely beaded keel (Figs. XIV:22-24) represents individual features. Occurrence: Țâța Valley, Pietrosița- Fieni area Stratigraphic distribution: Maastrichtian. Specimens: LPB.VI. 12428 + + + + \ No newline at end of file diff --git a/data/D6/47/B8/D647B8442F0F4412FC1AC51EFB9AF8E4.xml b/data/D6/47/B8/D647B8442F0F4412FC1AC51EFB9AF8E4.xml new file mode 100644 index 00000000000..4ce195297b1 --- /dev/null +++ b/data/D6/47/B8/D647B8442F0F4412FC1AC51EFB9AF8E4.xml @@ -0,0 +1,104 @@ + + + +Micropaleontological Study Of The Gura Beliei Red Marls Formation From The Pietroșița Area (Turonian - Maastrichtian). Part Iii Campanian-Maastrichtian Planktonic Foraminifera + + + +Author + +Neagu, Theodor + +text + + +Acta Palaeontologica Romaniae + + +2016 + +2016-12-27 + + +12 + + +2 + + +67 +91 + + + +journal article +1842-371x + + + + + + +Globigerinella glaessneri +( +Gandolfi 1955 +) + + + + + + +Figs. 15 +: 1-3, +Figs. 8 +: 4-6 + + +1955 + +Rugoglobigerina glaessneri glaessneri +Gandolfi + +, p.55, pl.3, figs.10 a-c + + +Dimensions: D=0,26- +0,21 mm +; d=0,24- +0,12 mm +; g=0,14- +0,09 mm + + +Remarks: +Gandolfi (1955 +, p.50) show for this taxon ".... +loosely arranged chambers on both sides......test without keel +". From + +G. messinae +Brönnimann (1952) + +this species differ very clear by the globulous spherical chambers and not laterally compressed as + +G. messinae +Bronimann (1952) + +to with are resembles. + +Occurence: Țâța Valley, Pietrosița- Fieni area Stratigraphic distribution: Upper Senonian + + +Specimens: L. +P.B. +IV; 12445 ( +Laboratory of Palaeontology University +of +Bucharest +) + + + + + \ No newline at end of file diff --git a/data/D6/47/B8/D647B8442F0F4416FCA7C784FE44FE10.xml b/data/D6/47/B8/D647B8442F0F4416FCA7C784FE44FE10.xml new file mode 100644 index 00000000000..9789feb23fe --- /dev/null +++ b/data/D6/47/B8/D647B8442F0F4416FCA7C784FE44FE10.xml @@ -0,0 +1,244 @@ + + + +Micropaleontological Study Of The Gura Beliei Red Marls Formation From The Pietroșița Area (Turonian - Maastrichtian). Part Iii Campanian-Maastrichtian Planktonic Foraminifera + + + +Author + +Neagu, Theodor + +text + + +Acta Palaeontologica Romaniae + + +2016 + +2016-12-27 + + +12 + + +2 + + +67 +91 + + + +journal article +1842-371x + + + + + + +Schackoina multispinata +(Cushman & Wickenden 1940) + + + + + + +Fig. 3 +: 31 + + + +Fig. 1: 1-3 + +Rugoglobigerina subbotinae +Maslakova 1978 + +, Maastrichtian, Țâța Valley, Pietrosița, LPB.IV. 12446; +4 + +Rugoglobigerina macrocephalla +Brönnimann 1952 + +, Maastrichtian, Tata Valley-Pietrositza, LPB.IV. 12413; +5-6 + +Rugoglobigerina rotundata +Brönnimann, 1952 + +, Maastrichtian, Țâța Valley, Pietrosița, LPB.IV.12416; +7-15 + +Rugoglobigerina subbotinae +Maslakova 1978 + +, Maastrichtian, Țâța Valley, Pietrosița, LPB.IV.12419; +16-27 + +Rugotruncana subrugosa +(Gadolfi 1955) + +, Maastrichtian, Țâța Valley, Pietrosița, LPB.IV.12420; +28-33 + +Globotruncanella subpetaloidea +( +Gandolfi 1955 +) + +, Maastrichtian, Țâța Valley, LPB.IV. 12442; +34-36 + +Rugotruncana subcircumnodifer +( +Gandolfi 1955 +) + +, Maastrichtian, Țâța Valley, LPB.IV. 12439 + +(All specimens x 90). + + + +Fig. 2: 1-3 + +Rugoglobigerina pennyi +Brönnimann 1952 + +, Maastrichtian, Țâța Valley, Pietrosița, LPB.IV. 12417; +4-9 + +Rugoglobigerina subbotinae +Maslakova 1978 + +, Maastrichtian, Țâța Valley, LPB.IV. 12411; +10-12 + +Rugoglobigerina kingi +Trujillo 1960 Maastrichtian + +, Țâța Valley, L.P.B.IV. 12450; +13- 15 + +Rugoglobigerina ordinaria +( +Subbotina 1953 +) + +, Maastrictian, Țâța Valley, LPB.IV.12446; +16-21 + +Rugotruncana subglaessneri +( +Gandolfi 1955 +) + +, Maatrichtian, Țâța Valley, PietroȘița, LPB.IV.12421, +22- 25 + +Rugotruncana subornata +( +Gandolfi 1955 +) + +, Maatrichtian, Țâța Valley, LPB.IV.12440; +26-28 + +Rugotruncana subrugosa +( +Gandolfi 1955 +) + +, Țâța Valley, LPB.IV. 12436; +29-31 + +Rugotruncana subhexacamerata +( +Gandolfi 1955 +) + +, Maastrichtian, Țâța Valley, LPB.IV.12426; +32-34 + +Rugotruncana subcircumnodifer +( +Gandolfi 1955 +) + +, Maastrichtian, Țâța Valley, LPB.IV.12431 (All specimens x 90). + + + + +Fig. 3: 1-9 + +Globotruncanella coarctata +(Bolli 1957) + +, Maastrichtian, Țâța Valley, PietroȘița, LPB.IV. 12427; +10-17 + +Globotruncanella pshadae +(Keller 1946) + +, Maastrichtian, Țâța Valley, PietroȘița, LPB.IV.12427; +18-20 + +Globotruncanella petaloidea +( +Gandolfi 1955 +) + +, Maastrichtian, Țâța Valley, PietroȘița, LPB.IV.12428; +21-24 + +Globotruncanella havanensis +(Voorwjik 1937) + +, Maastrichtian, Țâța Valley, PietroȘița, LPB.IV.12329; +25-27 + +Globotruncanella saratogensis +(Applin 1920) + +, Maastrichtian, Țâța Valley, PietroȘița, LPB.IV. 12441; +28-30 + +Rugotruncana subrugosa +( +Gandolfi 1955 +) + +, Maastrichtian, Țâța Valley, PietroȘița, LPB.IV.12420; +31 + +Schsckoina multispinata +(Cush.Wick 1940) + +, Maastrichtian, Țâța Valley, PietroȘița- Fieni + +(All specimens x 90). + + +1946 + +Schackoina multispinata +(Cushman & Wickenden) Cushman + +, p.148, pl.61, figs.11-12 + + +Dimensions: D = +0,24 mm +; d = +0,096 mm + +Remarks: Specimens from the Upper Maastrichtian differs from the Cushmsan's species by the more elongated chambers. +Occurrence: Țâța Valley, Pietrosița- Fieni area Stratigraphic distribution: Maastrichtian +Specimen: L.P.B.IV.12430 + + + \ No newline at end of file diff --git a/data/D6/47/B8/D647B8442F184405FEBFC452FE40F9A3.xml b/data/D6/47/B8/D647B8442F184405FEBFC452FE40F9A3.xml new file mode 100644 index 00000000000..b3e71b37ef5 --- /dev/null +++ b/data/D6/47/B8/D647B8442F184405FEBFC452FE40F9A3.xml @@ -0,0 +1,92 @@ + + + +Micropaleontological Study Of The Gura Beliei Red Marls Formation From The Pietroșița Area (Turonian - Maastrichtian). Part Iii Campanian-Maastrichtian Planktonic Foraminifera + + + +Author + +Neagu, Theodor + +text + + +Acta Palaeontologica Romaniae + + +2016 + +2016-12-27 + + +12 + + +2 + + +67 +91 + + + +journal article +1842-371x + + + + + + +Gansseria gansseri +( +Bolli 1951 +) + + + + + + +Figs. 11 +: 22-27; +Figs. 12 +: 1-3 + + +1951 + +Globotruncana gansseri +Bolli + +, p.196, pl.35, figs. +1-3 1955 + +Globotruncana gansseri gansseri +Bolli, Gandolfi + +, p.69, pl.6, fig.8 a-c, text-fig.11b + + +1984 +Gansseria gansseti +(Bolli) Caron, Gonzales Donoso, Robaszynski, Wonders, p. 294, pl.53, fig.5 + + +Dimensions: D = 0,39-0,3 +4mm +; d = 0,39- +0,29 mm +; g = 0,26- +0,17 mm + + +Remarks: By the extremely rough test (small irregular tubers) together with one peripheral keel, this species is very near to +Rugogtruncana +. + +Occurrences: Țâța Valley, Pietrosița- Fieni area Stratigraphic distribution: Upper Maastrichtian Specimens: LPB.IV. 12442 + + + \ No newline at end of file diff --git a/data/D6/47/B8/D647B8442F184405FF45C194FE40FC0E.xml b/data/D6/47/B8/D647B8442F184405FF45C194FE40FC0E.xml new file mode 100644 index 00000000000..2b1bca70dba --- /dev/null +++ b/data/D6/47/B8/D647B8442F184405FF45C194FE40FC0E.xml @@ -0,0 +1,82 @@ + + + +Micropaleontological Study Of The Gura Beliei Red Marls Formation From The Pietroșița Area (Turonian - Maastrichtian). Part Iii Campanian-Maastrichtian Planktonic Foraminifera + + + +Author + +Neagu, Theodor + +text + + +Acta Palaeontologica Romaniae + + +2016 + +2016-12-27 + + +12 + + +2 + + +67 +91 + + + +journal article +1842-371x + + + + + + +Rugotruncana subglaessneri +( +Gandolfi 1955 +) + + + + + + +Figs. 2 +: 16-21; +Figs. 7 +: 19-21, 24-29; +Figs. 10 +: 22-27; + + +Figs. 12 +: 7-9 + + +1955 + +Rugoglobigerina glaessneri subglaessneri +Gandolfi + +, p.51, pl.3, fig. 9 a-c + + +Dimensions: D = 0,26- +0,15 mm +;d = 0,24- +0,15 mm +Remarks: specimens from the Țâța Valley has the general aspect (in all respect) with Gandolfi's species by four to five chambers in the last whorls, high protruding (in aspect) periphery fairly petaloid with a finely beading diverging double keel; the umbilical chambers moderate inflated and as usual, ornate by radial costellae or rough. + +Occurrences: Țâța Valley, Pietrosița- Fieni area Stratigraphic distribution: Maastrichtian +Specimens: LPB.IV. 12421 + + + \ No newline at end of file diff --git a/data/D6/47/B8/D647B8442F184405FF76C67AFBABFF0F.xml b/data/D6/47/B8/D647B8442F184405FF76C67AFBABFF0F.xml new file mode 100644 index 00000000000..3d97570efa5 --- /dev/null +++ b/data/D6/47/B8/D647B8442F184405FF76C67AFBABFF0F.xml @@ -0,0 +1,92 @@ + + + +Micropaleontological Study Of The Gura Beliei Red Marls Formation From The Pietroșița Area (Turonian - Maastrichtian). Part Iii Campanian-Maastrichtian Planktonic Foraminifera + + + +Author + +Neagu, Theodor + +text + + +Acta Palaeontologica Romaniae + + +2016 + +2016-12-27 + + +12 + + +2 + + +67 +91 + + + +journal article +1842-371x + + + + + + +Gansserina wiedenmayeri +( +Gandolfi 1955 +) + + + + + + +Figs. 12 +: 4-6 + + +1955 + +Globotruncana wiedenmayeri wiedenmayeri +Gandolfi + +, p.71, pl.7, figs.4 a-c + + +1984 + +Gansseria wiedenmayeri +(Gandolfi) Robaszynski, Caron, Gonzales Donoso, Wonders + +, p.298, pl.54, figs.3 a-c + + +Dimensions: D = +0,50 mm +; d = +0,40 mm +; g = +0,34 mm + + +Remarks: With its so high umbilical side (as +Glo- + + +borotsalitres +from calcareous benthic species) the extremely rougher ornamentation, the spiral side low trochospiral near flat and a double keel on the periphery of the test, this species is very clear delimited. + +Occurrences: Țâța Valley, Pietrosița- Fieni area +Stratigraphic distribution: Upper Maastrichtian +Specimens: LPB.IV. 12431 + + + \ No newline at end of file diff --git a/data/D6/47/B8/D647B8442F1C4401FC1EC52CFBABF94A.xml b/data/D6/47/B8/D647B8442F1C4401FC1EC52CFBABF94A.xml new file mode 100644 index 00000000000..6c6498cfd8e --- /dev/null +++ b/data/D6/47/B8/D647B8442F1C4401FC1EC52CFBABF94A.xml @@ -0,0 +1,77 @@ + + + +Micropaleontological Study Of The Gura Beliei Red Marls Formation From The Pietroșița Area (Turonian - Maastrichtian). Part Iii Campanian-Maastrichtian Planktonic Foraminifera + + + +Author + +Neagu, Theodor + +text + + +Acta Palaeontologica Romaniae + + +2016 + +2016-12-27 + + +12 + + +2 + + +67 +91 + + + +journal article +1842-371x + + + + + + +Rugotruncana subloetterli +( +Gandolfi 1955 +) + + + + + + +Figs. 6 +: 16-21; +Figs. 9 +: 22-24; +Figs. 16 +: 21-26 + + +1955 + +Globotruncana (Rugoglobigerina) loetterli subloetterli +Gandolfi + +, p. 36, pl.1, fig.14 + + +Dimensions: D = +0,36-0,38 mm +; d = 0,40- +0,36 mm +Remarks: By its low trochospiral test, the presence of two peripheral keels and the moderate inflated chambers, smooth or with a weak ornamentation (small tubercles of fine costellaes) this species is well delimited. + +Occurrences: Țâța Valley, Pietrosița- Fieni area Stratigraphic distribution: Upper Maastrichtian Specimens: LPB.IV. 12423 + + + \ No newline at end of file diff --git a/data/D6/47/B8/D647B8442F1C4401FCC1C099FBABFD46.xml b/data/D6/47/B8/D647B8442F1C4401FCC1C099FBABFD46.xml new file mode 100644 index 00000000000..5098fc7ec99 --- /dev/null +++ b/data/D6/47/B8/D647B8442F1C4401FCC1C099FBABFD46.xml @@ -0,0 +1,89 @@ + + + +Micropaleontological Study Of The Gura Beliei Red Marls Formation From The Pietroșița Area (Turonian - Maastrichtian). Part Iii Campanian-Maastrichtian Planktonic Foraminifera + + + +Author + +Neagu, Theodor + +text + + +Acta Palaeontologica Romaniae + + +2016 + +2016-12-27 + + +12 + + +2 + + +67 +91 + + + +journal article +1842-371x + + + + + + +Rugotruncana subcircumnodifer +( +Gandolfi 1955 +) + + + + + + +Figs. 1 +: 34-36; +Figs. 2 +: 32-34; +Figs. 9 +: 25-27; +Figs. 15 +: 4- 12 + + +1955 + +Globotruncana (Rugoglobigerina) circumnodifer subcircumnodifer +Gandolfi + +, p.44, pl.2, fig.8 + + +1967 + +Rugotruncana subcircumnodifer +(Gandolfi) Pessagno + +, p.369, pl.62, fig.14 16, pl.74, fig.1-3 Dimensions: D = +0,32-0,36 mm +; d = +0,27-0,32 mm +; Remarks: +Gandolfi (1955) +shows: " +the test is slightly convex, chambers are inflated more pronounced in the umbilical side the faintly beaded double keel is not exactly in the middle of the chambers.........test is rough especially in the early stage +". All these features defined clear this taxon. + +Occurrences: Țâța Valley, Pietrosița- Fieni area Stratigtraphic distribution: Maastrichtian +Specimens: LPB.IV. 12439 + + + \ No newline at end of file diff --git a/data/D6/47/B8/D647B8442F1C4401FCF6C367FAFAFAF9.xml b/data/D6/47/B8/D647B8442F1C4401FCF6C367FAFAFAF9.xml new file mode 100644 index 00000000000..ae52a3f396b --- /dev/null +++ b/data/D6/47/B8/D647B8442F1C4401FCF6C367FAFAFAF9.xml @@ -0,0 +1,83 @@ + + + +Micropaleontological Study Of The Gura Beliei Red Marls Formation From The Pietroșița Area (Turonian - Maastrichtian). Part Iii Campanian-Maastrichtian Planktonic Foraminifera + + + +Author + +Neagu, Theodor + +text + + +Acta Palaeontologica Romaniae + + +2016 + +2016-12-27 + + +12 + + +2 + + +67 +91 + + + +journal article +1842-371x + + + + + + +Rugotruncana subhexacamerata +Gandolfi 1955 + + + + + + +Figs. 2 +: 29-31; +Figs. 10 +: 28-30; +Figs. 13 +: 4-6 + + +1955 + +Globotruncana (Rugoglobigerina) hexacamerata subhexacamerata +Gandolfi + +, p.34, pl.1, fig.11 Dimensions: D = 0,34- +0,32 mm +; d = 0,34- +0,34 mm +; g = +0,19 mm + + +Remarks: +Gandolfi (1955 +, p.34) characterized this taxon: “ +its flat to slightly convex dorsal(spiral) side, double keeled in the early stages, keels finely beaded, often not continuous way: chambers five to six on the last whorl..........Test rough in the early stage +". On our specimens on the periphery of the last chambers the keel is exactly a finely beaded often not continuous ( +Figs. 10 +: 28-30) + +Occurrences: Țâța Valley, Pietrosița- Fieni area Stratigraphic distribution: Maastrichtian +Specimens: LPB.IV.12422; L.P.B.IV.12444 + + + \ No newline at end of file diff --git a/data/D6/47/B8/D647B8442F1C4401FF54C17DFE39FD67.xml b/data/D6/47/B8/D647B8442F1C4401FF54C17DFE39FD67.xml new file mode 100644 index 00000000000..6c735b2a439 --- /dev/null +++ b/data/D6/47/B8/D647B8442F1C4401FF54C17DFE39FD67.xml @@ -0,0 +1,79 @@ + + + +Micropaleontological Study Of The Gura Beliei Red Marls Formation From The Pietroșița Area (Turonian - Maastrichtian). Part Iii Campanian-Maastrichtian Planktonic Foraminifera + + + +Author + +Neagu, Theodor + +text + + +Acta Palaeontologica Romaniae + + +2016 + +2016-12-27 + + +12 + + +2 + + +67 +91 + + + +journal article +1842-371x + + + + + + +Rugotruncana tilevi +Brönnimann & Brown 1955 + + + + + + +Figs. 8 +: 19-21 + + +1955 + +Rugotruncana tilevi +Brönnimann & Brown + +, p.547, pl.22, figs.1-3 + + +Dimensions: D = 0,40 - +0,36 mm +; d = +0,36 mm +; g = +0,14 mm + + +Remarks: Presence of a double keel and the radial disposition of the costellae particularly on the umbilical side are the features which make the difference from the + +Rugotruncana subrugosa +Gandolfi. + + +Occurrences: Țâța Valley, Pietrosița- Fieni area Stratigraphic distribution: Upper Maastrichtian Specimens: LP B.IV. 12436 + + + \ No newline at end of file diff --git a/data/D6/47/B8/D647B8442F1C4401FF54C341FE40FB5D.xml b/data/D6/47/B8/D647B8442F1C4401FF54C341FE40FB5D.xml new file mode 100644 index 00000000000..20a93ac7242 --- /dev/null +++ b/data/D6/47/B8/D647B8442F1C4401FF54C341FE40FB5D.xml @@ -0,0 +1,80 @@ + + + +Micropaleontological Study Of The Gura Beliei Red Marls Formation From The Pietroșița Area (Turonian - Maastrichtian). Part Iii Campanian-Maastrichtian Planktonic Foraminifera + + + +Author + +Neagu, Theodor + +text + + +Acta Palaeontologica Romaniae + + +2016 + +2016-12-27 + + +12 + + +2 + + +67 +91 + + + +journal article +1842-371x + + + + + + +Rugotruncana ellisi +Brönnimann & Brown 1955 + + + + + + +Figs. 5 +: 13-15, 19-24; +Figs. 11 +:16-21 + + +1955 + +Rugotruncana ellisi +Brönnimann & Brown + +, p.547, pl.22, figs.7-9 + + +Dimensions: D = 0,39- +0,39 mm +; d = +0,29-0,36 mm +; g = +0,19 mm + + +Remarks: The authors characterized very conclusive this species: " +Some or all chambers exhibit a very weak double keeled peripheral band. The two keels are very faint and may be missing from a few or last chambers, the costellae which are barely discernible give the surface a roughened appearance +". + +Occurrences: Țâța Valley, Pietrosița- Fieni area Stratigraphic distribution: Maastrichtian +Specimens: LPB.IV. 12426 + + + \ No newline at end of file diff --git a/data/D6/47/B8/D647B8442F1C4401FF70C69CFBABFF0F.xml b/data/D6/47/B8/D647B8442F1C4401FF70C69CFBABFF0F.xml new file mode 100644 index 00000000000..ac328bab6ef --- /dev/null +++ b/data/D6/47/B8/D647B8442F1C4401FF70C69CFBABFF0F.xml @@ -0,0 +1,84 @@ + + + +Micropaleontological Study Of The Gura Beliei Red Marls Formation From The Pietroșița Area (Turonian - Maastrichtian). Part Iii Campanian-Maastrichtian Planktonic Foraminifera + + + +Author + +Neagu, Theodor + +text + + +Acta Palaeontologica Romaniae + + +2016 + +2016-12-27 + + +12 + + +2 + + +67 +91 + + + +journal article +1842-371x + + + + + + +Rugotruncana subornata +( +Gandolfi 1955 +) + + + + + + +Figs. 2 +: 22-25 + + +1955 + +Globotruncana (Rugoglobigerina) ornata subornata +Gandolfi + +, p.50, pl.3, fig.6 a-c + + +Dimensions: D = +0,22 mm +; d = +0,20 mm +; g = +0,12 mm + + +Remarks: By the presence of two finely beaded keels this species differs from + +Rugoglobigerina ornata +Brönnimann + + +1952. +Occurrences: Țâța Valley, Pietrosița- Fieni area +Stratigraphic distribution: Upper Maastrichtian +Specimens: LPB.IV. 12440 + + + \ No newline at end of file diff --git a/data/D6/47/B8/D647B8442F1C4401FF72C548FE48F909.xml b/data/D6/47/B8/D647B8442F1C4401FF72C548FE48F909.xml new file mode 100644 index 00000000000..d1e947c35e4 --- /dev/null +++ b/data/D6/47/B8/D647B8442F1C4401FF72C548FE48F909.xml @@ -0,0 +1,92 @@ + + + +Micropaleontological Study Of The Gura Beliei Red Marls Formation From The Pietroșița Area (Turonian - Maastrichtian). Part Iii Campanian-Maastrichtian Planktonic Foraminifera + + + +Author + +Neagu, Theodor + +text + + +Acta Palaeontologica Romaniae + + +2016 + +2016-12-27 + + +12 + + +2 + + +67 +91 + + + +journal article +1842-371x + + + + + + +Rugotruncana subrugosa +( +Gandolfi 1955 +) + + + + + + +Figs. 1 +: 16-27; +Figs. 2 +: 26-28; +Figs. 3 +: 28-30; +Figs. 6 +: 7-9 + + +1955 + +Globotruncana (Rugoglobigerina) rugosa subrugosa +Gandolfi + +, figs.5a-c + + +Dimensions: D = +0,32-0,40 mm +; d = +0,24-0,36 mm +; g = +0,17-0,19 mm + + +Remarks: By the presence of two peripheral keels this species differs + +from +Rugoglobigrerina rugosa + +, even if the chambers on the umbilical side present ordinary a + +Rugoglobigerina rugosa + +radial costellae. + +Occurrences: Țâța Valley, Pietrosița- Fieni area Stratigraphic distribution: Upper Maastrichtian Specimens: LPB.IV.12420 + + + \ No newline at end of file diff --git a/data/D6/47/B8/D647B8442F1C4405FC19C753FE40FE10.xml b/data/D6/47/B8/D647B8442F1C4405FC19C753FE40FE10.xml new file mode 100644 index 00000000000..a78256609bd --- /dev/null +++ b/data/D6/47/B8/D647B8442F1C4405FC19C753FE40FE10.xml @@ -0,0 +1,199 @@ + + + +Micropaleontological Study Of The Gura Beliei Red Marls Formation From The Pietroșița Area (Turonian - Maastrichtian). Part Iii Campanian-Maastrichtian Planktonic Foraminifera + + + +Author + +Neagu, Theodor + +text + + +Acta Palaeontologica Romaniae + + +2016 + +2016-12-27 + + +12 + + +2 + + +67 +91 + + + +journal article +1842-371x + + + + + + +Rugotruncana subpennyi +( +Gandolfi 1955 +) + + + + + + +Figs. 6 +: 13-15; +Figs. 7 +: 1-6, 10-15, 22-27; +Figs. 8 +: 10-12; + + +Figs. 9 +: 13-21, +Figs. 13 +: 1-3 + + +1955 + +Globotruncana (Rugoglobigerina) pennyi subpennyi +Gandolfi + +, p.73, fig.7 + + +1967 + +Rugotruncana subpennyi +(Gandolfi) Pessagno + +, p. 370, pl.76, figs.12-14 + + + +Fig. 15: 1-3 + +Globigerinella glaessneri +( +Gandolfi 1955 +) + +, Maastrichtian, Țâța Valley, PietroȘița, LPB.IV.12418; +4-12 + +Rugotruncana subcircumnodifer +( +Gandolfi 1955 +) + +, Maastrichtian, Țâța Valley, PietroȘița, LPB.IV.12439; +13-24 + +Globotruncanella sarmientoi +( +Gandolfi 1955 +) + +, Maastrichtian, Țâța Valley, PietroȘița, LPB.IV.12448; +25-27 + +Rugoglobigerina kingi +Trujillo 1960 + +, Maastrichtian, Țâța Valley, PietroȘița, LPB.IV.12450 (All specimens x 90). + + + + +Fig. 16: 1-17 + +Abatomphalus pessagnoi +( +Longoria 1973 +) + +, Maastrichtian, Țâța Valley, PietroȘița, LPB.IV.12434; +18-20 + +Rugotruncana subbeldigi +( +Gandolfi 1955 +) + +, Maastrichtian, Țâța Valley, PietroȘița, LPB.IV.12452; +21-26 + +Rugotruncana subloetterli +( +Gandolfi 1955 +) + +, Maastrichtian, Țâța Valley, PietroȘița, LPB.IV.12423 (All specimens x 90). + + + + +Fig. 17: +Reproductions of different + +Globotruncanella + +taxa from the original papers. +1-6 + +Globigerina cretacea +var. +saratogensis +Applin 1920 + +(modified from Applin, 1920); +7-9 + +Globotruncana havanensis +Voorwjik 1937 + +(modified from Voorwjik, 1937); +10-15 + +Rugotruncana havanensis +(Voorwjik 1937) emend. Brönnimann & Brown 1955 + +, LPB.IV. 12429 (specimens x 90, Neagu Collection); +16-33 + +Globorotalia pshadae +Keller 1946 + +(modified from +Subbotina, 1953 +). + + + +Dimensions: D = 0,36- +0,26 mm +; d = 0,40- +0,32 mm +; g = +0,22 mm + + +Remarks: This species differs from + +Rugotruncana subrugosa + +by the presence of a double peripheral keel and the radial costellae on the umbilical side is flat or very low trochospiral without a typical ornamentation. + +Occurrences: Țâța Valley, Pietrosița- Fieni area Stratigraphic distribution: Upper Maastrichtian Specimens: LPB.IV. 12426 + + + \ No newline at end of file diff --git a/data/F5/4F/87/F54F87FCFFA4FFA37E691DE32B275B3D.xml b/data/F5/4F/87/F54F87FCFFA4FFA37E691DE32B275B3D.xml new file mode 100644 index 00000000000..d2596da0efc --- /dev/null +++ b/data/F5/4F/87/F54F87FCFFA4FFA37E691DE32B275B3D.xml @@ -0,0 +1,341 @@ + + + +Orbitolinid Foraminifera From The Late Maastrichtian Of The Tarbur Formation (Zagros Zone, Sw Iran) + + + +Author + +Rashidi, Felix Schlagintweit Koorosh + + + +Author + +Babadipour, Movlud +Department of Geology, Payame Noor University, Po Box 19395 - 3697 Tehran, Iran, kooroshrashidi @ pnu. ac. ir, moloud 65 _ 89 @ yahoo. com +kooroshrashidi@pnu.ac.ir + +text + + +Acta Palaeontologica Romaniae + + +2016 + +2016-12-23 + + +12 + + +2 + + +29 +46 + + + +journal article +1842-371x + + + + + +Genus + +Pseudorbitolina +Douvillé, 1910 + + + + + + +Remarks: +The genus + +Pseudorbitolina + +is monospecific with the +type +species being + +Pseudorbitolina marthae +Douvillé, 1910 + +. + + + +Fig. 8 + +Dictyoconus bakhtiari + +n. sp. +from the late Maastrichtian of the Tarbur Formation, Mandegan section ( +c +) and Naghan section (all others), SW Iran. +a +Oblique section passing the eccentric initial spire. +b–e, h–j +Oblique sections; affecting five chambers in +b +. Note the broadening of the distal end of the beams in +b–d, i +. +f +Tangential-oblique section. +g +Tangential oblique section of a microspheric specimen. Abbreviations: be = beam, fo = foramen, is = initial spire, pi = pillar, s = septum. Thin-sections: Ng 53-2 ( +a +), 2NG 52 ( +b +), Rt 62-1 ( +c +), Ng 53-1 ( +d, h +), Ng 52-1 ( +e +), 2NG 32 ( +f, j +), Ng 87-2 ( +g +), 2NG 53 ( +i +). + + + + +Fig. 9 + +Dictyoconus bakhtiari + +n. sp. +from the late Maastrichtian of the Tarbur Formation, Naghan section, SW Iran. +a +Oblique section. +b–c +Oblique sections cutting the initial spire with the embryo. +d, g +Subaxial sections. +e–f, j +Axial sections. +h +Obliquetransverse section. +i +Tangential section. Abbreviations: be = beam, de = deuteroconch, ib = intercalary beam, p = protoconch. Thinsections: Ng 21 ( +a +), Ng 85 ( +b +), Ng 53-1 ( +c +), Ng 52-2 ( +d, h +), 2Ng 87-2 ( +e-f +), Ng 53-2 ( +g +), Ng 55 ( +i +), 2NG 27 ( +j +). + + + + +Pseudorbitolina +cf. +marthae +Douvillé, 1910 + + + +Figs. 3e–f +, +11 + + +*1910 + +Pseudorbitolina marthae + +n. gen., n. sp. +– Douvillé, p. 57, text-fig. 1–4. + + +1948 + +Pseudorbitolina marthae +Douvillé + +– Henson, p. 102, pl. 6, fig. 17, pl. 11, fig. 6?, text-fig. 16 (Maastrichtian Simsima Formation of +Qatar +, see +Sugden and Standring, 1975 +). + + +1978 + +Pseudorbitolina marthae +Douvillé + +– Neumann, p. 198, figs. 1–3, pls. 1–2 (with synonymy). + + +1979 + +Pseudorbitolina marthae +Douvillé + +– Radoičić, pl. 8, figs. 1-3. + + +Non 2008 + +Pseudorbitolina +cf. +marthae +Douvillé + +– Al-Kubaysi, fig. 2-12 = random section of + +Loftusia +sp. + +(Maastrichtian Aqra Formation of +Iraq +). + + +2008 + +Pseudorbitolina marthae +Douvillé + +– Boudagher-Fadel, pl. 5.7, figs. 8, 14 (Maastrichtian of Dukhan no. 1 well, +Qatar +; original material of Henson, 1947). + + +Non 2016 + +Pseudorbitolina marthae +Douvillé + +– Al-Kubaysi and Abid, fig. 6-1 to 6-3 = random section of + +Loftusia +sp. + +(Maastrichtian Aqra Formation of +Iraq +) (see +Fig. 12 +). + + + + +Description: +Test mostly low, more rarely high conicoconcave and irregularly curved. The specimens display a rather wide range of apical angle and consequently the ratio test diameter to height. The chambers do not cover the complete basal cone surface but exhibit marginal annuli only ( +type +annular-concentric, e.g., Hottinger, 2008, fig. 37.4), becoming slightly broader during ontogeny. Adult specimens consist of up to 35 chambers (specimen in +Fig. 11a +). The chambers display a marginal zone with a fine subepidermal network of intercalary beams and rafters ( +Fig. 11f +, lower part). There are up to two rafters; numbers of vertical partitions unknown. As can be seen in tangential sections, the primary beams are radially aligned between successive chambers ( +Fig. 11e, h +). Towards the central part, an undivided zone connects the chamberlets of each chamber. Large foramina (tubular aperture of Henson, 1947) connect these undivided zones of succeeding chambers. + + +Dimensions +(in mm): + + +Test diameter (D): ~ +1.6 mm +to +4.6 mm +(Douvillé, 1910: ~ +2–3 mm +) + +Test height (H): 0.75–1.2 +D/H: 2.0–6.0 + +Diameter proloculus: +0.1 mm +(1 value) + + + + +Remarks: +First of all we have to stress that the available sections are not convenient for a detailed description of the test architecture. In any case, with its annular-concentric chambers more or less throughout the complete ontogeny, + +Pseudorbitolina + +represents a rather unusual chamber arrangement among the orbitolinids. According to the drawing of Douvillé (1910, fig. 3), the monospecific genus + +Pseudorbitolina + +shows a subspherical proloculus in apical position displaying a septulated supraembryonic zone at its top (like in + +Palorbitolina + +, see +Schroeder, 1963 +, fig. 1). The thin-section specimens illustrated by +Neumann (1978 +, pl. 1, fig. 7, pl. 2, fig. 6) in transverse sections instead shows an embryo in apical position consisting of a spherical proloculus and a hemispherical septulated deuteroconch arranged laterally to the former. In the Maastrichtian material, only +one specimen +was cut passing the proloculus ( +Fig. 11a +). + + +In the revision of the species provided by +Neumann (1978) +, the author concludes that it represents a good marker for the Campanian. Obviously there is a stratigraphic discrepancy of the occurrence of + +Pseudorbitolina marthae + +between the western Europe +type +region and +Iran +/ +Iraq +(see synonymy). In the Campanian-Maastrichtian deposits of +Turkey +, + +P. marthae + +is restricted to the southeastern part belonging to the Arabian platform ( +Özer et al., 2009 +). In the Maastrichtian of the Iraqian Aqra Formation, random sections of + +Loftusia +sp. + +have been confounded with + +Pseudorbitolina marthae +Douvillé + +(see synonymy) ( +Fig. 12 +). + + + + \ No newline at end of file diff --git a/data/F5/4F/87/F54F87FCFFA8FFAA7DCE19302AF15E54.xml b/data/F5/4F/87/F54F87FCFFA8FFAA7DCE19302AF15E54.xml new file mode 100644 index 00000000000..1f4db990f15 --- /dev/null +++ b/data/F5/4F/87/F54F87FCFFA8FFAA7DCE19302AF15E54.xml @@ -0,0 +1,273 @@ + + + +Orbitolinid Foraminifera From The Late Maastrichtian Of The Tarbur Formation (Zagros Zone, Sw Iran) + + + +Author + +Rashidi, Felix Schlagintweit Koorosh + + + +Author + +Babadipour, Movlud +Department of Geology, Payame Noor University, Po Box 19395 - 3697 Tehran, Iran, kooroshrashidi @ pnu. ac. ir, moloud 65 _ 89 @ yahoo. com +kooroshrashidi@pnu.ac.ir + +text + + +Acta Palaeontologica Romaniae + + +2016 + +2016-12-23 + + +12 + + +2 + + +29 +46 + + + +journal article +1842-371x + + + + + + +Dictyoconella +? +minima +Henson, 1948 + + + + + + +Figs. 3a–b +pars, 5–6 + + +*1948 + +Dictyoconella minima + +n. sp. +– Henson, p. 25, pl. 11, fig. 3, 8-10. + + +2008 + +Dictyoconella minima +Henson + +– Boudagher Fadel, pl. 5.7, figs. 1-3 ( +paratypes +). + + +2016 + +Montseciella +sp. + +– Afghah, fig. 5d (not indicated in the legend of the figure but in the text on page 175; Tarbur Formation of south Zagros Basin). + + +Description: +Test medium conical (apical angles 50–90 degrees); both sides and cone base slightly convex. Some transverse sections display an oval outline ( +Figs. 3b +, +5j +). + + +The initial part is characterized by a small spire (?trochospiral,?planspiral) of few chambers and with acute margin; its axis is almost parallel to the test side wall ( +Fig. 6e, g, l +). The embryo is poorly visible and its detailed structure unknown ( +Fig. 6h–i +). The exoskeleton consists of horizontal (rafters) and radial vertical partitions (beams) subdividing the chamber margins. The beams are continuous from one chamber to the next ( +Fig. 5c, 5e, 5n–m +). They extend to a marginal through marking the boundary to the central zone. Their distal ends slightly bend upwards in direction to the apex ( +Fig. 5k +). There are 2 to 3 shorter intercalary beams intercalated between the beams ( +Fig. 5b, 5o–p +). There are two rafters of inequal length per chamberlet in the marginal zone ( +Fig. 5a +). Shallow-tangential sections display a pattern of subrounded alveolar compartments (subepidermal network) ( +Fig. 5f +). The boundary between the marginal and central zones is marked by a marginal through, in close proximity to the marginal foramina ( + +Fig. +5g +, 5j, 5p + +). The latter with oblique axis ( +Fig. 5k +) form a row of circular openings corresponding to the number of beams in transverse sections ( +Fig. 5o +). Indistinct parts of the central zone are filled with opaque micritic masses (fused pillars and/or secondary deposits) masking the original structure ( +Fig. 5a, 5h +, middle part of the cone; +Fig. 6b–e +). In other parts of the central zone vertical interseptal elements (pillars) alternating between successive chambers are discernible (see +Fig. 5h +, youngest chambers; +Fig. 6k +). The non-marginal foramenal axes in the central zone maybe vertical (as the pillars) but also oblique. + + +Dimensions +(in mm; data from +Henson, 1948 +, between brackets): + + +Test diameter (D): +0.7–1.9 mm +( +0.7–1.8 mm +) + + +Test height (H): 0.8–1.4 (1.0– +1.5 mm +) + +D/H: 0.8–1.35 + +Numbers of chambers per +1 mm +axial length: 12–16, mostly 15–16 (15) + + + + +Remarks: +Henson (1948 +, p. 25) noted that the test of + +D. minima + +is conical but slightly compressed, so that the base shows an elliptical outline. Elliptical (or oval) outline of the test base is rare in orbitolinids. It is reported from the early Albian + +Mesorbitolina ovalis + +throughout its ontogeny (see +Görög and Arnaud-Vanneau, 1996 +), and the juvenile part of the late Albian + +Carinoconus casterasi +(Bilotte, Canérot, Moullade & Peybernès) + +(see +Schroeder, 1985 +). The acute margin of the initial spire of + +D +.? +minima + +however shows affinities to + +Carinoconus + +(see further remarks below) thus offering an explanation that only transverse sections of the juvenile test part might be ellipsoidal in outline. + + +Another typical feature of + +D +.? +minima + +are the dark, irregular distributed microgranular masses of fused pillars (and/or secondary deposits?) in the central zone. This was also observed by +Henson (1948 +, p. 26), stating that interseptal structures are sporadic and poorly defined in the central part of the test. Among the +Orbitolinidae +, secondary deposits in the central zone are an extreme exception. An example is the genus + +Carinoconus +Cherchi & Schroeder + +, with the type-species + +C. casterasi + +from the Late Albian of Spain (Bilotte, Canérot, Moullade & Peybernès) (Cherchi and Schroeder, 1983; +Schroeder, 1985 +; +Loeblich and Tappan, 1987 +). A second species has been described as + +Carinoconus iraqiensis + +by +Bernaus and Masse (2006) +from the Cenomanian of +Iraq +. Marginal foramina and main partitions (beams) arranged in vertical lines in subsequent chambers however are not reported from the genus + +Carinoconus + +. Without further details on the structure of the embryonic apparatus and the initial part in centered sections however a reliable attribution of + +Dictyoconella +? +minima + +to any known ( + +Carinoconus + +?, or new?) orbitolinid genus is not possible for the moment being. + + +Henson (1948) +reported + +D +.? +minima + +“most probably” from the late Cenomanian or Turonian of +Qatar +(Dukhan no. 2 and 3 wells; Wasia Group, see figs. +1-2 in +Sugden and Standring, 1975 +). In addition, Henson (op. cit, p. 26) noted “a single specimen, possibly of this species” from the Maastrichtian of +Iraq +. For the Dukhan oil field of +Qatar +, +Hewaidy and Al-Hitmi (1994) +established a Late Cenomanian “ + +Dictyoconella minima + +total range Zone”. Curiously, +Boudagher-Fadel (2008 +, chart 5.2) indicated the range of + +D. +? +minima + +as Late Cenomanian–Santonian. + + + + \ No newline at end of file diff --git a/data/F9/0B/87/F90B87DFFF8DFFE3D23BF9A1FC0503EE.xml b/data/F9/0B/87/F90B87DFFF8DFFE3D23BF9A1FC0503EE.xml new file mode 100644 index 00000000000..63e97593319 --- /dev/null +++ b/data/F9/0B/87/F90B87DFFF8DFFE3D23BF9A1FC0503EE.xml @@ -0,0 +1,397 @@ + + + +Entogonia Briggeri N. Sp., A New Diatom Species From The Middle Miocene Of Romania And New Insights On The Fossil Marine Diatom Genus Entogonia Greville + + + +Author + +Dumitrică, Paulian +Institute of Earth Science, Université de Lausanne, Géopolis, 1015 Lausanne, Switzerland; Paulian. Dumitrica @ unil. ch +Paulian.Dumitrica@unil.ch + + + +Author + +Martin, Simona Saint +UMR 7202 CR 2 P MNHN / CNRS / SU Muséum National d’Histoire Naturelle Paris, Département Origines et Evolution, + +text + + +Acta Palaeontologica Romaniae + + +2017 + +2018-02-28 + + +13 + + +2 + + +21 +35 + + + +journal article +1842-371x + + + + + + +Entogonia briggeri +Dumitrică + +and +Saint Martin +nov. sp. + + + + + +Figs. 3-7 + + +Description. The valves are tripolar with straight to slightly convex sides in valve view and round poles ( +Figs. 3 +a-f, 4a, 4c, 4f, 5a-b, 7a). Each pole bears an elevation circular to oval in outline and slightly raised above the surface of valve, with a height of about 17.5 µm. They are perforated by irregularly scattered areolae that are smaller than the valve areolae ( +Figs. 3 +a-f, 4b, 4c, 4e). Apices of the elevations are flat, finely punctate (perforate) with no particular arrangement of puncta as it can be seen in external valve view ( +Figs. 3e +, +4d +) and also in internal valve view ( +Fig. 5f +). The diameter of apices is of circa 17 µm. On each apex there is a flat, triangular, claw-like linking spine on one lateral border ( +Figs. 4b +, +6b +). The length of spines is variable between 24-25 µm. Exit pores arise gently from the valve face close to elevations; they are circular to oval in outline, with a diameter smaller than that of the elevations, of about 8.7- 10.5 µm. ( +Figs. 3a, 3c, 3e +, +4a, 4c +, +7a +). They have a protruding hyaline lip which does not surround the entire circumference of the exit pores as they are missing towards the projections ( +Fig. 4d +). The valve face is perforated by poroid areolae exhibiting different dimensions and distribution patterns that delimit an outer triangle and an inner triangle ( +Figs. 3 +a-e, 4a, 4c, 4f, 7a). In external oblique view the outer triangle is gently elevated relative to inner triangle ( +Fig. 4e +). The outer triangle is broad, convex in girdle view, with areolae arranged in 2-3 transverse rows between two internal costae as follows: the rows adjacent to internal costae comprise larger and closely spaced areolae (4-5 within a row); the rows locat- ed away from internal costae comprise smaller and more distantly spaced areolae (2-4 within a row); sometimes the rows of these smaller areolae are incomplete. The row of larger areolae which lie next to and parallel to each internal costae of the outer triangle are also much larger than those of the inner triangle ( +Figs. 3a, 3b, 3e +, +4a, 4c - d +). Rows are generally perpendicular to the valve face margins. Internal costae vary in number from 10 to 12 depending, but not compulsorily, on the size of the valve and continue down the mantle until they fuse with the margin of the mantle ( +Figs. 4f +, +5 +a-b, 7b). The internal costae of the outer triangle define sectors for areolae both on the valve face and on the mantle. The inner triangle presents straight or concave sides of circa 90-110 µm outlined on the valve surface by a deep constriction corresponding on the inner face to a costa ( +Figs. 4f +, +5 +a-b). The central part of this triangle is depressed as seen in external oblique view ( +Fig. 4e +) and sometimes hyaline ( +Fig. 3c +). In internal view, from this center radiate a large number of dense costae which reach the boundary between the inner and outer triangles and which can be simple or bifurcate ( +Figs. 5 +a-b, 7b). Three such costae extend along the bisectors of the three corners and continuously ramify on both sides forming a dense network of costae. These three bisecting costae are never straight as in other species or more prominent than the resulted branches ( +Figs. 5 +c-e). The fine areolae of the inner triangle are dense, small and arranged in radial, circular or spiral rows, neither of them perfect ( +Figs. 4a, 4c +, +7a +). Inner coils very delicate, with annular costae joined to one another by curved and more delicate bars ( +Figs. 5 +a-f). There is no clear distinction between valve face and valve mantle since valve areolae pattern is continuous on the mantle. Mantle vertical of about 29-35 µm height. There is also a basal ring of enlarged pores with protruding lips, which occur between internal costae on the valve mantle ( +Figs. 4b, 4e +, +6a +, and especially 6c). A thin hyaline ridge is placed on the mantle edge, bordering this latter with the valvocopula ( +Figs. 4b, 4e +). In internal view, it can be observed inwardly expanded hyaline mantle margin ( +Figs. 4f +, +5 +a-b). + + + +Figs. 3a-f + +Entogonia briggeri + +n. sp. +, sample 1315. LM views; +a +Holotype, valve view; +b +Same specimen figured in 3a focused on internal coil; +c +Isotype 1, valve view; +d +Same specimen figured in 3c focused on internal coil; +e +Isotype 2, valve view; +f +Isotype 3, valve view. Scale bars: 20 µm. + + + + +Figs. 4a-f + +Entogonia briggeri + +n. sp. +, sample 1315; SEM external views (a-e) and SEM internal view (f). +a +Valve face exhibiting specific morphological features; +b +Girdle view showing elevations and one triangular spine on each elevation; +c +Valve face showing valve shape, round apices, elevations to poles (arrow) and exit pores (head arrow), areolae pattern on inner and outer triangles; +d +Detail showing the finely punctuated apices of elevation and exit pore close to elevation with a protruding hyaline lip; +e +Oblique valve view showing raised outer triangle, depressed central part of inner triangle, vertical mantle with one ring of enlarged pores (arrows); +f +Internal view showing the outer and inner triangles, internal costae, internal coil system. Scale bars: 20 µm. + + + +Cingulum composed of a closed valvocopula and one or two closed copulae. All are ornamented by areolae, but areolae of valvocopula are slightly smaller than those of copulae and of mantle. Valvocopula, with a pars exterior varying between 12.6-20 µm high, bears areolae arranged in almost vertical rows ( +Figs. 6 +a-b). There is a more conspicuous row of coarser and regularly arranged areolae of 2 µm diameter adjacent to the valve mantle ( +Figs. 6 +a-b). The copulae, with a pars exterior varying between 24-30 µm heigh, bear areolae arranged in diagonal rows ( +Figs. 6 +a-b). Sometimes, at the corners of copulae the pattern of the areolae seems slightly disturbed ( +Figs. 6 +a-b). All girdle elements observed (valvocopula and copulae) have a hyaline abvalvar margin 3-4 µm deep. + + +In girdle and oblique views the mantle margin appears slightly undulate ( +Figs. 4e +, +6a +). + + + +Holotype +: +Figs. 3a,b +, +MNHN +.F. F62406 ( +Muséum National d’Histoire Naturelle +, +Paris +, +France +) + + + + +Isotype +1: +Figs. 3c,d +, +MNHN +.F. F62407 ( +Muséum National d’Histoire Naturelle +, +Paris +, +France +) + + + + +Isotype +2: +Fig. 3e +, +MNHN +.F. F62408 ( +Muséum National d’Histoire Naturelle +, +Paris +, +France +) + + + + +Isotype +3: +Fig 3f +, +MNHN +.F. F62409 ( +Muséum National d’Histoire Naturelle +, +Paris +, +France +) + + +Dimensions. Length of sides of the outer triangle 150-200 µm. + +Remarks. Study of + +Entogonia + +specimens recorded in the three stratigraphic levels mentioned above has proven that all of them belong to a single species, + +Entogonia briggeri + +n. sp. +, that has many characters in common with both + +Entogonia hungarica +Holmes & Brigger, 1979 + +( +Holmes & Brigger, 1979 +, p. 182, figs. 66-72) and + +Entogonia formosa +(Truan & Witt) Bergon 1892 + +( +Holmes & Brigger, 1977 +, fig. 55-57; 1979, p. 179, figs 54-57, 58- 59). + + + + + +Entogonia briggeri + +n. sp. +resembles very much + +E. hungarica + +Holmes & Brigger, +1979 + + +in the morphology of the outer triangle, shape of the inner triangle and sometimes the ratio between the diameter of the exit pores and of the elevations. However, the diameter of the exit pores is generally smaller in this species than in + +E. hungarica + +. The most evident difference from the latter species regards the costae of the inner triangle, which are here and there absent or interrupted in + +E. hungarica + +, leaving areas without costae. Also, in + +E. hungarica + +there is no hyaline central area onto the inner triangle, at the origin of the internal costae, as we observed in + +E. briggeri + +n. sp. +Another evident difference concerns a row of enlarged pores which occur between the internal costae on the valve mantle. This character is present in + +E. briggeri + +and absent in + +E +. +hungarica + +. + + + +Entogonia briggeri + +n. sp. +is wholly comparable with the early Middle Eocene specimens from Conset, +Barbados +, assigned to + +E. formosa +(Truan & Witt) Bergon + +by +Holmes & Brigger (1977 +, fig. 55-57), from which it differs especially in the greater number of costae in the inner triangle, denser areolae in the outer triangle, and in the presence of enlarged pores which occur between to the internal costae on the valve mantle. These pores, as observed by +Holmes & Brigger (1979) +, are characteristic in some species as for instance: + +Entogonia amabilis +Greville, 1863 + +, + +E +. +marginata +(Bright.) Greville, 1863 + +, + +E. pulcherrima +(Greville) Greville, 1863 + +, + +E. reinholdii +Holmes & Brigger, 1979 + +, + +E. robinsonii +Holmes & Brigger, 1979 + +. + + +Range and occurrence. Upper Middle Miocene, (lower part of Upper Badenian = Kossovian substage): Radiolarian Shale Formation from Getic Depression: Tilvici Valley, Păuşeşti Otăsău village, and Valea Sărată (Salted Valley), Ocnele Mari village, both in Râmnicu +Vâlcea district +, +Romania +; also lower Sarmatian (late Vohynian) from Borod Basin, +Romania +. + + + + +Type locality. Tilvici valley, Păuşeşti Otăsău village, Râmnicu +Vâlcea district +, +Romania + + +Etymology. The species is dedicated to A. L. Brigger to honor his contribution to the knowledge of the genus + +Entogonia +. + + + + + \ No newline at end of file diff --git a/data/FF/13/87/FF1387C3C315256013E8F47DFB18FED8.xml b/data/FF/13/87/FF1387C3C315256013E8F47DFB18FED8.xml new file mode 100644 index 00000000000..1e922719fb2 --- /dev/null +++ b/data/FF/13/87/FF1387C3C315256013E8F47DFB18FED8.xml @@ -0,0 +1,212 @@ + + + +New Trees Identified In The Petrified Forest Of Middle Miocene From Zarand, Apuseni Mountains, Romania. + + + +Author + +Iamandei, Stănilă +* Geological Institute of Romania (GIR), 1 Caransebeş Street, 012271 - Bucharest, Romania, iamandei @ gmail. com +iamandei@gmail.com + + + +Author + +Iamandei, Eugenia +* Geological Institute of Romania (GIR), 1 Caransebeş Street, 012271 - Bucharest, Romania, iamandei @ gmail. com +iamandei@gmail.com + +text + + +Acta Palaeontologica Romaniae + + +2017 + +2018-03-16 + + +13 + + +2 + + +37 +90 + + + +journal article +1842-371x + + + + + + +Aceroxylon zarandense + +sp. nov. + + + + + +Fig. 17 +, photos a-i. + + + + +Material + + +From a sample of dispersed petrified wood (field number 26), collected from Prăvăleni area from the left side of Prăvăleni valley at the confluence with BodiȘteanu brook from Mid-Miocene volcano-sedimentary deposits (Late Badenian-Early Sarmatian). The centimetric sized samples representing a silicified wood fragment of whitish-beige color with brownish and is kept now in +GIR +collection at National Geological Museum - +Bucharest +under the inventory number 26,279 (field number: 26). Under the magnifying glass fibrous structure can be seen, distinct annual rings, short thin and sinuous medullary rays, and vessels, typical for a dicotyledonate wood. + + +Microscopic description + + +The growth rings +are relatively distinct in cross section, not very wide, the boundary marked by the presence of a terminal wood made up of mainly ground tissue. Otherwise, the structure is diffuse-porous, smaller vessels appear only in the close proximity of the terminal wood, and the rays are slightly dilated at the boundaries of the annual rings. + + +The vessels +in cross section are solitary and in radial multiples of 2-3, or groups of 4-5 pores. The solitary ones have an oval or circular cross section and show sometimes solid brown deposits. The walls are moderately thick of 4-8.5 μm double wall. The radial / tangential diameters for solitary pores are of 42-75(84)/42-51(60) µm and their density is 35-60(85) vessels per mm +2 +. The vessels have simple perforations on inclined plates. The vertical walls of vessels, especially of those vessels with lower lumen, exhibit relatively thick spiral thickenings, with repeated and obvious turns. Rounded to oval bordered pitting, relatively numerous, small of 4-7 μm, alternate to sub-opposite without touching each other, with circular apertures of 2-3.5 μm in diameter horizontally elongated or point like. The average length of the vascular elements is 500-640 μm. Inside vessels, rarely large thin walled tyloses appear. + + +The axial parenchyma +- is of apotracheal +type +, a few short or long uniseriate lines interleaved with fibers, constituting the terminal bands of 3-4 cells thick, which are marking the distinct boundary of the growth ring. It occurs also diffuse, as cells dispersed among the fibers within the annual ring, and also as vasicentric uniseriate. In the longitudinal sections the parenchyma consists of nearly square empty rectangular cells in vertical strands of over 8 cells, pitted and sometimes with solitary crystals. + + +The medullary rays +- in cross section appear 1-3(4)- seriate, and have a special behavior: the thicker rays have continuity on 2-3 annual rings, the uniseriates have continuity only on an annual ring. Near the vessels they have a slight inflection and may come in contact with them, but generally have a linear trajectory, and the thicker ones show a slight dilation at the boundary of the growth ring. Also, the cells have a dark content. In tangential section, the uniseriates appear relatively numerous, they have 3- 12 cells in height (up to 125 μm), the ray cells round or slightly vertically elongated, mixed. The 2-4-seriates rays have 15-77 cells in height, that is, 192-500 μm and have uniseriate endings of 1-8 rounded cells, the last being narrower and elongated. The ordinary ray body cells tend to be more rounded and more equal in size (8-11 μm), and contain residual gums. Sometimes marginal, noticeably larger rounded cells (of 15-24 μm in diameter) and brighter, which appear to be mucilaginous cells. The frequency is 8-10 rays per horizontal tangential mm. Radially the rays are homocellular, formed from procumbent cells whose length varies from the early to late wood, when the cells can be squared with the same height. Ray cells have very small spaced pits of 2 μm on two rows in the early wood, or a single, larger, round or oval pit with small circular aperture, in the late wood. Sometimes, the ray cells contain large, solitary crystals. + + +The fibers +have a polygonal cross section of 15-20 μm in diameters, relatively thick walled of 4-6 μm, especially in the late wood made up of 6-10 radial rows. Vertically are pitted and sometimes have long rows of crystals. + + +Affinities and discussions + + +The xylotomical characters observed in this specimen are very similar to those described by Metcalfe & Chalk (1950), +Greguss (1959) +, and Schweingruber (1990) for members of the former +Aceraceae +family, especially of + +Acer + +type +, now belonging to the +Sapindaceae +family, the +Hippocastanoideae +subfamily ( +APG IV, 2016 +). + + +We do not repeat the discussion on the affinities of the specimens described above to whom also we have seen similitudes, but note the description of the generic xylotomic characters of the + +Acer + +genus from Schweingruber (1990), which is more similar to our specimen description: the obvious growth rings, marked by some rows of flattened fibers, the diffuse-porous wood, with spaced solitary pores or as short multiples, with simple perforations, alternate pitting and spiral thickenings with diffuse apotracheal parenchyma, occasionally paratracheal, rarely terminal, slightly dilated rays at the ring boundary, 1-3-5(6)-seriate, of 40-50(60) cells high, homocellular, cells all procumbent, rarely marginals square with increased pits. + + + +Comparing the xylotomy of our specimen with the fossil aceraceous species previously described, including the species described in this paper, we think we have studied here a wood structure more similar in terms of distribution and shape of the vessels, parenchyma, fibers and rays, the +type +of perforations, pitting and spiral thickenings with the current species + +Acer cappadocicum +Gled + +, a species with a living area comprising the southern regions of +Central +and +Eastern Europe +and +Asia +, a maple native to central +Turkey +(ancient Cappadocia), east along the +Caucasus +, the +Hymalaya +, to southwestern +China +, areas marked by a temperate to warm-temperate climate up to the subtropical of the +Mediterranean +wetlands + +. + + +An advanced comparison with respect to other fossil forms described until present maybe could suggest a possible identification, but in the present case we believe we are in the face of a new species, which we named + +Aceroxylon zarandense + +sp. nov. +, according to the name of the region where it was found the +holotype +(inv. no. 26,279), as a fossil equivalent of the extant maple + +Acer cappadocicum + +. The material studied here was initially wrongly identified as a member of the +Meliaceae +family (Iamandei & Iamandei, 1998), with which it has possibly similar features, but the revision of the original material and the taxonomic reidentification, have denied the assignment of this specimen to the + +Carapoxylon +cf. +porosum +(Felix) Mädel, 1960 + +. + + + + +Diagnosis of + +Aceroxylon zarandense + +sp. nov. + + +( + +Holotype +: inv. no.: 26,279 kept now in +GIR +collection at +National Geological Museum +- +Bucharest +) + +. + + +Secondary wood diffuse-porous with relatively distinct growth rings, marked by slightly flattened terminal fibers and dilated rays at ring boundary. Vessels solitary and in radial groups of 2-3(5), the solitary oval or circular in cross section, of 42-75(84) / 42-51(60) µm, and thick-walled of 4-8.5 μm double wall, density of 35-60(85) vessels on mm +2 +, simple perforations, spiral thickenings frequent and relatively thick, bordered pitting, pits round to oval, numerous, alternate to sub-opposite without touching each other, small of 4-7 μm, with circular apertures of 2-3.5 μm to horizontally elongated, or point like. The vascular elements have 500-640 μm in length, large thin-walled tyloses inside and solitary crystals or colored crystal-sand. Parenchyma apotracheal diffuse, as short or long uniseriate bands interleaved in the latest wood, and rarely paratracheal. Vertically the parenchyma appears as near square empty cells in vertical strands of 2-4 cells, sometimes pitted and with crystals. Rays 1-4-seriate, the uniseriates of 3-12 cells tall, the 2-4-seriates fusiform, of 15-77 cells tall, with endings of 1-8 cells. In the ray-body sometimes larger mucillaginous cells appear. Ray frequency is of 8-10 rays on tangential mm. Rays homocellular, with ray-cells all procumbent, sometimes square, with spaced simple, very small pits, of 2 μm, on two rows arranged in the cross-fields with vessels and with solitary crystals. The fibers have polygonal section of 15-20 μm in diameter, thick walls, spiral thickenings, septa, and rare, small, simple pitting in a vertical row. + + + + \ No newline at end of file diff --git a/data/FF/13/87/FF1387C3C31E256F104EF6D8FE0EFAF2.xml b/data/FF/13/87/FF1387C3C31E256F104EF6D8FE0EFAF2.xml new file mode 100644 index 00000000000..49637fc5dfb --- /dev/null +++ b/data/FF/13/87/FF1387C3C31E256F104EF6D8FE0EFAF2.xml @@ -0,0 +1,207 @@ + + + +New Trees Identified In The Petrified Forest Of Middle Miocene From Zarand, Apuseni Mountains, Romania. + + + +Author + +Iamandei, Stănilă +* Geological Institute of Romania (GIR), 1 Caransebeş Street, 012271 - Bucharest, Romania, iamandei @ gmail. com +iamandei@gmail.com + + + +Author + +Iamandei, Eugenia +* Geological Institute of Romania (GIR), 1 Caransebeş Street, 012271 - Bucharest, Romania, iamandei @ gmail. com +iamandei@gmail.com + +text + + +Acta Palaeontologica Romaniae + + +2017 + +2018-03-16 + + +13 + + +2 + + +37 +90 + + + +journal article +1842-371x + + + + + + +Piranheoxylon perfectum + +sp. nov. + + + + + +Fig. 15 +, photos a-i. + + + + +Material + + +From a sample of dispersed petrified wood collected from Prăvăleni area, from Cremenea Hill (field number 171) from Mid-Miocene volcano-sedimentary deposits (Late Badenian-Early Sarmatian). The centimetric sized sample represent a silicified wood fragment of beige color or beige with rusty tint and is kept now in +GIR +collection at National Geological Museum - +Bucharest +under the inventory number 26,354 (field number: 171). Under the magnifying glass fibrous structure, less distinct annual rings and visible vessels and rays can be observed, suggesting dicotyledonate wood. + + + +Fig. 18 + +Aceroxylon pravalense + +sp.nov. +a - cross section: semi-ring-porous wood, solitary vessels, fine to broad rays, less distinct ring boundary - x50; b, c - cross-section: fine and multiseriate rays, solitary vessels, less distinct ring boundary - x100; d, e, f - tangential section: fine and multiseriate fusiform rays, vessels with almost horizontal simple perforated plates - x100; g, h, i - radial section: simple perforations (g), bad preserved opposite pitting (h) cystalliferous cross-field (i) - x200. + + + +Microscopic description + + +The growth rings +are less distinct in the secondary wood, slightly marked by terminal (latest) parenchyma as tangential discontinuous bands of 2-9 cells thick, devoid of vessels and rays slightly dilated at the limit of the annual ring. Some local traumatic aspects (as disorganizations) disturb the porous wood structure. + + +The vessels +are usually solitary and in radial multiples also or irregular groups of 2-5, sometimes with tangential pairs included, defining a porous wood +type +. Sometimes the vessels are separated by a short radial row tracheid, or radially continue with 1-5 smaller vessels or vascular tracheid. The solitary vessels have polygonal-rounded or oval shape, sometimes irregular or star like, even crushed in the disorganized areas. The vascular walls are moderately thick, of 4-8 μm double wall. The lumen of solitary vessels has the radial / tangential diameters of 40-80(96) / 40-50 μm (mean values: 52 / 42 μm). The pores' size is relatively constant within a growth ring, from which the appearance of diffuse-porous wood and the density is 64- 90 pores per mm +2 +. The vessels have scalariform perforations relatively high, with 8-30 bars, sometimes corrugat- ed, with bifurcations and vertical anastomoses. The pitting is scalariform or with oval bodered pits, opposite or horizontally elongated, often coalescent to scalariformes and numerous, especially on the the vessel endings, since the vascular elements have length of 450-975 μm and present high "tails". Sometimes very short vessel elements, of 80-90 μm, appear. Frequently spiral thickenings on the narrower vessels appear and also on the vessel tails and even on the thicker vessel body. On some vessels, rare, large tyloses appear and content of granular gums isolated or agglomerated up to compact, clogging the lumen. In addition, fungi as hyphae and fruiting corps appear. + + +The axial parenchyma +- is very few, diffuse or of scanty-paratracheal +type +as 1-2 (3) cells, crushed to the vessels, and as discontinuous bands of 2-9 cells in the latest wood, sometimes with cells wider than the fibers. Vertically is relatively difficult to detect, it occurs in strands of 6-8 vertical rectangular thin-walled cells, with rare simple pits, irregularly arranged. The terminal parenchyma appears as bundles of numerous rectangular vertical cells (more than 16), storied. Sometimes dark granular gumremains of and hyphae and fruiting corps of fungi are present. Dispersed among the fibers, chambered cells with rounded solitary crystals inside appear. + + +The medullary rays +are uni- or biseriate, rarely triseriate, and in cross section appear constituted by radially elongated rectangular cells. The rays have linear trajectory and slight dilations and deviations at the annual ring boundary, and sometimes touch vessels. Tangentially they are frequently tall, of 2-52 cells in height or more (i.e. up to 1270 μm), compact and rarely articulated. The uniseriate rays have sometimes short biseriate storeys, with pairs of the same thickness as the uniseriate part. The ray-body cells appear rounded to polygonal and the uniseriate endings consist of 1-12 vertically elongated cells, the last being more elongated triangular. The frequency is 7-10 rays per mm tangential. Radially the rays are heterocellular, the ray-body cells having all procumbent cells, of 16-18 μm in height, and the marginals slightly higher or even upright, of 18-32 μm. In the cross fields with vessels the pitting is round or elliptical, to scalariform of 5-6.5 / 8-11 μm especially on marginal fields. In the ray cells also 1-3 crystals or more and gum remains appear. + + +The fibers +- in cross section appear arranged in 1-15 radial rows between two successive rays. The fiber cells are moderately thick-walled, 4-5.5 μm double wall, and have a polygonal section rounded at the corners, causing frequent triangular or rhombic intercellular spaces, and have large polygonal-rounded lumina, of 8-25 μm. Often there are narrower fibers dispersed among the others, which sometimes can be confused with the intercellular spaces, since often they +form discontinuous +radial rows. In the areas with disorganized structure the fibers are also deformed, even crushed. Vertically, inside fibers, the septa are rare, and the longitudinal walls have rare pits in an irregular row. + + +The fibrotracheids +have vertical bordered oval pitting to slightly horizontally elongated, even scalariform on the +vascular tracheids +of the rows with narrow vessels from the complex multiples of large vessels already observed in the cross section. They are obviously wider than the ordinary fibers and even the length of the tracheidal elements is smaller (length 40-250 μm, diameter 15-28 μm). + + +Affinities and discussions + + +The xylotomic characters of the studied specimen are similar to those of the "euphorbiaceous" woods of "phyllanthoideae group" +type +as it is presented in Metcalfe & Chalk (1950) and in +Mädel (1962) +, and in a first instance would appear that genus + +Securinega + +is xylotomically similar to our specimen since it presents scalariform perforations, but also another "euphorbiaceous" genus, namely + +Piranhea + +. However, using the old taxonomy Metcalfe & Chalk 1950 (p. 1222) separated the Phyllanthoidee from a group of special characters (called "other phyllantoideae") that includes the current genera + +Piranhea +, +Uapaca +, +Savia +, +Androstachys +, +Breynia, Dissilaria +, +Longetia +, +Mischodon +, +Oldfieldia +, +Petalostigma + +, whose xylotomic characters appear to match those of our specimen. + + +Comparing our specimen with the fossil correspondent genus + +Piranheoxylon +Grambast, 1961 + +which was created based on a species described from the Eocene of +Belgium +( + +Piranheoxylon stockmansi +Grambast, 1961 + +), we found many similitudes related to the shape, size and distribution of the vessels in cross-section, the +types +of pitting and the perforations, the +type +of parenchyma and the presence of the crystalliferous chambered parenchyma cells, the +type +, the height and the cellular composition of the rays as well as the appearance of the fibers. + +Our specimen has also some specific characters such as follows: the presence of growth rings marked by 2-9 cell parenchymal terminal bands, the slight dilation of the rays at the ring boundary, the predominant scalariform pitting, spiral thickenings on the vessel tails, on the narrow and on the large vessels also, the crystalliferous unchambered ray-cells, ray usually biseriate, higher, with elliptic to scalariform pitting on the marginal cross fields, fibers thick-walled, with polygonal-rounded section, oval elongated to scalariform pitted. + +Following this critical discussion we believe that the studied specimen is a new species which we have named + +Piranheoxylon perfectum + +sp. nov. +, for the perfection of the anatomical details offered. + + + + + +Diagnosis of + +Piranheoxylon perfectum + +sp. nov. +: + +Porous wood with less distinct growth rings and terminal parenchyma. Solitary vessels and in radial multiples with indentations, and in irregular groups of 2-5 small vessels and tracheids, fibrotraheides. Solitary vessels roundedpolygonally shaped, to oval or irregularly star-like with moderate thick walls, radial/tangential diameters of 52/42 μm, density of 64-90 pores on mm +2 +. Scalariform perforations, storied, with 8-30 thin bars, corrugated, bifurcated and anastomosed. Intervascular pitting scalariform or oval bordered to horizontally elongate up to scalariform pits. Vascular elements length of 450-975 μm, having spiral thickenings on the high tails and tyloses. Parenchyma diffuse, scanty-paratracheal and in discontinuous bands in the latest wood. Storied vertical strands of 6-8- 16 cells with simple pitted walls, and chambered with rounded crystals inside. Rays 1-2(3)-seriate, with platanoid dilations, of 2-52 cells in height, uniseriate, with short biseriate storeys of the same size as uniseriate. Radially the ray cells appear all procumbent, with 1-12 marginal rows of slightly higher or even upright cells and with round or elliptical pits to scalariformes. Ray frequency is 7-10 rays on tangential mm. Often 1-3 or more crystals on fields and gums appear. Fibers with rounded polygonal large section of lumens (8-25μm), relatively thick walled, severed, rare septa and irregular pitting. Fibrotracheids and vascular tracheids with oval bordered pits, elongated to scalariformes. + + + + \ No newline at end of file