diff --git a/data/03/D7/84/03D78450FFE2D5738A1250C7C0F77942.xml b/data/03/D7/84/03D78450FFE2D5738A1250C7C0F77942.xml index 20531ecd300..7fb9205b059 100644 --- a/data/03/D7/84/03D78450FFE2D5738A1250C7C0F77942.xml +++ b/data/03/D7/84/03D78450FFE2D5738A1250C7C0F77942.xml @@ -1,60 +1,63 @@ - - - -Fig. 4 in Fig. 22 in Paralbunea dayriti + + + +Fig. 4 in Fig. 22 in Paralbunea dayriti - - -Author + + +Author -Stec, Daniel -Institute of Zoology and Biomedical Research, Jagiellonian University, Gronostajowa 9, 30 - 387 Kraków, Poland. +Stec, Daniel +Institute of Zoology and Biomedical Research, Jagiellonian University, Gronostajowa 9, 30 - 387 Kraków, Poland. - - -Author + + +Author -Dudziak, Magdalena -Institute of Zoology and Biomedical Research, Jagiellonian University, Gronostajowa 9, 30 - 387 Kraków, Poland. +Dudziak, Magdalena +Institute of Zoology and Biomedical Research, Jagiellonian University, Gronostajowa 9, 30 - 387 Kraków, Poland. - - -Author + + +Author -Michalczyk, Łukasz -Institute of Zoology and Biomedical Research, Jagiellonian University, Gronostajowa 9, 30 - 387 Kraków, Poland. +Michalczyk, Łukasz +Institute of Zoology and Biomedical Research, Jagiellonian University, Gronostajowa 9, 30 - 387 Kraków, Poland. -text - - -Zoological Studies +text + + +Zoological Studies - -2020 - -Zool. Stud. + +2020 + +Zool. Stud. - -2020-07-02 + +2020-07-02 - -59 + +59 - -23 + +23 - -1 -25 + +1 +25 - -http://dx.doi.org/10.5281/zenodo.12822113 + +http://dx.doi.org/10.5281/zenodo.12822113 -journal article -10.6620/ZS.2020.59-23 -1810-522X +journal article +10.6620/ZS.2020.59-23 +1810-522X +PMC7689055 +33262846 +12822226 @@ -72,7 +75,7 @@ Dudziak, Stec & Michalczyk ( -Figs. 9–13 +Figs. 9–13 , Tables 4–5 ) @@ -742,7 +745,7 @@ and Etymology : We take great pleasure in dedicating this new species to Filip Dudziak, son of the second author. - + Fig. 1. @@ -752,7 +755,7 @@ and , habitus and cuticular pores (PCM). A, dorso-ventral projection (holotype, Hoyer’s medium); B–C, cuticular pores on the dorso-cephalic (B) and dorso-caudal (C) part of the body. Scale bars in μm. - + Fig. 2. @@ -769,15 +772,15 @@ and (measurements and statistics in Table 4 ): Before mounting in Hoyer’s medium, body almost transparent in juveniles and white in adults, eyes absent; after fixation on microscope slides body transparent ( -Fig. 9A +Fig. 9A ). Body cuticle covered with fine granulation clearly visible on the dorsal side of the caudal body region ( -Fig. 9B +Fig. 9B ). On legs I–III, a patch of fine granulation is placed on the external surface of the legs, near the claws ( -Fig. 9C +Fig. 9C ), whereas granulation on legs IV extends from the claws onto the entire dorsolateral surface of the legs, being denser towards the claws ( -Fig. 9E +Fig. 9E ). A pulvinus is present on the internal surface of legs I–III ( -Fig. 9D +Fig. 9D ). @@ -787,9 +790,9 @@ Claws slender, of the type . Primary branches with distinct accessory points, a long common tract, and with an evident stalk connecting the claw to the lunula ( -Fig. 10A–B +Fig. 10A–B ). Lunulae on all legs smooth ( -Fig. 10A–B +Fig. 10A–B ). Bars under claws absent. @@ -799,28 +802,28 @@ Mouth antero-ventral, bucco-pharyngeal apparatus of the type ( -Fig. 11A +Fig. 11A ). The oral cavity armature well-developed and composed of three bands of teeth ( -Fig. 11B–E +Fig. 11B–E ). The first band of teeth comprises numerous small granules arranged in a several rows situated anteriorly in the oral cavity, just behind the bases of the peribuccal lamellae ( -Fig. 11B–E +Fig. 11B–E ). The second band of teeth is situated between the ring fold and the third band of teeth, and is composed of ridges parallel to the main axis of the buccal tube ( -Fig. 11B– E +Fig. 11B– E ). The teeth of the third band are located within the posterior portion of the oral cavity, between the second band of teeth and the buccal tube opening ( -Fig. 11B– E +Fig. 11B– E ). The third band of teeth is divided into the dorsal and the ventral portion. Under PCM , both dorsal and ventral teeth are visible as two lateral and one median transverse ridges ( -Fig. 11B–E +Fig. 11B–E ). The ventro-median tooth is divided into two roundish teeth of which one is sometimes larger ( -Fig. 11C, E +Fig. 11C, E ). Pharyngeal bulb spherical, with triangular apophyses, three rod-shaped macroplacoids and a microplacoid clearly distant (more than its length) from the third macroplacoid ( -Fig. 11A, F–G +Fig. 11A, F–G ). The macroplacoid length sequence is 2 <1 <3. The first macroplacoid is anteriorly narrowed and the third has a subterminal constriction ( -Fig. 11F–G +Fig. 11F–G ). - + Fig. 3. @@ -830,7 +833,7 @@ Mouth antero-ventral, bucco-pharyngeal apparatus of the , claws (paratypes). A–B, claws III (A) and IV (B) seen in PCM; C–D, claws I (C) and IV (D) seen in SEM. Filled flat arrowheads indicate double muscle attachments under the claws. Scale bars in μm. - + Fig. 4. @@ -849,33 +852,33 @@ type ( (measurements and statistics in Table 5 ): Laid freely, white, spherical with conical processes with the elongated terminal portion terminated with a small concave disc with an irregular edge ( -Figs. 12A–F +Figs. 12A–F , -13A– F +13A– F ). The labyrinthine layer between the process walls is visible under PCM as a reticular pattern with slightly sinuous margins ( -Fig. 12A–B +Fig. 12A–B ). Eight to ten areoles are present around each process ( -Figs. 12A–B +Figs. 12A–B , -13A–B +13A–B ). The surface of the areoles is sculptured and porous ( -Figs. 12A–B +Figs. 12A–B , -13A–D +13A–D ). Pores large and visible both under PCM and SEM ( -Figs. 12A–B +Figs. 12A–B , -13A–D +13A–D , respectively). The ridges separating each areole are narrower than the areole diameter ( -Figs. 12A–B +Figs. 12A–B , -13A–D +13A–D ). @@ -900,7 +903,7 @@ haplotype 2 sequence (GenBank: MT 260373), 658 bp long. - + Fig. 5. diff --git a/data/03/D7/84/03D78450FFEAD571898750C7C73979C2.xml b/data/03/D7/84/03D78450FFEAD571898750C7C73979C2.xml index 07c433928ca..d929bc7cb02 100644 --- a/data/03/D7/84/03D78450FFEAD571898750C7C73979C2.xml +++ b/data/03/D7/84/03D78450FFEAD571898750C7C73979C2.xml @@ -1,62 +1,65 @@ - - - -Fig. 4 in Fig. 22 in Paralbunea dayriti + + + +Fig. 4 in Fig. 22 in Paralbunea dayriti - - -Author + + +Author -Stec, Daniel -Institute of Zoology and Biomedical Research, Jagiellonian University, Gronostajowa 9, 30 - 387 Kraków, Poland. +Stec, Daniel +Institute of Zoology and Biomedical Research, Jagiellonian University, Gronostajowa 9, 30 - 387 Kraków, Poland. - - -Author + + +Author -Dudziak, Magdalena -Institute of Zoology and Biomedical Research, Jagiellonian University, Gronostajowa 9, 30 - 387 Kraków, Poland. +Dudziak, Magdalena +Institute of Zoology and Biomedical Research, Jagiellonian University, Gronostajowa 9, 30 - 387 Kraków, Poland. - - -Author + + +Author -Michalczyk, Łukasz -Institute of Zoology and Biomedical Research, Jagiellonian University, Gronostajowa 9, 30 - 387 Kraków, Poland. +Michalczyk, Łukasz +Institute of Zoology and Biomedical Research, Jagiellonian University, Gronostajowa 9, 30 - 387 Kraków, Poland. -text - - -Zoological Studies +text + + +Zoological Studies - -2020 - -Zool. Stud. + +2020 + +Zool. Stud. - -2020-07-02 + +2020-07-02 - -59 + +59 - -23 + +23 - -1 -25 + +1 +25 - -http://dx.doi.org/10.5281/zenodo.12822113 + +http://dx.doi.org/10.5281/zenodo.12822113 -journal article -10.6620/ZS.2020.59-23 -1810-522X +journal article +10.6620/ZS.2020.59-23 +1810-522X +PMC7689055 +33262846 +12822226 - + @@ -95,15 +98,15 @@ from the type series. : According to the original description, the granulation is absent on the first three pairs of legs and lunules IV are faintly dentate. However, our re-examination of the type material revealed the presence of faint granulation present on the external surface of legs I–III in larger animals ( -Fig. 14A +Fig. 14A ) whereas in smaller specimens the granulation can be hardly or even not visible. Moreover, we found that lunules on all the legs are smooth ( -Fig. 14A–B +Fig. 14A–B ). The original description also states that indistinct reticular sculpture is present within the areolae. We confirmed that the areolae surface is sculptured, however only wrinkles are present whereas reticulation or pores are absent or not visible under PCM ( -Fig. 14C–D +Fig. 14C–D ). We also confirmed multiple divisions of the medio-ventral tooth in the third band of teeth into several roundish teeth ( -Fig. 14E–F +Fig. 14E–F ) and the absence or invisibility of the body granulation under PCM . diff --git a/data/03/E4/18/03E41861FFCAFF85FCFCCD2AD0CAFD00.xml b/data/03/E4/18/03E41861FFCAFF85FCFCCD2AD0CAFD00.xml new file mode 100644 index 00000000000..bfa9860267b --- /dev/null +++ b/data/03/E4/18/03E41861FFCAFF85FCFCCD2AD0CAFD00.xml @@ -0,0 +1,247 @@ + + + +Fig. 5 in Paralbunea dayriti + + + +Author + +Monferran, Mateo D. +Centro de Ecología Aplicada del Litoral - CONICET-UNNE and Dpto. Biología - Área Ciencias de la Tierra - FaCENA-UNNE, Ruta Prov. + + + +Author + +Gallego, Oscar F. +Centro de Ecología Aplicada del Litoral - CONICET-UNNE and Dpto. Biología - Área Ciencias de la Tierra - FaCENA-UNNE, Ruta Prov. + + + +Author + +Cabaleri, Nora G. +Instituto de Geocronología y Geología Isotópica, Consejo Nacional de Investigaciones Científicas y Técnicas, Universidad de Buenos Aires, Ciudad Universitaria, C 1428 EHA Buenos Aires, Argentina. E-mail: cabaleri @ ingeis. uba. ar (Cabaleri) +cabaleri@ingeis.uba.ar + +text + + +Zoological Studies + + +2020 + +Zool. Stud. + + +2020-08-05 + + +59 + + +37 + + +1 +11 + + + + +http://dx.doi.org/10.5281/zenodo.12822327 + +journal article +10.6620/ZS.2020.59-37 +1810-522X +PMC7689052 +33262859 +12822507 + + + + + + +Genus + +Wolfestheria +Monferran et al. 2013 + + + + + + + + +Type +species + +: + +Wolfestheria smekali +Monferran et al., 2013 +Cañadón Asfalto Formation + +, + + +Puesto Almada Member, Late Jurassic, +Chubut +, +Argentina +. + + + + +Wolfestheria patagoniensi + +s Tasch (in +Tasch and Volkheimer, 1970 +) comb. nov. + +( +Fig. 4 +) + +urn:lsid:zoobank.org:act: +4740A6B2-B4D5-46F8-B337- 679A535D0372 + + + + + +Fig. 3. + +Carapacestheria taschi +(Vallati) + +from the Las Chacritas Member, Cañadón Asfalto Formation. General carapace morphology; (A) UNPSJB-PI 282 paratype oval valve; (B) UNPSJB-PI 283 oval valve; SEM micrographs: (C) Details of the ornamentation from anterior area; (D) Ornamentation from dorsal area; (E) Details of the mid-dorsal ornamentation; (F) Ornamentation from postero-ventral area; (G) details of the postero-dorsal ornamentation. cr, cross bars; r, reticulate; rl, radial lirae. + + + + + +Cyzicus +( +Lioestheria +) +patagoniensis +Tasch + +(in +Tasch and Volkheimer, 1970 +). + + +Material +: +Holotype +MACN-Pi 4895; +Paratypes +: CTES-PZ-7.690, MEF-PI 1889. + + +Geographic provenance +: +Chubut province +( +Argentina +), Las Chacritas Member, Cañadón Asfalto Formation, Middle Jurassic. Cañadón Asfalto locality GPS: +43°30'4.3"S +, +69°10'34.6"W +. + + +Emended diagnosis +: Carapace medium to large in size with a shape varying from elongated oval to round (elliptical); short and small umbo marginal in submedial to anterior position; dorsal margin short to long, anterior and posterior margins curved to sharply curved; growth bands ornamented with punctae mesh on the dorsal part of the carapace changing to irregular radial lirae with numerous cross-bars. Thick radial lirae with fewer cross-bars restricted to ventral zone of the carapace. Measurements (mm): L = 3.3–5, H = 2.5–4.3, H/L = 0.6–0.86, l = 1.3–3.3, a = 0.3–0.7, b = 1–2, c = 0.8–1.1, d = 1.2–1.3, e = 2–2.6. + + +Description +: The carapace is medium to large in size with an outline varying from elongated oval to round (elliptical). The dorsal margin is short in round forms and long in elongated oval forms. The umbo is short/small marginal ( +0.4 mm +) and projects anterior position. The anterior margin slightly curved to curved and posterior margin is curved to sharply curved (c/d = 0.06–0.2). Growth lines smooth, from +30 to 60 in +number. Growth bands ornamented with evenly distributed punctae mesh (about 5 μm in diameter) on the dorsal-median part of the carapace ( +Fig. 4B–D +), changing to irregular radial lirae (7.5 µm in width) with numerous cross-bars from the median-dorsal to ventral part of the carapace ( +Fig. 4E–F +), and finally the radial lirae is thick (13.3 µm in width) with fewer cross-bars restricted to ventral zone of carapace and the interspaces between the radial lirae are wider (20 µm). + + +Remarks +: + +Wolfestheria patagoniensis + +(Tasch, in +Tasch and Volkheimer, 1970 +) was defined originally by Tasch as + +Cyzicus +( +Lioestheria +) +patagoniensis +Tasch + +(in +Tasch and Volkheimer 1970 +). According to the new SEM images, the morphological features allow us to define this species as belong to the Family +Fushunograptidae +and to the genus + +Wolfestheria + +. This genus was defined by +Monferran et al. (2013) +from the Upper Jurassic Puesto Almada Member of the Cañadón Asfalto Formation. + +Wolfestheria patagoniensis + +show similarities with the +type +species + +W. smekali +Monferran et al., 2013 + +, in that species the outline varying from elongated oval to round and the radial lirae show numerous cross-bars from the median-dorsal to median-ventral part of the carapace changing to fewer cross-bars on ventral part. However, + +W. patagoniensis + +exhibits punctate mesh on the dorsal part, whereas + +W. smekali + +exhibits a lattice-like reticulation originated by abundant cross-bars. Also, in + +W. patagoniensis + +, the irregular radial lirae reach the upper part of the growth bands and the fewer cross-bars are limited to a few growth bands from ventral part of carapace. Comparisons with another fushunograptid genera, +Cratostracus +Huang, 1977, shows different outlines and growth lines pronounced with slightly serrated lower margin ( +Li and Batten 2004 +). + +Qinghaiestheria +Wang, 1983 + +from the Upper Jurassic Hongshuigou Formation in +Qinghai +and the Penglaizheng Formation in +Sichuan +( +Wang 1983 +; +Shen and Chen 1982 +; Li 2004) also has serrate structure along the lower margin of the growth lines. + + + + \ No newline at end of file diff --git a/data/03/F6/87/03F687D3FFF067139533FEEB92D67555.xml b/data/03/F6/87/03F687D3FFF067139533FEEB92D67555.xml new file mode 100644 index 00000000000..a27ecb52c9f --- /dev/null +++ b/data/03/F6/87/03F687D3FFF067139533FEEB92D67555.xml @@ -0,0 +1,197 @@ + + + +Stiatoandricus georgei Cuesta-Porta & Melika & Nicholls & Stone & Pujade-Villar 2022 + + + +Author + +Etilé, Raphaël N’doua + + + +Author + +Bédia, Théophile Aké + + + +Author + +Blahoua, Georges Kassi + + + +Author + +Bi, Gouli Goore + + + +Author + +Kouamelan, Paul Essetchi + + + +Author + +N’Douba, Valentin + +text + + +Zoological Studies + + +2020 + +2020-07-20 + + +59 + + +31 + + +1 +14 + + + + +http://dx.doi.org/10.5281/zenodo.8069124 + +journal article +10.6620/ZS.2020.59-31 +1810-522X +PMC7688398 +33262854 +12822346 + + + + + + + +Daphnia +( +Daphnia +) +longispina +O.F. Müller, 1776 + + + + + + + + +Distribution in +Côte d’Ivoire + +: Buyo Lake ( +Yté et al. 1996 +; +Kouamé et al. 2018 +). + + +Synonyms +: + +Daphne longispina +O.F. Müller 1776 + +; + +Daphnia rectispina +Krøyer 1838 + +; + +Daphnia muelleri +P.E. Müller 1867 + +; + +Daphnia leydigii +Hellich 1874 + +; + +Daphnia centricosa +Hellich 1877 + +; + +Daphnia paludicola +Hellich 1877 + +; + +Daphnia tenuitesta +Sars 1890 + +; + +Daphnia brevipennis +Sars 1890 + +; + +Daphnia hellichi +Stingelin 1895 + +; + +Daphnia rectifrons +Stingelin 1895 + +; + +Daphnia rotundirostris +Burckhardt 1899 + +; + +Daphnia pulchella +Sars 1903 + +; + +Daphnia aspina +Wereschagin 1911 + +. + + +World distribution +: + +D. +( +Daphnia +) +longispina + +is reported in Afrotropical and Palaearctic regions ( +Kotov et al. 2013b +), but also in Europa, Asia, and North Africa ( + +Benzie +2005 + +in +Chatterjee et al. 2013 +; +Jeong et al. 2014 +). + + + + \ No newline at end of file diff --git a/data/03/F6/87/03F687D3FFF0671396D0F91A957C7735.xml b/data/03/F6/87/03F687D3FFF0671396D0F91A957C7735.xml new file mode 100644 index 00000000000..6ebb33a4fcc --- /dev/null +++ b/data/03/F6/87/03F687D3FFF0671396D0F91A957C7735.xml @@ -0,0 +1,126 @@ + + + +Stiatoandricus georgei Cuesta-Porta & Melika & Nicholls & Stone & Pujade-Villar 2022 + + + +Author + +Etilé, Raphaël N’doua + + + +Author + +Bédia, Théophile Aké + + + +Author + +Blahoua, Georges Kassi + + + +Author + +Bi, Gouli Goore + + + +Author + +Kouamelan, Paul Essetchi + + + +Author + +N’Douba, Valentin + +text + + +Zoological Studies + + +2020 + +2020-07-20 + + +59 + + +31 + + +1 +14 + + + + +http://dx.doi.org/10.5281/zenodo.8069124 + +journal article +10.6620/ZS.2020.59-31 +1810-522X +PMC7688398 +33262854 +12822346 + + + + + + + +Daphnia +( +Ctenodaphnia +) +barbata +Weltner, 1898 + + + + + + + + +Distribution in +Côte d’Ivoire + +: Buyo Lake ( +Yté et al. 1996 +; +Kouamé et al. 2018 +). + + +Synonyms +: No synonyms available. + + +World distribution +: + +D. +( +Ctenodaphnia +) +barbata + +is reported from Afrotropical and Palaearctic regions + + +( +Kotov et al. 2013b +). + + + + \ No newline at end of file diff --git a/data/03/F6/87/03F687D3FFF1671295ECFDEA92F47555.xml b/data/03/F6/87/03F687D3FFF1671295ECFDEA92F47555.xml new file mode 100644 index 00000000000..53af78f47c8 --- /dev/null +++ b/data/03/F6/87/03F687D3FFF1671295ECFDEA92F47555.xml @@ -0,0 +1,120 @@ + + + +Stiatoandricus georgei Cuesta-Porta & Melika & Nicholls & Stone & Pujade-Villar 2022 + + + +Author + +Etilé, Raphaël N’doua + + + +Author + +Bédia, Théophile Aké + + + +Author + +Blahoua, Georges Kassi + + + +Author + +Bi, Gouli Goore + + + +Author + +Kouamelan, Paul Essetchi + + + +Author + +N’Douba, Valentin + +text + + +Zoological Studies + + +2020 + +2020-07-20 + + +59 + + +31 + + +1 +14 + + + + +http://dx.doi.org/10.5281/zenodo.8069124 + +journal article +10.6620/ZS.2020.59-31 +1810-522X +PMC7688398 +33262854 +12822346 + + + + + + + +Grimaldina brazzai +Richard, 1892 + + + + + + + + +Distribution in +Côte d’Ivoire + +: Ebrie Lagoon: Dabou (Rham 1964). + + +Synonyms +: No synonyms available. + + +World distribution +: + +Grimaldina brazzai + +has been described from +Gabon +( + +Richard +1892 + +in +Chatterjee et al. 2013 +) and is reported to be from Afrotropical, Australasian, Neotropical, and Oriental regions ( +Kotov et al. 2013b +). + + + + \ No newline at end of file diff --git a/data/03/F6/87/03F687D3FFF1671295FCFB9A95197065.xml b/data/03/F6/87/03F687D3FFF1671295FCFB9A95197065.xml new file mode 100644 index 00000000000..77a288711f5 --- /dev/null +++ b/data/03/F6/87/03F687D3FFF1671295FCFB9A95197065.xml @@ -0,0 +1,153 @@ + + + +Stiatoandricus georgei Cuesta-Porta & Melika & Nicholls & Stone & Pujade-Villar 2022 + + + +Author + +Etilé, Raphaël N’doua + + + +Author + +Bédia, Théophile Aké + + + +Author + +Blahoua, Georges Kassi + + + +Author + +Bi, Gouli Goore + + + +Author + +Kouamelan, Paul Essetchi + + + +Author + +N’Douba, Valentin + +text + + +Zoological Studies + + +2020 + +2020-07-20 + + +59 + + +31 + + +1 +14 + + + + +http://dx.doi.org/10.5281/zenodo.8069124 + +journal article +10.6620/ZS.2020.59-31 +1810-522X +PMC7688398 +33262854 +12822346 + + + + + + + +Macrothrix spinosa +King, 1853 + + + + + + + + +Distribution in +Côte d’Ivoire + +: Buyo Lake ( +Yté et al. 1996 +; +Kouamé et al. 2018 +); low ground at Gagnoa ( +Yté et al. 2009 +). + + +Synonyms +: + +Macrothrix goeldi +Richard 1897 + +; + +Macrothrix squamosa +Sars 1901 + +; + +Macrothrix affinis +Brady 1904 + +; + +Macrothrix dentata +Playfair 1915 + +; + +Macrothrix murati +Gauthier 1939 + +. + + +World distribution +: + +M. spinosa + +is regarded as a circumtropical species ( +Maiphae et al. 2008 +; + +Smirnov +1992 + +in +Chatterjee et al. 2013 +); it is also believed to be widely distributed in Afrotropical, Australasian, Nearctic, Neotropical, +Oriental +, Pacific Ocean islands, and Palaearctic regions, but not from the Antarctic region ( +Kotov et al. 2013b +). + + + + \ No newline at end of file diff --git a/data/03/F6/87/03F687D3FFF167129686FC21903A73D0.xml b/data/03/F6/87/03F687D3FFF167129686FC21903A73D0.xml new file mode 100644 index 00000000000..2ed2768203d --- /dev/null +++ b/data/03/F6/87/03F687D3FFF167129686FC21903A73D0.xml @@ -0,0 +1,136 @@ + + + +Stiatoandricus georgei Cuesta-Porta & Melika & Nicholls & Stone & Pujade-Villar 2022 + + + +Author + +Etilé, Raphaël N’doua + + + +Author + +Bédia, Théophile Aké + + + +Author + +Blahoua, Georges Kassi + + + +Author + +Bi, Gouli Goore + + + +Author + +Kouamelan, Paul Essetchi + + + +Author + +N’Douba, Valentin + +text + + +Zoological Studies + + +2020 + +2020-07-20 + + +59 + + +31 + + +1 +14 + + + + +http://dx.doi.org/10.5281/zenodo.8069124 + +journal article +10.6620/ZS.2020.59-31 +1810-522X +PMC7688398 +33262854 +12822346 + + + + + + + +Ilyocryptus sordidus +Liévin, 1848 + + + + + + + + +Distribution in +Côte d’Ivoire + +: Ebrie Lagoon: Toupah (Rham 1964); Ayame Lake I (Yté et al. 1983). + + +Synonyms +: + +Acanthocercus sordidus +Liévin 1848 + +; + +Iliocryptus aequalis +Romijn 1919 + +; + +Iliocryptus balatonicus +Hankó 1926 + +; + +Iliocryptus inaequalis +Romijn 1919 + +; + +Ilyocryptus alexandrinae +Negrea 1987 + +. + + +World distribution +: This species is distributed in the Northern Palearctic, but close forms are widely distributed worldwide according to +Ghaouaci et al. (2018) +. On the other hand, +Kotov et al. (2013b) +reported it like species from Afrotropical, Nearctic, Neotropical, and Palaearctic regions on the one hand and exclude it from the +Oriental +, Australasian, Pacific Ocean islands, and Antarctic regions. + + + + \ No newline at end of file diff --git a/data/03/F6/87/03F687D3FFF167129687F9C1958677F5.xml b/data/03/F6/87/03F687D3FFF167129687F9C1958677F5.xml new file mode 100644 index 00000000000..2f4bdc5c676 --- /dev/null +++ b/data/03/F6/87/03F687D3FFF167129687F9C1958677F5.xml @@ -0,0 +1,152 @@ + + + +Stiatoandricus georgei Cuesta-Porta & Melika & Nicholls & Stone & Pujade-Villar 2022 + + + +Author + +Etilé, Raphaël N’doua + + + +Author + +Bédia, Théophile Aké + + + +Author + +Blahoua, Georges Kassi + + + +Author + +Bi, Gouli Goore + + + +Author + +Kouamelan, Paul Essetchi + + + +Author + +N’Douba, Valentin + +text + + +Zoological Studies + + +2020 + +2020-07-20 + + +59 + + +31 + + +1 +14 + + + + +http://dx.doi.org/10.5281/zenodo.8069124 + +journal article +10.6620/ZS.2020.59-31 +1810-522X +PMC7688398 +33262854 +12822346 + + + + + + + +Ilyocryptus spinifer +Herrick, 1882 + + + + + + + + +Distribution in +Côte d’Ivoire + +: Ebrie Lagoon (Dabou, Eloka, Bengerville) (Rham 1964); Ayame Lake I (Yté et al. 1983); Buyo Lake ( +Yté et al. 1996 +; +Kouamé et al. 2018 +); Sassandra River main stem ( +Kouamé et al. 2018 +). + + +Synonyms +: + +Ilyocryptus halyi +Brady 1886 + +: + +Ilyocryptus longiremis +Sars 1888 + +; + +Acanthocercus immundus +Ihering 1895 + +; + +Iliocryptus verrucosus +Daday 1905 + +; + +Iliocryptus tetraspinatus +Bergamin 1939 + +. + + +World distribution +: + +Ilyocryptus spinifer + +is signaled as widely distributed in the tropics and subtropics ( +Kotov and Dumont 2000 +). On the other hand, +Kotov et al. (2013b) +reported it to be like species from Afrotropical, Australasian, Nearctic, Neotropical, +Oriental +, Pacific Ocean islands, and Palaearctic regions, and excludes only the Antarctic region. According to +Sousa and Elmoor-Loureiro (2019) +, + +I. spinifer + +is a cosmopolitan species with high ecological plasticity. + + + + \ No newline at end of file diff --git a/data/03/F6/87/03F687D3FFF1671D95ECF9BA937A7775.xml b/data/03/F6/87/03F687D3FFF1671D95ECF9BA937A7775.xml new file mode 100644 index 00000000000..a78833a814b --- /dev/null +++ b/data/03/F6/87/03F687D3FFF1671D95ECF9BA937A7775.xml @@ -0,0 +1,125 @@ + + + +Stiatoandricus georgei Cuesta-Porta & Melika & Nicholls & Stone & Pujade-Villar 2022 + + + +Author + +Etilé, Raphaël N’doua + + + +Author + +Bédia, Théophile Aké + + + +Author + +Blahoua, Georges Kassi + + + +Author + +Bi, Gouli Goore + + + +Author + +Kouamelan, Paul Essetchi + + + +Author + +N’Douba, Valentin + +text + + +Zoological Studies + + +2020 + +2020-07-20 + + +59 + + +31 + + +1 +14 + + + + +http://dx.doi.org/10.5281/zenodo.8069124 + +journal article +10.6620/ZS.2020.59-31 +1810-522X +PMC7688398 +33262854 +12822346 + + + + + + + +Macrothrix triserialis +Brady, 1886 + + + + + + + + +Distribution in +Côte d’Ivoire + +: Ebrie Lagoon: Dabou, Toupah, Bengerville (Rham 1964); Buyo Lake ( +Yté et al. 1996 +; +Kouamé et al. 2018 +); Sassandra River main stem and Lobo River ( +Kouamé et al. 2018 +). + + +Synonym +: + +Macrothrix chevreuxi +Guerne and +Richard 1892 + +. + + +World distribution +: + +M. triserialis + +is considered a tropical and subtropical cladocera species (Dumont et al. 2002); it is also believed to be from Afrotropical, Australasian, Neotropical, +Oriental +, and Pacific Ocean islands regions ( +Kotov et al. 2013b +). + + + + \ No newline at end of file diff --git a/data/03/F6/87/03F687D3FFF367109682FC4B909072D5.xml b/data/03/F6/87/03F687D3FFF367109682FC4B909072D5.xml new file mode 100644 index 00000000000..a24874ecee9 --- /dev/null +++ b/data/03/F6/87/03F687D3FFF367109682FC4B909072D5.xml @@ -0,0 +1,125 @@ + + + +Stiatoandricus georgei Cuesta-Porta & Melika & Nicholls & Stone & Pujade-Villar 2022 + + + +Author + +Etilé, Raphaël N’doua + + + +Author + +Bédia, Théophile Aké + + + +Author + +Blahoua, Georges Kassi + + + +Author + +Bi, Gouli Goore + + + +Author + +Kouamelan, Paul Essetchi + + + +Author + +N’Douba, Valentin + +text + + +Zoological Studies + + +2020 + +2020-07-20 + + +59 + + +31 + + +1 +14 + + + + +http://dx.doi.org/10.5281/zenodo.8069124 + +journal article +10.6620/ZS.2020.59-31 +1810-522X +PMC7688398 +33262854 +12822346 + + + + + + + +Euryalana orientalis +Daday, 1898 + + + + + + + + +Distribution in +Côte d’Ivoire + +: Ayame Lake I (Yté et al. 1983). + + +Synonyms +: + +Alonopsis orientalis +Daday 1898 + +; + +Euryalona occidentalis +Sar 1901 + +. + + +World distribution +: According to +Kotov et al. (2013a) +, + +E. orientalis + +is a very characteristic circumtropical species, but it is reported as species from the Afrotropical, Australasian, Neotropical, +Oriental +regions by +Kotov et al. (2013b) +. + + + + \ No newline at end of file diff --git a/data/03/F6/87/03F687D3FFF467169537FE21904A7495.xml b/data/03/F6/87/03F687D3FFF467169537FE21904A7495.xml new file mode 100644 index 00000000000..795e75c193c --- /dev/null +++ b/data/03/F6/87/03F687D3FFF467169537FE21904A7495.xml @@ -0,0 +1,194 @@ + + + +Stiatoandricus georgei Cuesta-Porta & Melika & Nicholls & Stone & Pujade-Villar 2022 + + + +Author + +Etilé, Raphaël N’doua + + + +Author + +Bédia, Théophile Aké + + + +Author + +Blahoua, Georges Kassi + + + +Author + +Bi, Gouli Goore + + + +Author + +Kouamelan, Paul Essetchi + + + +Author + +N’Douba, Valentin + +text + + +Zoological Studies + + +2020 + +2020-07-20 + + +59 + + +31 + + +1 +14 + + + + +http://dx.doi.org/10.5281/zenodo.8069124 + +journal article +10.6620/ZS.2020.59-31 +1810-522X +PMC7688398 +33262854 +12822346 + + + + + + + +Bosmina +( +Bosmina +) +longirostris +O.F. Müller, 1776 + + + + + + + + +Distribution in +Côte d’Ivoire + +: Ebrié Lagoon ( +Arfi et al. 1987 +); +Comoé +River ( +Comoé +National Park) ( +Yao et al. 2015 +); Ebrié Lagoon (Aghien) ( +Aka et al. 2016b +). + + + +Fig. 1. +Map showing the different sites visited by authors of the scientific works cited here that were focused on the cladocera community of Côte d’Ivoire. 1- Shallow reservoirs of the northern of Côte d’Ivoire. 2 - Ebrié Lagoon. 3 - Pisciculture pond at Daloa. 4 - Hana River in Taï Park. 5 - Grand-Lahou Lagoon. 6 - Fresco Lagoon. 7 - Lobo River (Sassandra Basin). 8 - Davo River (Sassandra Basin). 9 - Buyo Lake (Sassandra Basin). 10 - Sassandra River Main Reach. 11 - Kossou Lake. 12 - Tendo-Ehy-Aby lagoonal system. 13 - Bagoe River. 14 - Ayame Lake I. 15 - Agnebi River. 16 - Bia River. 17 - Gagnoa (low ground). 18 - Comoé River in the Comoé National Park. 19 - Fae Lake. + + + +Synonyms +: + +Lynceus longirostris +O.F. Müller 1776 + +; + +Monoculus cornuta +Jurine 1820 + +; + +Bosmina curvirostris +Fischer 1854 + +; + +Bosmina brevicornis +Hellich 1877 + +; + +Bosmina japonica +Poppe and Richard 1890 + +; + +Bosmina pelagica +Stingelin 1895 + +; + +Bosmina pellucida +Stingelin 1895 + +; + +Bosmina stuhlmanni +Weltner 1898 + +; + +Garbinia adriani +Grochowski 1910 + +; + +Bosmina africanaaustralis +Methuen 1911 + +; + +Bosmina arostris +Schiklejew 1930 + +. + + +World distribution +: + +B. +( +Bosmina +) +longirostris + +is reported in all the main biogeographical areas described by +Forró et al. (2008) +, but it is reported as not present in the Pacific Ocean islands or Antarctic region ( +Maiphae et al. 2008 +); it is considered cosmopolitan by +Kotov et al. (2013b) +. + + + + \ No newline at end of file diff --git a/data/03/F6/87/03F687D3FFF5671696B7FAC195A67755.xml b/data/03/F6/87/03F687D3FFF5671696B7FAC195A67755.xml new file mode 100644 index 00000000000..1071a8c6ce0 --- /dev/null +++ b/data/03/F6/87/03F687D3FFF5671696B7FAC195A67755.xml @@ -0,0 +1,185 @@ + + + +Stiatoandricus georgei Cuesta-Porta & Melika & Nicholls & Stone & Pujade-Villar 2022 + + + +Author + +Etilé, Raphaël N’doua + + + +Author + +Bédia, Théophile Aké + + + +Author + +Blahoua, Georges Kassi + + + +Author + +Bi, Gouli Goore + + + +Author + +Kouamelan, Paul Essetchi + + + +Author + +N’Douba, Valentin + +text + + +Zoological Studies + + +2020 + +2020-07-20 + + +59 + + +31 + + +1 +14 + + + + +http://dx.doi.org/10.5281/zenodo.8069124 + +journal article +10.6620/ZS.2020.59-31 +1810-522X +PMC7688398 +33262854 +12822346 + + + + + + + +Bosminopsis deitersi +Richard, 1895 + + + + + + + + +Distribution in +Côte d’Ivoire + +: Ebrié Lagoon: Grand Bassam, Eloka, Bingerville, Banco, Cosrou, and Toupah (Rham 1964), Aghien ( +Aka et al. 2016b +); Ayame Lake I (Yté et al. 1983); the Bagoe River ( +N’da et al. 2015 +). + + +Synonyms +: + +Bosminopsis zernowi +Linko 1901 + +; + +Bosminopsis ishikawai +Klocke 1903 + +; + +Bosminella anisitsi +Daday 1903 + +; + +Bosminella africana +Daday 1908 + +; + +Bosminopsis stingelini +Burckhardt 1909 + +; + +Bosminopsis typica +Burckhardt 1909 + +; + +Bosminopsis birgei +Burckhardt 1924 + +; + +Bosminopsis brehmi +Burckhardt 1924 + +; + +Bosminopsis pernodi +Burckhardt 1924 + +; + +Bosminopsis schroeteri +Burckhardt 1924 + +; + +Bosminopsis devendrari +Rane 1984 + +; + +Bosminopsis macaguensis +Rey and Vasquez 1986 + +. + + +World distribution +: + +B. deitersi + +was regarded as circumtropical by +Maiphae et al. (2008) +, while +Kotov et al. (2013a) +reported it as tropicopolitan, very common in the tropics-subtropics of the old and new worlds. For +Kotov et al. (2013b) +, + +B. deitersi + +is found in Afrotropical, Australasian, Nearctic, Neotropical, +Oriental +and Palaearctic regions. So, it is reported as not present in Pacific Ocean islands or Antarctic region. + + + + \ No newline at end of file diff --git a/data/03/F6/87/03F687D3FFF5671696C0FD0B93567255.xml b/data/03/F6/87/03F687D3FFF5671696C0FD0B93567255.xml new file mode 100644 index 00000000000..cdec614206b --- /dev/null +++ b/data/03/F6/87/03F687D3FFF5671696C0FD0B93567255.xml @@ -0,0 +1,142 @@ + + + +Stiatoandricus georgei Cuesta-Porta & Melika & Nicholls & Stone & Pujade-Villar 2022 + + + +Author + +Etilé, Raphaël N’doua + + + +Author + +Bédia, Théophile Aké + + + +Author + +Blahoua, Georges Kassi + + + +Author + +Bi, Gouli Goore + + + +Author + +Kouamelan, Paul Essetchi + + + +Author + +N’Douba, Valentin + +text + + +Zoological Studies + + +2020 + +2020-07-20 + + +59 + + +31 + + +1 +14 + + + + +http://dx.doi.org/10.5281/zenodo.8069124 + +journal article +10.6620/ZS.2020.59-31 +1810-522X +PMC7688398 +33262854 +12822346 + + + + + + + +Bosmina +( +Liederobosmina +) +tubicen +Brehm, 1953 + + + + + + + + +Distribution in +Côte d’Ivoire + +: Ayame Lake I ( +Rey and Yté 1982 +; +Yté et al. 1982 +1983; +Ouattara et al. 2007 +); Buyo Lake ( +Yté et al. 1996 +); Bia River ( +Ouattara et al. 2007 +); the Agnebi River ( +Ouattara et al. 2007 +); the Sassandra River watershed ( +Kouamé et al. 2018 +). + + +Synonyms +: + +Bosmina americana +Aurich 1934 + +; + +Eubosmina tubicen +(Brehm 1953) + + + +World distribution: + +B. +( +Liederobosmina +) +tubicen +Brehm 1953 + +was reported by +Kotov et al. (2013b) +from the Nearctic and Neotropical regions. + + + + \ No newline at end of file diff --git a/data/03/F6/87/03F687D3FFFE671D95C6FEA1928874D0.xml b/data/03/F6/87/03F687D3FFFE671D95C6FEA1928874D0.xml new file mode 100644 index 00000000000..0b88c028024 --- /dev/null +++ b/data/03/F6/87/03F687D3FFFE671D95C6FEA1928874D0.xml @@ -0,0 +1,137 @@ + + + +Stiatoandricus georgei Cuesta-Porta & Melika & Nicholls & Stone & Pujade-Villar 2022 + + + +Author + +Etilé, Raphaël N’doua + + + +Author + +Bédia, Théophile Aké + + + +Author + +Blahoua, Georges Kassi + + + +Author + +Bi, Gouli Goore + + + +Author + +Kouamelan, Paul Essetchi + + + +Author + +N’Douba, Valentin + +text + + +Zoological Studies + + +2020 + +2020-07-20 + + +59 + + +31 + + +1 +14 + + + + +http://dx.doi.org/10.5281/zenodo.8069124 + +journal article +10.6620/ZS.2020.59-31 +1810-522X +PMC7688398 +33262854 +12822346 + + + + + + + +Moinodaphnia macleayi +King, 1853 + + + + + + + + +Distribution in +Côte d’Ivoire + +: Ebrie Lagoon: Bingerville, Aghien (Rham 1964; +Aka et al. 2016a b +); Grand-Lahou Lagoon ( +Etilé et al. 2009 +). + + +Synonyms +: + +Moina macleayi +King 1853 + +; + +Moina submucronata +Brady 1886 + +; + +Moinodaphnia alabamensis +Herrick 1887 + +; + +Moinodaphnia mocquerysi +Richard 1892 + +. + + +World distribution +: + +M. macleayi + +is widely distributed, in Afrotropical, Australasian, Nearctic, Neotropical, +Oriental +, and Palaearctic regions ( +Kotov et al. 2013b +). + + + + \ No newline at end of file diff --git a/data/03/F6/87/03F687D3FFFE671D9680FDC190A77530.xml b/data/03/F6/87/03F687D3FFFE671D9680FDC190A77530.xml new file mode 100644 index 00000000000..638cfa841b8 --- /dev/null +++ b/data/03/F6/87/03F687D3FFFE671D9680FDC190A77530.xml @@ -0,0 +1,114 @@ + + + +Stiatoandricus georgei Cuesta-Porta & Melika & Nicholls & Stone & Pujade-Villar 2022 + + + +Author + +Etilé, Raphaël N’doua + + + +Author + +Bédia, Théophile Aké + + + +Author + +Blahoua, Georges Kassi + + + +Author + +Bi, Gouli Goore + + + +Author + +Kouamelan, Paul Essetchi + + + +Author + +N’Douba, Valentin + +text + + +Zoological Studies + + +2020 + +2020-07-20 + + +59 + + +31 + + +1 +14 + + + + +http://dx.doi.org/10.5281/zenodo.8069124 + +journal article +10.6620/ZS.2020.59-31 +1810-522X +PMC7688398 +33262854 +12822346 + + + + + + + +Moina dubia +Guerne and +Richard, 1892 + + + + + + + + +Distribution in +Côte d’Ivoire + +: Ebrie Lagoon: Bengerville, Bimbresso (Rham 1964). + + +Synonyms +: No synonyms available. + + +World distribution +: + +M. dubia + +is mentioned as being from Afrotropical and Palaearctic regions ( +Chatterjee et al. 2013 +; +Kotov et al. 2013b +). + + + + \ No newline at end of file diff --git a/data/03/F6/87/03F687D3FFFE671D9741FCE193DD722F.xml b/data/03/F6/87/03F687D3FFFE671D9741FCE193DD722F.xml new file mode 100644 index 00000000000..b38126e105e --- /dev/null +++ b/data/03/F6/87/03F687D3FFFE671D9741FCE193DD722F.xml @@ -0,0 +1,110 @@ + + + +Stiatoandricus georgei Cuesta-Porta & Melika & Nicholls & Stone & Pujade-Villar 2022 + + + +Author + +Etilé, Raphaël N’doua + + + +Author + +Bédia, Théophile Aké + + + +Author + +Blahoua, Georges Kassi + + + +Author + +Bi, Gouli Goore + + + +Author + +Kouamelan, Paul Essetchi + + + +Author + +N’Douba, Valentin + +text + + +Zoological Studies + + +2020 + +2020-07-20 + + +59 + + +31 + + +1 +14 + + + + +http://dx.doi.org/10.5281/zenodo.8069124 + +journal article +10.6620/ZS.2020.59-31 +1810-522X +PMC7688398 +33262854 +12822346 + + + + + + + +Moina reticulata +Daday, 1905 + + + + + + + + +Distribution in +Côte d’Ivoire + +: Kossou Lake ( +Lamoot and Dumont 1974 +). +Synonym +: + +Moinodaphnia reticulata +Daday 1905 + +. +World distribution +: Mentioned as an Afrotropical and Neotropical species ( +Kotov et al. 2013b +). + + + + \ No newline at end of file diff --git a/data/03/F6/87/03F687D3FFFE671D975DFBE090EA714F.xml b/data/03/F6/87/03F687D3FFFE671D975DFBE090EA714F.xml new file mode 100644 index 00000000000..7f4b274894e --- /dev/null +++ b/data/03/F6/87/03F687D3FFFE671D975DFBE090EA714F.xml @@ -0,0 +1,188 @@ + + + +Stiatoandricus georgei Cuesta-Porta & Melika & Nicholls & Stone & Pujade-Villar 2022 + + + +Author + +Etilé, Raphaël N’doua + + + +Author + +Bédia, Théophile Aké + + + +Author + +Blahoua, Georges Kassi + + + +Author + +Bi, Gouli Goore + + + +Author + +Kouamelan, Paul Essetchi + + + +Author + +N’Douba, Valentin + +text + + +Zoological Studies + + +2020 + +2020-07-20 + + +59 + + +31 + + +1 +14 + + + + +http://dx.doi.org/10.5281/zenodo.8069124 + +journal article +10.6620/ZS.2020.59-31 +1810-522X +PMC7688398 +33262854 +12822346 + + + + + + + +Moina micrura +Kurz, 1875 + + + + + + + + +Distribution in +Côte d’Ivoire + +: Ayame Lake I ( +Yté et al. 1982 +1983; +Ouattara et al. 2007 +); Ebrie Lagoon: Aghien, Layo ( +Arfi et al. 1987 +; +Legendre et al. 1987 +; +Aka et al. 2016a b +); Bia and Agnebi Rivers ( +Ouattara et al. 2007 +); Grand-Lahou Lagoon ( +Etilé et al. 2009 +); Tendo-Ehy-Aby lagoonal system ( +Monney et al. 2015 +); Bagoe River ( +N’da et al. 2015 +); +Comoé +River in +Comoé +National Park ( +Yao et al. 2015 +); Buyo Lake ( +Yté et al. 1996 +; +Kouamé et al. 2018 +); fish ponds in Gagnoa ( +Amian et al. 2018 +); Sassandra River main stem, Lobo and Davo Rivers ( +Kouamé et al. 2018 +); Fresco Lagoon ( +Etilé et al. 2018 +); Hana River in Taï National Park ( +Diomande et al. 2018 +). + + +Synonyms +: + +Moina weberi +Richard 1891 + +; + +Moina macrophtalma +Stingelin 1913 + +; + +Moina lacustris +Rammner 1931 + +; + +Moina macrocephala +Rammner 1933 + +; + +Moina latidens +Brehm 1933 + +; + +Moina parva +Jenkin 1934 + +; + +Moina dodhui +Rane 1987 + +. + + +World distribution +: According to +Chatterjee et al. (2013) +and +Jeong et al. (2014) +, + +M. micrura + +is widely distributed in tropical and subtropical regions and southern Europe; it was considered a cosmopolitan species by De los Ríos-Escalante and +Kotov (2015) +and +Ghaouaci et al. (2018) +. + + + + \ No newline at end of file diff --git a/data/13/47/30/13473026FFCB6128A672EE05FE8984E2.xml b/data/13/47/30/13473026FFCB6128A672EE05FE8984E2.xml index d435ef953da..b6438f9f2d4 100644 --- a/data/13/47/30/13473026FFCB6128A672EE05FE8984E2.xml +++ b/data/13/47/30/13473026FFCB6128A672EE05FE8984E2.xml @@ -1,52 +1,55 @@ - - - -Fig. 6 in Bruggmanniella sanlianensis Lin, Yang & Tokuda, 2020, sp. nov. + + + +Fig. 6 in Bruggmanniella sanlianensis Lin, Yang & Tokuda, 2020, sp. nov. - - -Author + + +Author -Hirose, Euichi -Department of Chemistry, Biology and Marine Science, Faculty of Science, University of the Ryukyus, Nishihara, Okinawa 903 - 0213, Japan. * Correspondence: E-mail: euichi @ sci. u-ryukyu. ac. jp (Hirose) -euichi@sci.u-ryukyu.ac.jp +Hirose, Euichi +Department of Chemistry, Biology and Marine Science, Faculty of Science, University of the Ryukyus, Nishihara, Okinawa 903 - 0213, Japan. * Correspondence: E-mail: euichi @ sci. u-ryukyu. ac. jp (Hirose) +euichi@sci.u-ryukyu.ac.jp - - -Author + + +Author -Nozawa, Yoko -Biodiversity Research Center, No. 128, Academia Road Sec. 2, Nankang, Taipei 115, Taiwan. E-mail: nozaway @ gate. sinica. edu. tw (Nozawa) -nozaway@gate.sinica.edu.tw +Nozawa, Yoko +Biodiversity Research Center, No. 128, Academia Road Sec. 2, Nankang, Taipei 115, Taiwan. E-mail: nozaway @ gate. sinica. edu. tw (Nozawa) +nozaway@gate.sinica.edu.tw -text - - -Zoological Studies +text + + +Zoological Studies - -2020 - -2020-06-15 + +2020 + +2020-06-15 - -59 + +59 - -19 + +19 - -1 -11 + +1 +11 - -http://dx.doi.org/10.5281/zenodo.12822057 + +http://dx.doi.org/10.5281/zenodo.12822057 -journal article -10.6620/ZS.2020.59-19 -1810-522X +journal article +10.6620/ZS.2020.59-19 +1810-522X +PMC7688397 +33262843 +12822130 @@ -65,17 +68,17 @@ Michaelsen, 1921 The colonies were oval or elongated cushions and aggregated on a side wall of a tide pool ( -Fig. 3M +Fig. 3M ). They were green due to Prochloron in the common cloacal cavities, while the colony peripheries and substratum side were white due to tunic spicules with burred surfaces ( -Fig. 3N +Fig. 3N ). In an enlarged image of the colonies, there was a black spot in each zooid ( -Fig. 3O +Fig. 3O ). This is a black (or dark brown) pigmentation at the apical end of the endostyle referred to as pigment cap ( -Fig. 3P +Fig. 3P ), which is unique to the T. cyclops diff --git a/data/13/47/30/13473026FFCB612BA5C5EFC5FB758701.xml b/data/13/47/30/13473026FFCB612BA5C5EFC5FB758701.xml index b71ec85f2a7..32196fb798d 100644 --- a/data/13/47/30/13473026FFCB612BA5C5EFC5FB758701.xml +++ b/data/13/47/30/13473026FFCB612BA5C5EFC5FB758701.xml @@ -1,54 +1,57 @@ - - - -Fig. 6 in Bruggmanniella sanlianensis Lin, Yang & Tokuda, 2020, sp. nov. + + + +Fig. 6 in Bruggmanniella sanlianensis Lin, Yang & Tokuda, 2020, sp. nov. - - -Author + + +Author -Hirose, Euichi -Department of Chemistry, Biology and Marine Science, Faculty of Science, University of the Ryukyus, Nishihara, Okinawa 903 - 0213, Japan. * Correspondence: E-mail: euichi @ sci. u-ryukyu. ac. jp (Hirose) -euichi@sci.u-ryukyu.ac.jp +Hirose, Euichi +Department of Chemistry, Biology and Marine Science, Faculty of Science, University of the Ryukyus, Nishihara, Okinawa 903 - 0213, Japan. * Correspondence: E-mail: euichi @ sci. u-ryukyu. ac. jp (Hirose) +euichi@sci.u-ryukyu.ac.jp - - -Author + + +Author -Nozawa, Yoko -Biodiversity Research Center, No. 128, Academia Road Sec. 2, Nankang, Taipei 115, Taiwan. E-mail: nozaway @ gate. sinica. edu. tw (Nozawa) -nozaway@gate.sinica.edu.tw +Nozawa, Yoko +Biodiversity Research Center, No. 128, Academia Road Sec. 2, Nankang, Taipei 115, Taiwan. E-mail: nozaway @ gate. sinica. edu. tw (Nozawa) +nozaway@gate.sinica.edu.tw -text - - -Zoological Studies +text + + +Zoological Studies - -2020 - -2020-06-15 + +2020 + +2020-06-15 - -59 + +59 - -19 + +19 - -1 -11 + +1 +11 - -http://dx.doi.org/10.5281/zenodo.12822057 + +http://dx.doi.org/10.5281/zenodo.12822057 -journal article -10.6620/ZS.2020.59-19 -1810-522X +journal article +10.6620/ZS.2020.59-19 +1810-522X +PMC7688397 +33262843 +12822130 - + @@ -65,15 +68,15 @@ Kott, 1977 Irregularly shaped colonies were attached to hydrozoan colonies. Live colonies were yellow or light brown ( -Fig. 3I +Fig. 3I ). The fixed specimens gradually turned greenish, probably because the yellowish colors were dissolved or discolored in the fixative. Tunic spicules consisted of rod-like rays ( -Fig. 3J +Fig. 3J ). Three types of cyanobacterial species were found in the tunic, i.e. , greenish-unicellular, reddish-unicellular, and reddishfilamentous cyanobacteria ( -Fig. 3K and L +Fig. 3K and L ). diff --git a/data/13/47/30/13473026FFCC612CA590EE65FABF8781.xml b/data/13/47/30/13473026FFCC612CA590EE65FABF8781.xml index da4a55f984d..c117cfd4889 100644 --- a/data/13/47/30/13473026FFCC612CA590EE65FABF8781.xml +++ b/data/13/47/30/13473026FFCC612CA590EE65FABF8781.xml @@ -1,54 +1,57 @@ - - - -Fig. 6 in Bruggmanniella sanlianensis Lin, Yang & Tokuda, 2020, sp. nov. + + + +Fig. 6 in Bruggmanniella sanlianensis Lin, Yang & Tokuda, 2020, sp. nov. - - -Author + + +Author -Hirose, Euichi -Department of Chemistry, Biology and Marine Science, Faculty of Science, University of the Ryukyus, Nishihara, Okinawa 903 - 0213, Japan. * Correspondence: E-mail: euichi @ sci. u-ryukyu. ac. jp (Hirose) -euichi@sci.u-ryukyu.ac.jp +Hirose, Euichi +Department of Chemistry, Biology and Marine Science, Faculty of Science, University of the Ryukyus, Nishihara, Okinawa 903 - 0213, Japan. * Correspondence: E-mail: euichi @ sci. u-ryukyu. ac. jp (Hirose) +euichi@sci.u-ryukyu.ac.jp - - -Author + + +Author -Nozawa, Yoko -Biodiversity Research Center, No. 128, Academia Road Sec. 2, Nankang, Taipei 115, Taiwan. E-mail: nozaway @ gate. sinica. edu. tw (Nozawa) -nozaway@gate.sinica.edu.tw +Nozawa, Yoko +Biodiversity Research Center, No. 128, Academia Road Sec. 2, Nankang, Taipei 115, Taiwan. E-mail: nozaway @ gate. sinica. edu. tw (Nozawa) +nozaway@gate.sinica.edu.tw -text - - -Zoological Studies +text + + +Zoological Studies - -2020 - -2020-06-15 + +2020 + +2020-06-15 - -59 + +59 - -19 + +19 - -1 -11 + +1 +11 - -http://dx.doi.org/10.5281/zenodo.12822057 + +http://dx.doi.org/10.5281/zenodo.12822057 -journal article -10.6620/ZS.2020.59-19 -1810-522X +journal article +10.6620/ZS.2020.59-19 +1810-522X +PMC7688397 +33262843 +12822130 - + @@ -68,7 +71,7 @@ Hirose and Oka, 2009 D. gumavirens colonies occurred on coral limestone in Maobitou, and many were also found on hydrozoan colonies in Shimen, Wushibi, and Xiaoyeliu ( -Fig. 2C +Fig. 2C ). The colonies were small cushions of about 1 mm thick and entirely green due to @@ -87,9 +90,9 @@ the second row, the third row, and 4 in the fourth (bottom) row ( -Fig. 2D +Fig. 2D ). The retractor muscle emerged from halfway down the esophagus ( -Fig. 2D +Fig. 2D ). diff --git a/data/13/47/30/13473026FFCC612CA646EE85FB1584DC.xml b/data/13/47/30/13473026FFCC612CA646EE85FB1584DC.xml index 432d73d1b9f..5924feb7df0 100644 --- a/data/13/47/30/13473026FFCC612CA646EE85FB1584DC.xml +++ b/data/13/47/30/13473026FFCC612CA646EE85FB1584DC.xml @@ -1,54 +1,57 @@ - - - -Fig. 6 in Bruggmanniella sanlianensis Lin, Yang & Tokuda, 2020, sp. nov. + + + +Fig. 6 in Bruggmanniella sanlianensis Lin, Yang & Tokuda, 2020, sp. nov. - - -Author + + +Author -Hirose, Euichi -Department of Chemistry, Biology and Marine Science, Faculty of Science, University of the Ryukyus, Nishihara, Okinawa 903 - 0213, Japan. * Correspondence: E-mail: euichi @ sci. u-ryukyu. ac. jp (Hirose) -euichi@sci.u-ryukyu.ac.jp +Hirose, Euichi +Department of Chemistry, Biology and Marine Science, Faculty of Science, University of the Ryukyus, Nishihara, Okinawa 903 - 0213, Japan. * Correspondence: E-mail: euichi @ sci. u-ryukyu. ac. jp (Hirose) +euichi@sci.u-ryukyu.ac.jp - - -Author + + +Author -Nozawa, Yoko -Biodiversity Research Center, No. 128, Academia Road Sec. 2, Nankang, Taipei 115, Taiwan. E-mail: nozaway @ gate. sinica. edu. tw (Nozawa) -nozaway@gate.sinica.edu.tw +Nozawa, Yoko +Biodiversity Research Center, No. 128, Academia Road Sec. 2, Nankang, Taipei 115, Taiwan. E-mail: nozaway @ gate. sinica. edu. tw (Nozawa) +nozaway@gate.sinica.edu.tw -text - - -Zoological Studies +text + + +Zoological Studies - -2020 - -2020-06-15 + +2020 + +2020-06-15 - -59 + +59 - -19 + +19 - -1 -11 + +1 +11 - -http://dx.doi.org/10.5281/zenodo.12822057 + +http://dx.doi.org/10.5281/zenodo.12822057 -journal article -10.6620/ZS.2020.59-19 -1810-522X +journal article +10.6620/ZS.2020.59-19 +1810-522X +PMC7688397 +33262843 +12822130 - + @@ -67,9 +70,9 @@ Suetsugu and Hirose, 2005 Colonies were thin, irregularly shaped sheets of ≤ 1 mm thick ( -Fig. 2E +Fig. 2E ). The pattern of stigmata was 5-6-5-4, and the retractor muscle emerged from the bottom of the thorax ( -Fig. 2F +Fig. 2F ). diff --git a/data/13/47/30/13473026FFCD612DA58FEBBFFDD9838D.xml b/data/13/47/30/13473026FFCD612DA58FEBBFFDD9838D.xml index 5edb0b2d60b..c842f7ce2c3 100644 --- a/data/13/47/30/13473026FFCD612DA58FEBBFFDD9838D.xml +++ b/data/13/47/30/13473026FFCD612DA58FEBBFFDD9838D.xml @@ -1,54 +1,57 @@ - - - -Fig. 6 in Bruggmanniella sanlianensis Lin, Yang & Tokuda, 2020, sp. nov. + + + +Fig. 6 in Bruggmanniella sanlianensis Lin, Yang & Tokuda, 2020, sp. nov. - - -Author + + +Author -Hirose, Euichi -Department of Chemistry, Biology and Marine Science, Faculty of Science, University of the Ryukyus, Nishihara, Okinawa 903 - 0213, Japan. * Correspondence: E-mail: euichi @ sci. u-ryukyu. ac. jp (Hirose) -euichi@sci.u-ryukyu.ac.jp +Hirose, Euichi +Department of Chemistry, Biology and Marine Science, Faculty of Science, University of the Ryukyus, Nishihara, Okinawa 903 - 0213, Japan. * Correspondence: E-mail: euichi @ sci. u-ryukyu. ac. jp (Hirose) +euichi@sci.u-ryukyu.ac.jp - - -Author + + +Author -Nozawa, Yoko -Biodiversity Research Center, No. 128, Academia Road Sec. 2, Nankang, Taipei 115, Taiwan. E-mail: nozaway @ gate. sinica. edu. tw (Nozawa) -nozaway@gate.sinica.edu.tw +Nozawa, Yoko +Biodiversity Research Center, No. 128, Academia Road Sec. 2, Nankang, Taipei 115, Taiwan. E-mail: nozaway @ gate. sinica. edu. tw (Nozawa) +nozaway@gate.sinica.edu.tw -text - - -Zoological Studies +text + + +Zoological Studies - -2020 - -2020-06-15 + +2020 + +2020-06-15 - -59 + +59 - -19 + +19 - -1 -11 + +1 +11 - -http://dx.doi.org/10.5281/zenodo.12822057 + +http://dx.doi.org/10.5281/zenodo.12822057 -journal article -10.6620/ZS.2020.59-19 -1810-522X +journal article +10.6620/ZS.2020.59-19 +1810-522X +PMC7688397 +33262843 +12822130 - + @@ -67,9 +70,9 @@ Hirose and Oka, 2009 Colonies were thin, irregularly shaped sheets of ≤ 1 mm thick ( -Fig. 2K +Fig. 2K ). The pattern of stigmata was 6-7-6-5 ( -Fig. 2L +Fig. 2L ), and the retractor muscle emerged from the bottom of the thorax. This is the first time D. watanabei diff --git a/data/13/47/30/13473026FFCD612DA5C1EFC5FDB2851C.xml b/data/13/47/30/13473026FFCD612DA5C1EFC5FDB2851C.xml index c70db1e5416..00319bdcda6 100644 --- a/data/13/47/30/13473026FFCD612DA5C1EFC5FDB2851C.xml +++ b/data/13/47/30/13473026FFCD612DA5C1EFC5FDB2851C.xml @@ -1,54 +1,57 @@ - - - -Fig. 6 in Bruggmanniella sanlianensis Lin, Yang & Tokuda, 2020, sp. nov. + + + +Fig. 6 in Bruggmanniella sanlianensis Lin, Yang & Tokuda, 2020, sp. nov. - - -Author + + +Author -Hirose, Euichi -Department of Chemistry, Biology and Marine Science, Faculty of Science, University of the Ryukyus, Nishihara, Okinawa 903 - 0213, Japan. * Correspondence: E-mail: euichi @ sci. u-ryukyu. ac. jp (Hirose) -euichi@sci.u-ryukyu.ac.jp +Hirose, Euichi +Department of Chemistry, Biology and Marine Science, Faculty of Science, University of the Ryukyus, Nishihara, Okinawa 903 - 0213, Japan. * Correspondence: E-mail: euichi @ sci. u-ryukyu. ac. jp (Hirose) +euichi@sci.u-ryukyu.ac.jp - - -Author + + +Author -Nozawa, Yoko -Biodiversity Research Center, No. 128, Academia Road Sec. 2, Nankang, Taipei 115, Taiwan. E-mail: nozaway @ gate. sinica. edu. tw (Nozawa) -nozaway@gate.sinica.edu.tw +Nozawa, Yoko +Biodiversity Research Center, No. 128, Academia Road Sec. 2, Nankang, Taipei 115, Taiwan. E-mail: nozaway @ gate. sinica. edu. tw (Nozawa) +nozaway@gate.sinica.edu.tw -text - - -Zoological Studies +text + + +Zoological Studies - -2020 - -2020-06-15 + +2020 + +2020-06-15 - -59 + +59 - -19 + +19 - -1 -11 + +1 +11 - -http://dx.doi.org/10.5281/zenodo.12822057 + +http://dx.doi.org/10.5281/zenodo.12822057 -journal article -10.6620/ZS.2020.59-19 -1810-522X +journal article +10.6620/ZS.2020.59-19 +1810-522X +PMC7688397 +33262843 +12822130 - + @@ -67,9 +70,9 @@ Colonies were irregularly shaped sheets of 1-2 mm thick and firmly attached to the dead coral branch and coral limestone ( -Fig. 2G +Fig. 2G ). The pattern of stigmata was 6-6-6-5, and the retractor muscle emerged from the bottom of the thorax ( -Fig. 2H +Fig. 2H ). diff --git a/data/13/47/30/13473026FFCD612DA5E1EAF9FA0984A2.xml b/data/13/47/30/13473026FFCD612DA5E1EAF9FA0984A2.xml index 4a01d866bf4..d6eba067e00 100644 --- a/data/13/47/30/13473026FFCD612DA5E1EAF9FA0984A2.xml +++ b/data/13/47/30/13473026FFCD612DA5E1EAF9FA0984A2.xml @@ -1,54 +1,57 @@ - - - -Fig. 6 in Bruggmanniella sanlianensis Lin, Yang & Tokuda, 2020, sp. nov. + + + +Fig. 6 in Bruggmanniella sanlianensis Lin, Yang & Tokuda, 2020, sp. nov. - - -Author + + +Author -Hirose, Euichi -Department of Chemistry, Biology and Marine Science, Faculty of Science, University of the Ryukyus, Nishihara, Okinawa 903 - 0213, Japan. * Correspondence: E-mail: euichi @ sci. u-ryukyu. ac. jp (Hirose) -euichi@sci.u-ryukyu.ac.jp +Hirose, Euichi +Department of Chemistry, Biology and Marine Science, Faculty of Science, University of the Ryukyus, Nishihara, Okinawa 903 - 0213, Japan. * Correspondence: E-mail: euichi @ sci. u-ryukyu. ac. jp (Hirose) +euichi@sci.u-ryukyu.ac.jp - - -Author + + +Author -Nozawa, Yoko -Biodiversity Research Center, No. 128, Academia Road Sec. 2, Nankang, Taipei 115, Taiwan. E-mail: nozaway @ gate. sinica. edu. tw (Nozawa) -nozaway@gate.sinica.edu.tw +Nozawa, Yoko +Biodiversity Research Center, No. 128, Academia Road Sec. 2, Nankang, Taipei 115, Taiwan. E-mail: nozaway @ gate. sinica. edu. tw (Nozawa) +nozaway@gate.sinica.edu.tw -text - - -Zoological Studies +text + + +Zoological Studies - -2020 - -2020-06-15 + +2020 + +2020-06-15 - -59 + +59 - -19 + +19 - -1 -11 + +1 +11 - -http://dx.doi.org/10.5281/zenodo.12822057 + +http://dx.doi.org/10.5281/zenodo.12822057 -journal article -10.6620/ZS.2020.59-19 -1810-522X +journal article +10.6620/ZS.2020.59-19 +1810-522X +PMC7688397 +33262843 +12822130 - + @@ -69,9 +72,9 @@ Colonies were flat, irregularly shaped sheets and usually green due to the Prochloron distributed in the common cloacal cavities ( -Fig. 3A +Fig. 3A ). The peripheries and the substratum side of the colony sheets were white due to globular spicules densely distributed in the tunic ( -Fig. 3B +Fig. 3B ). diff --git a/data/13/47/30/13473026FFCD612DA5FEEC0AFDEE8277.xml b/data/13/47/30/13473026FFCD612DA5FEEC0AFDEE8277.xml index 4467d49b73f..39fbf95de7f 100644 --- a/data/13/47/30/13473026FFCD612DA5FEEC0AFDEE8277.xml +++ b/data/13/47/30/13473026FFCD612DA5FEEC0AFDEE8277.xml @@ -1,54 +1,57 @@ - - - -Fig. 6 in Bruggmanniella sanlianensis Lin, Yang & Tokuda, 2020, sp. nov. + + + +Fig. 6 in Bruggmanniella sanlianensis Lin, Yang & Tokuda, 2020, sp. nov. - - -Author + + +Author -Hirose, Euichi -Department of Chemistry, Biology and Marine Science, Faculty of Science, University of the Ryukyus, Nishihara, Okinawa 903 - 0213, Japan. * Correspondence: E-mail: euichi @ sci. u-ryukyu. ac. jp (Hirose) -euichi@sci.u-ryukyu.ac.jp +Hirose, Euichi +Department of Chemistry, Biology and Marine Science, Faculty of Science, University of the Ryukyus, Nishihara, Okinawa 903 - 0213, Japan. * Correspondence: E-mail: euichi @ sci. u-ryukyu. ac. jp (Hirose) +euichi@sci.u-ryukyu.ac.jp - - -Author + + +Author -Nozawa, Yoko -Biodiversity Research Center, No. 128, Academia Road Sec. 2, Nankang, Taipei 115, Taiwan. E-mail: nozaway @ gate. sinica. edu. tw (Nozawa) -nozaway@gate.sinica.edu.tw +Nozawa, Yoko +Biodiversity Research Center, No. 128, Academia Road Sec. 2, Nankang, Taipei 115, Taiwan. E-mail: nozaway @ gate. sinica. edu. tw (Nozawa) +nozaway@gate.sinica.edu.tw -text - - -Zoological Studies +text + + +Zoological Studies - -2020 - -2020-06-15 + +2020 + +2020-06-15 - -59 + +59 - -19 + +19 - -1 -11 + +1 +11 - -http://dx.doi.org/10.5281/zenodo.12822057 + +http://dx.doi.org/10.5281/zenodo.12822057 -journal article -10.6620/ZS.2020.59-19 -1810-522X +journal article +10.6620/ZS.2020.59-19 +1810-522X +PMC7688397 +33262843 +12822130 - + @@ -67,14 +70,14 @@ Colonies were irregularly shaped sheets about 2-5 mm thick ( -Fig. 2I +Fig. 2I ). The tunic was tougher than in other photosymbiotic Diplosoma species. The pattern of stigmata was 6-6-6-5 ( -Fig. 2J +Fig. 2J ), and the retractor muscle emerged from halfway down the esophagus. diff --git a/data/13/47/30/13473026FFCD612DA667EDE5FB668347.xml b/data/13/47/30/13473026FFCD612DA667EDE5FB668347.xml index f7b79c214d2..c5af7d9e8cb 100644 --- a/data/13/47/30/13473026FFCD612DA667EDE5FB668347.xml +++ b/data/13/47/30/13473026FFCD612DA667EDE5FB668347.xml @@ -1,54 +1,57 @@ - - - -Fig. 6 in Bruggmanniella sanlianensis Lin, Yang & Tokuda, 2020, sp. nov. + + + +Fig. 6 in Bruggmanniella sanlianensis Lin, Yang & Tokuda, 2020, sp. nov. - - -Author + + +Author -Hirose, Euichi -Department of Chemistry, Biology and Marine Science, Faculty of Science, University of the Ryukyus, Nishihara, Okinawa 903 - 0213, Japan. * Correspondence: E-mail: euichi @ sci. u-ryukyu. ac. jp (Hirose) -euichi@sci.u-ryukyu.ac.jp +Hirose, Euichi +Department of Chemistry, Biology and Marine Science, Faculty of Science, University of the Ryukyus, Nishihara, Okinawa 903 - 0213, Japan. * Correspondence: E-mail: euichi @ sci. u-ryukyu. ac. jp (Hirose) +euichi@sci.u-ryukyu.ac.jp - - -Author + + +Author -Nozawa, Yoko -Biodiversity Research Center, No. 128, Academia Road Sec. 2, Nankang, Taipei 115, Taiwan. E-mail: nozaway @ gate. sinica. edu. tw (Nozawa) -nozaway@gate.sinica.edu.tw +Nozawa, Yoko +Biodiversity Research Center, No. 128, Academia Road Sec. 2, Nankang, Taipei 115, Taiwan. E-mail: nozaway @ gate. sinica. edu. tw (Nozawa) +nozaway@gate.sinica.edu.tw -text - - -Zoological Studies +text + + +Zoological Studies - -2020 - -2020-06-15 + +2020 + +2020-06-15 - -59 + +59 - -19 + +19 - -1 -11 + +1 +11 - -http://dx.doi.org/10.5281/zenodo.12822057 + +http://dx.doi.org/10.5281/zenodo.12822057 -journal article -10.6620/ZS.2020.59-19 -1810-522X +journal article +10.6620/ZS.2020.59-19 +1810-522X +PMC7688397 +33262843 +12822130 - + @@ -65,19 +68,19 @@ Small colonies comprising 10 or fewer zooids often attached to or partly fused with neighbor colonies ( -Fig. 3C +Fig. 3C ). Colonies were entirely green due to Prochloron cells distributed in the tunic. There was an unknown organ beneath the thorax of each zooid ( -Fig. 3D +Fig. 3D ). This character is unique to L. midui . Tunic spicules were globular ( -Fig. 3E +Fig. 3E ). The type locality of the species was the out reef off Shinri-hama (Kumejima Is., Ryukyu Archipelago, diff --git a/data/13/47/30/13473026FFCD612DA6ADEA4FFB71817D.xml b/data/13/47/30/13473026FFCD612DA6ADEA4FFB71817D.xml index d7e4eb54bcf..03c6ae26ffc 100644 --- a/data/13/47/30/13473026FFCD612DA6ADEA4FFB71817D.xml +++ b/data/13/47/30/13473026FFCD612DA6ADEA4FFB71817D.xml @@ -1,54 +1,57 @@ - - - -Fig. 6 in Bruggmanniella sanlianensis Lin, Yang & Tokuda, 2020, sp. nov. + + + +Fig. 6 in Bruggmanniella sanlianensis Lin, Yang & Tokuda, 2020, sp. nov. - - -Author + + +Author -Hirose, Euichi -Department of Chemistry, Biology and Marine Science, Faculty of Science, University of the Ryukyus, Nishihara, Okinawa 903 - 0213, Japan. * Correspondence: E-mail: euichi @ sci. u-ryukyu. ac. jp (Hirose) -euichi@sci.u-ryukyu.ac.jp +Hirose, Euichi +Department of Chemistry, Biology and Marine Science, Faculty of Science, University of the Ryukyus, Nishihara, Okinawa 903 - 0213, Japan. * Correspondence: E-mail: euichi @ sci. u-ryukyu. ac. jp (Hirose) +euichi@sci.u-ryukyu.ac.jp - - -Author + + +Author -Nozawa, Yoko -Biodiversity Research Center, No. 128, Academia Road Sec. 2, Nankang, Taipei 115, Taiwan. E-mail: nozaway @ gate. sinica. edu. tw (Nozawa) -nozaway@gate.sinica.edu.tw +Nozawa, Yoko +Biodiversity Research Center, No. 128, Academia Road Sec. 2, Nankang, Taipei 115, Taiwan. E-mail: nozaway @ gate. sinica. edu. tw (Nozawa) +nozaway@gate.sinica.edu.tw -text - - -Zoological Studies +text + + +Zoological Studies - -2020 - -2020-06-15 + +2020 + +2020-06-15 - -59 + +59 - -19 + +19 - -1 -11 + +1 +11 - -http://dx.doi.org/10.5281/zenodo.12822057 + +http://dx.doi.org/10.5281/zenodo.12822057 -journal article -10.6620/ZS.2020.59-19 -1810-522X +journal article +10.6620/ZS.2020.59-19 +1810-522X +PMC7688397 +33262843 +12822130 - + @@ -65,7 +68,7 @@ Kott, 1977 Colonies were irregularly shaped, fragile sheets ( -Fig. 3F +Fig. 3F ). They were entirely green due to Prochloron @@ -79,7 +82,7 @@ cells in the tunic were located in the tunic cells, , tunic phycocytes ( Hirose et al. 1996 ) ( -Fig. 3G +Fig. 3G ). Intracellular distribution of the cyanobacterial cells is unique to L. punctatum @@ -87,7 +90,7 @@ cells in the tunic were located in the tunic cells, , and photosymbionts are not associated with any tunic cells in the other host ascidians harboring cyanobacteria in the tunic (reviewed in Hirose 2015 ). Tunic spicules were globular and densely aggregated around each zooid ( -Fig. 3H +Fig. 3H ). This is a new record of L. punctatum diff --git a/data/13/47/30/13473026FFCF612CA6AFEB85FD508722.xml b/data/13/47/30/13473026FFCF612CA6AFEB85FD508722.xml index 45011c5f14a..ca43880b8a8 100644 --- a/data/13/47/30/13473026FFCF612CA6AFEB85FD508722.xml +++ b/data/13/47/30/13473026FFCF612CA6AFEB85FD508722.xml @@ -1,54 +1,57 @@ - - - -Fig. 6 in Bruggmanniella sanlianensis Lin, Yang & Tokuda, 2020, sp. nov. + + + +Fig. 6 in Bruggmanniella sanlianensis Lin, Yang & Tokuda, 2020, sp. nov. - - -Author + + +Author -Hirose, Euichi -Department of Chemistry, Biology and Marine Science, Faculty of Science, University of the Ryukyus, Nishihara, Okinawa 903 - 0213, Japan. * Correspondence: E-mail: euichi @ sci. u-ryukyu. ac. jp (Hirose) -euichi@sci.u-ryukyu.ac.jp +Hirose, Euichi +Department of Chemistry, Biology and Marine Science, Faculty of Science, University of the Ryukyus, Nishihara, Okinawa 903 - 0213, Japan. * Correspondence: E-mail: euichi @ sci. u-ryukyu. ac. jp (Hirose) +euichi@sci.u-ryukyu.ac.jp - - -Author + + +Author -Nozawa, Yoko -Biodiversity Research Center, No. 128, Academia Road Sec. 2, Nankang, Taipei 115, Taiwan. E-mail: nozaway @ gate. sinica. edu. tw (Nozawa) -nozaway@gate.sinica.edu.tw +Nozawa, Yoko +Biodiversity Research Center, No. 128, Academia Road Sec. 2, Nankang, Taipei 115, Taiwan. E-mail: nozaway @ gate. sinica. edu. tw (Nozawa) +nozaway@gate.sinica.edu.tw -text - - -Zoological Studies +text + + +Zoological Studies - -2020 - -2020-06-15 + +2020 + +2020-06-15 - -59 + +59 - -19 + +19 - -1 -11 + +1 +11 - -http://dx.doi.org/10.5281/zenodo.12822057 + +http://dx.doi.org/10.5281/zenodo.12822057 -journal article -10.6620/ZS.2020.59-19 -1810-522X +journal article +10.6620/ZS.2020.59-19 +1810-522X +PMC7688397 +33262843 +12822130 - + @@ -67,11 +70,11 @@ Dome- or irregularly-shaped colonies of about 5 mm or larger were attached to hydrozoan colonies ( -Fig. 2A +Fig. 2A ). Each colony had one or a few cloacal apertures (white arrows in -Fig. 2A +Fig. 2A ). Colonies were entirely white with brown patches. Globular spicules in the tunic reflected light, resulting in the white color of the colony ( -Fig. 2B +Fig. 2B ). Several morphotypes are genetically defined in D. molle diff --git a/data/78/2F/6F/782F6F06FF98FFE8FC3B44DAFAA7FB49.xml b/data/78/2F/6F/782F6F06FF98FFE8FC3B44DAFAA7FB49.xml new file mode 100644 index 00000000000..f9af01cc1d1 --- /dev/null +++ b/data/78/2F/6F/782F6F06FF98FFE8FC3B44DAFAA7FB49.xml @@ -0,0 +1,120 @@ + + + +Fig. 5 in Paralbunea dayriti + + + +Author + +Timms, Brian V. +Honorary Research Associate, Australian Museum, 10 William St, Sydney, 2010 and Centre for Ecosystem Science, School of Biological, Earth and Environmental Sciences, University of New South Wales, Kensington, NSW 2052, Australia. * Correspondence: E-mail: brian. timms @ unsw. edu. au (Timms) +brian.timms@unsw.edu.au + + + +Author + +Rogers, D. Christopher +Kansas Biological Survey, and The Biodiversity Institute, The University of Kansas, Higuchi Hall, 2101 Constant Avenue, Lawrence, KS 66047 - 3759, USA. E-mail: Branchiopod @ gmail. com (Rogers) +Branchiopod@gmail.com + +text + + +Zoological Studies + + +2020 + +Zool. Stud. + + +2020-08-05 + + +59 + + +38 + + +1 +10 + + + + +http://dx.doi.org/10.5281/zenodo.12822326 + +journal article +10.6620/ZS.2020.59-38 +1810-522X +PMC7736776 +33335588 +12822538 + + + + + + + +Paralimnadia marplesi + +comb. nov. + + + + + + + += + + +Eulimnadia marplesi +Timms and McLay, 2005: 409–414 + + +, +Figs. 1–4 + + + + + +Comments +: This +New Zealand +species also lacks a true subcercopodal spiniform process, instead having a triangular process ( +Timms and McLay 2005 +, +Figs. 2G +, +3C +). Moreover, its cercopod spinal position is at 50% of the cercopod length, there are 9–12 antennomeres per flagellum, and in the only collection available there are +nine males +and +two females +, hardly a ratio expected for + +Eulimnadia + +, but indicative that gonochoristic reproduction is likely. There is a small mound on the endite IV corm medial surface, again not definitive. This species has far more affinities with + +Paralimnadia + +than + +Eulimnadia + +and so should be shifted to + +Paralimnadia +. + + + + + \ No newline at end of file diff --git a/data/78/2F/6F/782F6F06FF98FFE8FCCE429BFC0DF949.xml b/data/78/2F/6F/782F6F06FF98FFE8FCCE429BFC0DF949.xml new file mode 100644 index 00000000000..41ddfcc61d6 --- /dev/null +++ b/data/78/2F/6F/782F6F06FF98FFE8FCCE429BFC0DF949.xml @@ -0,0 +1,97 @@ + + + +Fig. 5 in Paralbunea dayriti + + + +Author + +Timms, Brian V. +Honorary Research Associate, Australian Museum, 10 William St, Sydney, 2010 and Centre for Ecosystem Science, School of Biological, Earth and Environmental Sciences, University of New South Wales, Kensington, NSW 2052, Australia. * Correspondence: E-mail: brian. timms @ unsw. edu. au (Timms) +brian.timms@unsw.edu.au + + + +Author + +Rogers, D. Christopher +Kansas Biological Survey, and The Biodiversity Institute, The University of Kansas, Higuchi Hall, 2101 Constant Avenue, Lawrence, KS 66047 - 3759, USA. E-mail: Branchiopod @ gmail. com (Rogers) +Branchiopod@gmail.com + +text + + +Zoological Studies + + +2020 + +Zool. Stud. + + +2020-08-05 + + +59 + + +38 + + +1 +10 + + + + +http://dx.doi.org/10.5281/zenodo.12822326 + +journal article +10.6620/ZS.2020.59-38 +1810-522X +PMC7736776 +33335588 +12822538 + + + + + + + +Paralimnadia vinculuma + +comb. nov. + + + + + + + += + + +Eulimnadia vinculuma +Timms, 2015: 449–451 + + +, Figs. 5, 7 + + + + + +Comments +: This species has a similar sharp triangular to spiniform subcercopodal process as in + +E. palustera + +so that differentiation on this character is problematic. However, the cercopod spine position at 48% of the cercopod length is distinctive and there are 11 antennomeres ( +Table 1 +) per flagellum. The mating position for this species is unknown, but the sex ratio is very nearly 1:1, and there is a distinct hamulus on the clasper; its length is slightly less than half the apical club diameter. + + + + \ No newline at end of file diff --git a/data/78/2F/6F/782F6F06FF98FFE8FF6345BBFECAF8C9.xml b/data/78/2F/6F/782F6F06FF98FFE8FF6345BBFECAF8C9.xml new file mode 100644 index 00000000000..85d1bd23c70 --- /dev/null +++ b/data/78/2F/6F/782F6F06FF98FFE8FF6345BBFECAF8C9.xml @@ -0,0 +1,103 @@ + + + +Fig. 5 in Paralbunea dayriti + + + +Author + +Timms, Brian V. +Honorary Research Associate, Australian Museum, 10 William St, Sydney, 2010 and Centre for Ecosystem Science, School of Biological, Earth and Environmental Sciences, University of New South Wales, Kensington, NSW 2052, Australia. * Correspondence: E-mail: brian. timms @ unsw. edu. au (Timms) +brian.timms@unsw.edu.au + + + +Author + +Rogers, D. Christopher +Kansas Biological Survey, and The Biodiversity Institute, The University of Kansas, Higuchi Hall, 2101 Constant Avenue, Lawrence, KS 66047 - 3759, USA. E-mail: Branchiopod @ gmail. com (Rogers) +Branchiopod@gmail.com + +text + + +Zoological Studies + + +2020 + +Zool. Stud. + + +2020-08-05 + + +59 + + +38 + + +1 +10 + + + + +http://dx.doi.org/10.5281/zenodo.12822326 + +journal article +10.6620/ZS.2020.59-38 +1810-522X +PMC7736776 +33335588 +12822538 + + + + + + + +Paralimnadia datsonae + +comb. nov. + + + + + + + += + + +Eulimnadia datsonae +Timms, 2015: 445–447 + + +, +Figs. 4 +–5 + + + + + +Comments +: This species lacks a true spiniform subcercopodal process, instead having a triangular projection covered with denticulae. Furthermore, the cercopod spine is placed at about 35% of the cercopod length, there are 11 antennomeres on each flagellum, mating is in line and sex ratios are approximately 1:1 ( +Table 1 +), all + +Paralimnadia + +characteristics. In addition, there is a robust hamulus projecting at a right angle from the endite corm IV, with its length 0.5x the apical club diameter ( +Fig. 4D +in +Timms 2016b +). Specimens from Jurien Bay, WA, are slightly different (BVT unpublished data). Significantly, there is variation in the ventroposterior area of the telson, so that it varies from rounded to somewhat triangular and always without denticles, there are 12 antennomeres on each flagellum and the hamulus is even more protruding and is slightly curved distally. The cercopod setae are absent, and the spine is small, placed midlength, and in females the cercopod is apparently geniculated. It is assumed that the nearly inerm geniculate cercopod is aberrant in this population. + + + + \ No newline at end of file diff --git a/data/78/2F/6F/782F6F06FF98FFE8FF67411BFBC8FD89.xml b/data/78/2F/6F/782F6F06FF98FFE8FF67411BFBC8FD89.xml new file mode 100644 index 00000000000..3ca2b8b05c5 --- /dev/null +++ b/data/78/2F/6F/782F6F06FF98FFE8FF67411BFBC8FD89.xml @@ -0,0 +1,118 @@ + + + +Fig. 5 in Paralbunea dayriti + + + +Author + +Timms, Brian V. +Honorary Research Associate, Australian Museum, 10 William St, Sydney, 2010 and Centre for Ecosystem Science, School of Biological, Earth and Environmental Sciences, University of New South Wales, Kensington, NSW 2052, Australia. * Correspondence: E-mail: brian. timms @ unsw. edu. au (Timms) +brian.timms@unsw.edu.au + + + +Author + +Rogers, D. Christopher +Kansas Biological Survey, and The Biodiversity Institute, The University of Kansas, Higuchi Hall, 2101 Constant Avenue, Lawrence, KS 66047 - 3759, USA. E-mail: Branchiopod @ gmail. com (Rogers) +Branchiopod@gmail.com + +text + + +Zoological Studies + + +2020 + +Zool. Stud. + + +2020-08-05 + + +59 + + +38 + + +1 +10 + + + + +http://dx.doi.org/10.5281/zenodo.12822326 + +journal article +10.6620/ZS.2020.59-38 +1810-522X +PMC7736776 +33335588 +12822538 + + + + + + + +Paralimnadia feriensis + +comb. nov. + + + + + + + += + + +Eulimnadia feriensis +Dakin, 1914: 300 + + +. Pl. 2, Figs. + + + +14–18; +Richter and Timms, 2005: 348 +; +Timms, 2015: 441–445 +, +Figs. 1–3 + + + += + + +Limnadia feriensis +Brtek, 1997: 57 + + +(list) + + + + + +Comments +: This species lacks a true spiniform subcercopodal process, instead having a rounded process covered in short spines, as observed in some juvenile + +Eulimnadia +species + +(DCR personal observation). The cercopod spine is placed at about 40% of the cercopod length, and there are 13 antennomeres on each flagellum ( +Table 2 +). Amplexus position and sex ratios are unknown. + + + + \ No newline at end of file diff --git a/data/78/2F/6F/782F6F06FF98FFE8FF6B479BFE1DFC29.xml b/data/78/2F/6F/782F6F06FF98FFE8FF6B479BFE1DFC29.xml new file mode 100644 index 00000000000..7f71d527fb6 --- /dev/null +++ b/data/78/2F/6F/782F6F06FF98FFE8FF6B479BFE1DFC29.xml @@ -0,0 +1,111 @@ + + + +Fig. 5 in Paralbunea dayriti + + + +Author + +Timms, Brian V. +Honorary Research Associate, Australian Museum, 10 William St, Sydney, 2010 and Centre for Ecosystem Science, School of Biological, Earth and Environmental Sciences, University of New South Wales, Kensington, NSW 2052, Australia. * Correspondence: E-mail: brian. timms @ unsw. edu. au (Timms) +brian.timms@unsw.edu.au + + + +Author + +Rogers, D. Christopher +Kansas Biological Survey, and The Biodiversity Institute, The University of Kansas, Higuchi Hall, 2101 Constant Avenue, Lawrence, KS 66047 - 3759, USA. E-mail: Branchiopod @ gmail. com (Rogers) +Branchiopod@gmail.com + +text + + +Zoological Studies + + +2020 + +Zool. Stud. + + +2020-08-05 + + +59 + + +38 + + +1 +10 + + + + +http://dx.doi.org/10.5281/zenodo.12822326 + +journal article +10.6620/ZS.2020.59-38 +1810-522X +PMC7736776 +33335588 +12822538 + + + + + + + +Paralimnadia centenaria + +comb. nov. + + + + + + + += + + +Eulimnadia centenaria +Timms 2016a: 365–367 + + +, +Figs. 3H, I +, 8 + + + + + +Comments +: This is another species without a true spiniform subcercopodal process, but has a rounded protrusion instead. Among the 11 species of Australian + +Eulimnadia + +described in +Timms (2016a) +, its metrics are distinctly different with a cercopod spine at 56% of the cercopod length, and 12 antennomeres per flagellum. The sex ratio in the only collection available is +12 males +to +26 females +, an indeterminate ratio but less likely to characterise + +Eulimnadia + +than + +Paralimnadia + +. It lacks a hamulus but this is not diagnostic. Unfortunately, its amplexus position is unknown. + + + + \ No newline at end of file diff --git a/data/78/2F/6F/782F6F06FF98FFEAFCDC409BFE9CFAA9.xml b/data/78/2F/6F/782F6F06FF98FFEAFCDC409BFE9CFAA9.xml new file mode 100644 index 00000000000..7e482498c32 --- /dev/null +++ b/data/78/2F/6F/782F6F06FF98FFEAFCDC409BFE9CFAA9.xml @@ -0,0 +1,190 @@ + + + +Fig. 5 in Paralbunea dayriti + + + +Author + +Timms, Brian V. +Honorary Research Associate, Australian Museum, 10 William St, Sydney, 2010 and Centre for Ecosystem Science, School of Biological, Earth and Environmental Sciences, University of New South Wales, Kensington, NSW 2052, Australia. * Correspondence: E-mail: brian. timms @ unsw. edu. au (Timms) +brian.timms@unsw.edu.au + + + +Author + +Rogers, D. Christopher +Kansas Biological Survey, and The Biodiversity Institute, The University of Kansas, Higuchi Hall, 2101 Constant Avenue, Lawrence, KS 66047 - 3759, USA. E-mail: Branchiopod @ gmail. com (Rogers) +Branchiopod@gmail.com + +text + + +Zoological Studies + + +2020 + +Zool. Stud. + + +2020-08-05 + + +59 + + +38 + + +1 +10 + + + + +http://dx.doi.org/10.5281/zenodo.12822326 + +journal article +10.6620/ZS.2020.59-38 +1810-522X +PMC7736776 +33335588 +12822538 + + + + + + + +Eulimnadia gnammaphila +Timms, 2016 + + + + + + + +Comments +: Now that + +E. feriensis + +is considered a + +Paralimnadia + +, if +Reed et al. (2015) +had correctly identified their specimens, they would have appeared as + +Paralimnadia + +and + +Eulimnadia + +in their phylogenies, but they sequenced them only as + +Eulimnadia + +. The Gene Bank accession numbers in their table 1 for + +E. dahli + +and + +E. feriensis + +, both misidentified, should be reassigned to + +E. gnammaphila +. + + + +Comments on taxonomy + + +Besides a strict interpretation of the subcercopodal projection, three other characters may be used in distinguishing between + +Eulimnadia + +and + +Paralimnadia + +: 1) cercopod setal row terminating with a small spine at or near 75–80% of cercopod length in + +Eulimnadia + +and at or near 40–65% in + +Paralimnadia + +; 2) second antenna with entire/unregenerated flagellae with antennomeres numbering ca +8 in + +Eulimnadia + +and ca +12 in + +Paralimnadia + +, and; 3) the very few or no males to females ratio suggest androdioecy and probably + +Eulimnadia + +, while 1:1 ratios indicate gonochory and + +Paralimnadia + +. It is possible some + +Eulimnadia + +( +e.g. +, + +E. hansoni + +) are gonochoristic ( +Timms 2016a +) so this character is not absolute, though there are no known + +Paralimnadia + +which reproduce androdioeciously. + +We have no molecular data to confirm the new generic placements of the species listed above in the results section. However, analyses are in progress. Based on these characters and our associated results, we revise the diagnoses for the two genera. + + + +Eulimnadia +Packard, 1874 + + + + +Diagnosis +: (modified from +Rogers et al. 2012 +). Populations composed of males and hermaphrodites or hermaphrodites only; amplexus is transverse (venter to venter). Rostrum variable, blunt to acute, long or short. Angle between rostrum and frons 100° to 80°. Occipital notch and occipital condyle absent. Pedunculate frontal organ length approximately 1.55 x distance of organ from ocular tubercle. Second antenna with ~8 antennomeres per flagellum. Carapace dorsal margin smooth, lacking carinae, hinge line arcuate, rarely sinuate. Carapace intervals smooth. Umbone absent. Carapace occasionally pigmented. Muscle scar angle from 0° to 90° from the longitudinal axis of the animal. Clasper endopods each bearing an apical suctorial organ. Endite IV may be broadly transverse or bear dense apical field of short setae, or a few long setae or spines. Thoracic segments smooth or with dorsoposterior ridge rimmed with spines or setae. Eggs attaching to prolonged exopods of thoracopods VII and VIII or VIII, VIII to IX or XII, IX and X, X and XI, or XI and XII. Telson with posteriorly directed subcercopodal spiniform projection on ventroposterior angle, anteriad of cercopod base. Telson posterior margin posteriolateral spine rows confluent dorsally, with confluence not projecting. Each row has from 6 to 22 spines. Caudal filament originating between spine rows at second, third, fourth, fifth, or seventh spine from confluence. Caudal filament borne on projecting mound. Cercopods arcuate, occasionally sinuate. Cercopod with medial longitudinal setal row on proximal 75–80%. Setae plumose and long. Setal row terminates with single spine. Cercopod with subapical, dorsal cirrus, extending from 5–30% of cercopod length. Eggs 170–250 μm in diameter. Shape spherical to subspherical or cylindrical to subcylindrical with one end larger than other. Eggs with large rectilinear polygonal depressions separated by ridges, occasionally with lamellar or setaform spines at polygon ridge line confluences ( +Belk 1989 +, Martin 1989, +Martin and Belk 1989 +, +Rabet 2010 +). Australian ( +Australia +), Afrotropical, Nearctic, Neotropical, Oriental, and Palaearctic (North Africa) bioregions. + + + + \ No newline at end of file diff --git a/data/78/2F/6F/782F6F06FF9AFFEAFF2F433AFC25FACA.xml b/data/78/2F/6F/782F6F06FF9AFFEAFF2F433AFC25FACA.xml new file mode 100644 index 00000000000..1fbc473c27d --- /dev/null +++ b/data/78/2F/6F/782F6F06FF9AFFEAFF2F433AFC25FACA.xml @@ -0,0 +1,125 @@ + + + +Fig. 5 in Paralbunea dayriti + + + +Author + +Timms, Brian V. +Honorary Research Associate, Australian Museum, 10 William St, Sydney, 2010 and Centre for Ecosystem Science, School of Biological, Earth and Environmental Sciences, University of New South Wales, Kensington, NSW 2052, Australia. * Correspondence: E-mail: brian. timms @ unsw. edu. au (Timms) +brian.timms@unsw.edu.au + + + +Author + +Rogers, D. Christopher +Kansas Biological Survey, and The Biodiversity Institute, The University of Kansas, Higuchi Hall, 2101 Constant Avenue, Lawrence, KS 66047 - 3759, USA. E-mail: Branchiopod @ gmail. com (Rogers) +Branchiopod@gmail.com + +text + + +Zoological Studies + + +2020 + +Zool. Stud. + + +2020-08-05 + + +59 + + +38 + + +1 +10 + + + + +http://dx.doi.org/10.5281/zenodo.12822326 + +journal article +10.6620/ZS.2020.59-38 +1810-522X +PMC7736776 +33335588 +12822538 + + + + + + + +Paralimnadia +Sars, 1896 + +, +sensu +Rogers et al., 2012 + + + + + + +Diagnosis +: (modified from +Rogers et al. 2012 +). Populations composed of males and females (1:1); male amplexes female on posterior carapace margin, keeping body in line, single file, behind female. Rostrum variable, from blunt to acute, long or short, in both sexes. Angle between rostrum and frons 100° to 80°. Occipital notch and condyle absent. Frontal organ pedunculate. Frontal organ length 0.5 to 1.5 times distance between base of frontal organ and base of ocular tubercle. Second antenna with ~12 antennomeres per flagellum. Carapace dorsal margin smooth, lacking carinae, hinge line arcuate, rarely sinuate. Carapace intervals smooth. Umbone absent. Carapace with or without pigmentation. Muscle scar angle 10° to 80° from normal. Thoracic segments with dorsoposterior ridge margined with spines or setae. Male first two thoracopods with endopod bearing apical suctorial organ. Endite IV typical for family, although sometimes broadly transverse or bearing dense, apical setal field. Eggs attaching to prolonged exopods of thoracopods IX and X, X and XI, or XI and XII. Telson without spiniform projection on ventroposterior angle, anteriad of cercopod base. Telson posterior margin spine rows confluent dorsally, with confluence projecting or not. Each row averaging 5–25 spines. Caudal filament originating between spine rows at third, fourth, or fifth spine from confluence, born on a mound. Cercopod with proximal portion cylindrical, distal portion narrowing. Cercopod medial surface with longitudinal row of setae along proximal 40–60%. Setae plumose, sometimes long or short. Setal row terminates with one spine. Cercopod with subapical, dorsal cirrus, extending 10–50% of cercopod length. Eggs 100–170 μm in diameter, spherical to subspherical in shape. Eggs with large rectilinear polygonal depressions separated by ridges, occasionally with lamellar or setaform spines at polygon ridge line confluences. Australian ( +Australia +, +New Zealand +) and Oriental (Sulawesi) bioregions. + + +Many authors, +e.g. +, Martin (1989), +Martin and Belk (1989) +, +Rogers et al. (2012) +, +Reed et al. (2015) +have proposed that + +Eulimnadia + +is in need of revision. Major problems centre around variability among individuals within and between populations ( +e.g. +, Straškraba 1964, +Belk 1989 +), inadequate description and illustration of species, mainly prior to the 1980s, and problems in the morphological definition of + +Eulimnadia + +( +e.g. +, +Sars 1895 +, +Daday 1925 +, +Mattox 1954 +, +Webb and Bell 1979 +, Martin 1989, +Belk 1989 +, +Brtek 1997 +, +Pereira and García 2001 +). + + + + \ No newline at end of file diff --git a/data/95/5A/2B/955A2B6A5D31FFD5020BFF6B1808FA85.xml b/data/95/5A/2B/955A2B6A5D31FFD5020BFF6B1808FA85.xml new file mode 100644 index 00000000000..167b2339687 --- /dev/null +++ b/data/95/5A/2B/955A2B6A5D31FFD5020BFF6B1808FA85.xml @@ -0,0 +1,224 @@ + + + +Gli ammonoidi della Formazione di Besano pubblicati da Airaghi nel 1912 conservati al Museo Kosmos di Pavia + + + +Author + +Pieroni, Vittorio + +text + + +Natural History Sciences + + +2023 + +2023-04-20 + + +10 + + +1 + + +13 +26 + + + + +http://dx.doi.org/10.4081/nhs.2023.610 + +journal article +10.4081/nhs.2023.610 +2385-0922 +12753673 + + + + +? + +Nevadites bassanii +(Airaghi 1912) + +comb. nov. + + + + +Fig. 1j +; +Fig. 3 +j-k + + + + +1912 + +Balatonites Bassanii +Airaghi + +, p. 26, tav. 4, fig. 8. + + + + +Locus typicus: +Tre Fontane ( +Airaghi, 1912b: 4 +). + + +Stratum typicum: +Formazione di Besano ( +Airaghi, 1912b: 4 +). + + + + +Materiale tipico: +un esemplare (olotipo per monotipia probabilmente andato perduto) descritto e figurato da +Airaghi (1912b: 26 +, tav. 4, fig. 8). Un esemplare qui considerato oloplastotipo ( +MSNPV +22944) rappresentato dal calco in gesso (positivo) dell’esemplare figurato da +Airaghi (1912b: 26 +, tav. 4, fig. 8) senza cartellino autografo di Airaghi. + + + + +Diagnosi originale +(da +Airaghi 1912b: 26 +): “È una specie piatta, discoidale, a grande ombelico col dorso (= ventre) stretto. I fianchi sono ornati da coste principali e secondarie e da quattro serie di nodi. Le coste principali sono rare e molto sviluppate e tra l’una e l’altra vi si trovano dapprima due coste secondarie e di poi una sola. Le coste principali sono fornite da tre nodi principali, uno ombelicale, uno marginale e uno laterale, quest’ultimo, però, posto molto in alto, cioè molto più vicino a quello marginale che non a quello ombelicale. Inoltre nel breve spazio compreso tra la spira dei grossi nodi laterali e quella dei grossi nodi marginali, portano un quarto nodo molto più piccolo. Le coste secondarie oltre che essere più corte sono anche meno alte, ma leggermente tortuose e sono fornite da un grosso nodo marginale e da uno e, talvolta, due piccoli nodi laterali”. + + + + +Descrizione: +Forma con avvolgimento abbastanza evoluto. La parete ombelicale non è visibile. La superficie laterale del giro è piatta, un pò convergente verso il dorso. Le coste radiali o proverse, nascono sul bordo ombelicale con un nodo arrotondato evidente, e raggiungono il bordo marginale terminando con un piccolo nodo. Su di esse sono visibili tracce di altre due file di nodi a diverse altezze del fianco. Le coste primarie abbastanza forti sono alternate da una o due coste secondarie che si sviluppano nei tre quarti esterni del fianco. Due delle coste primarie si biforcano a ¾ dell’altezza del fianco, in corrispondenza di un nodo evidente. Si contano 8 coste principali in mezzo giro. Il margine è angoloso, ma deformato, e forma colla superficie ventrale un angolo di meno di 90°. Il ventre, poco conservato, è apparentemente piano. + + +MSNPV +22944 +Airaghi (1912b: 26 +, tav. 4, fig. 8) D = 50 D = 49 + +H = 17,8 H = 18 +L = - L = 8 +O = 21 O = 19 + + + +Osservazioni: +Cartellino di anonimo con determinazione e indicazione della provenienza da “Cave Tre Fontane (Besano)”. + + +Discussione: +L’osservazione diretta dell’esemplare (calco) qui ridescritto rivela alcuni caratteri non così evidenti nella figura 8 (tav. 4) di +Airaghi 1912b +(qui riproposta: +Fig. 3k +). Il quarto nodo posto tra il nodo marginale e quello laterale più evidente è in realtà poco osservabile. Airaghi non descrive le biforcazioni di due delle coste primarie. Le coste primarie sono molto forti e diritte soprattutto nell’ultima parte di giro conservata. I fianchi sono uniformemente convergenti verso l’ombelico. +Airaghi (1912b: 28) +distingue + +Balatonites De Alessandrii + +sp. nov. +da + +Balatonites Bassanii + +sp. nov. +“per le coste più rare, più diritte e per la mancanza dei nodi laterali secondari” (= il quarto nodo presente su +B. Bassanii +). +Rieber (1973: 66) +pone proprio questo esemplare figurato da Airaghi in sinonimia con + +Protrachyceras dealessandri + +che +Brack & Rieber 1986 +assegnano al genere + +Nevadites + +. +Rieber (1973: 66) +nella diagnosi emendata di + +Protrachyceras + +(= + +Nevadites + +) + +dealessandrii +(Airaghi 1912) + +descrive per questa specie tre o quattro file di nodi, giustificando quindi la sinonimia, che non viene discussa nel dettaglio. Le forme assegnate da +Rieber 1973 +a + +Nevadites dealessandrii + +mostrano una certa variabilità soprattutto nello spessore delle coste secondarie, talvolta del tutto simili a quelle primarie, così come anche il quarto nodo è un carattere variabile. Tuttavia la specie di Airaghi con coste primarie molto forti, con nodi marginali più simili a ingrossamenti latero-marginali delle stesse coste e superficie del fianco convergente verso l’ombelico, appare differente sia dalle altre forme descritte da Airaghi, sia da quelle descritte da Rieber. L’area ventrale mal conservata dell’esemplare qui descritto appare piatta, mentre negli esemplari di + +Balatonites dealessandrii + +e + +Balatonites ambrosionii +Airaghi 1912 + +così come in + +Protrachyceras + +(= + +Nevadites + +) + +dealessandrii + +e in + +Protrachyceras + +(= + +Nevadites + +) + +ambrosionii +(Airaghi 1912) + +illustrati da Rieber, i nodi marginali spinosi sono spostati verso il ventre. Queste differenze appaiono sufficienti per ritenere la specie + +Balatonites Bassanii + +distinta dalle altre forme simili. L’attribuzione al genere + +Nevadites + +, dato lo stato di conservazione dell’area ventrale del presente esemplare, rimane incerta. + + + + \ No newline at end of file diff --git a/data/95/5A/2B/955A2B6A5D32FFD4020BF8B4180BF879.xml b/data/95/5A/2B/955A2B6A5D32FFD4020BF8B4180BF879.xml new file mode 100644 index 00000000000..d95a39f8231 --- /dev/null +++ b/data/95/5A/2B/955A2B6A5D32FFD4020BF8B4180BF879.xml @@ -0,0 +1,189 @@ + + + +Gli ammonoidi della Formazione di Besano pubblicati da Airaghi nel 1912 conservati al Museo Kosmos di Pavia + + + +Author + +Pieroni, Vittorio + +text + + +Natural History Sciences + + +2023 + +2023-04-20 + + +10 + + +1 + + +13 +26 + + + + +http://dx.doi.org/10.4081/nhs.2023.610 + +journal article +10.4081/nhs.2023.610 +2385-0922 +12753673 + + + + + +Genere + +Ticinites +Rieber 1973 + + + + + + +Specie tipo: + +Ticinites ticinensis +Rieber 1973 + + + + + + +Ticinites +cf. +ticinensis +Rieber 1973 + + + + + +Fig. 1 +f-g; +Fig. 3 +f-i + + + + +1912 + +Celtites Fumagallii + +(Stabile in +Stoppani +1860) – Airaghi, p. 9, tav. 4, fig. 1. + + + + +Materiale: +un esemplare ( +MSNPV +22945), costituito dal calco in gesso (positivo) dell’esemplare descritto e figurato da +Airaghi (1912b: 9 +, tav. 4, fig. 1) proveniente da “Cave Tre Fontane”. + + + + +Descrizione: +Questa forma con avvolgimento evoluto mostra sezione del giro subrettangolare quasi trapezoidale, arrotondata, più alta che larga. La parete ombelicale è relativamente alta e obliqua, distinta da uno scalino arrotondato dalla superficie laterale del giro, che è poco convessa, convergente verso il ventre. Le coste radiali, nascono sul bordo ombelicale con un nodo arrotondato, e raggiungono il bordo marginale terminando con un nodo evidente. L’esemplare reca nell’ultimo giro 19 coste semplici. Il margine è angoloso, poco arrotondato, e forma colla superficie ventrale un angolo di circa 100°. Il ventre è convesso, lievemente carenato. I giri interni recano tracce di coste mal conservate. + + + + + + + + + + + + + + + + + + + + + + + + +
MSNPV 22945 +Airaghi (1912b: 9 +, tav. 4, fig. 1) +
D = 44,4D = 40
H = 14 (a D = 40, H = 13,2)H = 12
L = 11,5 (a D = 40, L = 10,7)L = 8
O = 19,3 (a D = 40, O = 18)O = 19
+ + + +Osservazioni: +Privo di cartellino autografo di Airaghi. Cartellino di anonimo con determinazione e indicazione della provenienza da Besano. Il cartellino non autografo di Airaghi riporta erroneamente Airaghi come autore della specie: “ + +Celtites Fumagallii +Airaghi + +”. Si tratta evidentemente di un cartellino compilato senza controllare la pubblicazione di +Airaghi (1912b) +. + + +Discussione: +L’esemplare (calco) mostra alcune differenze rispetto al disegno di +Airaghi (1912b +, tav. 4, fig. 1): le coste dell’ultimo giro sono 19 anziché 22 e sono ben visibili tubercoli marginali; il calco appare completo mentre nel disegno ci sono due parti mancanti con diametro tratteggiato; i giri interni sono meno ben conservati che nel disegno. Inoltre il calco mostra ventre convesso lievemente carenato. Il calco ha diametro massimo di +44,4 mm +, mentre la figura di Airaghi essendo incompleta può essere misurata solo a diametro di +40 mm +(come riportato da +Airaghi, 1912b: 10 +). Lo spessore del giro (larghezza) è maggiore nel calco: a diametro +40 mm + +è +10,7 mm + +, invece di +8 mm +. I caratteri di questo esemplare, più che corrispondere alla specie di Stabile (figurata da +Mariani, 1901: 50 +, qui riprodotta in figura 4), la quale ha crescita più lenta, totalmente mancante dei tubercoli marginali e con parete ombelicale molto bassa, sembra corrispondere a + +Ticinites ticinensis +Rieber 1973 + +. Quest’ultimo infatti ha crescita più rapida e ombelico più stretto, tubercoli marginali, parete ombelicale alta e sezione del giro più trapezoidale. Per tali motivi +MSNPV +22945 non corrisponde al tipo di + +Celtites fumagallii + +figurato da +Mariani (1901) +come indicato da Airaghi (1912), mentre è più probabilmente avvicinabile alla specie + +Ticinites ticinensis +Rieber 1973 + +. + + + + \ No newline at end of file diff --git a/data/95/5A/2B/955A2B6A5D32FFD70145F94C1EF8F90C.xml b/data/95/5A/2B/955A2B6A5D32FFD70145F94C1EF8F90C.xml new file mode 100644 index 00000000000..40d2b3c4897 --- /dev/null +++ b/data/95/5A/2B/955A2B6A5D32FFD70145F94C1EF8F90C.xml @@ -0,0 +1,171 @@ + + + +Gli ammonoidi della Formazione di Besano pubblicati da Airaghi nel 1912 conservati al Museo Kosmos di Pavia + + + +Author + +Pieroni, Vittorio + +text + + +Natural History Sciences + + +2023 + +2023-04-20 + + +10 + + +1 + + +13 +26 + + + + +http://dx.doi.org/10.4081/nhs.2023.610 + +journal article +10.4081/nhs.2023.610 +2385-0922 +12753673 + + + + +“ + +Ceratites +” +repossii +Airaghi 1912 + + + + + +Fig. 1h +; +Fig. 3 +d-e + + + + +1912 + +Ceratites Repossii +Airaghi + +, p. 16, tav. 2, fig. 6. + + +Locus typicus: +Tre Fontane ( +Airaghi, 1912b: 3 +). + + +Stratum typicum: +Formazione di Besano ( +Airaghi, 1912b: 3 +). + + + + +Materiale tipico: +un esemplare (olotipo per monotipia probabilmente andato perduto) descritto e figurato da +Airaghi (1912b: 16 +, tav. 2, fig. 6). Un esemplare qui considerato oloplastotipo ( +MSNPV +22941) rappresentato dal calco in gesso (positivo) dell’esemplare descritto e figurato da +Airaghi (1912b: 16 +, tav. 2, fig. 6) senza cartellino autografo di Airaghi. + + + + +Descrizione: +forma con avvolgimento relativamente evoluto. La parete ombelicale è molto bassa e subverticale, la superficie laterale del giro è piatta, parallela al piano di avvolgimento. Le coste proverse, nascono sul bordo ombelicale con un piccolo nodo e recano un nodo laterale ben visibile dal quale le coste si biforcano. La biforcazione però è appena visibile poiché le coste quasi svaniscono per ricomparire poco prima dei nodi marginali allungati in avanti. Il numero dei nodi laterali è circa la metà dei nodi marginali. Si contano circa 8 coste in mezzo giro. Il margine è angoloso, poco arrotondato, e forma colla superficie ventrale un angolo di poco più di 90°. La regione ventrale, incompleta, è poco convessa. + + + + +Osservazioni: +Cartellino di anonimo con determinazione e indicazione della provenienza da “Cave Tre Fontane (Besano)”. + + +Discussione: +L’ampiezza ombelicale e la scultura del fianco conservato sono compatibili con i caratteri del genere + +Stoppaniceras +Rieber 1973 + +. Rieber mette in sinonimia + +Ceratites repossi +Airaghi 1912 + +con + +C. artinii +Airaghi 1912 + +. Tuttavia la prima specie mostra nodi ombelicali estremamente ridotti e tra i nodi laterali e quelli marginali le coste sono appena visibili, mentre in + +C. artinii + +(esemplare di dimensioni nettamente maggiori) la scultura è più sviluppata e nell’ultima metà giro le coste non si biforcano e sono molto forti. +Airaghi (1912b: 16) +sottolinea nella sua descrizione la forte carena ventrale di + +Ceratites repossi + +(= “ +dorso fortemente carenato +”). Purtroppo sull’esemplare (calco) qui descritto non è osservabile l’area ventrale. L’esemplare giovanile figurato da +Rieber 1973 +a tav. 14, fig. 4, di + +Stoppaniceras artinii + +mostra caratteri della scultura abbastanza simili a quelli dell’esemplare di + +Ceratites repossi +di Airaghi + +, che potrebbe rappresentare uno stadio ontogenetico giovanile di + +C. artinii + +. Considerando lo stato di conservazione del presente esemplare e il probabile stadio ontogenetico giovanile, appare comunque almeno probabile la messa in sinonimia di + +Ceratites repossi +Airaghi 1912 + +con + +C. artinii +Airaghi 1912 + += + +Stoppaniceras artinii + +in +Rieber (1973) +. + + + + \ No newline at end of file diff --git a/data/95/5A/2B/955A2B6A5D38FFDB020BFDC51E9EFD12.xml b/data/95/5A/2B/955A2B6A5D38FFDB020BFDC51E9EFD12.xml new file mode 100644 index 00000000000..7f0b38c43a3 --- /dev/null +++ b/data/95/5A/2B/955A2B6A5D38FFDB020BFDC51E9EFD12.xml @@ -0,0 +1,330 @@ + + + +Gli ammonoidi della Formazione di Besano pubblicati da Airaghi nel 1912 conservati al Museo Kosmos di Pavia + + + +Author + +Pieroni, Vittorio + +text + + +Natural History Sciences + + +2023 + +2023-04-20 + + +10 + + +1 + + +13 +26 + + + + +http://dx.doi.org/10.4081/nhs.2023.610 + +journal article +10.4081/nhs.2023.610 +2385-0922 +12753673 + + + + + +Serpianites serpianensis +(Airaghi 1912) + + + + + +Fig. 1 +l-m; +Fig. 2 +d-f + + + + +1912 + +Ceratites serpianensis + +sp. nov. +Airaghi, p. 15, tav. 2, fig. 2, 4. + + +?1912 + +Ceratites serpianensis + +sp. nov. +Airaghi, p. 15, tav. 2, fig. 3, 5. + + +1912 + +Ceratites besanensis + +sp. nov. +Airaghi, p. 23, tav. 3, fig. 1, 2. + + +?1912 + +Ceratites comottii +Mojsisovics 1882 + +– Airaghi, p. 12. + + +Fig. 1 - Esemplari conservati al Museo di Pavia con i rispettivi cartellini originali e i numeri di inventario. Genere e specie come originariamente riportati da Airaghi. Per le dimensioni degli esemplari vedi testo e le Fig. 3 e 4. / Specimens stored in the museum of Pavia, paired with the matching original labels and inventory numbers. Genera and species after Airaghi. For dimensions of specimens see the text and Fig. 3 and 4. + +a: MSNPV 21564 +: + +Celtites taramellii +Airaghi 1912 + +. Calco in gesso con cartellino autografo di Airaghi e cartellino della Regia Università di Pavia, Museo di Geologia. / Plaster cast paired with label hand written by Airaghi and label headed “Regia Università di Pavia, Museo di Geologia”. + + +b: MSNPV 21562 +: + +Ceratites artinii +Airaghi 1912 + +. Originale (impronta esterna) con cartellino autografo di Airaghi e cartellino della Regia Università di Pavia, Museo di Geologia. / Original specimen (external mould) paired with label hand written by Airaghi and label headed “Regia Università di Pavia, Museo di Geologia”. + + +c: MSNPV 21567a +: + +Celtites fumagallii + +(Stabile in +Stoppani, 1860 +) +Mariani, 1901 +. Tre originali (impronte esterne) con cartellino autografo di Airaghi e cartellino della Regia Università di Pavia, Museo di Geologia. / Three original specimens (external moulds) paired with handwritten label by Airaghi and headed “Regia Università di Pavia, Museo di Geologia”. + + +d: MSNPV 21567b +: + +Celtites fumagallii + +(Stabile in +Stoppani, 1860 +) +Mariani, 1901 +. Tre originali (impronte esterne) con cartellino autografo di Airaghi e cartellino della Regia Università di Pavia, Museo di Geologia. / Three original specimens (external moulds) paired with handwritten label by Airaghi and headed “Regia Università di Pavia, Museo di Geologia”. + + +e: MSNPV 21567c +: + +Celtites fumagallii + +(Stabile in +Stoppani, 1860 +) +Mariani, 1901 +. Tre originali (impronte esterne) con cartellino autografo di Airaghi e cartellino della Regia Università di Pavia, Museo di Geologia. / Three original specimens (external moulds) paired with handwritten label by Airaghi and headed “Regia Università di Pavia, Museo di Geologia”. + + +f: MSNPV 22945 +: + +Celtites fumagallii + +(Stabile in +Stoppani 1860 +) +Mariani 1901 +. Calco in gesso con cartellino della Regia Università di Pavia, Museo di Geologia (norma laterale). / Plaster cast paired with label headed “Regia Università di Pavia, Museo di Geologia” (lateral view). + + +g: MSNPV 22945 +: + +Celtites fumagallii + +(Stabile in +Stoppani 1860 +) +Mariani 1901 +. Calco in gesso con cartellino della Regia Università di Pavia, Museo di Geologia (norma ventrale). / Plaster cast paired with label headed “Regia Università di Pavia, Museo di Geologia” (ventral view). + + +h: MSNPV 22941 +: + +Ceratites repossii +Airaghi 1912 + +. Calco in gesso con cartellino della Regia Università di Pavia, Museo di Geologia. / Plaster cast paired with label headed “Regia Università di Pavia, Museo di Geologia”. + + +i: MSNPV 21569b +: + +Ceratites artinii +Airaghi 1912 + +. Calco in gesso privo di cartellino, conservato nella stessa scatoletta di MSNPV 21569a. / Plaster cast without label, found in the same box of MSNPV 21569a. + + +j: MSNPV 22944 +: + +Balatonites bassanii +Airaghi 1912 + +. Calco in gesso con cartellino della Regia Università di Pavia, Museo di Geologia. / Plaster cast paired with label headed “Regia Università di Pavia, Museo di Geologia”. + + +k: MSNPV 21569a +: + +Ceratites marianii +Airaghi 1912 + +. Calco in gesso con cartellino autografo di Airaghi e cartellino della Regia Università di Pavia, Museo di Geologia. / Plaster cast paired with handwritten label by Airaghi and headed “Regia Università di Pavia, Museo di Geologia”. + + +l: MSNPV 21565a +: + +Ceratites serpianensis +Airaghi 1912 + +. Due originali (impronta esterna) con cartellino autografo di Airaghi e cartellino della Regia Università di Pavia, Museo di Geologia. / Two original specimens (external moulds) paired with label hand written by Airaghi and label headed “Regia Università di Pavia, Museo di Geologia”. + + +m: MSNPV 21565b +: + +Ceratites serpianensis +Airaghi 1912 + +. Due originali (impronta esterna) con cartellino autografo di Airaghi e cartellino della Regia Università di Pavia, Museo di Geologia. / Two original specimens (external moulds) paired with label hand written by Airaghi and label headed “Regia Università di Pavia, Museo di Geologia”. + + + +V +1973 + +Serpianites serpianensis +(Airaghi 1912) + +– Rieber, p. 48, tav. 13, fig. 1-4, 10-13. + + +?1995 + +Serpianites +aff. +serpianensis + +– Mietto & Manfrin, p. 551, tav. 3, fig. 1 + + +V +2011 + +Serpianites serpianensis + +– Pieroni, p. 60, tav. 7 cefal., fig. 1-5 + + +Locus typicus: +Tre Fontane ( +Airaghi, 1912b: 3 +). + + +Stratum typicum: +Formazione di Besano ( +Airaghi, 1912b: 3 +). + + + + +Materiale tipico: +i 5 esemplari originali descritti e figurati da +Airaghi (1912b: 15 +, tav. 2, fig. 1-5) che rappresentavano la serie tipo sono andati perduti. Il +neotipo +per questa specie è stato istituito da +Rieber (1973: 48 +, tav. 13, fig. 1). Due esemplari ( +MSNPV +21565a-b) costituiti da due esemplari originali (impronte esterne) in matrice (dolomia bituminosa, Formazione di Besano) considerati qui come +topotipi +. Le due impronte esterne sono abbastanza ben conservate e sono conservate in un’unica scatola con il cartellino autografo di Airaghi: + +Ceratites serpianensis Airaghi. Zona Cerat. +trinodosus. Besano + +. + + + + +Descrizione: +Avvolgimento involuto e sezione del giro subrettangolare, più alta che larga. La parete ombelicale è molto arrotondata. I fianchi sono pressochè paralleli. Il forte ricoprimento dei giri lascia comunque scoperta la porzione più prossima al bordo ombelicale, anche nei giri interni. I primi giri recano coste larghe, poco sporgenti, ravvicinate. Poi tra lo stadio giovanile e lo stadio maturo (ultimo giro) queste coste ravvicinate scompaiono lasciando una zona (circa 90° di spira) quasi priva di scultura. Nello stadio maturo le lievi coste radiali nascono sul bordo ombelicale senza nodi. Prima di raggiungere la metà altezza del giro su di esse si sviluppa un forte nodo spinoso. Da questo nodo, nell’ultima parte del giro maturo conservato, le coste si biforcano raggiungendo il margine ventrale, dove si sviluppa un altro nodo spinoso molto forte, ma un po’ meno sporgente di quello sul fianco. Nell’ultimo mezzo giro si contano 5 coste, con 5 tubercoli laterali, di cui le ultime due coste sono biforcate, quindi al margine ventrale si contano 7 nodi. Il margine è angoloso, poco arrotondato, e forma colla superficie ventrale un angolo di 100°-110°. Il ventre è convesso, carenato. La convessità diminuisce verso l’apertura. Sia sull’esemplare di medie dimensioni, sia su quello più frammentario di grosse dimensioni, si notano le strie di accrescimento, radiali e un po’ flessuose. Le dimensioni in millimetri di +MSNPV +21565a sono: D = 45; H = 19,5; L = 14,6; O = 11,2. + + + + +Osservazioni: +Sul cartellino originale non è specificata la località di provenienza. Comunque, tutti gli esemplari di questa specie citati da +Airaghi (1912b) +provenivano da Tre Fontane. + + +Discussione: +Questi due esemplari non fanno parte della serie tipo perché non citati dall’autore ( +Airaghi 1912b +elenca solo i cinque esemplari illustrati) e possono essere considerati +topotipi +, in quanto provenienti dalla località tipo. L’esemplare più completo +MSNPV +21565a mostra evidente carena ventrale. Entrambi gli esemplari sono ben corrispondenti alla figura 4, tav. 2 di Airaghi1912b della serie tipo di + +Ceratites serpianensis + +nov. sp. +e al +neotipo +di + +Serpianites serpianensis +(Airaghi 1912) + +istituito da +Rieber (1973 +, tav. 13, fig. 1). Ottima corrispondenza soprattutto dell’esemplare +MSNPV +21565a che mostra 7 nodi marginali nell’ultima metà giro e ampiezza ombelicale molto simile. + + + + \ No newline at end of file diff --git a/data/95/5A/2B/955A2B6A5D39FFDD020BFEF018ADFE41.xml b/data/95/5A/2B/955A2B6A5D39FFDD020BFEF018ADFE41.xml new file mode 100644 index 00000000000..add7bbbadc2 --- /dev/null +++ b/data/95/5A/2B/955A2B6A5D39FFDD020BFEF018ADFE41.xml @@ -0,0 +1,159 @@ + + + +Gli ammonoidi della Formazione di Besano pubblicati da Airaghi nel 1912 conservati al Museo Kosmos di Pavia + + + +Author + +Pieroni, Vittorio + +text + + +Natural History Sciences + + +2023 + +2023-04-20 + + +10 + + +1 + + +13 +26 + + + + +http://dx.doi.org/10.4081/nhs.2023.610 + +journal article +10.4081/nhs.2023.610 +2385-0922 +12753673 + + + + +Specie tipo: + +Celtites epolensis + +Mojsisovics 1882 + + + + +“ +Celtites +” +taramellii +Airaghi 1912 + + + + +Fig. 1a +; +Fig. 2 +a-c + + +1912 +Celtites Taramellii +Airaghi, p. 11, tav. 3, fig. + +6. + + + +Locus typicus: +Tre Fontane ( +Airaghi, 1912b: 3 +). + + +Stratum typicum: +Formazione di Besano ( +Airaghi, 1912b: 3 +). + + + + +Diagnosi originale +(da +Airaghi 1912b: 16 +): “È una specie compressa, discoidale, con un dorso quasi uniformemente convesso e privo di carena, coi fianchi forniti da coste alquanto sviluppate e numerose, +26 in +un sol giro, e tutte quante rivolte molto all’avanti. Queste coste incominciano lungo il margine ombelicale da un piccolo nodo e attraversano il fianco terminando al margine dorsale talora in un altro nodo molto più piccolo”. + + + + +Descrizione: +Questa forma con avvolgimento evoluto mostra sezione del giro subquadrata. La parete ombelicale è molto bassa e subverticale, distinta da uno scalino più o meno netto dalla superficie laterale del giro, che è piatta, parallela al piano di avvolgimento. Le coste proverse, nascono sul bordo ombelicale con un nodo arrotondato un po’ arretrato rispetto alla costa, e raggiungono il bordo marginale terminando con un piccolo nodo che si allunga leggermente oltre la spalla marginale, nell’area ventrale. L’esemplare incompleto reca 13 coste in mezzo giro (Airaghi ne riportava +26 in +un giro completo). Nello spazio intermedio tra le coste, sono presenti lievi accenni a costicine secondarie più proverse delle coste principali. Il margine è angoloso, poco arrotondato, e forma colla superficie ventrale un angolo di 90°. Il ventre è piano, poco convesso, privo di carena. Sulla porzione più esterna conservata dell’ultimo giro le coste laterali divengono più sporgenti e massive, senza tubercoli visibili. + + + + + + + + + + + + + + + + + + + + + + + + +
MSNPV 21564 +Airaghi (1912b:11 +, tav. 3, fig. 6) +
D = 30,1D = 30
H = 6,4H = 7
L = 6?L = 6
O = 17,6O = 17
+ + + +Discussione: +L’attribuzione di questa forma, come delle altre forme simili descritte da +Airaghi 1912b +, al genere +Celtites +è probabilmente da rivedere. La specie tipo +Celtites epolensis +Mojsisovics, 1882 +ha sezione del giro più ovale, il passaggio tra l’area ventrale e i fianchi non è marcato da spalla angolosa, le coste sono più fitte e sottili senza forti tubercoli ombelicali. +Rieber (1973) +propone di riunire le varie specie di +Celtites +presenti nella Formazione di Besano sotto un’unica specie con grande variabilità infraspecifica. Tuttavia al momento la documentazione paleontologica di queste forme, di cui si conosce assai poco la linea di sutura, non sembra sufficiente per prendere una decisione in merito. +Airaghi (1912b: 11) +avvicina la presente specie a +Celtites evolutus +Salomon, 1895 +. Anche se la forma generale e il grado di evoluzione di quest’ultima specie è molto simile a +C. taramellii +, la forma di Salomon rimane ben distinta soprattutto per la sezione dei giri più arrotondata e le coste più massive e semplici. + + + + \ No newline at end of file diff --git a/data/95/5A/2B/955A2B6A5D3CFFD7020BFE3C18AFF970.xml b/data/95/5A/2B/955A2B6A5D3CFFD7020BFE3C18AFF970.xml new file mode 100644 index 00000000000..7fdb65bd01b --- /dev/null +++ b/data/95/5A/2B/955A2B6A5D3CFFD7020BFE3C18AFF970.xml @@ -0,0 +1,407 @@ + + + +Gli ammonoidi della Formazione di Besano pubblicati da Airaghi nel 1912 conservati al Museo Kosmos di Pavia + + + +Author + +Pieroni, Vittorio + +text + + +Natural History Sciences + + +2023 + +2023-04-20 + + +10 + + +1 + + +13 +26 + + + + +http://dx.doi.org/10.4081/nhs.2023.610 + +journal article +10.4081/nhs.2023.610 +2385-0922 +12753673 + + + + + +Genere + +Stoppaniceras +Rieber 1973 + + + + + + +Specie tipo: + +Stoppaniceras variabilis +Rieber 1973 + + +Stoppaniceras artinii +(Airaghi 1912) + + + + + +Fig. 1b, 1i +; +Fig. 3 +a-c + + +1912 + +Ceratites Artinii +Airaghi + +, p. 23, tav. 3, fig. 5 + + +V +1973 + +Stoppaniceras artinii + +- Rieber, p. 42, tav. 14, fig. 1. 3, 4, 6, 9, 10 + + +V +2011 + +Stoppaniceras variabilis + +- Pieroni, p. 63, tav. + +8cefal., fig. 4 + +Locus typicus: +Tre Fontane ( +Airaghi, 1912b: 4 +). + + +Stratum typicum: +Formazione di Besano ( +Airaghi, 1912b: 4 +). + + + + +Materiale tipico: +un esemplare (olotipo per monotipia probabilmente andato perduto) descritto e figurato da +Airaghi, 1912b +, p. 23, tav. 3, fig. 5. Il +neotipo +per questa specie è stato istituito da +Rieber (1973 +, tav. 14, fig. 1). Un esemplare rappresentato da un calco in gesso ( +MSNPV +21569b, +Fig. 1i +, +Fig. 3 +a-b) dell’esemplare descritto e figurato da +Airaghi (1912b: 23 +, tav. 3, fig. 5) proveniente da “Cave Tre Fontane”, qui considerato oloplastotipo. + + + +Un esemplare originale ( +MSNPV 21562 +, impronta esterna, +Fig. 1b +, +Fig. 3c +) in matrice (dolomia bituminosa, + +Formazione +di Besano + +) qui considerato come +topotipo +. Cartellino autografo +di Airaghi +: + +Ceratites Artinii Airaghi. Zona Cerat. +trinodosus. +Cave Tre Fontane +(Besano + +) + +. + + +Descrizione: +MSNPV +21569b Forma con avvolgimento evoluto. La parete ombelicale è molto bassa, la superficie laterale del giro è piatta, parallela al piano di avvolgimento. Le coste appena proverse, nascono sul bordo ombelicale con un nodo arrotondato, poco prima della metà altezza del giro si sviluppa un secondo nodo da cui solo alcune coste si biforcano. Le coste raggiungono il bordo marginale terminando con un piccolo nodo quasi spinoso. Prima di formare il nodo marginale le coste tendono a piegarsi in avanti. L’esemplare maturo +MSNPV +21569b reca 9 coste in mezzo giro, che biforcandosi divengono 13 nella regione esterna del fianco. Il ventre non è osservabile. Sulla porzione più esterna conservata dell’ultimo giro le coste laterali divengono più sporgenti e non si biforcano più. L’esemplare giovanile +MSNPV +21562 mostra avvolgimento poco evoluto. La parete ombelicale è molto bassa. La superficie laterale del giro è piatta, parallela al piano di avvolgimento. Le coste sono radiali nell’area interna del giro, mentre divengono proverse nella metà esterna. Le coste nascono sul bordo ombelicale con un nodo arrotondato, poco prima della metà altezza del giro si viluppa un secondo nodo da cui le coste si biforcano, divenendo più sottili. Le coste raggiungono il bordo marginale terminando con un piccolo nodo allungato. Si contano 6 coste in mezzo giro, che si biforcano più o meno tutte, quindi i tubercoli marginali risultano circa il doppio di quelli laterali. Il ventre non è conservato. Le dimensioni in millimetri dell’esemplare sono: D = 38,3; H = 16,8; L non rilevabile; O = 10,8. + + + + +Fig. 3 - Nuovi calchi in silicone ricavati dagli esemplari originali (impronte esterne), conservati al Museo di Pavia, non pubblicati da +Airaghi (1912b) +e confronto tra il materiale conservato al Museo di Pavia e le figure pubblicate da +Airaghi (1912b) +. Genere e specie rivisti nel presente lavoro e come originariamente riportati da Airaghi. / New silicon rubber casts produced from the original specimens (external moulds), stored in the museum of Pavia, not published by +Airaghi (1912b) +, and comparison between the material stored in the museum of Pavia and the figures published by +Airaghi (1912b) +. Taxa (genera and species) are listed as follows: taxon herein revised = taxon after Airaghi. + + +a-b: + +Stoppaniceras artinii +(Airaghi 1912) + += + +Ceratites artinii +Airaghi 1912 + +. +a: +Calco in gesso imbiancato di MSNPV 21569b (oloplastotipo); +b: +figura 5, tav. 3, da +Airaghi (1912b) +. / +a +: whitened plaster cast of MSNPV 21569b (holoplastotype); +b +: figure 5, pl. 3, after +Airaghi (1912b) +. + + +c: + +Stoppaniceras artinii +(Airaghi 1912) + += + +Ceratites artinii +Airaghi 1912 + +, MSNPV 21562 (topotipo / topotype). Nuovo calco in silicone. / New silicon rubber cast. + + +d-e: +“ + +Ceratites +” +repossii +Airaghi 1912 + += + +Ceratites repossii +Airaghi 1912 + +. +d: +Calco in gesso imbiancato di MSNPV 22941 (oloplastotipo); +e: +figura 6, tav. 2, da +Airaghi (1912b) +. / +d +: Whitened plaster cast of MSNPV 22941 (holoplastotype); +e +: figure 6, pl. 2, after +Airaghi (1912b) +. + + +f-i: + +Ticinites +cf. +ticinensis +Rieber, 1973 + += + +Celtites fumagallii + +(Stabile in +Stoppani 1860 +) +Mariani, 1901 +. +f,h,i: +Calco in gesso imbiancato di MSNPV 22945; +g: +figura 1, tav. 4, da +Airaghi (1912b) +. / +f +, +h +, +i +: whitened plaster cast of MSNPV 22945; +g +: figure 1, pl. 4, after +Airaghi (1912b) +. + + +j-k: +? + +Nevadites bassanii +(Airaghi 1912) + +comb. nov. += + +Balatonites bassanii +Airaghi 1912 + +. +j: +Calco in gesso imbiancato di MSNPV 22944 (oloplastotipo); +k: +figura 8, tav. 4, da +Airaghi (1912b) +. / +j +: whitened plaster cast of MSNPV 22944 (holoplastotype); +k +: figure 8, pl. 4, after +Airaghi (1912b) +. + + + + + + + + + + + + + + + + + + + + + + + + +
MSNPV 22941Airaghi (1912: 16, tav. 2, fig. 6)
D = 42,2D = 43
H = 17H = 18
L = -L = 8
O = 13,7O = 15
+ + + + + + + + + + + + + + + + + + + + + + + +
MSNPV 21569b +Airaghi (1912b: 23 +, tav. 3, fig. 5) +
D = 85D = 90
H = 26H = 29
L = -L = -
O = 35,6O = 38
+ + + +Osservazioni: +Il calco +MSNPV +21569b, privo di cartellino, era conservato con +MSNPV +21569a. + + +Discussione: +L’ampiezza ombelicale e la scultura del fianco conservato sono compatibili con i caratteri del genere + +Stoppaniceras +Rieber, 1973 + +. L’esemplare (calco) +MSNPV +21569b, privo della regione ventrale, corrisponde bene alla figura 5, tav. 3, di Airaghi. Esso corrisponde bene ai caratteri dell’esemplare figurato da +Rieber (1973 +, tav. 14, fig. 1) e designato quale +neotipo +di + +Stoppaniceras artinii +(Airaghi 1912) + +. L’esemplare +MSNPV +21562 molto mal conservato non fa parte della serie tipo perché non citato dall’autore. Può essere considerato +topotipo +in quanto proveniente dalla località tipo e con cartellino autografo di Airaghi. Nonostante la conservazione l’esemplare mostra caratteri simili a + +Ceratites artinii +Airaghi 1912 + +. In particolare si notano i nodi laterali posti a circa metà altezza del giro. Anche le forme descritte da +Rieber (1973) +come + +Stoppaniceras artinii +(Airaghi 1912) + +mostrano caratteri abbastanza corrispondenti al presente esemplare. + + + + \ No newline at end of file diff --git a/data/95/5A/2B/955A2B6A5D3EFFD9020BFD6A1FA4FEA6.xml b/data/95/5A/2B/955A2B6A5D3EFFD9020BFD6A1FA4FEA6.xml new file mode 100644 index 00000000000..5bb42f59e94 --- /dev/null +++ b/data/95/5A/2B/955A2B6A5D3EFFD9020BFD6A1FA4FEA6.xml @@ -0,0 +1,276 @@ + + + +Gli ammonoidi della Formazione di Besano pubblicati da Airaghi nel 1912 conservati al Museo Kosmos di Pavia + + + +Author + +Pieroni, Vittorio + +text + + +Natural History Sciences + + +2023 + +2023-04-20 + + +10 + + +1 + + +13 +26 + + + + +http://dx.doi.org/10.4081/nhs.2023.610 + +journal article +10.4081/nhs.2023.610 +2385-0922 +12753673 + + + + + + +Serpianites marianii +(Airaghi 1912) + + +comb. nov. + + + + +Fig. 1k +; +Fig. 2 +g-h + + +1912 + +Ceratites Marianii + +sp. nov. +Airaghi, p. 16, tav. 1, fig. 6. + + +Locus typicus: +Tre Fontane ( +Airaghi, 1912b: 3 +). + + +Stratum typicum: +Formazione di Besano ( +Airaghi, 1912b: 3 +). + + +Materiale tipico: +un esemplare (olotipo per monotipia probabilmente andato perduto) descritto e figurato da +Airaghi (1912b: 16 +, tav. 1, fig.6). Un esemplare qui considerato oloplastotipo ( +MSNPV +21569a) rappresentato dal calco in gesso dell’esemplare figurato da +Airaghi (1912b: 16 +, tav. 1, fig. 6). Cartellino autografo di Airaghi: “ + +Ceratites Marianii Airaghi. Zona Cerat. +trinodosus. Cave Tre Fontane. Besano + +”. + + +Diagnosi originale +(da +Airaghi 1912b: 16 +): “È una bella specie a spira molto rapida, coi giri molto alti che si ricoprono un po’ più di metà; l’ombelico è ampio; i fianchi sono quasi piani, il dorso largo e leggermente convesso. Le coste dapprima sono diritte, grosse, larghe, rare e fornite da nodi laterali molto sviluppati e alquanto allungati, e da nodi marginali più grossi. Più tardi le coste si appiattiscono e si allargano diventando flessuose e falciformi e contemporaneamente, a distanze varie dell’ombelico, si staccono dalle coste secondarie di diversa larghezza e grossezza. Anche i nodi laterali diventono sempre più allungati e meno forti, mentre invece quelli marginali gradatamente diventono sempre più grossi. Le coste secondarie sono sempre prive dei nodi e laterali e marginali +”. + + + +Fig. 2 - Nuovi calchi in silicone ricavati dagli esemplari originali (impronte esterne), conservati al Museo di Pavia, non pubblicati da +Airaghi (1912b) +e confronto tra il materiale conservato al Museo di Pavia e le figure pubblicate da +Airaghi (1912b) +. Genere e specie rivisti nel presente lavoro e come originariamente riportati da Airaghi. / New silicon rubber casts obtained from the original specimens (external moulds), stored in the museum of Pavia, not published by +Airaghi (1912b) +, and comparison between the material stored in the museum of Pavia and the figures published by +Airaghi (1912b) +. Taxa (genera and species) are listed as follows: taxon herein revised = taxon after Airaghi. + + +a-c: +“ + +Celtites +” +taramellii +Airaghi 1912 + += + +Celtites taramellii +Airaghi 1912 + +. +a-b: +Calco in gesso imbiancato di MSNPV 21564 (oloplastotipo); +c: +figura 6, tav. 3, da +Airaghi (1912b) +. / +a -b +: Whitened plaster cast of MSNPV 21564 (holoplastotype); +c +: figura 6, pl. 3, after +Airaghi (1912b) +. + + +d-e: + +Serpianites serpianensis +(Airaghi 1912) + += + +Ceratites serpianensis +Airaghi 1912 + +, MSNPV 21565a (topotipo / topotype). Nuovo calco in silicone. / New silicon rubber cast. + + +f: + +Serpianites serpianensis +(Airaghi 1912) + += + +Ceratites serpianensis +Airaghi 1912 + +, MSNPV 21565b (topotipo / topotype). Nuovo calco in silicone. / New silicon rubber cast. + + +g-h: + +Serpianites marianii +(Airaghi 1912) + +comb. nov. += + +Ceratites marianii +Airaghi 1912 + +. +g: +Calco in gesso imbiancato di MSNPV 21569a (oloplastotipo); +h: +figura 6, tav. 1, da +Airaghi (1912b) +. / +g +: whitened plaster cast of MSNPV 21569a (holoplastotype); +h +: figure 6, pl. 1, after +Airaghi (1912b) +. + + + +Descrizione: +Forma con avvolgimento relativamente involuto. La parete ombelicale è molto bassa e obliqua. La regione interna del fianco degrada lentamente verso l’ombelico, mentre verso il ventre il fianco è subparallelo al piano di avvolgimento. Le coste appena proverse, nascono molto lievi a poca distanza dal bordo ombelicale senza nodi, un nodo basso, quasi un ingrossamento della costa, si sviluppa prima della metà altezza del giro, poi le coste raggiungono il bordo marginale terminando con un nodo spinoso. Si contano 9 coste in mezzo giro, senza biforcazioni. Nell’ultima parte di giro conservata le coste tendono a svanire, assumendo l’aspetto di strie di accrescimento sinuose. Il margine è angoloso, poco arrotondato. Il ventre non è visibile. + + + + + + + + + + + + + + + + + + + + + + + +
MSNPV 21569a +Airaghi (1912b: 16 +, tav. 1, fig. 6) +
D = 93D = 92
H = 43,2H = 46
L = -L = 32
O = 25,3O = 25
+ + +Osservazioni: +Questo calco, pur non presentando la regione ventrale, corrisponde bene alla figura 6, tav. 1, di +Airaghi (1912b) +. + + +Discussione: +L’ampiezza ombelicale e la scultura del fianco conservato sono compatibili con i caratteri del genere + +Serpianites +Rieber, 1973 + +. Tra le forme descritte da +Airaghi 1912b +quella che più si avvicina all’esemplare (calco) di + +Ceratites marianii + +qui descritto è + +Ceratites zinae + +nov. sp. +Tuttavia questa seconda specie come descrive +Airaghi (1912b: 14) +ha fianchi rigonfi, carena evidente, nodi laterali ben sviluppati (non allungati) e il numero dei nodi marginali di poco superiore a quello dei nodi laterali. Un confronto tra il +neotipo +di +Rieber 1973 +di + +Serpianites zinae +( +Airaghi 1912b +) + +, che ha dimensioni molto simili al presente esemplare, mostra differenze in particolare nei nodi: nell’esemplare di Rieber i nodi laterali sono corti e spinosi, mentre in + +C. marianii + +sono allungati e bassi. In entrambe le forme l’ultima parte del giro è quasi priva di scultura evidente sui fianchi, con strie di accrescimento un poco sinuose, ma nell’esemplare di Rieber sono presenti lievi coste biforcate in corrispondenza dei nodi laterali, mentre in + +C. marianii + +le coste non sono mai biforcate. + + + + \ No newline at end of file