diff --git a/data/03/8C/8F/038C8F41F820096E62B1D5F1FAF58F37.xml b/data/03/8C/8F/038C8F41F820096E62B1D5F1FAF58F37.xml new file mode 100644 index 00000000000..6e1cbd2e041 --- /dev/null +++ b/data/03/8C/8F/038C8F41F820096E62B1D5F1FAF58F37.xml @@ -0,0 +1,141 @@ + + + +New dinosauromorph specimens from Petrified Forest National Park and a global biostratigraphic review of Triassic dinosauromorph body fossils + + + +Author + +Marsh, Adam D. + + + +Author + +Parker, William G. + +text + + +PaleoBios + + +2022 + +37 + + +1 +56 + + + +journal article +10.5070/P9371050859 +0031-0298 + + + + + + +ARCHOSAURIA COPE, 1869 +SENSU +NESBITT, 2011 AVEMETATARSALIA BENTON, 1999 +SENSU +NESBITT ET AL. + +, + + + +2017 ORNITHODIRA GAUTHIER, 1986 +SENSU +NESBITT ET AL., 2017 + + + + +FIG. 4A–J + + + + +Referred specimens and localities +— +PEFO +36741 ( +Fig. 4A–E +), left metatarsal I, +PFV +215: Zuni Well Mound, +PFM +; +PEFO +44217 ( +Fig. 4F–J +), right metatarsal I, +PFV +217: Dinosaur Wash, +BMM +. + + + + +Description and rationale for assignment +—Metatarsals I of PEFO 36741 and PEFO 44217 are proportionally long and slender metapodials and, as observed by the crushing of PEFO 34741, hollow. The proximal end of PEFO 34371 is twisted with respect to the distal end. In proximal view, the medial surface is nearly straight where it would articulate with metatarsal II, and the lateral edge is rounded, making a subtriangular proximal outline ( +Fig. 4D, I +). The proximal outline is mediolaterally narrow, which indicates that the metatarsus was compact, not splayed (Ezcurra 2016:565-1). A compact metatarsus is present in ornithodirans and some early crocodylomorphs (Nesbitt 2011, Ezcurra 2016). The proximal surface of PEFO 36741 and PEFO 44217 is flat, would articulate with the distal tarsals, and would reach the proximal extent of metatarsal II, unlike in neotheropods where metatarsal I is more distally placed along the back of the metatarsus (Rauhut 2003, Nesbitt 2011:385-1). The distal end is asymmetrical, such that the medial condyle is more prominent than the lateral ( +Fig. 4E, J +). Both distal condyles have a collateral ligament fossa. In dorsal view, the medial condyle projects distally further than the lateral. The distal condyles of metatarsal I in the crocodylomorphs + +Protosuchus richardsoni +Brown (1933) + +(AMNH FR 3024), Colbert and Mook 1951: fig. 20b) and + +Terrestrisuchus gracilis +Crush (1984) + +are not asymmetrical (Crush 1984: fig. 10e). Asymmetrical distal condyles of metatarsal I are found in + +Heterodontosaurus tucki +Crompton and Charig + +(1962, SAM-PK-K1332) (Santa Lucas 1980: fig. 20b), + +Eoraptor lunensis +Sereno et al. + +(1993, PVSJ 512) (Sereno et al. 2012: fig. 91b), + +Saturnalia tupiniquim +Langer et al. + +(1999, MCP PV 3844) (Langer 2003: fig. 7e), + +Herrerasaurus ischigualastensis +Reig + +(1963, PVSJ 373) (Novas 1993: fig. 9j) and + +Coelophysis bauri + +(MNA V3320, Nesbitt 2011: fig. 48f), but not in the non-dinosaur dinosauriform + +Asilisaurus kongwe +Nesbitt et al. + +(2010, NMT RB159) (Nesbitt et al. 2019: fig. 53e). The PEFO specimens are identical to metatarsal I of GR 1033 (Nesbitt et al. 2009a: fig. 2j), a partial skeleton of +Tawa + +hallae +Nesbitt et al. (2009a) + +. We assign PEFO 36741 and PEFO 44217 to non-neotheropod Ornithodira owing to the presence of a compact metatarsal I that is not distally positioned down the metatarsus. + + + + \ No newline at end of file diff --git a/data/03/8C/8F/038C8F41F824096A6288D2ADFB2D8F15.xml b/data/03/8C/8F/038C8F41F824096A6288D2ADFB2D8F15.xml new file mode 100644 index 00000000000..81b926e918a --- /dev/null +++ b/data/03/8C/8F/038C8F41F824096A6288D2ADFB2D8F15.xml @@ -0,0 +1,136 @@ + + + +New dinosauromorph specimens from Petrified Forest National Park and a global biostratigraphic review of Triassic dinosauromorph body fossils + + + +Author + +Marsh, Adam D. + + + +Author + +Parker, William G. + +text + + +PaleoBios + + +2022 + +37 + + +1 +56 + + + +journal article +10.5070/P9371050859 +0031-0298 + + + + + + +DINOSAURIA OWEN, 1842 +SENSU +PADIAN AND + +MAY, 1993 + + + + + +FIG. 6A–H + + + + +Referred specimens and localities +— +PEFO +44475 ( +Fig. 6A–D +), proximal ends of left and right femora, +PFV +376: Scour Sandstone, +PFM +; +PEFO +34583 ( +Fig. 6E, F +), proximal end of left femur, +PFV +332: Chinde Valley Pin- nacle, +PFM +; +PEFO +34863 ( +Fig. 6G, H +), proximal end of left femur, +PFV +215: Zuni Well Mound, +PFM +. + + + + +Description and rationale for assignment +—These proximal ends of femora are highly fragmentary and weathered; each of them is broken proximal to the fourth trochanter. Each preserves a mound-like anterior trochanter that remains attached to the shaft proximally (Nesbitt 2011:308-1) ( +Fig. 6D +), which is a feature present in Dinosauriformes, e.g., + +Marasuchus lilloensis + +(PVL + + +3871, Sereno and Arcucci 1994: fig. 8b), + +Asilisaurus kongwe + +(NMT RB159, Nesbitt et al. 2019: fig. 42d), and + +Buriolestes schultzi + +(ULBRA-PVT280, Cabreira et al. 2016: fig. 1n). Unlike the smooth transition between the ventromedial margin of the femoral head and the shaft (Nesbitt 2011:304-0) found in early dinosauromorphs, e.g., + +Lagerpeton chanarensis +Romer + +(1971, PVL 4619) (Nesbitt et al. 2009b: fig. 3a), and + +Dromomeron romeri + +(GR 218, Nesbitt et al. 2009b: fig. 1a) and the ventral notch (Nesbitt 2011:304-1) present on silesaurid femora (see above), these femora exhibit a concave emargination ventral to the femoral head (Nesbitt 2011:304-2) ( +Fig. 6H +), which is apomorphic for dinosaurs, e.g., + +Eocursor parvus + +(SAM-PK-K8025, Butler 2009: fig. 15d), + +Eodromaeus murphi +Martínez et al. + +(2011, PVSJ 562: fig. 2k), and + +Herrerasaurus ischigualastensis + +(PVSJ 373, Novas 1993: fig. 7c). Thus, we assign these fragmentary proximal ends of femora to +Dinosauria +. + + + + \ No newline at end of file diff --git a/data/03/8C/8F/038C8F41F8240974614CD462FF3489E9.xml b/data/03/8C/8F/038C8F41F8240974614CD462FF3489E9.xml new file mode 100644 index 00000000000..bb6b3bd4469 --- /dev/null +++ b/data/03/8C/8F/038C8F41F8240974614CD462FF3489E9.xml @@ -0,0 +1,339 @@ + + + +New dinosauromorph specimens from Petrified Forest National Park and a global biostratigraphic review of Triassic dinosauromorph body fossils + + + +Author + +Marsh, Adam D. + + + +Author + +Parker, William G. + +text + + +PaleoBios + + +2022 + +37 + + +1 +56 + + + +journal article +10.5070/P9371050859 +0031-0298 + + + + + + +SAURISCHIA SEELEY, 1887 +SENSU +GAUTHIER, 1986 + +(=EUSAU- RISCHIA PADIAN ET AL., 1999) + + + + + +FIG. 6I–T + + + + +Referred specimens and localities +— +PEFO +21660/ +UCMP +126751 ( +Fig. 6I, J +), distal end of right femur, +PFV +071: Flattops W, +UCMP +V +82259, +PFM +; +PEFO +33956 ( +Fig. 6K–L +), distal end of right femur, +PFV +231: The Giving Site, +PFM +; +PEFO +44469 ( +Fig. 6M, N +), distal end of right femur, +PFV +451: Black Knoll E, +PFM +; +PEFO +34562 ( +Fig. 6O, P +), distal end of left femur, +PFV +184: Clambake Amphitheater, +PFM +; +PEFO +44474 ( +Fig. 6Q, R +), distal end of left femur, +PFV +492: Dead Wash NW2, +PFM +; +PEFO +42987/ +UWBM +117640 ( +Fig. 6S, T +), distal end of left femur, +PFV +410: Kaye Quarry, +UWBM +C2226, Jim Camp Wash beds, +SM +. + + + + +Description and rationale for assignment +—These distal ends of femora are all broken distal to the fourth trochanter, but they all preserve the distal medial and lateral condyles and +crista tibiofibularis +, except PEFO 33956 ( +Fig. 6K +), which is lacking most of the +crista tibiofibularis +. In all of the specimens, a groove divides the lateral condyle and +crista tibiofibularis +in distal view (Nesbitt 2011:322-1) ( +Fig. 6I +), which is a synapomor- phy of +Saurischia +, e.g., + +Herrerasaurus ischigualastensis + +(PVSJ 373, Novas 1993: fig. 7f), + +Saturnalia tupiniquim + +(MCP PV 3844, Langer 2003: fig. 4d), and ‘ + +Syntarsus + +’ +kayentakatae +(MNA +V2623 +). Furthermore, this groove opens posterolaterally in an obtuse angle in distal view in all these specimens. Shuvosaurid pseudosuchians have a similar morphology in the distal end of the femur but can be differentiated as their groove opens at a 90° angle (Parker and Irmis 2005). A similar groove is also + +A C E +G +B F H +mc ctf g ctf g K mc +lc +N +ctf +lc mc lc +mc + + +Figure 6 +. +A–D +. Proximal ends of right and left dinosaur femora, PEFO 44475 in proximal ( +A +, +C +) and anterior view ( +B +, +D +). +E +, +F +. Proximal end of left dinosaur femur, PEFO 34583 in proximal ( +E +) and anterior ( +F +) view. +G +, +H +. Proximal end of left dinosaur femur, PEFO 34863 in proximal ( +G +) and anterior ( +H +) view. +I +, +J +. Distal end of right saurischian femur, PEFO 21660/UCMP 126751 in distal ( +I +) and posterior ( +J +) view. +K +, +L +. Distal end of right saurischian femur, PEFO 33956 in distal ( +K +) and posterior ( +L +) view. +M +, +N +. Distal end of right saurischian femur, PEFO 44469 in distal ( +M +) and posterior ( +N +) view. +O +, +P +. Distal end of left saurischian femur, PEFO 34562 in distal ( +O +) and posterior ( +P +) view. +Q +, +R +. Distal end of left saurischian femur, PEFO 44474 in distal ( +Q +) and posterior ( +R +) view. +S +, +T +. Distal end of left saurischian femur, PEFO 42987/UWBM 117640 in distal ( +S +) and posterior ( +T +) view. Abbreviations: +at +, anterior trochanter; +ctf +, +crista tibiofibularis +; +g +, groove; +lc +, lateral condyle; +mc +, medial condyle; +ve +, ventral emargination. Scale bars=1 cm, arrows point in anterior direction. + + + +present convergently in lagerpetids (Garcia et al. 2019: fig. 7a–h), but in that group the +crista tibiofibularis +is greatly enlarged and is larger than the medial condyle in distal view (Nesbitt 2011:326-1), e.g., + +Dromomeron romeri + +(GR 218, Nesbitt et al. 2009b: fig. 1d). + + +In distal view, the posterior margin of the medial condyle is rounded in PEFO 21660/UCMP 126751 ( +Fig. 6I +), PEFO 44469 ( +Fig. 6M +), and PEFO 44474 ( +Fig. 6Q +), and pointed in PEFO 33956 ( +Fig. 6K +), PEFO 34562 ( +Fig. 6O +), and PEFO 42987/UWBM 117640 ( +Fig. 6S +). A round medial condyle is present in most early dinosaur groups, including ornithischians, e.g., + +Eocursor parvus + +(SAM-PK-K8025, Butler 2009: fig. 15f), and + +Scutellosaurus lawleri + +(MNA V175), early sauropodomorphs, e.g., + +Buriolestes schultzi + +(ULBRA-PVT280, Cabriera et al. 2016: fig. s2e), and + +Sa. tupiniquim + +(MCP PV 3844, Langer 2003: fig. 4d), early theropods, e.g., + +Tawa +hallae + +(GR 244, Nesbitt 2011: fig. 39b), and + +H. ischigualastensis + +(PVSJ 373, Novas 1993: fig. 7f), and stem-averostrans, e.g., + +Dilophosaurus wetherilli + +(UCMP 37302, Marsh and Rowe 2020: fig. 20.6), and + +Cryolophosaurus ellioti +Hammer and Hickerson + +(1994, FMNH +PR +4923). A pointed medial condyle is present in the large-bodied coelophysid specimens from PEFO (PEFO 21373/UCMP 129618 and PEFO 33981). In distal view, the +crista tibiofibularis +and lateral condyle are not well separated from one another in PEFO 44474 ( +Fig. 6Q +), much like the condition found in + +Chindesaurus bryansmalli + +(PEFO 10395, +Marsh et al. 2019a +: fig. 7f) and + +T. hallae + +(GR 244, Nesbit 2011: fig. 39b). In the other specimens ( +Fig. 6O +), the +crista tibiofibularis +and lateral condyle are distinctly separate structures and resemble the distal outline of theropods such as coelophysids and stem-averostran (Ezcurra 2017: figs. 4.1, 4.3, 4.4, 4.6, 4.7). We assign these distal femora to +Saurischia +owing to the presence of a groove between the lateral condyle and +crista tibiofibularis +that opens at an obtuse angle in distal view. + + + + \ No newline at end of file diff --git a/data/03/FA/86/03FA864EFF842F75FF1AFAECFB4AFE18.xml b/data/03/FA/86/03FA864EFF842F75FF1AFAECFB4AFE18.xml index 55fc4d612ad..3f06a6c3f25 100644 --- a/data/03/FA/86/03FA864EFF842F75FF1AFAECFB4AFE18.xml +++ b/data/03/FA/86/03FA864EFF842F75FF1AFAECFB4AFE18.xml @@ -1,66 +1,66 @@ - - - -Small island but great diversity: thirty six species of Parmotrema (Parmeliaceae, lichenized Ascomycota), including sixteen new species, on Réunion (Mascarenes), with additional data from the Western Indian Ocean + + + +Small island but great diversity: thirty six species of Parmotrema (Parmeliaceae, lichenized Ascomycota), including sixteen new species, on Réunion (Mascarenes), with additional data from the Western Indian Ocean - - -Author + + +Author -Masson, Didier -0000-0002-3340-5472 -Vertevoye, 2860 route d’Irieu, F- 40390 Saint-Martin-de-Seignanx, France di. masson @ wanadoo. fr; https: // orcid. org / 0000 - 0002 - 3340 - 5472 -di.masson@wanadoo.fr +Masson, Didier +0000-0002-3340-5472 +Vertevoye, 2860 route d’Irieu, F- 40390 Saint-Martin-de-Seignanx, France di. masson @ wanadoo. fr; https: // orcid. org / 0000 - 0002 - 3340 - 5472 +di.masson@wanadoo.fr - - -Author + + +Author -Magain, Nicolas -0000-0001-5409-9518 -Evolution and Conservation Biology, InBios research centre, Sart Tilman B 22, Quartier Vallée 1, Chemin de la vallée 4, B- 4000 Liège, Belgium nicolas. magain @ uliege. be; https: // orcid. org / 0000 - 0001 - 5409 - 9518 -nicolas.magain@uliege.be +Magain, Nicolas +0000-0001-5409-9518 +Evolution and Conservation Biology, InBios research centre, Sart Tilman B 22, Quartier Vallée 1, Chemin de la vallée 4, B- 4000 Liège, Belgium nicolas. magain @ uliege. be; https: // orcid. org / 0000 - 0001 - 5409 - 9518 +nicolas.magain@uliege.be - - -Author + + +Author -Sérusiaux, Emmanuël -0000-0002-3340-5472 -Vertevoye, 2860 route d’Irieu, F- 40390 Saint-Martin-de-Seignanx, France di. masson @ wanadoo. fr; https: // orcid. org / 0000 - 0002 - 3340 - 5472 & Evolution and Conservation Biology, InBios research centre, Sart Tilman B 22, Quartier Vallée 1, Chemin de la vallée 4, B- 4000 Liège, Belgium e. serusiaux @ uliege. be; https: // orcid. org / 0000 - 0002 - 0456 - 0131 * Corresponding author & Vertevoye, 2860 route d’Irieu, F- 40390 Saint-Martin-de-Seignanx, France di. masson @ wanadoo. fr; https: // orcid. org / 0000 - 0002 - 3340 - 5472 -di.masson@wanadoo.fr +Sérusiaux, Emmanuël +0000-0002-3340-5472 +Vertevoye, 2860 route d’Irieu, F- 40390 Saint-Martin-de-Seignanx, France di. masson @ wanadoo. fr; https: // orcid. org / 0000 - 0002 - 3340 - 5472 & Evolution and Conservation Biology, InBios research centre, Sart Tilman B 22, Quartier Vallée 1, Chemin de la vallée 4, B- 4000 Liège, Belgium e. serusiaux @ uliege. be; https: // orcid. org / 0000 - 0002 - 0456 - 0131 * Corresponding author & Vertevoye, 2860 route d’Irieu, F- 40390 Saint-Martin-de-Seignanx, France di. masson @ wanadoo. fr; https: // orcid. org / 0000 - 0002 - 3340 - 5472 +di.masson@wanadoo.fr -text - - -Phytotaxa +text + + +Phytotaxa - -2024 - -2024-06-27 + +2024 + +2024-06-27 - -657 + +657 - -1 + +1 - -1 -138 + +1 +138 - -http://dx.doi.org/10.11646/phytotaxa.657.1.1 + +http://dx.doi.org/10.11646/phytotaxa.657.1.1 -journal article -10.11646/phytotaxa.657.1.1 -1179-3163 -13217474 +journal article +10.11646/phytotaxa.657.1.1 +1179-3163 +13217474 - + @@ -745,7 +745,7 @@ montane forest, on bark of a branch of (Hb. DM). - + MADAGASCAR . Analamanga diff --git a/data/03/FA/86/03FA864EFF8F2F71FF1AFCCFFF58FE50.xml b/data/03/FA/86/03FA864EFF8F2F71FF1AFCCFFF58FE50.xml index e0aa58543df..7abadbb407b 100644 --- a/data/03/FA/86/03FA864EFF8F2F71FF1AFCCFFF58FE50.xml +++ b/data/03/FA/86/03FA864EFF8F2F71FF1AFCCFFF58FE50.xml @@ -1,66 +1,66 @@ - - - -Small island but great diversity: thirty six species of Parmotrema (Parmeliaceae, lichenized Ascomycota), including sixteen new species, on Réunion (Mascarenes), with additional data from the Western Indian Ocean + + + +Small island but great diversity: thirty six species of Parmotrema (Parmeliaceae, lichenized Ascomycota), including sixteen new species, on Réunion (Mascarenes), with additional data from the Western Indian Ocean - - -Author + + +Author -Masson, Didier -0000-0002-3340-5472 -Vertevoye, 2860 route d’Irieu, F- 40390 Saint-Martin-de-Seignanx, France di. masson @ wanadoo. fr; https: // orcid. org / 0000 - 0002 - 3340 - 5472 -di.masson@wanadoo.fr +Masson, Didier +0000-0002-3340-5472 +Vertevoye, 2860 route d’Irieu, F- 40390 Saint-Martin-de-Seignanx, France di. masson @ wanadoo. fr; https: // orcid. org / 0000 - 0002 - 3340 - 5472 +di.masson@wanadoo.fr - - -Author + + +Author -Magain, Nicolas -0000-0001-5409-9518 -Evolution and Conservation Biology, InBios research centre, Sart Tilman B 22, Quartier Vallée 1, Chemin de la vallée 4, B- 4000 Liège, Belgium nicolas. magain @ uliege. be; https: // orcid. org / 0000 - 0001 - 5409 - 9518 -nicolas.magain@uliege.be +Magain, Nicolas +0000-0001-5409-9518 +Evolution and Conservation Biology, InBios research centre, Sart Tilman B 22, Quartier Vallée 1, Chemin de la vallée 4, B- 4000 Liège, Belgium nicolas. magain @ uliege. be; https: // orcid. org / 0000 - 0001 - 5409 - 9518 +nicolas.magain@uliege.be - - -Author + + +Author -Sérusiaux, Emmanuël -0000-0002-3340-5472 -Vertevoye, 2860 route d’Irieu, F- 40390 Saint-Martin-de-Seignanx, France di. masson @ wanadoo. fr; https: // orcid. org / 0000 - 0002 - 3340 - 5472 & Evolution and Conservation Biology, InBios research centre, Sart Tilman B 22, Quartier Vallée 1, Chemin de la vallée 4, B- 4000 Liège, Belgium e. serusiaux @ uliege. be; https: // orcid. org / 0000 - 0002 - 0456 - 0131 * Corresponding author & Vertevoye, 2860 route d’Irieu, F- 40390 Saint-Martin-de-Seignanx, France di. masson @ wanadoo. fr; https: // orcid. org / 0000 - 0002 - 3340 - 5472 -di.masson@wanadoo.fr +Sérusiaux, Emmanuël +0000-0002-3340-5472 +Vertevoye, 2860 route d’Irieu, F- 40390 Saint-Martin-de-Seignanx, France di. masson @ wanadoo. fr; https: // orcid. org / 0000 - 0002 - 3340 - 5472 & Evolution and Conservation Biology, InBios research centre, Sart Tilman B 22, Quartier Vallée 1, Chemin de la vallée 4, B- 4000 Liège, Belgium e. serusiaux @ uliege. be; https: // orcid. org / 0000 - 0002 - 0456 - 0131 * Corresponding author & Vertevoye, 2860 route d’Irieu, F- 40390 Saint-Martin-de-Seignanx, France di. masson @ wanadoo. fr; https: // orcid. org / 0000 - 0002 - 3340 - 5472 +di.masson@wanadoo.fr -text - - -Phytotaxa +text + + +Phytotaxa - -2024 - -2024-06-27 + +2024 + +2024-06-27 - -657 + +657 - -1 + +1 - -1 -138 + +1 +138 - -http://dx.doi.org/10.11646/phytotaxa.657.1.1 + +http://dx.doi.org/10.11646/phytotaxa.657.1.1 -journal article -10.11646/phytotaxa.657.1.1 -1179-3163 -13217474 +journal article +10.11646/phytotaxa.657.1.1 +1179-3163 +13217474 - + @@ -839,7 +839,7 @@ on Parmotrema subarnoldii .— - + MADAGASCAR . Analamanga @@ -889,22 +889,23 @@ H. des Abbayes 2357 + + ( REN 000061 , lectotype ; - -US -[image!], + +US [image!], isolectotype ) . - + RWANDA . diff --git a/data/03/FA/86/03FA864EFFED2F12FF1AFAA8FA9EF891.xml b/data/03/FA/86/03FA864EFFED2F12FF1AFAA8FA9EF891.xml new file mode 100644 index 00000000000..c27457597ae --- /dev/null +++ b/data/03/FA/86/03FA864EFFED2F12FF1AFAA8FA9EF891.xml @@ -0,0 +1,862 @@ + + + +Small island but great diversity: thirty six species of Parmotrema (Parmeliaceae, lichenized Ascomycota), including sixteen new species, on Réunion (Mascarenes), with additional data from the Western Indian Ocean + + + +Author + +Masson, Didier +0000-0002-3340-5472 +Vertevoye, 2860 route d’Irieu, F- 40390 Saint-Martin-de-Seignanx, France di. masson @ wanadoo. fr; https: // orcid. org / 0000 - 0002 - 3340 - 5472 +di.masson@wanadoo.fr + + + +Author + +Magain, Nicolas +0000-0001-5409-9518 +Evolution and Conservation Biology, InBios research centre, Sart Tilman B 22, Quartier Vallée 1, Chemin de la vallée 4, B- 4000 Liège, Belgium nicolas. magain @ uliege. be; https: // orcid. org / 0000 - 0001 - 5409 - 9518 +nicolas.magain@uliege.be + + + +Author + +Sérusiaux, Emmanuël +0000-0002-3340-5472 +Vertevoye, 2860 route d’Irieu, F- 40390 Saint-Martin-de-Seignanx, France di. masson @ wanadoo. fr; https: // orcid. org / 0000 - 0002 - 3340 - 5472 & Evolution and Conservation Biology, InBios research centre, Sart Tilman B 22, Quartier Vallée 1, Chemin de la vallée 4, B- 4000 Liège, Belgium e. serusiaux @ uliege. be; https: // orcid. org / 0000 - 0002 - 0456 - 0131 * Corresponding author & Vertevoye, 2860 route d’Irieu, F- 40390 Saint-Martin-de-Seignanx, France di. masson @ wanadoo. fr; https: // orcid. org / 0000 - 0002 - 3340 - 5472 +di.masson@wanadoo.fr + +text + + +Phytotaxa + + +2024 + +2024-06-27 + + +657 + + +1 + + +1 +138 + + + + +http://dx.doi.org/10.11646/phytotaxa.657.1.1 + +journal article +10.11646/phytotaxa.657.1.1 +1179-3163 +13217474 + + + + + +Identification key to the + +Parmotrema + +species of +Réunion Island + + + + + + + +1. Medulla P− or P+ faint yellow ......................................................................................................................................................... 2 + + +- Medulla P+ orange ......................................................................................................................................................................... 18 + + + + +2. Medulla K−, C−, KC− ...................................................................................................................................................................... 3 + + +- At least one of these 3 tests positive ................................................................................................................................................. 5 + + + + + +3. Without vegetative propagules .......................................................................................................................... [ + +P. appendiculatum + +] (lobe margins and apothecia with corniculate laciniae, apothecial disc imperforate, medulla pigmented yellow near apothecia and containing barbatic acid and secalonic acid A; very rare species not recovered on +Réunion +since the 19 +th +century) + + + +- With vegetative propagules .............................................................................................................................................................. 4 + + + + + +4. Thallus sorediate, lobes without cilia ................................................................................................................... + +P. praesorediosum + +(upper surface emaculate, soralia linear marginal when young, becoming labriform and crescent-shaped [ +Fig. 34D +], medulla with fatty acids other than protolichesterinic acid; uncommon species on +Réunion +, at low elevations) + + + + +- Thallus isidiate and/or laciniate, cilia numerous ............................................................................................................. + +P. intonsum + +(shaggy appearance [ +Fig. 21E +], upper surface ± distinctly punctiform white-maculate, esorediate, medulla with protolichesterinic acid as major substance; rather common in Reunionese cloud forests) + + + + + + +5. Medulla K+ yellow, C−, KC− (atranorin, fatty acids) .......................................................................................... + +P. praesorediosum + +(chemotype with atranorin, in addition to fatty acids, in the medulla) + + + +- Other medullary reactions ................................................................................................................................................................ 6 + + + + + +6. Medulla K+ slowly pinkish brick red, C−, KC+ fleeting violet then brick red (lividic acid chemosyndrome) ......... + +P. reunionicum + +(lobe margins with conspicuous cilia, upper surface emaculate or faintly punctiform white-maculate, soralia mainly marginal and forming ± rounded clusters with age [ +Fig. 36C +]; rare species, only known from a single locality) + + + +- Medulla K−, C+ and/or KC+ pink, red, orange, or purple (lividic acid chemosyndrome absent) ................................................... 7 + + + + +7. Medulla C+ and KC+ pink, red or orange ........................................................................................................................................ 8 + + +- Medulla C−, KC+ purple, pinkish or orange .................................................................................................................................. 12 + + + + + +8. Medulla C+ and KC+ orange .............................................................................................................................. + +P. aurantioreagens + +(lobe margins ciliate, upper surface faintly to clearly effigurate white-maculate, soralia marginal at the tip of short laciniae [ +Fig. 7D +], medulla with barbatic and 4- +O +-demethylbarbatic acids as major substances; rare species, only known from a single locality) + + + +- Medulla C+ and KC+ pink or red ..................................................................................................................................................... 9 + + + + +9. Thallus sorediate ............................................................................................................................................................................. 10 + + +- Thallus isidiate ................................................................................................................................................................................ 11 + + + + + +10. Lobes with marginal cilia ................................................................................................................................................... + +P. cooperi + +(upper surface faintly effigurate white-maculate, soralia marginal at first, then submarginal on revolute lobe apices [ +Fig. 13D +], medulla with lecanoric acid; in leeward + +Acacia + +montane forests on +Réunion +) + + + + +- Lobes without cilia ................................................................................................................................................... + +P. austrosinense + +(upper surface emaculate or faintly effigurate white-maculate, soralia linear and marginal [ +Fig. 8D +], medulla with lecanoric acid; uncommon species on +Réunion +) + + + + + + +11. Lower surface at main lobe tips with a brown erhizinate marginal zone +1–3 mm +wide, lobes +2–9 mm +wide, medulla with evernic acid .......................................................................................................................................................................... + +P. meiospermum + +(lobe margins eciliate, upper surface faintly to clearly punctiform white-maculate, isidia marginal and laminal, eciliate and coralloid-branched, medulla with evernic and lecanoric acids; rare species) + + + + +- Lower surface at main lobe tips with a brown erhizinate marginal zone +4–15 mm +wide, lobes +5–20 mm +wide, medulla without evernic acid ..................................................................................................................................................................... + +P. tinctorum + +(lobe margins eciliate, upper surface emaculate to faintly white-maculate, isidia marginal and laminal, eciliate, simple to coralloid-branched, medulla with lecanoric acid; common species on +Réunion +, from sea level to the upper limit of cloud forests) + + + + + +12. Thallus without vegetative propagules ........................................................................................................................................... 13 + + +- Thallus with isidia or soralia .......................................................................................................................................................... 14 + + + + + +13. Pycnidia conspicuous, marginal, verruciform ( +Fig. 43B +); thalline exciple smooth to rugose .................................... [ + +P. thomsonii + +] (lobe margins ciliate, upper surface distinctly white-maculate, apothecial disc perforate, medulla with alectoronic and α-collatolic acids; very rare species not recovered on +Réunion +since the 19 +th +century) + + + + +- Pycnidia inconspicuous, immersed; thalline exciple with abundant and well-developed isidioid protuberances ( +Fig. 26C +) ............ .............................................................................................................................................................................................. + +P. mirum + +(lobe margins ciliate but cilia sometimes rare, upper surface emaculate, apothecial disc perforate or imperforate, medulla with alectoronic acid (constant) with or without α-collatolic acid; uncommon species on +Réunion +) + + + + + + +14. Thallus sorediate, without isidia ...................................................................................................................... + +P. +cf. +negrosorientale + +(lobe margins ciliate, upper surface faintly to clearly white-maculate, soralia generally terminal at the tip of laciniae [ +Fig. 27D +], never laminal, medulla with alectoronic and α-collatolic acids as major substances; uncommon species on +Réunion +) + + + +- Thallus isidiate, with or without soredia ........................................................................................................................................ 15 + + + + + +15. Medulla with norlobaridone .............................................................................................................................................. + +P. mezierii + +(lobe margins ciliate, upper surface ± distinctly punctiform white-maculate, isidia coralloid, often ciliate [ +Fig. 25C & 25D +], medulla with norlobaridone and protolichesterinic acid as major substances; uncommon species on +Réunion +) + + + +- Medulla without norlobaridone ...................................................................................................................................................... 16 + + + + + +16. Apothecia present, usually numerous; thalline exciple with abundant and well-developed isidioid protuberances .......... + +P. mirum + +(morphotype with laminal isidia [ +Fig. 26D +]) + + + +- Apothecia absent ............................................................................................................................................................................ 17 + + + + + +17. Isidia only present, upper cortex not fragile, medulla without α-collatolic acid ........................................................... + +P. crossotum + +(lobe margins conspicuously ciliate, upper surface emaculate or faintly white-maculate, isidia mainly marginal, often ciliate [ +Fig. 17C & 17D +], medulla with alectoronic acid; uncommon species on +Réunion +, in montane rainforests) + + + + +- Isidia and soredia present, upper cortex fragile, medulla with α-collatolic acid .............................................................. + +P. mellissii + +(lobe margins conspicuously ciliate, upper surface emaculate or faintly white-maculate, isidia mainly marginal, often ciliate, soon becoming sorediate [ +Fig. 24D +], medulla with alectoronic and α-collatolic acids; rare species on +Réunion +, in cloud forests) + + + + + +18. Thallus without vegetative propagules ........................................................................................................................................... 19 + + + +- Thallus with vegetative propagules ................................................................................................................................................ 21 + + +19. Medulla K+ yellow then dark red, lower surface often with rhizines to the margins, mean ascospore length <16 µm .................... ........................................................................................................................................................................................... + +P. cetratum + +(lobe margins ciliate, upper surface reticulate white-maculate, apothecial disc perforate, medulla with salazinic and consalazinic acids; very rare species on +Réunion +) + + + + +- Medulla K−, lower surface with a broad erhizinate marginal zone, mean ascospore length> 16 µm .......................................... 20 + + + + +20. Lobes ciliate, medulla UV+ blue-white, KC+ fleeting purple pink, then pink-orange, mean ascospore length> 22 µm .................. .......................................................................................................................................................................................... + +P. nemorum + +(upper surface emaculate, rarely faintly white-maculate, medulla white, sometimes tinged with a reddish purple pigment, apothecial disc imperforate, amphithecium and stipe with ± prominent veins and coarse isidioid protuberances [ +Fig. 28C +], medulla with alectoronic, protocetraric and protolichesterinic acids as major substances; uncommon in secondary lowland rainforests) + + + + +- Lobes eciliate, medulla UV−, KC+ pink, mean ascospore length <20 µm .................................................................. + +P. odontatum + +(upper surface faintly to clearly effigurate white-maculate, medulla white throughout, apothecial disc imperforate, amphithecium smooth [ +Fig. 31D +], medulla with protocetraric acid; uncommon at low elevations) + + + + + +21. Thallus with isidia, without soredia ................................................................................................................................................ 22 + + +- Thallus with soralia, with or without isidia .................................................................................................................................... 29 + + + + +22. Medulla K+ yellow persistent, KC− (with stictic acid) .................................................................................................................. 23 + + +- Other medullary reactions (stictic acid absent) .............................................................................................................................. 25 + + + + + +23. With conspicuous laciniae (up to +10 mm +long), branched and easily shed ............................................................... + +P. nephophilum + +(lobe margins ciliate but cilia sometimes rare, upper surface faintly to clearly white-maculate, marginal and submarginal isidia that mostly develop early into phyllidia and branched laciniae [ +Fig. 29E +]; fairly common species on +Réunion +, in montane and submontane rainforests) + + + + +- Without or with occasional short (up to +1.5 mm +long) laciniae ..................................................................................................... 24 + + + + + + +24. Average thickness of the cupular proper exciple <50 µm ( +Fig. 30C +) ............................................................................. + +P. crinitum + +(lobe margins ciliate, upper surface faintly to clearly white-maculate, isidia marginal and laminal, granular to coralloid, often ciliate [ +Fig. 14E +]; common species on +Réunion +, from submontane to subalpine belts) + + + + +- Average thickness of the cupular proper exciple> 55 µm .............................................................................................. + +P. occultum + +(phenotypically similar to + +P. crinitum + +, but differs by the greater thickness of the cupular proper exciple [ +Fig. 30C +] and the ITS sequence; rare species on +Réunion +, in cloud forests) + + + + + + +25. Medulla K+ yellow then red (with salazinic acid) .................................................................................................... + +P. subisidiosum + +(lobe margins ciliate but cilia sometimes rare, upper surface conspicuously reticulate white-maculate [ +Fig. 40D +], isidia mainly marginal and submarginal, coralloid; uncommon species on +Réunion +, in submontane and montane rainforests) + + + +- Other medullary reactions (salazinic acid absent) .......................................................................................................................... 26 + + + + + +26. Medulla UV+ blue-white, KC+ fleeting purple pink, then pink-orange (with alectoronic acid) .................................... + +P. nemorum + +(morphotype with some laminal or submarginal isidia [ +Fig. 28D +]) + + + +- Medulla UV–, KC– or KC+ pinkish (alectoronic acid absent) ...................................................................................................... 27 + + + + + +27. Medulla K−, KC+ pinkish (with protocetraric acid) ............................................................................................... + +P. subcorallinum + +(lobe margins ciliate, upper surface emaculate or faintly white-maculate, isidia mainly marginal and submarginal, coralloid or arbuscular, very often ciliate [ +Fig. 38D +], medulla with protocetraric and protolichesterinic acids; uncommon in the windward part of +Réunion +, in the submontane belt) + + + +- Medulla K+ slowly orange brown, KC− (with succinprotocetraric acid) ...................................................................................... 28 + + + + + +28. Thallus moderately adnate, lobes +2–13 mm +wide ................................................................................................... + +P. mascarenense + +(lobe margins eciliate or irregularly ciliate, upper surface effigurate white-maculate, isidia marginal to laminal, simple to coralloid, occasionally ciliate [ +Fig. 22C +], medulla with succinprotocetraric and fumarprotocetraric acids; fairly common on +Réunion +) + + + + +- Thallus adnate to tightly adnate, lobes +1–4 mm +wide ....................................................................................................... + +P. orarium + +(looks more like a + +Canoparmelia + +s. lat. +than a + +Parmotrema + +[ +Fig. 32D +], lobe margins eciliate to weakly ciliate, upper surface effigurate white-maculate, isidia marginal to laminal, simple or ± branched, rarely ciliate, usually quickly sorediate [ +Fig. 32E +], medulla with succinprotocetraric and fumarprotocetraric acids; in the southeastern part of +Réunion +, near the coast) + + + + + + +29. Medulla K+ yellow persistent, KC− (with stictic acid) ............................................................................................. + +P. nephophilum + +(sorediate morphotype, +Fig. 29F +) + + + +- Other medullary reactions (stictic acid absent) .............................................................................................................................. 30 + + + + +30. Medulla K+ yellow then red (with salazinic acid) ......................................................................................................................... 31 + + + +- Other medullary reactions (salazinic acid absent) .......................................................................................................................... 33 + + +31. Upper surface emaculate, rarely faintly punctiform maculate; lower surface with a broad erhizinate marginal zone ....................... ....................................................................................................................................................................................... + +P. cristiferum + +(lobe margins eciliate to clearly ciliate, soralia mainly marginal, linear to labriform [ +Fig. 16D +]; uncommon in the windward part of +Réunion +, at low elevation) + + + + +- Upper surface reticulate maculate; lower surface often with rhizines and papillae to the margins ............................................... 32 + + + + +32. Marginal zone of the lower surface of sorediate lobes dark brown or black ....................................................... + +P. reticulatum + +aggr. (lobe margins ciliate, soralia mainly capitate at the tips of laciniae or submarginal ± linear at the apex of revolute lobes [ +Fig. 35F +]; common and widespread on +Réunion +) + + + + +- Marginal zone of the lower surface of sorediate lobes often white or white mottled .......................................... + +P. +cf. +clavuliferum + +(lobe margins ciliate, soralia mainly capitate at the tips of laciniae [ +Fig. 12D +]; uncommon species on +Réunion +) + + + + + +33. Medulla K+ slowly orange brown, KC− (with succinprotocetraric acid) ...................................................................................... 34 + + +- Medulla K− or K± yellowish, KC+ pinkish (with protocetraric acid) ........................................................................................... 35 + + + + + +34. Thallus adnate to tightly adnate, lobes +1–4 mm +wide, isidia present (at least in the early stages of development) ........ + +P +. +orarium + +(looks more like a + +Canoparmelia + +s. lat. +than a + +Parmotrema + +[ +Fig. 32D +], lobe margins eciliate to weakly ciliate, upper surface effigurate white-maculate, isidia marginal to laminal, soralia marginal to laminal [ +Fig. 32F +], often originating from rapid decay of young isidia, more rarely from pustules, occasionally orbicular or subcapitate, medulla with succinprotocetraric and fumarprotocetraric acids; in the southeastern part of +Réunion +, near the coast) + + + + +- Thallus moderately adnate, lobes +3–8 mm +wide, isidia totally absent ............................................................. + +P. paramascarenense + +(lobe margins eciliate to irregularly ciliate, upper surface effigurate white-maculate, soralia terminal at the apex of tiny laciniae when young, then labriform or subcapitate, finally spreading submarginally on revolute lobes [ +Fig. 33D +], medulla with succinprotocetraric and fumarprotocetraric acids; rare species on +Réunion +) + + + + + + +35. Medulla with echinocarpic acid ...................................................................................................................................... + +P. dilatatum + +(lobe margins eciliate or very sparsely ciliate, upper surface emaculate or faintly punctiform white-maculate, soralia marginal, linear to labriform when young, then subcapitate and ± coalescing on arbuscular rising structures [ +Fig. 19D +], medulla with protocetraric and echinocarpic acids as major substances; very rare species on +Réunion +) + + + +- Medulla without echinocarpic acid ................................................................................................................................................ 36 + + + + +36. Medulla without protolichesterinic acid ......................................................................................................................................... 37 + + +- Medulla with protolichesterinic acid .............................................................................................................................................. 38 + + + + + +37. Medulla UV+, with alectoronic acid ......................................................................................................................... + +P. +cf. +deflectens + +(lobe margins conspicuously ciliate, upper surface emaculate or faintly punctiform white-maculate, upper cortex fragile, flaking, soralia mainly marginal, linear to labriform [ +Fig. 18C +], medulla with protocetraric and alectoronic acids as major substances; very rare species on +Réunion +) + + + + +- Medulla UV−, alectoronic acid absent ............................................................................................................................ + +P. robustum + +(lobe margins eciliate to ± irregularly ciliate, upper surface emaculate to punctiform white-maculate, soralia marginal at the apex of laciniae when young, then labriform or subcapitate and ± coalescing [ +Fig. 37D +], medulla with protocetraric acid as major substance; common species on +Réunion +, mainly in montane rainforests) + + + + + + +38. Medulla UV+, with alectoronic acid ........................................................................................................................ + +P. subdeflectens + +(lobe margins conspicuously ciliate, upper surface emaculate or faintly punctiform white-maculate, soralia either terminal labriform or subcapitate on very short laciniae [ +Fig. 39C +], or marginal and ± labriform [ +Fig. 39D +], medulla with protocetraric, alectoronic and protolichesterinic acids as major substances; rare species on +Réunion +, in leeward submontane forests) + + + +- Medulla UV−, without alectoronic acid ......................................................................................................................................... 39 + + + + + +39. Soralia submarginal, often pustulate ( +Fig. 42C +), never marginal linear; upper cortex fragile, here and there flaking ( +Fig. 42D +); soredia granulose (mean diameter> 50 µm) ............................................................................................................... + +P. udisilvestre + +(species of the + +P. subarnoldii + +group, lobe margins conspicuously ciliate, upper surface emaculate or faintly punctiform white-maculate, medulla with protocetraric and protolichesterinic acids as major substances; uncommon in the windward part of +Réunion +, in the submontane belt) + + + + +- Soralia marginal, linear discontinuous, then ± labriform ( +Fig. 9D +& +20D +), or subcapitate at the tip of very short laciniae ( +Fig. 20C +), never pustulate; upper cortex not fragile; soredia subgranulose (mean diameter <45 µm) .......................................................... 40 + + + + + + +40. Marginal cilia short (mean length < +3.5 mm +) .................................................................................................... + +P. brachyblepharum + + + + + +- Marginal cilia long (mean length> +3.5 mm +) ............................................................................................................... + +P. eleonomum + +(two species of the + +P. subarnoldii + +group, lobe margins conspicuously ciliate, upper surface emaculate or faintly punctiform white-maculate, medulla with protocetraric and protolichesterinic acids as major substances; rare species on +Réunion +) + + + + + + + \ No newline at end of file diff --git a/data/1A/29/50/1A295062FFA1FFA8F9C3F4C0FCBA6E3E.xml b/data/1A/29/50/1A295062FFA1FFA8F9C3F4C0FCBA6E3E.xml new file mode 100644 index 00000000000..54577038581 --- /dev/null +++ b/data/1A/29/50/1A295062FFA1FFA8F9C3F4C0FCBA6E3E.xml @@ -0,0 +1,125 @@ + + + +Cryptoxyleborus brevicauda, a new species of xyleborine ambrosia beetle from Thailand (Coleoptera: Curculionidae: Scolytinae: Xyleborini) + + + +Author + +Sittichaya, Wisut +Agricultural Innovation and Management Division, Faculty of Natural Resources, Prince of Songkla University, Songkhla, 90110, Thailand. + + + +Author + +Beaver, Roger A. +161 / 2 Mu 5, Soi Wat Pranon, T. Donkaew, A. Maerim, Chiangmai 50180, Thailand. + +text + + +Zootaxa + + +2024 + +2024-09-09 + + +5506 + + +3 + + +396 +401 + + + + +http://dx.doi.org/10.11646/zootaxa.5506.3.5 + +journal article +10.11646/zootaxa.5506.3.5 +1175-5326 +13747205 +7A5924B2-6F4D-4EEE-9493-40E2A9F92B96 + + + + + + + +Cryptoxyleborus turbineus +( +Sampson, 1923 +) + + + + + + + + + + +Xyleborus turbineus +Sampson, 1923: 288 + + +. + + + + + +Cryptoxyleborus turbineus +(Sampson) + +: + +Schedl, 1937: 551 + +. + + + +Thai distribution: N +: +Chiang Mai +( +Beaver & Browne 1975 +), +Phetchabun +; +N-E +: +Loei +( + +Beaver +et al. +2014 + +). + +Habitat +types +: + +mixed deciduous forest ( + +Beaver +et al. +2014 + +). + + + + \ No newline at end of file diff --git a/data/1A/29/50/1A295062FFA1FFA8F9C3F4C0FA4B6CE9.xml b/data/1A/29/50/1A295062FFA1FFA8F9C3F586FA4B6CE9.xml similarity index 50% rename from data/1A/29/50/1A295062FFA1FFA8F9C3F4C0FA4B6CE9.xml rename to data/1A/29/50/1A295062FFA1FFA8F9C3F586FA4B6CE9.xml index e47a7cc1652..e2e82a78d70 100644 --- a/data/1A/29/50/1A295062FFA1FFA8F9C3F4C0FA4B6CE9.xml +++ b/data/1A/29/50/1A295062FFA1FFA8F9C3F586FA4B6CE9.xml @@ -1,126 +1,55 @@ - - - -Cryptoxyleborus brevicauda, a new species of xyleborine ambrosia beetle from Thailand (Coleoptera: Curculionidae: Scolytinae: Xyleborini) + + + +Cryptoxyleborus brevicauda, a new species of xyleborine ambrosia beetle from Thailand (Coleoptera: Curculionidae: Scolytinae: Xyleborini) - - -Author + + +Author -Sittichaya, Wisut -Agricultural Innovation and Management Division, Faculty of Natural Resources, Prince of Songkla University, Songkhla, 90110, Thailand. +Sittichaya, Wisut +Agricultural Innovation and Management Division, Faculty of Natural Resources, Prince of Songkla University, Songkhla, 90110, Thailand. - - -Author + + +Author -Beaver, Roger A. -161 / 2 Mu 5, Soi Wat Pranon, T. Donkaew, A. Maerim, Chiangmai 50180, Thailand. +Beaver, Roger A. +161 / 2 Mu 5, Soi Wat Pranon, T. Donkaew, A. Maerim, Chiangmai 50180, Thailand. -text - - -Zootaxa +text + + +Zootaxa - -2024 - -2024-09-09 + +2024 + +2024-09-09 - -5506 + +5506 - -3 + +3 - -396 -401 + +396 +401 - -http://dx.doi.org/10.11646/zootaxa.5506.3.5 + +http://dx.doi.org/10.11646/zootaxa.5506.3.5 -journal article -10.11646/zootaxa.5506.3.5 -1175-5326 -7A5924B2-6F4D-4EEE-9493-40E2A9F92B96 +journal article +10.11646/zootaxa.5506.3.5 +1175-5326 +13747205 +7A5924B2-6F4D-4EEE-9493-40E2A9F92B96 - - - - - - -Cryptoxyleborus turbineus -( -Sampson, 1923 -) - - - - - - - - - - -Xyleborus turbineus -Sampson, 1923: 288 - - -. - - - - - -Cryptoxyleborus turbineus -(Sampson) - -: - -Schedl, 1937: 551 - -. - - - -Thai distribution: N -: -Chiang Mai -( -Beaver & Browne 1975 -), -Phetchabun -; -N-E -: -Loei -( - -Beaver -et al. -2014 - -). - -Habitat -types -: - -mixed deciduous forest ( - -Beaver -et al. -2014 - -). - - - + + Key to the species of @@ -135,6 +64,8 @@ of et al. 2020] + + diff --git a/data/7A/6D/87/7A6D87C5FFC01E0879C64CA6FEEFFB02.xml b/data/7A/6D/87/7A6D87C5FFC01E0879C64CA6FEEFFB02.xml index 1a95a53d3db..c0104605312 100644 --- a/data/7A/6D/87/7A6D87C5FFC01E0879C64CA6FEEFFB02.xml +++ b/data/7A/6D/87/7A6D87C5FFC01E0879C64CA6FEEFFB02.xml @@ -1,46 +1,47 @@ - - - -Miocene marine macropaleontology of the fourth bore Caldecott Tunnel excavation, Berkeley Hills, Oakland, California, USA + + + +Miocene marine macropaleontology of the fourth bore Caldecott Tunnel excavation, Berkeley Hills, Oakland, California, USA - - -Author + + +Author -Charles L. Powell, Ii +Charles L. Powell, Ii - - -Author + + +Author -Clites, Erica C. +Clites, Erica C. - - -Author + + +Author -Poust, Ashley W. +Poust, Ashley W. -text - - -PaleoBios +text + + +PaleoBios - -2022 - -36 + +2022 + +36 - -1 -34 + +1 +34 -journal article -10.5070/P9361044567 -0031-0298 -EFED8DE6-E976-43A5-BD7B-F478EF0B6FF9 +journal article +10.5070/P9361044567 +0031-0298 +13750345 +EFED8DE6-E976-43A5-BD7B-F478EF0B6FF9 @@ -55,9 +56,9 @@ LESUEUR, 1818 -FIG. 41 +FIG. 41 - + Figure 41. diff --git a/data/7A/6D/87/7A6D87C5FFC01E097AA24BDAFE96FB02.xml b/data/7A/6D/87/7A6D87C5FFC01E097AA24BDAFE96FB02.xml index 8a502175e11..6d661c72ca0 100644 --- a/data/7A/6D/87/7A6D87C5FFC01E097AA24BDAFE96FB02.xml +++ b/data/7A/6D/87/7A6D87C5FFC01E097AA24BDAFE96FB02.xml @@ -1,46 +1,47 @@ - - - -Miocene marine macropaleontology of the fourth bore Caldecott Tunnel excavation, Berkeley Hills, Oakland, California, USA + + + +Miocene marine macropaleontology of the fourth bore Caldecott Tunnel excavation, Berkeley Hills, Oakland, California, USA - - -Author + + +Author -Charles L. Powell, Ii +Charles L. Powell, Ii - - -Author + + +Author -Clites, Erica C. +Clites, Erica C. - - -Author + + +Author -Poust, Ashley W. +Poust, Ashley W. -text - - -PaleoBios +text + + +PaleoBios - -2022 - -36 + +2022 + +36 - -1 -34 + +1 +34 -journal article -10.5070/P9361044567 -0031-0298 -EFED8DE6-E976-43A5-BD7B-F478EF0B6FF9 +journal article +10.5070/P9361044567 +0031-0298 +13750345 +EFED8DE6-E976-43A5-BD7B-F478EF0B6FF9 @@ -56,7 +57,7 @@ BALANIDAE -FIG. 40 +FIG. 40 A very small mold and cast appear to represent a small, short, possibly smooth-sided barnacle. It is not well enough preserved to identify beyond family and that is questionable. The family goes back to the Cambrian UCMP 218505 is a shark tooth exposed in lingual view and, being mesio-distally wide and concave right in this view, represents an upper tooth from the middle to rear of the tooth row. It is a small, asymmetrical tooth measuring 7.6 mm in crown height, 4.2 mm in crown width and 11.6 mm wide at the root. @@ -97,7 +98,7 @@ which typically has fine serrations along the entire edge but still resembles th , the bull shark. It can be distinguished from this last due to its greater asymmetry. - + Figure 42. @@ -106,7 +107,7 @@ which typically has fine serrations along the entire edge but still resembles th vertebra, hypotype, UCMP 218506. - + Figure 43. Cycloid teleost scale, hypotype UCMP 270032. diff --git a/data/7A/6D/87/7A6D87C5FFCB1E037B5A4FE9FE3DFC28.xml b/data/7A/6D/87/7A6D87C5FFCB1E037B5A4FE9FE3DFC28.xml index edd738f35ba..5a37cba23d5 100644 --- a/data/7A/6D/87/7A6D87C5FFCB1E037B5A4FE9FE3DFC28.xml +++ b/data/7A/6D/87/7A6D87C5FFCB1E037B5A4FE9FE3DFC28.xml @@ -1,48 +1,49 @@ - - - -Miocene marine macropaleontology of the fourth bore Caldecott Tunnel excavation, Berkeley Hills, Oakland, California, USA + + + +Miocene marine macropaleontology of the fourth bore Caldecott Tunnel excavation, Berkeley Hills, Oakland, California, USA - - -Author + + +Author -Charles L. Powell, Ii +Charles L. Powell, Ii - - -Author + + +Author -Clites, Erica C. +Clites, Erica C. - - -Author + + +Author -Poust, Ashley W. +Poust, Ashley W. -text - - -PaleoBios +text + + +PaleoBios - -2022 - -36 + +2022 + +36 - -1 -34 + +1 +34 -journal article -10.5070/P9361044567 -0031-0298 -EFED8DE6-E976-43A5-BD7B-F478EF0B6FF9 +journal article +10.5070/P9361044567 +0031-0298 +13750345 +EFED8DE6-E976-43A5-BD7B-F478EF0B6FF9 - + @@ -52,7 +53,7 @@ -FIG. 32 +FIG. 32 A very small mold and cast appear to represent a small, short, possibly smooth-sided barnacle. It is not well enough preserved to identify beyond family level. The family goes back to the Cambrian ( diff --git a/data/7A/6D/87/7A6D87C5FFCC1E047B3A4FE8FE60FB31.xml b/data/7A/6D/87/7A6D87C5FFCC1E047B3A4FE8FE60FB31.xml index ca0a9876692..d77d93951f1 100644 --- a/data/7A/6D/87/7A6D87C5FFCC1E047B3A4FE8FE60FB31.xml +++ b/data/7A/6D/87/7A6D87C5FFCC1E047B3A4FE8FE60FB31.xml @@ -1,48 +1,49 @@ - - - -Miocene marine macropaleontology of the fourth bore Caldecott Tunnel excavation, Berkeley Hills, Oakland, California, USA + + + +Miocene marine macropaleontology of the fourth bore Caldecott Tunnel excavation, Berkeley Hills, Oakland, California, USA - - -Author + + +Author -Charles L. Powell, Ii +Charles L. Powell, Ii - - -Author + + +Author -Clites, Erica C. +Clites, Erica C. - - -Author + + +Author -Poust, Ashley W. +Poust, Ashley W. -text - - -PaleoBios +text + + +PaleoBios - -2022 - -36 + +2022 + +36 - -1 -34 + +1 +34 -journal article -10.5070/P9361044567 -0031-0298 -EFED8DE6-E976-43A5-BD7B-F478EF0B6FF9 +journal article +10.5070/P9361044567 +0031-0298 +13750345 +EFED8DE6-E976-43A5-BD7B-F478EF0B6FF9 - + @@ -52,7 +53,7 @@ -FIG. 34 +FIG. 34 UCMP 270019 and 270092 are partial mid-shaft fragments of what appear to be pinniped ribs. They resemble pinniped ribs in cross-sectional shape and marrow cavity area, but we cannot fully rule out small odontocete cetaceans with ribs of similar size. diff --git a/data/7A/6D/87/7A6D87C5FFCC1E057E6E4ED6FE48FAAA.xml b/data/7A/6D/87/7A6D87C5FFCC1E057E6E4ED6FE48FAAA.xml index 75caaf2c2b8..1d6ed23c8fb 100644 --- a/data/7A/6D/87/7A6D87C5FFCC1E057E6E4ED6FE48FAAA.xml +++ b/data/7A/6D/87/7A6D87C5FFCC1E057E6E4ED6FE48FAAA.xml @@ -1,46 +1,47 @@ - - - -Miocene marine macropaleontology of the fourth bore Caldecott Tunnel excavation, Berkeley Hills, Oakland, California, USA + + + +Miocene marine macropaleontology of the fourth bore Caldecott Tunnel excavation, Berkeley Hills, Oakland, California, USA - - -Author + + +Author -Charles L. Powell, Ii +Charles L. Powell, Ii - - -Author + + +Author -Clites, Erica C. +Clites, Erica C. - - -Author + + +Author -Poust, Ashley W. +Poust, Ashley W. -text - - -PaleoBios +text + + +PaleoBios - -2022 - -36 + +2022 + +36 - -1 -34 + +1 +34 -journal article -10.5070/P9361044567 -0031-0298 -EFED8DE6-E976-43A5-BD7B-F478EF0B6FF9 +journal article +10.5070/P9361044567 +0031-0298 +13750345 +EFED8DE6-E976-43A5-BD7B-F478EF0B6FF9 @@ -63,14 +64,14 @@ ODONTOCETI FIGS. 35 , -36 +36 Cetacean remains recovered from the Caldecott Tunnel Tsm unit include a partial premaxilla (UCMP 269020) among other less identifiable fragments. The descriptive anatomical terminology used here follows Mead and Fordyce (2009). UCMP 269020 is a left mid-premaxilla of a medium-sized odontocete cetacean. T-shaped in cross-section, it has a sharp lateral edge which would have been flush with the maxilla and a more rounded medial border where it would have met the opposing right premaxilla in life. The ventral process is crushed and less distinguishable from the surrounding matrix, but does expand ventrally where the palatine surface would be visible in ventral view. The porcelanous part is gently convex. The labial surface, anterolateral sulcus, and any branches of the infraorbital canal are not visible, suggesting that this fragment is from the anterior half of the rostral portion. The convex rostral surface is 32.3 mm wide and the height from the palatine surface of the premaxilla is 32.5 mm. The entire fragment is 80 mm long. - + Figure 34. Mammalian rib fragment, hypotype, UCMP 270043. diff --git a/data/7A/6D/87/7A6D87C5FFCE1E06799C4E68FAFFFBDE.xml b/data/7A/6D/87/7A6D87C5FFCE1E06799C4E68FAFFFBDE.xml index fed0af17dce..a762542720a 100644 --- a/data/7A/6D/87/7A6D87C5FFCE1E06799C4E68FAFFFBDE.xml +++ b/data/7A/6D/87/7A6D87C5FFCE1E06799C4E68FAFFFBDE.xml @@ -1,48 +1,49 @@ - - - -Miocene marine macropaleontology of the fourth bore Caldecott Tunnel excavation, Berkeley Hills, Oakland, California, USA + + + +Miocene marine macropaleontology of the fourth bore Caldecott Tunnel excavation, Berkeley Hills, Oakland, California, USA - - -Author + + +Author -Charles L. Powell, Ii +Charles L. Powell, Ii - - -Author + + +Author -Clites, Erica C. +Clites, Erica C. - - -Author + + +Author -Poust, Ashley W. +Poust, Ashley W. -text - - -PaleoBios +text + + +PaleoBios - -2022 - -36 + +2022 + +36 - -1 -34 + +1 +34 -journal article -10.5070/P9361044567 -0031-0298 -EFED8DE6-E976-43A5-BD7B-F478EF0B6FF9 +journal article +10.5070/P9361044567 +0031-0298 +13750345 +EFED8DE6-E976-43A5-BD7B-F478EF0B6FF9 - + @@ -52,7 +53,7 @@ -FIG. 37 +FIG. 37 UCMP 412480 is a mold of a small indeterminate diff --git a/data/7A/6D/87/7A6D87C5FFCF1E087B754975FAD9FE8A.xml b/data/7A/6D/87/7A6D87C5FFCF1E087B754975FAD9FE8A.xml index 384fc3f2c63..dc0a0ecc3b8 100644 --- a/data/7A/6D/87/7A6D87C5FFCF1E087B754975FAD9FE8A.xml +++ b/data/7A/6D/87/7A6D87C5FFCF1E087B754975FAD9FE8A.xml @@ -1,48 +1,49 @@ - - - -Miocene marine macropaleontology of the fourth bore Caldecott Tunnel excavation, Berkeley Hills, Oakland, California, USA + + + +Miocene marine macropaleontology of the fourth bore Caldecott Tunnel excavation, Berkeley Hills, Oakland, California, USA - - -Author + + +Author -Charles L. Powell, Ii +Charles L. Powell, Ii - - -Author + + +Author -Clites, Erica C. +Clites, Erica C. - - -Author + + +Author -Poust, Ashley W. +Poust, Ashley W. -text - - -PaleoBios +text + + +PaleoBios - -2022 - -36 + +2022 + +36 - -1 -34 + +1 +34 -journal article -10.5070/P9361044567 -0031-0298 -EFED8DE6-E976-43A5-BD7B-F478EF0B6FF9 +journal article +10.5070/P9361044567 +0031-0298 +13750345 +EFED8DE6-E976-43A5-BD7B-F478EF0B6FF9 - + @@ -52,7 +53,7 @@ -FIG. 38 +FIG. 38 UCMP 218710, a single right valve in sandstone, is provisionally identified as diff --git a/data/7A/6D/87/7A6D87C5FFD01E187B2949FCFA53FCF0.xml b/data/7A/6D/87/7A6D87C5FFD01E187B2949FCFA53FCF0.xml index 7cbb00c22ed..0b5a116b694 100644 --- a/data/7A/6D/87/7A6D87C5FFD01E187B2949FCFA53FCF0.xml +++ b/data/7A/6D/87/7A6D87C5FFD01E187B2949FCFA53FCF0.xml @@ -1,46 +1,47 @@ - - - -Miocene marine macropaleontology of the fourth bore Caldecott Tunnel excavation, Berkeley Hills, Oakland, California, USA + + + +Miocene marine macropaleontology of the fourth bore Caldecott Tunnel excavation, Berkeley Hills, Oakland, California, USA - - -Author + + +Author -Charles L. Powell, Ii +Charles L. Powell, Ii - - -Author + + +Author -Clites, Erica C. +Clites, Erica C. - - -Author + + +Author -Poust, Ashley W. +Poust, Ashley W. -text - - -PaleoBios +text + + +PaleoBios - -2022 - -36 + +2022 + +36 - -1 -34 + +1 +34 -journal article -10.5070/P9361044567 -0031-0298 -EFED8DE6-E976-43A5-BD7B-F478EF0B6FF9 +journal article +10.5070/P9361044567 +0031-0298 +13750345 +EFED8DE6-E976-43A5-BD7B-F478EF0B6FF9 @@ -55,7 +56,7 @@ MÖLLER, 1842 -FIGS. 6 +FIGS. 6 , 7 @@ -72,7 +73,7 @@ cf. Arnold, 1908 ( -Figs. 6 +Figs. 6 , 7 ). @@ -91,7 +92,7 @@ cf. Arnold, 1908 ( -Fig. 8 +Fig. 8 ). This species occurs in California from the Hambre Sandstone ( diff --git a/data/7A/6D/87/7A6D87C5FFD21E1A7B584CE6FDE5FD6C.xml b/data/7A/6D/87/7A6D87C5FFD21E1A7B584CE6FDE5FD6C.xml index efe3c26f7d6..276f12ddd68 100644 --- a/data/7A/6D/87/7A6D87C5FFD21E1A7B584CE6FDE5FD6C.xml +++ b/data/7A/6D/87/7A6D87C5FFD21E1A7B584CE6FDE5FD6C.xml @@ -1,48 +1,49 @@ - - - -Miocene marine macropaleontology of the fourth bore Caldecott Tunnel excavation, Berkeley Hills, Oakland, California, USA + + + +Miocene marine macropaleontology of the fourth bore Caldecott Tunnel excavation, Berkeley Hills, Oakland, California, USA - - -Author + + +Author -Charles L. Powell, Ii +Charles L. Powell, Ii - - -Author + + +Author -Clites, Erica C. +Clites, Erica C. - - -Author + + +Author -Poust, Ashley W. +Poust, Ashley W. -text - - -PaleoBios +text + + +PaleoBios - -2022 - -36 + +2022 + +36 - -1 -34 + +1 +34 -journal article -10.5070/P9361044567 -0031-0298 -EFED8DE6-E976-43A5-BD7B-F478EF0B6FF9 +journal article +10.5070/P9361044567 +0031-0298 +13750345 +EFED8DE6-E976-43A5-BD7B-F478EF0B6FF9 - + @@ -55,7 +56,7 @@ -FIG. 12 +FIG. 12 A single small cast is questionably identified as the genus diff --git a/data/7A/6D/87/7A6D87C5FFD21E1A7B664E65FA9FFEA9.xml b/data/7A/6D/87/7A6D87C5FFD21E1A7B664E65FA9FFEA9.xml index 46e0816634b..71c8964c27c 100644 --- a/data/7A/6D/87/7A6D87C5FFD21E1A7B664E65FA9FFEA9.xml +++ b/data/7A/6D/87/7A6D87C5FFD21E1A7B664E65FA9FFEA9.xml @@ -1,48 +1,49 @@ - - - -Miocene marine macropaleontology of the fourth bore Caldecott Tunnel excavation, Berkeley Hills, Oakland, California, USA + + + +Miocene marine macropaleontology of the fourth bore Caldecott Tunnel excavation, Berkeley Hills, Oakland, California, USA - - -Author + + +Author -Charles L. Powell, Ii +Charles L. Powell, Ii - - -Author + + +Author -Clites, Erica C. +Clites, Erica C. - - -Author + + +Author -Poust, Ashley W. +Poust, Ashley W. -text - - -PaleoBios +text + + +PaleoBios - -2022 - -36 + +2022 + +36 - -1 -34 + +1 +34 -journal article -10.5070/P9361044567 -0031-0298 -EFED8DE6-E976-43A5-BD7B-F478EF0B6FF9 +journal article +10.5070/P9361044567 +0031-0298 +13750345 +EFED8DE6-E976-43A5-BD7B-F478EF0B6FF9 - + @@ -55,7 +56,7 @@ PROPEAMUSSIIDAE -FIG. 13 +FIG. 13 Two partial, mostly decorticated, possibly right, valves of an indeterminate diff --git a/data/7A/6D/87/7A6D87C5FFD21E1B79854E30FDBFFA16.xml b/data/7A/6D/87/7A6D87C5FFD21E1B79854E30FDBFFA16.xml index 46b424bab79..8c190ec8b49 100644 --- a/data/7A/6D/87/7A6D87C5FFD21E1B79854E30FDBFFA16.xml +++ b/data/7A/6D/87/7A6D87C5FFD21E1B79854E30FDBFFA16.xml @@ -1,46 +1,47 @@ - - - -Miocene marine macropaleontology of the fourth bore Caldecott Tunnel excavation, Berkeley Hills, Oakland, California, USA + + + +Miocene marine macropaleontology of the fourth bore Caldecott Tunnel excavation, Berkeley Hills, Oakland, California, USA - - -Author + + +Author -Charles L. Powell, Ii +Charles L. Powell, Ii - - -Author + + +Author -Clites, Erica C. +Clites, Erica C. - - -Author + + +Author -Poust, Ashley W. +Poust, Ashley W. -text - - -PaleoBios +text + + +PaleoBios - -2022 - -36 + +2022 + +36 - -1 -34 + +1 +34 -journal article -10.5070/P9361044567 -0031-0298 -EFED8DE6-E976-43A5-BD7B-F478EF0B6FF9 +journal article +10.5070/P9361044567 +0031-0298 +13750345 +EFED8DE6-E976-43A5-BD7B-F478EF0B6FF9 @@ -52,7 +53,7 @@ -FIG. 14 +FIG. 14 UCMP 218741 is a single specimen that may represent a new genus and species within the subfamily diff --git a/data/7A/6D/87/7A6D87C5FFD31E1B7B7C48AAFB04FC23.xml b/data/7A/6D/87/7A6D87C5FFD31E1B7B7C48AAFB04FC23.xml index 1a2c874cf13..e78147bbbb8 100644 --- a/data/7A/6D/87/7A6D87C5FFD31E1B7B7C48AAFB04FC23.xml +++ b/data/7A/6D/87/7A6D87C5FFD31E1B7B7C48AAFB04FC23.xml @@ -1,48 +1,49 @@ - - - -Miocene marine macropaleontology of the fourth bore Caldecott Tunnel excavation, Berkeley Hills, Oakland, California, USA + + + +Miocene marine macropaleontology of the fourth bore Caldecott Tunnel excavation, Berkeley Hills, Oakland, California, USA - - -Author + + +Author -Charles L. Powell, Ii +Charles L. Powell, Ii - - -Author + + +Author -Clites, Erica C. +Clites, Erica C. - - -Author + + +Author -Poust, Ashley W. +Poust, Ashley W. -text - - -PaleoBios +text + + +PaleoBios - -2022 - -36 + +2022 + +36 - -1 -34 + +1 +34 -journal article -10.5070/P9361044567 -0031-0298 -EFED8DE6-E976-43A5-BD7B-F478EF0B6FF9 +journal article +10.5070/P9361044567 +0031-0298 +13750345 +EFED8DE6-E976-43A5-BD7B-F478EF0B6FF9 - + @@ -56,7 +57,7 @@ MYRTEINAE -FIG. 15 +FIG. 15 The second lucinid in the Tsm Caldecott Tunnel fauna is similar to the previous one in having widely-spaced co-marginal lamellae, but differs in its low, broad umbo, wide, oval shape, and weak anterior dorsal sulcus. This lucinid is very similar in shape to genus diff --git a/data/7A/6D/87/7A6D87C5FFD31E1C799B4E80FA67FF57.xml b/data/7A/6D/87/7A6D87C5FFD31E1C799B4E80FA67FF57.xml index 0d887ea274a..3eef165e2d6 100644 --- a/data/7A/6D/87/7A6D87C5FFD31E1C799B4E80FA67FF57.xml +++ b/data/7A/6D/87/7A6D87C5FFD31E1C799B4E80FA67FF57.xml @@ -1,48 +1,49 @@ - - - -Miocene marine macropaleontology of the fourth bore Caldecott Tunnel excavation, Berkeley Hills, Oakland, California, USA + + + +Miocene marine macropaleontology of the fourth bore Caldecott Tunnel excavation, Berkeley Hills, Oakland, California, USA - - -Author + + +Author -Charles L. Powell, Ii +Charles L. Powell, Ii - - -Author + + +Author -Clites, Erica C. +Clites, Erica C. - - -Author + + +Author -Poust, Ashley W. +Poust, Ashley W. -text - - -PaleoBios +text + + +PaleoBios - -2022 - -36 + +2022 + +36 - -1 -34 + +1 +34 -journal article -10.5070/P9361044567 -0031-0298 -EFED8DE6-E976-43A5-BD7B-F478EF0B6FF9 +journal article +10.5070/P9361044567 +0031-0298 +13750345 +EFED8DE6-E976-43A5-BD7B-F478EF0B6FF9 - + @@ -55,7 +56,7 @@ CARDITIDAE -FIG. 16 +FIG. 16 One indeterminate diff --git a/data/7A/6D/87/7A6D87C5FFD51E1D798B4E82FB51F900.xml b/data/7A/6D/87/7A6D87C5FFD51E1D798B4E82FB51F900.xml index 0eac0ad8456..b410cd3ca1e 100644 --- a/data/7A/6D/87/7A6D87C5FFD51E1D798B4E82FB51F900.xml +++ b/data/7A/6D/87/7A6D87C5FFD51E1D798B4E82FB51F900.xml @@ -1,48 +1,49 @@ - - - -Miocene marine macropaleontology of the fourth bore Caldecott Tunnel excavation, Berkeley Hills, Oakland, California, USA + + + +Miocene marine macropaleontology of the fourth bore Caldecott Tunnel excavation, Berkeley Hills, Oakland, California, USA - - -Author + + +Author -Charles L. Powell, Ii +Charles L. Powell, Ii - - -Author + + +Author -Clites, Erica C. +Clites, Erica C. - - -Author + + +Author -Poust, Ashley W. +Poust, Ashley W. -text - - -PaleoBios +text + + +PaleoBios - -2022 - -36 + +2022 + +36 - -1 -34 + +1 +34 -journal article -10.5070/P9361044567 -0031-0298 -EFED8DE6-E976-43A5-BD7B-F478EF0B6FF9 +journal article +10.5070/P9361044567 +0031-0298 +13750345 +EFED8DE6-E976-43A5-BD7B-F478EF0B6FF9 - + @@ -52,7 +53,7 @@ -FIG. 21 +FIG. 21 UCMP 410418 is a single small specimen that shows an overall oval shell outline with the umbo positioned at about a third of the shell’s length. The umbo overhangs the dorso-anterior margin which is short and steeply inclined. The dorso-posterior margin broadly arches away from the umbo and is partially hidden. The ventral margin is broadly rounded from the anterior to the posterior. A fragment of the shell is present posterior of the umbo and appears moderately thick with strong concentric ribs. The cast shows that these ribs were co-marginal and moderately evenly spaced. These features and the shell outline matches well with some members of the family diff --git a/data/7A/6D/87/7A6D87C5FFD51E1D7B344897FA8AFC4E.xml b/data/7A/6D/87/7A6D87C5FFD51E1D7B344897FA8AFC4E.xml index e725a6a56e6..4b52e54f47f 100644 --- a/data/7A/6D/87/7A6D87C5FFD51E1D7B344897FA8AFC4E.xml +++ b/data/7A/6D/87/7A6D87C5FFD51E1D7B344897FA8AFC4E.xml @@ -1,48 +1,49 @@ - - - -Miocene marine macropaleontology of the fourth bore Caldecott Tunnel excavation, Berkeley Hills, Oakland, California, USA + + + +Miocene marine macropaleontology of the fourth bore Caldecott Tunnel excavation, Berkeley Hills, Oakland, California, USA - - -Author + + +Author -Charles L. Powell, Ii +Charles L. Powell, Ii - - -Author + + +Author -Clites, Erica C. +Clites, Erica C. - - -Author + + +Author -Poust, Ashley W. +Poust, Ashley W. -text - - -PaleoBios +text + + +PaleoBios - -2022 - -36 + +2022 + +36 - -1 -34 + +1 +34 -journal article -10.5070/P9361044567 -0031-0298 -EFED8DE6-E976-43A5-BD7B-F478EF0B6FF9 +journal article +10.5070/P9361044567 +0031-0298 +13750345 +EFED8DE6-E976-43A5-BD7B-F478EF0B6FF9 - + @@ -55,7 +56,7 @@ -FIG. 20 +FIG. 20 UCMP 410439 is provisionally referred to diff --git a/data/7A/6D/87/7A6D87C5FFD51E1E79F94A78FACAFF57.xml b/data/7A/6D/87/7A6D87C5FFD51E1E79F94A78FACAFF57.xml index 774f839eaa8..65d179fc079 100644 --- a/data/7A/6D/87/7A6D87C5FFD51E1E79F94A78FACAFF57.xml +++ b/data/7A/6D/87/7A6D87C5FFD51E1E79F94A78FACAFF57.xml @@ -1,48 +1,49 @@ - - - -Miocene marine macropaleontology of the fourth bore Caldecott Tunnel excavation, Berkeley Hills, Oakland, California, USA + + + +Miocene marine macropaleontology of the fourth bore Caldecott Tunnel excavation, Berkeley Hills, Oakland, California, USA - - -Author + + +Author -Charles L. Powell, Ii +Charles L. Powell, Ii - - -Author + + +Author -Clites, Erica C. +Clites, Erica C. - - -Author + + +Author -Poust, Ashley W. +Poust, Ashley W. -text - - -PaleoBios +text + + +PaleoBios - -2022 - -36 + +2022 + +36 - -1 -34 + +1 +34 -journal article -10.5070/P9361044567 -0031-0298 -EFED8DE6-E976-43A5-BD7B-F478EF0B6FF9 +journal article +10.5070/P9361044567 +0031-0298 +13750345 +EFED8DE6-E976-43A5-BD7B-F478EF0B6FF9 - + @@ -56,7 +57,7 @@ TRASK IN STEWART 1926 -FIG. 22 +FIG. 22 The genus