The Permotriassic branchiosaurid Tungussogyrinus Efremov, 1939 (Temnospondyli, Dissorophoidea) from Siberia restudied [PDF]
Fossil Record, 2009 The enigmatic temnospondyl amphibian Tungussogyrinus bergi Efremov, 1939 shares clear synapomorphies with other branchiosaurids indicated by an anteriorly elongated infratemporal fossa and small branchial denticles.
R. Werneburg
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Climatic drivers of latitudinal variation in Late Triassic tetrapod diversity
Palaeontology, Volume 64, Issue 1, Page 101-117, January 2021., 2021 Abstract The latitudinal biodiversity gradient (LBG), the increase in biodiversity from the poles to the equator, is one of the most widely recognized global macroecological patterns, yet its deep time evolution and drivers remain uncertain. The Late Triassic (237–201 Ma), a critical interval for the early evolution and radiation of modern tetrapod ...
Emma M. Dunne +5 more
wiley +1 more source
Figure 14 in A new Lower Permian trematopid (Temnospondyli: Dissorophoidea) from Richards Spur, Oklahoma [PDF]
, 2011 Figure 14. Acheloma dunni, referred specimen (OMNH 73514). Partial pelvic girdle and hindlimb. Abbreviations: c, centrale; fe, femur; fi, fibula; i, intermedium; il, ilium; is, ischium; obt, obturator foramen; pu, pubis; ti, tibia; tib, tibiale.
Reisz, Robert R., Polley, Brendan P.
core +3 more sources
The Permotriassic branchiosaurid Tungussogyrinus Efremov, 1939 (Temnospondyli, Dissorophoidea) from Siberia restudied [PDF]
Fossil Record, 2009 The enigmatic temnospondyl amphibian Tungussogyrinus bergi Efremov, 1939 shares clear synapomorphies with other branchiosaurids indicated by an anteriorly elongated infratemporal fossa and small branchial denticles.
R. Werneburg
doaj +1 more source
How not to disappear completely: new Stereospondyli fossils from the Rhaetian, Upper Triassic of Bonenburg, North Rhine-Westphalia and their implications for the Late Triassic extinction of Stereospondyli [PDF]
Acta Palaeontologica PolonicaTemnospondyli appeared in the early Carboniferous, became extinct in the Early Cretaceous and reached high diversity especially during the Permian and Triassic.
Andrea Prino +5 more
doaj +1 more source
New finds of Olenekian, Early Triassic, trematosaurid amphibians and prolocophonid reptiles from Poland [PDF]
Acta Palaeontologica PolonicaThe continental Lower Triassic (Middle Buntsandstein) siliciclastic deposits exposed along the margins of the Holy Cross Mountains, Poland, yield locally abundant vertebrate footprints and bones.
TOMASZ SULEJ +2 more
doaj +1 more source
Figure 15 in A new Lower Permian trematopid (Temnospondyli: Dissorophoidea) from Richards Spur, Oklahoma [PDF]
, 2011 Figure 15. Single most parsimonious tree of dissorophoid relationships derived from cladistic analysis using PAUP 4.0b10 with A, relevant synapomorphies mapped on (* indicates a synapomorphy that supports the clade, but appears elsewhere in the tree); B,
Reisz, Robert R., Polley, Brendan P.
core +3 more sources
Geologia USP. Série Científica, 2010 A região centro-leste do Estado de São Paulo possui boas exposições de sedimentos das sequencias permocarboníferas da Bacia intracratônica do Paraná.
Artur Chahud, Setembrino Petri
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Figure 13 in A new Lower Permian trematopid (Temnospondyli: Dissorophoidea) from Richards Spur, Oklahoma [PDF]
, 2011 Figure 13. Acheloma dunni, referred specimen (OMNH 52545). Right humerus in A, posterior view; B, extensor view; C, anterior view; D, flexor view; E, proximal view; F, distal view. Scale bar = 50 mm.Published as part of Polley, Brendan P. & Reisz, Robert
Reisz, Robert R., Polley, Brendan P.
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GEOMETRIC MORPHOMETRICS OF THE SKULL ROOF OF STEREOSPONDYLS (AMPHIBIA: TEMNOSPONDYLI) [PDF]
Palaeontology, 2006 Abstract: Geometric morphometric analysis using relative warps is applied to the skull roof of 62 species of stereospondyls and their closest outgroups (i.e. basal archegosauriforms) from among temnospondyl amphibians. Twenty‐one landmarks and five taxonomic groups are used for comparisons.
Stayton, CT, Ruta, M
openaire +2 more sources