Figure 8: Photographs and interpretive drawings of the palates of Russian gorgonopsians.
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When and how did the terrestrial mid-Permian mass extinction occur? Evidence from the tetrapod record of the Karoo Basin, South Africa. [PDF]
Day MO +6 more
europepmc +1 more source
Breeding Young as a Survival Strategy during Earth's Greatest Mass Extinction. [PDF]
Botha-Brink J +4 more
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Antiquity of forelimb ecomorphological diversity in the mammalian stem lineage (Synapsida). [PDF]
Lungmus JK, Angielczyk KD.
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Palaeoneurological clues to the evolution of defining mammalian soft tissue traits. [PDF]
Benoit J, Manger PR, Rubidge BS.
europepmc +1 more source
The rise of the ruling reptiles and ecosystem recovery from the Permo-Triassic mass extinction. [PDF]
Ezcurra MD, Butler RJ.
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Tetrapod distribution and temperature rise during the Permian-Triassic mass extinction. [PDF]
Bernardi M, Petti FM, Benton MJ.
europepmc +1 more source
Bone microstructure and the evolution of growth patterns in Permo-Triassic therocephalians (Amniota, Therapsida) of South Africa. [PDF]
Huttenlocker AK, Botha-Brink J.
europepmc +1 more source
Reappraisal of the envenoming capacity of Euchambersia mirabilis (Therapsida, Therocephalia) using μCT-scanning techniques. [PDF]
Benoit J +3 more
europepmc +1 more source
Gorgonopsians were widely distributed during the Permian, and went extinct by the end of Permian. However, their fossil localities in the North Hemisphere are concentrated in the eastern European portion of Russia, except for one possible canine from the
Wan Yang
exaly +2 more sources

