Impidens Temporal range: | |
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Life restoration of Impidens hancoxi | |
Scientific classification ![]() | |
Domain: | Eukaryota |
Kingdom: | Animalia |
Phylum: | Chordata |
Clade: | Synapsida |
Clade: | Therapsida |
Clade: | Cynodontia |
Family: | † Trirachodontidae |
Genus: | † Impidens Tolchard, Kammerer, Butler, Hendrickx, Benoit, Abdala, & Choiniere, 2021 |
Type species | |
Impidens hancoxi Tolchard, Kammerer, Butler, Hendrickx, Benoit, Abdala, & Choiniere, 2021 |
Impidens [a] is an extinct genus of large omnivorous cynodont from the Triassic of South Africa and Antarctica. Its type and only species is Impidens hancoxi. [b] Impidens inhabited high-latitude environments of southern Gondwana during the Middle Triassic, where it was probably the apex predator.
A specimen of Impidens was collected from Antarctica in 1986. In 1995, it was described as an indeterminate diademodontid possibly belonging to Titanogomphodon . [2] The holotype of Impidens hancoxi was found in South Africa in 2014. [3] It was described as a new species in 2021, with the Antarctic specimen and a less complete specimen from South Africa being referred to the species. [1]
Impidens was one of the largest non-mammalian cynodonts, with a skull well over 400 millimetres (16 in) long, though the herbivorous Scalenodontoides from the Late Triassic was even larger. [4]
Impidens is a member of Trirachodontidae, a family of gomphodont cynodonts. It is closely related to its smaller contemporary Cricodon as well as the earlier Langbergia and Trirachodon . [5] However, the phylogeny of Trirachodontidae is not well-understood, and the family may be paraphyletic, with some species more closely related to traversodontids than others.
Impidens fossils are known from the Cricodon-Ufudocyclops subzone of the Cynognathus Assemblage Zone of the Beaufort Group in South Africa and the upper Fremouw Formation in Antarctica. The dating of these strata is controversial; they are conventionally regarded as Middle Triassic in age, probably late Anisian or early Ladinian, but a biostratigraphically correlated fauna in South America has been dated to the beginning of the Late Triassic, in the early Carnian. [6] However, another biostratigraphically correlated fauna in China has been dated to the Anisian, suggesting the traditional dating may be correct. [7]
Impidens was probably the apex predator of its environment, as the only other large predator known to have coexisted with it was the somewhat smaller cynodont Cynognathus . The known large herbivores of the fauna are the cynodont Diademodon and the dicynodont Ufudocyclops . A smaller trirachodontid, Cricodon , was also present in the environment.
The Cricodon-Ufudocyclops subzone was deposited in a meandering river environment, with a deep channel and high banks. [8] Both it and the Fremouw Formation were high-paleolatitude environments, which may explain some of the faunal differences between them and lower-paleolatitude fauna. [4]