Puma pardoides

Extinct species of felid From Wikipedia, the free encyclopedia

Puma pardoides

Puma pardoides is an extinct prehistoric cat in the genus Puma known from fossils found across Eurasia.

Quick Facts Scientific classification, Binomial name ...
Puma pardoides
Temporal range: Pliocene-Pleistocene
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Skull
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Scientific classification
Domain: Eukaryota
Kingdom: Animalia
Phylum: Chordata
Class: Mammalia
Order: Carnivora
Suborder: Feliformia
Family: Felidae
Subfamily: Felinae
Genus: Puma
Species:
P. pardoides
Binomial name
Puma pardoides
(Owen, 1846)
Synonyms
  • Felis pardoides Owen, 1846
  • Panthera schaubi Viret, 1954
  • Viretailurus schaubi (Viret, 1954) sensu Hemmer, 1964
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History and naming

Puma pardoides was originally described in 1846 as Felis pardoides.[1] A complete skull was described in 1954 as Panthera schaubi,[2] but was assigned in 1965 to a new genus as Viretailurus schaubi due to distinct differences from other pantherine cats.[3] In 2001, however, it was pointed out that the various puma-like fossils in Eurasia could all be attributed to a single species, Puma pardoides.[4][5] And in 2004, Viretailurus schaubia was also found to be a junior synonym of Puma pardoides.[6]

Classification

Panthera schaubi or Viretailurus schaubi was historically often regarded as a basal member of the genus Panthera.[7] However, research in 2004 concluded that Viretailurus should actually be included in the genus Puma as a junior synonym of Puma pardoides.[6][8] Fossils of this leopard-sized animal are around 2 million years old and were found in France. However, their classification was difficult, due to the similarities between leopards and pumas, until teeth found at the Upper Pliocene Transcaucasian site of Kvabebi were found to be similar to those of pumas. [6] It is inferred that the species, Puma pardoides is related to living pumas, which can be supported by Eurasian origin of the puma lineage.[9]

Extinction

The last occurrences of Puma pardoides are from about 0.85 Ma. The extinction of this felid may have had something to do with the Mid-Pleistocene Transition.[10]

References

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