Paritatodon is an extinct mammaliaform which existed in Kyrgyzstan and England during the Jurassic period.[1] It was originally the holotype specimen of Shuotherium kermacki, but Martin and Averianov (2010)[1] argued that it resembled the genus Itatodon (Docodonta) and so renamed it Paritatodon.
| Paritatodon | |
|---|---|
Scientific classification 
| |
| Domain: | Eukaryota |
| Kingdom: | Animalia |
| Phylum: | Chordata |
| Clade: | Synapsida |
| Clade: | Therapsida |
| Clade: | Cynodontia |
| Clade: | Mammaliaformes |
| Genus: | †Paritatodon Martin & Averianov, 2010 |
| Species: | †P. kermacki
|
| Binomial name | |
| †Paritatodon kermacki (Sigogneau-Russell, 1998)
| |
Nonetheless, some recent phylogenetic studies assign it (and Itatodon) to Shuotheriidae,[2] while others continue to consider the taxon a docodont.
Like many Mesozoic mammals, this species is only known from its teeth, in this case two lower molars from the Forest Marble Formation in England,[3] and a single left lower molar from the Balabansai Formation in the Fergana Depression, Kyrgyzstan.[1]
References
edit- ^ a b c Thomas Martin & Alexander O. Averianov (2010). "Mammals from the Middle Jurassic Balbanasi Formation of the Fergana Depression, Kyrgyzstan". Journal of Vertebrate Paleontology. 30 (3): 855–871. doi:10.1080/02724631003758045. S2CID 128716878.
- ^ Wang, Y.-Q. and Li, C.-K. 2016. Reconsideration of the systematic position of the Middle Jurassic mammaliaforms Itatodon and Paritatodon. Palaeontologia Polonica 67, 249–256.
- ^ Denise Sigogneau-Russell (1998). "Discovery of a Late Jurassic Chinese mammal in the Upper Bathonian of England". Comptes Rendus de l'Académie des Sciences. 327 (8): 571–576. Bibcode:1998CRASE.327..571S. doi:10.1016/s1251-8050(99)80040-8.
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