Paritatodon
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Scientific classification 
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| Template:Taxon infoTemplate:Taxon italics (Sigogneau-Russell, 1998)
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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.
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
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- ^ a b c Page Module:Citation/CS1/styles.css has no content.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. Bibcode:2010JVPal..30..855M. 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.
- ^ Page Module:Citation/CS1/styles.css has no content.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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