Article · Wikipedia archive · Last revised Jun 11, 2026

Paritatodon

Paritatodon is an extinct mammaliaform which existed in Kyrgyzstan and England during the Jurassic period. It was originally the holotype specimen of Shuotherium kermacki, but Martin and Averianov (2010) argued that it resembled the genus Itatodon (Docodonta) and so renamed it Paritatodon.

Last revised
Jun 11, 2026
Read time
≈ 1 min
Length
213 w
Citations
5
Source
Paritatodon
Temporal range: Bathonian-Callovian
~
Scientific classification Edit this classification
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)

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

References

  1. 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.
  2. 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.
  3. 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.