Diplocynodon

Diplocynodon
Temporal range: Paleocene - Middle Miocene,
Diplocynodon ratelii
Scientific classification
Domain: Eukaryota
Kingdom: Animalia
Phylum: Chordata
Class: Reptilia
Clade: Archosauromorpha
Clade: Archosauriformes
Order: Crocodilia
Superfamily: Alligatoroidea
Subfamily: Diplocynodontinae
Brochu, 1999
Genus: Diplocynodon
Pomel, 1847
Species
  • D. dalpiazi Del Favero, 1999
  • D. darwini (Ludvig, 1877)
  • D. deponiae (Frey, Laemmert & Riess, 1987)
  • D. elavericus Martin, 2010
  • D. gervaisi
  • D. hantoniensis (Wood, 1846)
  • D. levantinicum Huene & Nikoloff, 1963
  • D. kochi (Venczel & Codrea, 2022)
  • D. muelleri (Kälin, 1936)
  • D. ratelii Pomel, 1847 (type)
  • D. tormis
  • D. ungeri (Prangner, 1845)
Synonyms
  • Baryphracta Frey, Laemmert & Riess, 1987
  • Enneodon Pranger, 1845
  • Hispanochampsa Kälin, 1936
  • Saurocainus

Diplocynodon is an extinct genus of alligatoroid crocodilian that lived during the Paleocene to Middle Miocene in Europe. Some species may have reached lengths of 3 metres (9.8 ft), while others probably did not exceed 1 metre (3.3 ft). They are almost exclusively found in freshwater environments. The various species are thought to have been opportunistic aquatic predators.

In the nineteenth century, D. steineri was named from Styria, Austria and D. styriacus was named from Austria and France. A third Austrian species, Enneodon ungeri, was placed in its own genus. The Austrian and French species of Diplocynodon were synonymized with E. ungeri in 2011, and because the name Diplocynodon has priority over Enneodon, the species is now called D. ungeri. Other genera have recently been found to be synonymous with Diplocynodon. Hispanochampsa muelleri of Spain was determined to be synonymous with Diplocynodon in 2006, and Baryphracta deponaie of Germany was confirmed to be synonymous with Diplocynodon in 2012.

Well preserved specimens have been found in the Messel Pit and the Geiseltal lignite deposit in Germany. Most articulated Diplocynodon specimens from these localities contain gastroliths. In the Eocene epoch, the German sites were either a swampy freshwater lake (Messel Pit) or a peat bog swamp (Geiseltal).

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