Gavialosuchus

Gavialosuchus
Temporal range: Late Oligocene - Early Pliocene
Skull of Gavialosuchus americanus
Scientific classification
Kingdom: Animalia
Phylum: Chordata
Class: Reptilia
Superorder: Crocodylomorpha
Order: Crocodilia
Subfamily: Tomistominae
Genus: Gavialosuchus
Toula and Kail, 1885
Species
  • G. eggenburgensis Toula and Kail, 1885 (type)
  • ?G. americanus (Sellards, 1915 [originally Tomistoma americanus])
  • ?G. carolinensis Erickson and Sawyer, 1996

Gavialosuchus is an extinct tomistomine from the late Oligocene and Miocene of eastern North America and early Miocene of Europe. Three species have been named: the type species G. eggenburgensis from the early Miocene of Austria; G. americanus, from the late Miocene to early Pliocene of Florida; and G. carolinensis, from the late Oligocene of South Carolina. Another species, as yet unnamed, may be present in the Miocene of Georgia. Unlike its modern fresh water relatives, Gavialosuchus was an estuarine and coastal water crocodilian, living in shallow marine waters alongside Metaxytherium, Pomatodelphis, and Hemipristis serra. It was long-snouted and large: G. carolinensis was at least 5.37 meters long (17.3 ft),[1] and one specimen of G. americanus is estimated at 9.75 meters (32.0 ft) long based on a 132 centimeters (52 in)-long skull.[2]

Gavialosuchus eggenburgensis skull

As is the case with many fossil taxa, what exactly constitutes Gavialosuchus is not a settled question. Myrick Jr. (2001) proposed synonymizing G. americanus with Thecachampsa antiqua.[3] Piras et al. (2007) advocated transferring both G. americanus and G. carolinensis to Thecachampsa as distinct species of the latter genus.[4] Jouve et al. (2008) retained G. americanus in Gavialosuchus and found it to be the sister group of G. eggenburgensis (G. carolinensis was not discussed).[5] However, Jouve et al. (2008) didn't test Thecachampsa antiqua in their phylogenetic analysis. Shan et al. (2009) found that G. americanus and G. eggenburgensis are not sister taxa. However, they didn't include T. antiqua and G. carolinensis in their analysis.[6] Christopher A. Brochu and Glenn W. Storrs (2012) tested all four species, along with other crocodyloids, and found relatively strong support for Piras et al. (2007) suggestion.[7]

References

  1. Erickson, Bruce R.; Sawyer, Glen T. (1996). The estuarine crocodile Gavialosuchus carolinensis n. sp. (Crocodylia: Eusuchia) from the late Oligocene of South Carolina, North America. The Science Museum of Minnesota St. Paul, Minnesota Monograph 3, Paleontology. St. Paul: The Science Museum of Minnesota. pp. 1–47.
  2. "Gavialosuchus skull replica". Skulls Unlimited. 2009-09-03. Archived from the original on November 19, 2008. Retrieved 2009-09-15.
  3. Myrick, A.C., Jr. (2001). "Thecachampsa antiqua (Leidy, 1852) (Crocodylidae: Thoracosaurinae) from the fossil marine deposits at Lee Creek Mine, Aurora, North Carolina, USA". Smithsonian Contributions to Paleobiology 90: 219–225.
  4. Piras, P.; Delfino, M.; Del Favero, L.; Kotsakis, T. (2007). "Phylogenetic position of the crocodylian Megadontosuchus arduini and tomistomine palaeobiogeography" (pdf). Acta Palaeontologica Polonica 52 (2): 315–328.
  5. Jouve, Stéphane; Bardet, Nathalie; Jalil, Nour-Eddine; Suberbiola, Xabier Pereda; Bouya; Baâda; Amaghzaz, Mbarek (2008). "The oldest African crocodylian: phylogeny, paleobiogeography, and differential survivorship of marine reptiles through the Cretaceous-Tertiary Boundary". Journal of Vertebrate Paleontology 28 (2): 409–421. doi:10.1671/0272-4634(2008)28[409:TOACPP]2.0.CO;2.
  6. Shan, Hsi-yin; Wu, Xiao-chun; Cheng, Yen-nien; Sato, Tamaki (2009). "A new tomistomine (Crocodylia) from the Miocene of Taiwan". Canadian Journal of Earth Sciences 46 (7): 529–555. doi:10.1139/E09-036.
  7. Brochu, C. A.; Storrs, G. W. (2012). "A giant crocodile from the Plio-Pleistocene of Kenya, the phylogenetic relationships of Neogene African crocodylines, and the antiquity of Crocodylus in Africa". Journal of Vertebrate Paleontology 32 (3): 587. doi:10.1080/02724634.2012.652324.
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