Sarkastodon
{{short description|Oxyaenid genus from upper Eocene Epoch}}
{{Use dmy dates|date=February 2024}}
{{Automatic taxobox
|fossil_range = {{Fossil range|45.0|39.9}} Middle Eocene
|image = Sarkastodon mongoliensis NT.jpg
|image_caption = Reconstruction of Sarkastodon mongoliensis
|image2 = Sarkastodon scull AMNH.jpg
|image2_caption = Skull reconstructions of Sarkastodon mongolensis
|taxon = Sarkastodon
|authority = Granger, 1938Granger, W. (1938.) [http://digitallibrary.amnh.org/dspace/bitstream/2246/2199/1/N0969.pdf "A giant oxyaenid from the upper Eocene of Mongolia."] American Museum Novitates 969.
|type_species = †Sarkastodon mongoliensis
|type_species_authority = Granger, 1938
|subdivision_ranks = Species
|subdivision =
- †Sarkastodon henanensis (Tong & Lei, 1986)Y. Tong and Y. Lei (1986.) "Fossil Creodonts and Carnivores (Mammalia) from the Hetaoyuan Eocene of Henan." Vertebrata PalAsiatica 24(3):210-221
- †Sarkastodon mongoliensis (Granger, 1938)
}}
Sarkastodon ("meaty tooth") is an extinct genus of placental mammals from extinct subfamily Oxyaeninae within extinct family Oxyaenidae, that lived in Asia (in today's China and Mongolia) during the middle Eocene. It was a genus of large, carnivorous animals known only from a skull and jawbones. Sarkastodon was probably a hypercarnivore that preyed on large mammals in its range during the Middle Eocene, such as brontotheres, chalicotheres, and rhinoceroses. Its weight is estimated at {{convert|800|kg|lb|abbr=on}},{{Cite journal |last=Sorkin |first=B. |title=A biomechanical constraint on body mass in terrestrial mammalian predators |journal=Lethaia |volume=41 |issue=4 |pages=333–347 |year=2008 |doi=10.1111/j.1502-3931.2007.00091.x|bibcode=2008Letha..41..333S }} and its length at 3 m (10 ft).{{cite book |last=Prothero |first=Donald R. |title=The Princeton Field Guide to Prehistoric Mammals |publisher=Princeton University Press |url=https://books.google.com/books?id=eiftDAAAQBAJ&pg=PA125 |year=2016 |page=125 |isbn=9781400884452}}
Discovery
The type specimens of S. mongoliensis are known from Eocene deposits from the Irdin Manha Formation of Mongolia. Additional material referred to Sarkastodon is known from the Ulan Shireb beds ({{convert|100|mi|km|abbr=off|order=flip|disp=or}} from the holotype locality) of Inner Mongolia. These specimens were discovered by Walter W. Granger in 1930, on an expedition to the Gobi Desert.
Palaeobiology
Sarkastodon was a hypercarnivore, with hyaena-like dentition specialised in bone-cracking.Rose KD. (2006.) The Beginning of the Age of Mammals. JHU Press: page 122{{cite journal |last1=Werdelin |first1=L. |year=1989 |title=Constraints and adaptations in the bone-cracking canid Osteoborus (Mammalia: Canidae) |journal=Paleobiology |volume=15 |issue=4 |pages=387–401 |doi=10.1017/S009483730000957X|bibcode=1989Pbio...15..387W |s2cid=82128868 }} The sharp, slicing premolars (which form roughly rectilinear cutting blades){{cite journal |last1=Muizon |first1=C. de |last2=Lange-Badré |first2=B. |year=2007 |title=Carnivorous dental adaptations in tribosphenic mammals and phylogenetic reconstruction |journal=Lethaia |volume=30 |issue=4 |pages=353–366 |doi=10.1111/j.1502-3931.1997.tb00481.x}} and crushing molars enabled Sarkastodon to eat both bone and flesh.Gunnell, GF. (1998.) "Creodonta", p. 91-109. In: Janis CM., Scott K.M., and Jacobs LL. (eds.). Evolution of Tertiary Mammals of North America, Volume 1: Terrestrial Carnivores, Ungulates, and Ungulatelike Mammals. Cambridge University Press, Cambridge. It was probably an ambush predator, not a fast runner.
References
{{Reflist|2}}
External links
- [http://www.johnsibbick.com/window/andrew.asp Artistic reconstruction of Sarkastodon], shown waiting for Andrewsarchus to finish eating from a dead brontothere.
{{Pan-Carnivora|P.|state=collapsed}}
{{Taxonbar|from=Q527627}}
Category:Eocene mammals of Asia
Category:Eocene genus first appearances