Stegodon

Stegodon
Temporal range: Late MioceneLate Pleistocene,
Stegodon skeleton at the Gansu Provincial Museum
Scientific classification Edit this classification
Domain: Eukaryota
Kingdom: Animalia
Phylum: Chordata
Class: Mammalia
Order: Proboscidea
Family: Stegodontidae
Genus: Stegodon
Falconer, 1847
Species
  • S. aurorae (Matsumoto, 1918)
  • S. elephantoides (Clift, 1828)
  • S. florensis Hooijer, 1957
  • S. ganesha
    (Faloner and Cautley, 1846)
  • S. kaisensis Hopwood, 1939
  • S. luzonensis
    von Koenigswald, 1956
  • S. miensis (Matsumoto, 1941)
  • S. mindanensis (Naumann, 1890)
  • S. orientalis Owen, 1870
  • S. protoaurorae (Aiba et al., 2010)
  • S. sompoensis Hooijer, 1964
  • S. sondaari van den Bergh, 1999
  • S. trigonocephalus (Martin, 1887)
  • S. zdanskyi Hopwood, 1935

Stegodon ("roofed tooth" from the Ancient Greek words στέγω, stégō, 'to cover', + ὀδούς, odoús, 'tooth' because of the distinctive ridges on the animal's molars) is an extinct genus of proboscidean, related to elephants. It was originally assigned to the family Elephantidae along with modern elephants but is now placed in the extinct family Stegodontidae. Like elephants, Stegodon had teeth with plate-like lophs that are different from those of more primitive proboscideans like gomphotheres and mammutids.[1] The oldest fossils of the genus are found in Late Miocene strata in Asia, likely originating from the more archaic Stegolophodon, subsequently migrating into Africa.[2] While the genus became extinct in Africa during the Pliocene, Stegodon remained widespread in South, Southeast and East Asia until the end of the Pleistocene.[3]

  1. ^ Saegusa, Haruo (March 2020). "Stegodontidae and Anancus: Keys to understanding dental evolution in Elephantidae". Quaternary Science Reviews. 231: 106176. Bibcode:2020QSRv..23106176S. doi:10.1016/j.quascirev.2020.106176. S2CID 214094348.
  2. ^ Ao, Hong; Zhang, Peng; Dekkers, Mark J.; Roberts, Andrew P.; An, Zhisheng; Li, Yongxiang; Lu, Fengyan; Lin, Shan; Li, Xingwen (January 2016). "New magnetochronology of Late Miocene mammal fauna, NE Tibetan Plateau, China: Mammal migration and paleoenvironments". Earth and Planetary Science Letters. 434: 220–230. Bibcode:2016E&PSL.434..220A. doi:10.1016/j.epsl.2015.11.019. hdl:1874/330309.
  3. ^ O’Regan, H. J.; Bishop, L. C.; Lamb, A.; Elton, S.; Turner, A. (1 January 2005). "Large mammal turnover in Africa and the Levant between 1.0 and 0.5 Ma". Geological Society, London, Special Publications. 247 (1): 231–249. Bibcode:2005GSLSP.247..231O. doi:10.1144/GSL.SP.2005.247.01.13. ISSN 0305-8719. S2CID 129900545.

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