Equus ovodovi Temporal range: Late Pleistocene-Holocene
Scientific classification
Domain:	Eukaryota
Kingdom:	Animalia
Phylum:	Chordata
Class:	Mammalia
Order:	Perissodactyla
Family:	Equidae
Genus:	Equus
Species:	E. ovodovi
Binomial name
Equus ovodovi Eisenmann and Vasiliev, 2011

Equus ovodovi is an extinct species of equine known from the Late Pleistocene and Holocene of Northern and East Asia. It was the last surviving member of the subgenus Sussemionus, which first appeared in North America over 2 million years ago, and was formerly present across Afro-Eurasia.^[1][2] Remains are known spanning from southern Western Siberia to Northern China, with the youngest remains dating to around 3500 years ago (~1500 BC) in Northern China. Genetic evidence suggests that it more closely related to zebras and asses than to horses. Initial genetic analysis based on the mitochondrial DNA found the exact relationship to be uncertain, but analysis of the full nuclear genome suggests that zebras and asses are more closely related to each other than either are to E. ovodovi, though there had been gene flow into Sussemonius lineage from both the last common ancesor of zebras and asses and the last common ancestor of zebras, as well as gene flow from the Sussemonius lineage into the last common ancestor of asses.^[3] It was slightly larger than the Asiatic wild ass,^[1] from which it can be distinguished based on its larger and more robust limb bones.^[4] Isotopic analysis of specimens from the Holocene of China suggests a preference for C4 plants.^[5] Its genetic diversity progressively declined to very low levels over the course of the Late Pleistocene and Holocene prior to its extinction.^[3]

References