Hipparionini is an extinct tribe of three-toed horses in the subfamily Equinae. They had body forms similar to modern equines, with high-crowned teeth. They first appeared in North America during the Early Miocene around 17 million years ago,[1] before migrating into the Old World around 11.4-11.0 million years ago.[2] The youngest species date to the Early Pleistocene, becoming extinct following the arrival of modern equines of the genus Equus to the Old World.[3]
Hipparionines varied widely in size, with the smallest species like Hipparion periafricanum having a body mass of only 23 kilograms (51lb), considerably smaller than living equines,[4] while the largest species had body masses over 300 kilograms (660lb).[2] The smallest species were North American with the smallest Old World hipparionines probably no smaller than 70 kilograms (150lb).[5] Unlike modern horses, they bore three functional toes on each foot. Their teeth are somewhat lower crowned compared to modern equines, though they had relatively complex enamel patterns that exceed the enamel complexity of teeth of members of the tribe Equini, which is thought to have been an adaption to increasing wear resistance. Compared to modern equines, the metapodial bones of the leg/foot were longer, as is ancestrally found in equids.[6] Some Old World hipparionines like Proboscidipparion developed retracted nasals and elongated snouts that may indicate the presence of a tapir-like proboscis.[5]
Evolutionary history
Hipparionini originated in North America during the late Early Miocene, around 17 million years ago.[1] In North America, hipparionins were equally diverse to equins during the Middle Miocene but overtook them in species richness during the Late Miocene and Early Pliocene. At the end of the Hemphillian (during the latest Miocene) hipparionins severely declined in diversity.[7] Hipparionines eventually went extinct in North America during the Early Pleistocene, by which time they were confined to the southern latitudes of the continent. Following the end of the Miocene, hipparionines were only represented in North America by very small (sheep-sized) species of Cormohipparion and Nannippus.[5]
Following their origin in North America, a member of the genus Cormohipparion crossed over into Eurasia via the Bering Land Bridge around 11.4-11 million years ago, becoming ancestral to all Old World hipparionines[2][5] which was followed shortly afterwards by a migration into Africa around 10.5 million years ago, though hipparionines did not begin significantly diversifying in Africa until around 7.5 million years ago.[5] During their first few million years in Eurasia, they coexised alongside more primitive anchitheriin horses, which had cross the Bering Land Bridge from North America 8 million years earlier, which subsequently became extinct around 9 million years ago.[8] Hipparionines subsequently diversified in Afro-Eurasia, reaching maximum diversity around 7.6-6.8 million years ago, though at the end of the Miocene, around 6.8-5.3 million years ago, numerous lineages of Old World hipparionine lineages became extinct. During the following Pliocene, Old World hipparionines exhibted developed larger body sizes and higher crowned teeth to cope with environmental change. At the Pliocene-Pleistocene boundary, approximately 2.6 million years ago "stenonine" equines of the genus Equus migrated into Eurasia from North America, providing direct competition with the hipparionines. The last hipparionines in the Old World are Proboscidipparion sinense from China, and Eurygnathohippus cornelianus from Africa, dating to the end of the Early Pleistocene, approximately 1 million years ago.[2]
Ecology
In North America, Cormohipparion aff. C. quinni from the Barstovian (15-16 mya) and Neohipparion eurystyle from the Hemphillian (early Pliocene 4.7-4.8 mya) of Mexico have been suggested to have been mixed feeders (both browsing and grazing).[9][10]
In the Old World hipparionins were initially browsers and mixed feeders (both browsing and grazing), over time there was increasing proportion of pure grazers, though the groups ecology remained diverse, with mixed feeding being the dominant ecology during the Pliocene.[2] Hipparionins in the western Mediterranean during the Vallesian and Turolian stages of the late Miocene exhibited noticeable niche partitioning, with smaller forms being mixed feeders while larger species had more grazing diets. In contrast, contemporaneous eastern Mediterranean hipparionins did not exhibit such niche partitioning.[11]
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