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Hipparion

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The following article is from The Great Soviet Encyclopedia (1979). It might be outdated or ideologically biased.

Hipparion

 

a genus of tridactylous fossil horse; existed from the Upper Miocene until the end of the Pliocene. Hipparion was a small horse (height, up to 1.5 m at the withers). The molars were shorter than in horses of the genus Equus, and the side toes (second and fourth) were small and could not spread outward to prevent the limbs from sinking into the ground. Hipparion lived in large herds (up to several thousand) on grassy, savanna-like plains with occasional groves and bodies of water. During the Upper Miocene they were distributed throughout North America, which is the first place they appeared; later they settled all the continents except South America and Australia.

More than 50 species of Hipparion are known; they all became extinct and left no descendants. Hipparion was replaced by the single-hoofed horse, which arose from the closely related genus Pliohippus. Better adapted to the conditions of life in the plains, Pliohippus moved from North America to all continents.

REFERENCES

Kovalevskii, V. O. Paleontologiia loshadei. Moscow, 1948.
Gromova, V. “Gipparion (rod Hipparion).” Tr. Paleontologicheskogo in-ta, 1952, vol. 36.
Gabuniia, L. K. K istorii gipparionov. Moscow, 1959.

B. A. TROFIMOV

The Great Soviet Encyclopedia, 3rd Edition (1970-1979). © 2010 The Gale Group, Inc. All rights reserved.
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References in periodicals archive
"No, no," said the guide, "they found many other bones." He motioned towards a meticulously reassembled Hipparion skeleton.
Systematics and phylogeny of Hipparion, Neohipparion, Nannippus, and Cormohipparion (Mammalia, Equidae) from the Miocene and Pliocene of the New World.
Rich number of Hipparion and artiodactyls are present in this Formation.
The highlights of this field season so far have been the discovery and excavation of a well-preserved elephant jaw from Jaw Al Dibsa, as well as a pair of jaws of a primitive horse (known as a 'hipparion') and a crocodile skeleton from Hamra.
The findings described here are also supported, as (1) the Cervini and Muntiacicni split is reported at the transition of Miocene-Pliocene; due to this reason Early Pliocene age is referred to these fossil sites, (2) Some isolated molar remains of Hipparion also indicate the Early Pliocene age, and (3) an unconformity is present close to the Miocene-Pliocene boundary.
The identified species of hipparionines include Hipparion sp.
Keywords: Perissodactyl fauna, Hipparion, Sivalhippus, Miocene, hipparionine horses.
Studies done on dental micro-wear and oxygen and carbon isotopes on tooth enamel on a few other Siwalik mammals (bovids, Hipparion, Sivapithecus, etc.) also point towards a time of ecological stress for these animals (Nelson, 2007; Morgan et al., 1994).
The Hasnot tragulids are placed in Late Miocene to Pliocene age based on its associated fauna of the Late Miocene to Pliocene taxa such as Selenoportax Pachyportax Tragoportax and Hipparion. The tragulid-associated fauna shows abundant vegetation with significant food supply for the diversified mostly brachydont large mammalian fauna.
Keywords: Vertebrate fossils, Cremohipparion, Hipparion, Sivalhippus, Siwaliks.
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