Paleofauna de Aguacaliente de Cartago, Costa Rica parte i: Equus cf. e. Conversidens Owen, 1869

Ana Lucía Valerio Z.; César Alberto Laurito M.

doi:10.15517/rgac.v0i31.7249

Vol. 31 (2004), Articles

Vol. 31 (2004)

PALEOFAUNA DE AGUACALIENTE DE CARTAGO, COSTA RICA PARTE I: <i>EQUUS CF. E.</i> CONVERSIDENS OWEN, 1869

Articles

https://doi.org/10.15517/rgac.v0i31.7249

Published June 1, 2011

Ana Lucía Valerio Z.⁺⁻
César Alberto Laurito M.⁺⁻

Ana Lucía Valerio Z.

Museo Nacional de Costa Rica, Departamento de Historia Natural.

César Alberto Laurito M.

Instituto Nacional de Aprendizaje, Núcleo de Turismo.

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Keywords

perissodactyla
equidae
equus
pleistoceno superior
intercambio biótico
costa rica
perissodactyla
equidae
equus
biotic interchange
costa rica

How to Cite

Valerio Z., A. L., & Laurito M., C. A. (2011). PALEOFAUNA DE AGUACALIENTE DE CARTAGO, COSTA RICA PARTE I: <i>EQUUS CF. E.</i> CONVERSIDENS OWEN, 1869. Revista geológica De América Central, 31. https://doi.org/10.15517/rgac.v0i31.7249

Abstract

An isolated tooth of Equus cf. E. conversidens Owen is recorded for the first time from the UpperPleistocene of Costa Rica and Central America. This premolar was found with some molars of an unidentifiedruminant. This species is very common in the Pleistocene of North America and was firstly described for theValley of Mexico. The Costa Rican found represents the most austral distribution of the species.

https://doi.org/10.15517/rgac.v0i31.7249

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