SciELO - Scientific Electronic Library Online

 
vol.70 issue1The rise of a novel, plankton-based marine ecosystem during the Mesozoic: a bottom-up model to explain new higher-tier invertebrate morphotypesNew records of Humiriaceae fossil fruits from the Oligocene and Early Miocene of the western Azuero Peninsula, Panamá author indexsubject indexsearch form
Home Pagealphabetic serial listing  

Services on Demand

Journal

Article

Indicators

Related links

  • Have no similar articlesSimilars in SciELO

Share


Boletín de la Sociedad Geológica Mexicana

Print version ISSN 1405-3322

Abstract

DIAZ-SIBAJA, Roberto; JIMENEZ-HIDALGO, Eduardo  and  GARCIA-ZEPEDA, Ma. Luisa. A new fossiliferous site in Oaxaca (Mexico) and the suthernmost record fro Bison latifrons. Paleobiogeographic, paleoecologic and paleoenvironmental consequences. Bol. Soc. Geol. Mex [online]. 2018, vol.70, n.1, pp.201-222. ISSN 1405-3322.  https://doi.org/10.18268/bsgm2018v70n1a12.

We report the southernmost record of Bison latifrons in North America. This is the first record for the species in Oaxaca (Mexico), and for the Transmexican Volcanic Belt morphotectonic province; the known geographic distribution range of Bison latifrons is extended in more than 447 km, from Tequixquiac in the State of Mexico to central Oaxaca. This finding comes from a new fossiliferous locality at the municipality of San Dionisio Ocotepec, located in the Central Valleys region of the state of Oaxaca, Mexico. The associated fauna includes: Mammuthus columbi, Equus cf. E. conversidens, and Bison sp. By the presence of bison as well as mammoth, a Rancholabrean land mammal age (Late Pleistocene) is assigned to the fossil fauna. In addition, we performed a proboscidean mesowear analysis as well as a low magnification microwear analysis (35x) to the dental elements of the mammoth. Our findings suggest that the mammoth individual was a grazer. Due to the mammoth’s feeding habits and the habitat described for Mexican samples of bison and horses, we concluded that during the Late Pleistocene, San Dionisio Ocotepec was dominated by open grassland in the lowlands. This new fossil site and its fauna contribute to improve the knowledge of the Rancholabrean in southern Mexico, and particularly in the Central Valleys of Oaxaca. This improves our understanding of the biotic and climatic changes during the foundation of the Holocene.

Keywords : Rancholabrean; Oaxaca; Bison; Mammuthus; Equus.

        · abstract in Spanish     · text in Spanish     · Spanish ( pdf )