The Oldest Camel Footprints from Mexico
Camel footprints have a well preserved record in Neogene strata from North America, including Mexico, however their Paleogene record is much less known. Here, we describe the oldest camel footprints from Mexico, located in the outskirts of Tezoatlán de Segura y Luna, northwestern Oaxaca, southern Me...
| Autores: | , |
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| Tipo de documento: | artigo |
| Estado: | Versão publicada |
| Data de publicação: | 2018 |
| País: | México |
| Recursos: | Universidad del Mar |
| Repositório: | Redalyc-UMAR |
| OAI Identifier: | oai:redalyc.org:94362562006 |
| Acesso em linha: | https://www.redalyc.org/articulo.oa?id=94362562006 https://www.redalyc.org/journal/943/94362562006/ https://www.redalyc.org/journal/943/94362562006/html/ https://www.redalyc.org/journal/943/94362562006/94362562006.epub https://www.redalyc.org/journal/943/94362562006/movil |
| Access Level: | Acceso aberto |
| Palavra-chave: | Ciencias de la Tierra Eocene Oaxaca Mixteca Camelidae Oligocene |
| Resumo: | Camel footprints have a well preserved record in Neogene strata from North America, including Mexico, however their Paleogene record is much less known. Here, we describe the oldest camel footprints from Mexico, located in the outskirts of Tezoatlán de Segura y Luna, northwestern Oaxaca, southern Mexico. The camel footprints are preserved as concave epirelief in fine-grained tuffaceous sandstone of the late Eocene-early Oligocene Huajuapan Formation. These footprints display the diagnostic features of Lamaichnum guanicoe, such as bidigital tracks with pointed anterior ends and rounded posterior ends, with digit impressions that do not converge anteriorly and footprints that have digit imprints connected. Potential track makers include Paratylopus, Paralabis and Pseudolabis. The concave axial surface and nail imprints of the Oaxacan footprints, indicate that the track makers shared some anatomical foot features with extant camels, suggesting that some characteristics of the peculiar camel foot had already evolved by the late Eocene-early Oligocene. |
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