A Pliocene–Pleistocene continental biota from Venezuela

The Pliocene–Pleistocene transition in the Neotropics is poorly understood despite the major climatic changes that occurred at the onset of the Quaternary. The San Gregorio Formation, the younger unit of the Urumaco Sequence, preserves a fauna that documents this critical transition. We report sting...

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Detalles Bibliográficos
Autores principales: Carrillo Briceño, Jorge D., Sánchez, Rodolfo, Scheyer, Torsten M., Carrillo, Juan David, Delfino, Massimo, Georgalis, Georgios L., Kerber, Leonardo, Ruiz Ramoni, Damián, Birindelli, José L. O., Cadena, Edwin A., Rincon, Aldo F., Chavez Hoffmeister, Martin, Carlini, Alfredo Armando, Carvalho, Mónica R., Trejos Tamayo, Raúl, Vallejo, Felipe, Jaramillo, Carlos, Jones, Douglas S., Sánchez Villagra, Marcelo R.
Formato: Articulo
Lenguaje:Inglés
Publicado: 2021
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Acceso en línea:http://sedici.unlp.edu.ar/handle/10915/123354
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