Significant shift in Neotropical plant diversity during the Paleocene-Eocene Thermal Maximum Event

The Paleocene-Eocene Thermal Maximum (PETM) is recognized by an increase in global temperatures of ~5ºC over a period of 10 to 20 ka. This warming is associated with a marked global decreasing in the carbon isotope (ä13C) signal, that has been recorded both in marine and terrestrial environments. We...

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Detalles Bibliográficos
Autores principales: Ochoa Lozano, D., Jaramillo, Carlos
Formato: Objeto de conferencia Resumen
Lenguaje:Inglés
Publicado: 2010
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Acceso en línea:http://sedici.unlp.edu.ar/handle/10915/16640
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