Fossil pollen records indicate that Patagonian desertification was not solely a consequence of Andean uplift

The Patagonian steppe—a massive rain-shadow on the lee side of the southern Andes—is assumed to have evolved ~15–12 Myr as a consequence of the southern Andean uplift. However, fossil evidence supporting this assumption is limited. Here we quantitatively estimate climatic conditions and plant richne...

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Autores principales: Palazzesi, Luis, Barreda, Viviana Dora, Cuitiño, José Ignacio, Guler, Maria Veronica, Tellería, María Cristina, Ventura Santos, R.
Formato: Articulo
Lenguaje:Inglés
Publicado: 2014
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Acceso en línea:http://sedici.unlp.edu.ar/handle/10915/95476
https://ri.conicet.gov.ar/11336/7533
http://www.nature.com/articles/ncomms4558
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