Impact of Bolivian paleolake evaporation on the ?18O of the Andean glaciers during the last deglaciation (18.5-11.7 ka): Diatom-inferred ?18O values and hydro-isotopic modeling

During the last deglaciation, the Bolivian Altiplano (15–23°S, 66–70°W) was occupied by paleolake Tauca covering, at least, ?51,000 km2 at its maximum highstand between 16.5 and 15 ka. Twenty-five hundred years later, after a massive regression, a new transgressive phase, produced paleolake Coipasa,...

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Detalles Bibliográficos
Autores Principales: Quesada, Benjamin, Sylvestre, Florence, Vimeux, Françoise, Black, Jessica, Paillès, Christine, Sonzogni, Corinne, Alexandre, Anne, Blardd, Pierre-Henri, Tonetto, Alain, Mazura, Jean-Charles, Bruneton, Hélène
Formato: Artículo (Article)
Lenguaje:Inglés (English)
Publicado: Elsevier 2015
Materias:
Acceso en línea:https://repository.urosario.edu.co/handle/10336/27849
https://doi.org/10.1016/j.quascirev.2015.04.022