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,...
Autores Principales: | , , , , , , , , , , |
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Formato: | Artículo (Article) |
Lenguaje: | Inglés (English) |
Publicado: |
Elsevier
2015
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Materias: | |
Acceso en línea: | https://repository.urosario.edu.co/handle/10336/27849 https://doi.org/10.1016/j.quascirev.2015.04.022 |