Resumen
A transfer function based on ostracod faunas was used to estimate past water depths of Lake Titicaca during the last 8000 yr BP. The results obtained on three cores revealed a complex evolution of the lacustrine basins. In general terms, the Holocene was characterized by low water levels, especially between ca 8000 and 3900 yr BP.
Título traducido de la contribución | Lake Titicaca paleohydrological evolution during the Holocene |
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Idioma original | Español |
Páginas (desde-hasta) | 573-583 |
Número de páginas | 11 |
Publicación | Bulletin - Institut Francais d'Etudes Andines |
Volumen | 24 |
N.º | 3 |
Estado | Publicada - 1995 |
Publicado de forma externa | Sí |