Impact of Bolivian Paleolake Evaporation on the Δ18O of the Andean Glaciers During the Last Deglaciation (18.5–11.7 Ka): Diatom-Inferred Δ18O Values and Hydro-Isotopic Modeling

Quaternary Science Reviews - United Kingdom
doi 10.1016/j.quascirev.2015.04.022

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