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This page is a summary of: 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, July 2015, Elsevier,
DOI: 10.1016/j.quascirev.2015.04.022.
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