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Sediment cores from three shallow (<10 m), saline lakes along a transect of the northern Chilean Altiplano (18 o S-27 o S) document changes in moisture balance for the mid- to late Holocene. Stable isotopic compositions of ostracods and authigenic carbonate were measured to test whether high altitude (>4000 m a.s.l.) paleoclimatic profiles show coherency within tropical-subtropical...
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