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“SOURCE-TO-SINK” DYNAMIC OF THE EASTERN SOUTH AMERICAN SLOPE SINCE THE LAST DEGLACIATION.

Martín et al.

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PALEOCLIMATE AND OCEAN–ATMOSPHERE COUPLING OFF SOUTHERN

PATAGONIA: EVIDENCE FROM MARINE SEDIMENT XRF GEOCHEMISTRY

AND PLANKTONIC FORAMINIFERA δ¹⁸O SINCE THE LAST GLACIAL MAXIMUM

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Arbieto et al.