Articles | Volume 13, issue 7
https://doi.org/10.5194/cp-13-879-2017
https://doi.org/10.5194/cp-13-879-2017
Research article
 | 
14 Jul 2017
Research article |  | 14 Jul 2017

The last glacial termination on the eastern flank of the central Patagonian Andes (47 ° S)

William I. Henríquez, Rodrigo Villa-Martínez, Isabel Vilanova, Ricardo De Pol-Holz, and Patricio I. Moreno

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Latest update: 20 Nov 2024
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Short summary
Results from Lago Edita, central-western Patagonia (47° S), allow examination of the timing and direction of paleoclimate signals during the last glacial termination (T1) in southern midlatitudes. Cold and wet conditions prevailed during T1, terminated by warm pulses at 13 000 and 11 000 yr BP. Delayed warming, relative to sites along the Pacific coast, raises the possibility that residual ice masses in the Andes induced regional cooling along downwind sectors of central Patagonia during T1.