Articles | Volume 13, issue 7
Clim. Past, 13, 879–895, 2017
https://doi.org/10.5194/cp-13-879-2017

Special issue: Southern perspectives on climate and the environment from...

Clim. Past, 13, 879–895, 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 et al.

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AC: Author comment | RC: Referee comment | SC: Short comment | EC: Editor comment
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Peer-review completion

AR: Author's response | RR: Referee report | ED: Editor decision
ED: Reconsider after major revisions (18 Jan 2017) by Helen Bostock
AR by Patricio Moreno on behalf of the Authors (05 Feb 2017)  Author's response    Manuscript
ED: Referee Nomination & Report Request started (17 Feb 2017) by Helen Bostock
RR by Anonymous Referee #1 (03 Apr 2017)
RR by Anonymous Referee #3 (04 May 2017)
ED: Publish subject to minor revisions (review by Editor) (04 May 2017) by Helen Bostock
AR by Patricio Moreno on behalf of the Authors (15 May 2017)  Author's response
ED: Publish subject to minor revisions (review by Editor) (29 May 2017) by Helen Bostock
AR by Patricio Moreno on behalf of the Authors (30 May 2017)  Author's response    Manuscript
ED: Publish subject to minor revisions (review by Editor) (01 Jun 2017) by Helen Bostock
AR by Patricio Moreno on behalf of the Authors (02 Jun 2017)  Author's response    Manuscript
ED: Publish as is (07 Jun 2017) by Helen Bostock
AR by Patricio Moreno on behalf of the Authors (08 Jun 2017)  Author's response    Manuscript
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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.