Glacier fuctuations in the northern Patagonian Andes (44°S) imply wind‑modulated interhemispheric in‑phase climate shifts during Termination 1
The Last Glacial Termination (T1) featured major changes in global circulation systems that led to a shift from glacial to interglacial climate. While polar ice cores attest to an antiphased thermal pattern at millennial timescales, recent well-dated moraine records from both hemispheres suggest in-...
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Online Access: | https://doi.org/10.1038/s41598-022-14921-4 https://repositorio.uchile.cl/handle/2250/187047 |
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ftunivchile:oai:repositorio.uchile.cl:2250/187047 2023-05-15T14:01:29+02:00 Glacier fuctuations in the northern Patagonian Andes (44°S) imply wind‑modulated interhemispheric in‑phase climate shifts during Termination 1 Soteres, Rodrigo L. Sagredo, Esteban A. Kaplan, Michael R. Martin, Mateo A. Moreno Moncada, Patricio Iván Reynhout, Scott Andrew Schwartz, Roseanne Schaefer, Joerg M. 2022 application/pdf https://doi.org/10.1038/s41598-022-14921-4 https://repositorio.uchile.cl/handle/2250/187047 en eng Nature Scientifc Reports (2022) 12:10842 doi:10.1038/s41598-022-14921-4 https://repositorio.uchile.cl/handle/2250/187047 Attribution-NonCommercial-NoDerivs 3.0 United States http://creativecommons.org/licenses/by-nc-nd/3.0/us/ CC-BY-NC-ND Scientifc Reports Nuclide production-rates Chilean lake district BE-10 production-rate Southern alps New-Zealand Radiocarbon chronology Isla Grande East Greenland European alps Rakaia Valley Artículo de revista 2022 ftunivchile https://doi.org/10.1038/s41598-022-14921-4 2022-07-30T23:49:45Z The Last Glacial Termination (T1) featured major changes in global circulation systems that led to a shift from glacial to interglacial climate. While polar ice cores attest to an antiphased thermal pattern at millennial timescales, recent well-dated moraine records from both hemispheres suggest in-phase fluctuations in glaciers through T1, which is inconsistent with the bipolar see-saw paradigm. Here, we present a glacier chronology based on 30 new Be-10 surface exposure ages from well-preserved moraines in the Lago Palena/General Vintter basin in northern Patagonia (similar to 44 degrees S). We find that the main glacier lobe underwent profound retreat after 19.7 +/- 0.7 ka. This recessional trend led to the individualization of the Cerro Rinon glacier by similar to 16.3 ka, which underwent minor readvances at 15.9 +/- 0.5 ka during Heinrich Stadial 1, during the Antarctic Cold Reversal with successive maxima at 13.5 +/- 0.4, 13.1 +/- 0.4, and 13.1 +/- 0.5 ka, and a minor culmination at 12.5 +/- 0.4 ka during Younger Dryas time. We conclude that fluctuations of Patagonian glaciers during T1 were controlled primarily by climate anomalies brought by shifts in the Southern Westerly Winds (SWW) locus. We posit that the global covariation of mountain glaciers during T1 was linked to variations in atmospheric CO2 (atmCO(2)) promoted by the interplay of the SWW-Southern Ocean system at millennial timescales. Comision Nacional de Investigacion Cientifica y Tecnologica 21161417 Millennium Science Initiative/Millennium Nucleus Paleoclimate NCN17_079 Comision Nacional de Investigacion Cientifica y Tecnologica (CONICYT) CONICYT FONDECYT 1160488 1191435 Royal Society Te Aparangi, Marsden Fund VUW-1701 Versión publicada - versión final del editor Article in Journal/Newspaper Antarc* Antarctic East Greenland glacier Greenland Southern Ocean Universidad de Chile: Repositorio académico Antarctic Greenland isla Grande ENVELOPE(140.025,140.025,-66.664,-66.664) Marsden ENVELOPE(66.067,66.067,-67.867,-67.867) New Zealand Patagonia Southern Ocean The Antarctic Scientific Reports 12 1 |
institution |
Open Polar |
collection |
Universidad de Chile: Repositorio académico |
op_collection_id |
ftunivchile |
language |
English |
topic |
Nuclide production-rates Chilean lake district BE-10 production-rate Southern alps New-Zealand Radiocarbon chronology Isla Grande East Greenland European alps Rakaia Valley |
spellingShingle |
Nuclide production-rates Chilean lake district BE-10 production-rate Southern alps New-Zealand Radiocarbon chronology Isla Grande East Greenland European alps Rakaia Valley Soteres, Rodrigo L. Sagredo, Esteban A. Kaplan, Michael R. Martin, Mateo A. Moreno Moncada, Patricio Iván Reynhout, Scott Andrew Schwartz, Roseanne Schaefer, Joerg M. Glacier fuctuations in the northern Patagonian Andes (44°S) imply wind‑modulated interhemispheric in‑phase climate shifts during Termination 1 |
topic_facet |
Nuclide production-rates Chilean lake district BE-10 production-rate Southern alps New-Zealand Radiocarbon chronology Isla Grande East Greenland European alps Rakaia Valley |
description |
The Last Glacial Termination (T1) featured major changes in global circulation systems that led to a shift from glacial to interglacial climate. While polar ice cores attest to an antiphased thermal pattern at millennial timescales, recent well-dated moraine records from both hemispheres suggest in-phase fluctuations in glaciers through T1, which is inconsistent with the bipolar see-saw paradigm. Here, we present a glacier chronology based on 30 new Be-10 surface exposure ages from well-preserved moraines in the Lago Palena/General Vintter basin in northern Patagonia (similar to 44 degrees S). We find that the main glacier lobe underwent profound retreat after 19.7 +/- 0.7 ka. This recessional trend led to the individualization of the Cerro Rinon glacier by similar to 16.3 ka, which underwent minor readvances at 15.9 +/- 0.5 ka during Heinrich Stadial 1, during the Antarctic Cold Reversal with successive maxima at 13.5 +/- 0.4, 13.1 +/- 0.4, and 13.1 +/- 0.5 ka, and a minor culmination at 12.5 +/- 0.4 ka during Younger Dryas time. We conclude that fluctuations of Patagonian glaciers during T1 were controlled primarily by climate anomalies brought by shifts in the Southern Westerly Winds (SWW) locus. We posit that the global covariation of mountain glaciers during T1 was linked to variations in atmospheric CO2 (atmCO(2)) promoted by the interplay of the SWW-Southern Ocean system at millennial timescales. Comision Nacional de Investigacion Cientifica y Tecnologica 21161417 Millennium Science Initiative/Millennium Nucleus Paleoclimate NCN17_079 Comision Nacional de Investigacion Cientifica y Tecnologica (CONICYT) CONICYT FONDECYT 1160488 1191435 Royal Society Te Aparangi, Marsden Fund VUW-1701 Versión publicada - versión final del editor |
format |
Article in Journal/Newspaper |
author |
Soteres, Rodrigo L. Sagredo, Esteban A. Kaplan, Michael R. Martin, Mateo A. Moreno Moncada, Patricio Iván Reynhout, Scott Andrew Schwartz, Roseanne Schaefer, Joerg M. |
author_facet |
Soteres, Rodrigo L. Sagredo, Esteban A. Kaplan, Michael R. Martin, Mateo A. Moreno Moncada, Patricio Iván Reynhout, Scott Andrew Schwartz, Roseanne Schaefer, Joerg M. |
author_sort |
Soteres, Rodrigo L. |
title |
Glacier fuctuations in the northern Patagonian Andes (44°S) imply wind‑modulated interhemispheric in‑phase climate shifts during Termination 1 |
title_short |
Glacier fuctuations in the northern Patagonian Andes (44°S) imply wind‑modulated interhemispheric in‑phase climate shifts during Termination 1 |
title_full |
Glacier fuctuations in the northern Patagonian Andes (44°S) imply wind‑modulated interhemispheric in‑phase climate shifts during Termination 1 |
title_fullStr |
Glacier fuctuations in the northern Patagonian Andes (44°S) imply wind‑modulated interhemispheric in‑phase climate shifts during Termination 1 |
title_full_unstemmed |
Glacier fuctuations in the northern Patagonian Andes (44°S) imply wind‑modulated interhemispheric in‑phase climate shifts during Termination 1 |
title_sort |
glacier fuctuations in the northern patagonian andes (44°s) imply wind‑modulated interhemispheric in‑phase climate shifts during termination 1 |
publisher |
Nature |
publishDate |
2022 |
url |
https://doi.org/10.1038/s41598-022-14921-4 https://repositorio.uchile.cl/handle/2250/187047 |
long_lat |
ENVELOPE(140.025,140.025,-66.664,-66.664) ENVELOPE(66.067,66.067,-67.867,-67.867) |
geographic |
Antarctic Greenland isla Grande Marsden New Zealand Patagonia Southern Ocean The Antarctic |
geographic_facet |
Antarctic Greenland isla Grande Marsden New Zealand Patagonia Southern Ocean The Antarctic |
genre |
Antarc* Antarctic East Greenland glacier Greenland Southern Ocean |
genre_facet |
Antarc* Antarctic East Greenland glacier Greenland Southern Ocean |
op_source |
Scientifc Reports |
op_relation |
Scientifc Reports (2022) 12:10842 doi:10.1038/s41598-022-14921-4 https://repositorio.uchile.cl/handle/2250/187047 |
op_rights |
Attribution-NonCommercial-NoDerivs 3.0 United States http://creativecommons.org/licenses/by-nc-nd/3.0/us/ |
op_rightsnorm |
CC-BY-NC-ND |
op_doi |
https://doi.org/10.1038/s41598-022-14921-4 |
container_title |
Scientific Reports |
container_volume |
12 |
container_issue |
1 |
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1766271326402641920 |