Late glacial and holocene palaeolake history of the Última Esperanza region of southern Patagonia
We undertook multi-proxy analyses on two sediment cores from Lago Pato, a small lake basin at 51 degrees S topographically separated from Lago del Toro in Torres del Paine (TdP), to provide insights into glacier dynamics and lake-level change in the TdP and ultima Esperanza region over the last simi...
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Online Access: | https://doi.org/10.3389/feart.2022.813396 https://repositorio.uchile.cl/handle/2250/186466 |
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ftunivchile:oai:repositorio.uchile.cl:2250/186466 2023-05-15T14:01:29+02:00 Late glacial and holocene palaeolake history of the Última Esperanza region of southern Patagonia Roberts, Stephen J. McCulloch, Robert D. Emmings, Joseph F. Davies, Sarah J. Van Nieuwenhuyze, Win Sterken, Mieke Heirman, Katrien Van Wichelen, Jeroen Díaz Prado, Carolina Van de Vyver, Evelien Whittle, Alex Vyverman, Win Hodgson, Dominic A. Verleyen, Elie 2022 application/pdf https://doi.org/10.3389/feart.2022.813396 https://repositorio.uchile.cl/handle/2250/186466 en eng MDPI Front. Earth Sci. 10:813396 doi:10.3389/feart.2022.813396 https://repositorio.uchile.cl/handle/2250/186466 Attribution-NonCommercial-NoDerivs 3.0 United States http://creativecommons.org/licenses/by-nc-nd/3.0/us/ CC-BY-NC-ND Frontiers in Earth Science Last glacial maximum (LGM) Palaeoclimate Palaeolimnology Glaciation Lake-level changes Patagonia Southern hemisphere westerly winds (SWW) Artículo de revista 2022 ftunivchile https://doi.org/10.3389/feart.2022.813396 2022-07-09T23:49:42Z We undertook multi-proxy analyses on two sediment cores from Lago Pato, a small lake basin at 51 degrees S topographically separated from Lago del Toro in Torres del Paine (TdP), to provide insights into glacier dynamics and lake-level change in the TdP and ultima Esperanza region over the last similar to 30,000 cal a BP (30 ka). Lago Pato is situated in a region overridden by the Southern Patagonian Ice Field during the Last Glacial and in a transitional climatic zone of Southern Patagonia sensitive to seasonal- to millennial-scale changes in the Southern Hemisphere Westerly Winds (SWW). Results show that a deep ice-dammed and enlarged palaeolake encompassed Lago del Toro and Lago Pato c. 30-20 ka after the ice had retreated from local-Last Glacial Maximum (l-LGM) limits at c. 48-34 ka and during the build-up to the global-Last Glacial Maximum (g-LGM), c. 26-19 ka. Gaps in both sediment records between c. 20-13.4 ka and c. 20-10 ka suggest hiatuses in sediment accumulation during the g-LGM and Antarctic Cold Reversal (ACR) readvances and/or removal by lake lowering or flushing during the Late Glacial-early Holocene. The palaeolake level dropped from >100 m a.s.l. to similar to 40-50 m a.s.l. towards the end of the ACR c. 13.4-13.0 ka, creating a shallower glaciolacustrine environment dammed by an ice tongue in the Estancia Puerto Consuelo-ultima Esperanza fjord. Further lowering of the enlarged palaeolake level occurred when the ice thinned to <40 m a.s.l., eventually isolating Lago Pato from Lago del Toro and glaciogenic sediment input at c. 11.7 ka. After isolation, the ecology and water levels in Lago Pato became sensitive to regional climate shifts. The shallow, stable, and highly anoxic environment that developed after c. 11.7 ka is associated with weaker (or poleward shifted) SWW at 51 degrees S and was replaced at c. 10 ka by an increasingly productive shallow-littoral lake with a variable lake-level and periodic shifts in anoxic-oxic bottom water conditions and ratios of benthic-planktonic ... Article in Journal/Newspaper Antarc* Antarctic Universidad de Chile: Repositorio académico Antarctic Esperanza ENVELOPE(-56.983,-56.983,-63.400,-63.400) Paine ENVELOPE(-147.533,-147.533,-86.767,-86.767) Patagonia Frontiers in Earth Science 10 |
institution |
Open Polar |
collection |
Universidad de Chile: Repositorio académico |
op_collection_id |
ftunivchile |
language |
English |
topic |
Last glacial maximum (LGM) Palaeoclimate Palaeolimnology Glaciation Lake-level changes Patagonia Southern hemisphere westerly winds (SWW) |
spellingShingle |
Last glacial maximum (LGM) Palaeoclimate Palaeolimnology Glaciation Lake-level changes Patagonia Southern hemisphere westerly winds (SWW) Roberts, Stephen J. McCulloch, Robert D. Emmings, Joseph F. Davies, Sarah J. Van Nieuwenhuyze, Win Sterken, Mieke Heirman, Katrien Van Wichelen, Jeroen Díaz Prado, Carolina Van de Vyver, Evelien Whittle, Alex Vyverman, Win Hodgson, Dominic A. Verleyen, Elie Late glacial and holocene palaeolake history of the Última Esperanza region of southern Patagonia |
topic_facet |
Last glacial maximum (LGM) Palaeoclimate Palaeolimnology Glaciation Lake-level changes Patagonia Southern hemisphere westerly winds (SWW) |
description |
We undertook multi-proxy analyses on two sediment cores from Lago Pato, a small lake basin at 51 degrees S topographically separated from Lago del Toro in Torres del Paine (TdP), to provide insights into glacier dynamics and lake-level change in the TdP and ultima Esperanza region over the last similar to 30,000 cal a BP (30 ka). Lago Pato is situated in a region overridden by the Southern Patagonian Ice Field during the Last Glacial and in a transitional climatic zone of Southern Patagonia sensitive to seasonal- to millennial-scale changes in the Southern Hemisphere Westerly Winds (SWW). Results show that a deep ice-dammed and enlarged palaeolake encompassed Lago del Toro and Lago Pato c. 30-20 ka after the ice had retreated from local-Last Glacial Maximum (l-LGM) limits at c. 48-34 ka and during the build-up to the global-Last Glacial Maximum (g-LGM), c. 26-19 ka. Gaps in both sediment records between c. 20-13.4 ka and c. 20-10 ka suggest hiatuses in sediment accumulation during the g-LGM and Antarctic Cold Reversal (ACR) readvances and/or removal by lake lowering or flushing during the Late Glacial-early Holocene. The palaeolake level dropped from >100 m a.s.l. to similar to 40-50 m a.s.l. towards the end of the ACR c. 13.4-13.0 ka, creating a shallower glaciolacustrine environment dammed by an ice tongue in the Estancia Puerto Consuelo-ultima Esperanza fjord. Further lowering of the enlarged palaeolake level occurred when the ice thinned to <40 m a.s.l., eventually isolating Lago Pato from Lago del Toro and glaciogenic sediment input at c. 11.7 ka. After isolation, the ecology and water levels in Lago Pato became sensitive to regional climate shifts. The shallow, stable, and highly anoxic environment that developed after c. 11.7 ka is associated with weaker (or poleward shifted) SWW at 51 degrees S and was replaced at c. 10 ka by an increasingly productive shallow-littoral lake with a variable lake-level and periodic shifts in anoxic-oxic bottom water conditions and ratios of benthic-planktonic ... |
format |
Article in Journal/Newspaper |
author |
Roberts, Stephen J. McCulloch, Robert D. Emmings, Joseph F. Davies, Sarah J. Van Nieuwenhuyze, Win Sterken, Mieke Heirman, Katrien Van Wichelen, Jeroen Díaz Prado, Carolina Van de Vyver, Evelien Whittle, Alex Vyverman, Win Hodgson, Dominic A. Verleyen, Elie |
author_facet |
Roberts, Stephen J. McCulloch, Robert D. Emmings, Joseph F. Davies, Sarah J. Van Nieuwenhuyze, Win Sterken, Mieke Heirman, Katrien Van Wichelen, Jeroen Díaz Prado, Carolina Van de Vyver, Evelien Whittle, Alex Vyverman, Win Hodgson, Dominic A. Verleyen, Elie |
author_sort |
Roberts, Stephen J. |
title |
Late glacial and holocene palaeolake history of the Última Esperanza region of southern Patagonia |
title_short |
Late glacial and holocene palaeolake history of the Última Esperanza region of southern Patagonia |
title_full |
Late glacial and holocene palaeolake history of the Última Esperanza region of southern Patagonia |
title_fullStr |
Late glacial and holocene palaeolake history of the Última Esperanza region of southern Patagonia |
title_full_unstemmed |
Late glacial and holocene palaeolake history of the Última Esperanza region of southern Patagonia |
title_sort |
late glacial and holocene palaeolake history of the última esperanza region of southern patagonia |
publisher |
MDPI |
publishDate |
2022 |
url |
https://doi.org/10.3389/feart.2022.813396 https://repositorio.uchile.cl/handle/2250/186466 |
long_lat |
ENVELOPE(-56.983,-56.983,-63.400,-63.400) ENVELOPE(-147.533,-147.533,-86.767,-86.767) |
geographic |
Antarctic Esperanza Paine Patagonia |
geographic_facet |
Antarctic Esperanza Paine Patagonia |
genre |
Antarc* Antarctic |
genre_facet |
Antarc* Antarctic |
op_source |
Frontiers in Earth Science |
op_relation |
Front. Earth Sci. 10:813396 doi:10.3389/feart.2022.813396 https://repositorio.uchile.cl/handle/2250/186466 |
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/10.3389/feart.2022.813396 |
container_title |
Frontiers in Earth Science |
container_volume |
10 |
_version_ |
1766271326040883200 |