Holocene glacier history of northeastern Cordillera Darwin, southernmost South America (55°S)

Abstract In the Cordillera Darwin, southernmost South America, we used 10 Be and 14 C dating, dendrochronology, and historical observations to reconstruct the glacial history of the Dalla Vedova valley from deglacial time to the present. After deglacial recession into northeastern Darwin and Dalla V...

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Published in:Quaternary Research
Main Authors: Reynhout, Scott A., Kaplan, Michael R., Sagredo, Esteban A., Aravena, Juan Carlos, Soteres, Rodrigo L., Schwartz, Roseanne, Schaefer, Joerg M.
Format: Article in Journal/Newspaper
Language:English
Published: Cambridge University Press (CUP) 2021
Subjects:
Online Access:http://dx.doi.org/10.1017/qua.2021.45
https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0033589421000454
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spelling crcambridgeupr:10.1017/qua.2021.45 2024-05-12T07:56:25+00:00 Holocene glacier history of northeastern Cordillera Darwin, southernmost South America (55°S) Reynhout, Scott A. Kaplan, Michael R. Sagredo, Esteban A. Aravena, Juan Carlos Soteres, Rodrigo L. Schwartz, Roseanne Schaefer, Joerg M. 2021 http://dx.doi.org/10.1017/qua.2021.45 https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0033589421000454 en eng Cambridge University Press (CUP) https://www.cambridge.org/core/terms Quaternary Research volume 105, page 166-181 ISSN 0033-5894 1096-0287 General Earth and Planetary Sciences Earth-Surface Processes Arts and Humanities (miscellaneous) journal-article 2021 crcambridgeupr https://doi.org/10.1017/qua.2021.45 2024-04-18T06:54:42Z Abstract In the Cordillera Darwin, southernmost South America, we used 10 Be and 14 C dating, dendrochronology, and historical observations to reconstruct the glacial history of the Dalla Vedova valley from deglacial time to the present. After deglacial recession into northeastern Darwin and Dalla Vedova, by ~16 ka, evidence indicates a glacial advance at ~13 ka coeval with the Antarctic Cold Reversal. The next robustly dated glacial expansion occurred at 870 ± 60 calendar yr ago (approximately AD 1150), followed by less-extensive dendrochronologically constrained advances from shortly before AD 1836 to the mid-twentieth century. Our record is consistent with most studies within the Cordillera Darwin that show that the Holocene glacial maximum occurred during the last millennium. This pattern contrasts with the extensive early- and mid-Holocene glacier expansions farther north in Patagonia; furthermore, an advance at 870 ± 60 yr ago may suggest out-of-phase glacial advances occurred within the Cordillera Darwin relative to Patagonia. We speculate that a southward shift of westerlies and associated climate regimes toward the southernmost tip of the continent, about 900–800 yr ago, provides a mechanism by which some glaciers advanced in the Cordillera Darwin during what is generally considered a warm and dry period to the north in Patagonia. Article in Journal/Newspaper Antarc* Antarctic Cambridge University Press Antarctic Patagonia The Antarctic Quaternary Research 1 16
institution Open Polar
collection Cambridge University Press
op_collection_id crcambridgeupr
language English
topic General Earth and Planetary Sciences
Earth-Surface Processes
Arts and Humanities (miscellaneous)
spellingShingle General Earth and Planetary Sciences
Earth-Surface Processes
Arts and Humanities (miscellaneous)
Reynhout, Scott A.
Kaplan, Michael R.
Sagredo, Esteban A.
Aravena, Juan Carlos
Soteres, Rodrigo L.
Schwartz, Roseanne
Schaefer, Joerg M.
Holocene glacier history of northeastern Cordillera Darwin, southernmost South America (55°S)
topic_facet General Earth and Planetary Sciences
Earth-Surface Processes
Arts and Humanities (miscellaneous)
description Abstract In the Cordillera Darwin, southernmost South America, we used 10 Be and 14 C dating, dendrochronology, and historical observations to reconstruct the glacial history of the Dalla Vedova valley from deglacial time to the present. After deglacial recession into northeastern Darwin and Dalla Vedova, by ~16 ka, evidence indicates a glacial advance at ~13 ka coeval with the Antarctic Cold Reversal. The next robustly dated glacial expansion occurred at 870 ± 60 calendar yr ago (approximately AD 1150), followed by less-extensive dendrochronologically constrained advances from shortly before AD 1836 to the mid-twentieth century. Our record is consistent with most studies within the Cordillera Darwin that show that the Holocene glacial maximum occurred during the last millennium. This pattern contrasts with the extensive early- and mid-Holocene glacier expansions farther north in Patagonia; furthermore, an advance at 870 ± 60 yr ago may suggest out-of-phase glacial advances occurred within the Cordillera Darwin relative to Patagonia. We speculate that a southward shift of westerlies and associated climate regimes toward the southernmost tip of the continent, about 900–800 yr ago, provides a mechanism by which some glaciers advanced in the Cordillera Darwin during what is generally considered a warm and dry period to the north in Patagonia.
format Article in Journal/Newspaper
author Reynhout, Scott A.
Kaplan, Michael R.
Sagredo, Esteban A.
Aravena, Juan Carlos
Soteres, Rodrigo L.
Schwartz, Roseanne
Schaefer, Joerg M.
author_facet Reynhout, Scott A.
Kaplan, Michael R.
Sagredo, Esteban A.
Aravena, Juan Carlos
Soteres, Rodrigo L.
Schwartz, Roseanne
Schaefer, Joerg M.
author_sort Reynhout, Scott A.
title Holocene glacier history of northeastern Cordillera Darwin, southernmost South America (55°S)
title_short Holocene glacier history of northeastern Cordillera Darwin, southernmost South America (55°S)
title_full Holocene glacier history of northeastern Cordillera Darwin, southernmost South America (55°S)
title_fullStr Holocene glacier history of northeastern Cordillera Darwin, southernmost South America (55°S)
title_full_unstemmed Holocene glacier history of northeastern Cordillera Darwin, southernmost South America (55°S)
title_sort holocene glacier history of northeastern cordillera darwin, southernmost south america (55°s)
publisher Cambridge University Press (CUP)
publishDate 2021
url http://dx.doi.org/10.1017/qua.2021.45
https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0033589421000454
geographic Antarctic
Patagonia
The Antarctic
geographic_facet Antarctic
Patagonia
The Antarctic
genre Antarc*
Antarctic
genre_facet Antarc*
Antarctic
op_source Quaternary Research
volume 105, page 166-181
ISSN 0033-5894 1096-0287
op_rights https://www.cambridge.org/core/terms
op_doi https://doi.org/10.1017/qua.2021.45
container_title Quaternary Research
container_start_page 1
op_container_end_page 16
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