Late Quaternary glacial maxima in southern Patagonia: insights from the Lago Argentino glacier lobe

Autores
Romero, Matias; Penprase, Shanti B.; Van Wyk de Vries, Maximillian S.; Wickert, Andrew D.; Jones, Andrew G.; Marcott, Shaun A.; Strelin, Jorge Adrián; Martini, Mateo Antonio; Rittenour, Tammy M.; Brignone, Guido; Shapley, Mark D.; Ito, Emi; MacGregor, Kelly R.; Caffee, Marc W.
Año de publicación
2024
Idioma
inglés
Tipo de recurso
artículo
Estado
versión publicada
Descripción
Determining the timing and extent of Quaternary glaciations around the globe is critical to understanding the drivers behind climate change and glacier fluctuations. Evidence from the southern mid-latitudes indicates that local glacial maxima preceded the global Last Glacial Maximum (LGM), implying that feedbacks in the climate system or ice dynamics played a role beyond the underlying orbital forcings. To shed light on these processes, we investigated the glacial landforms shaped and deposited by the Lago Argentino glacier (50° S), an outlet lobe of the former Patagonian Ice Sheet, in southern Argentina. We mapped geomorphological features on the landscape and dated moraine boulders and outwash sediments using 10Be cosmogenic nuclides and feldspar infrared stimulated luminescence (IRSL) to constrain the chronology of glacial advance and retreat. We report that the Lago Argentino glacier lobe reached more extensive limits prior to the global LGM, advancing during the middle to late Pleistocene between 243–132 ka and during Marine Isotope Stage 3 (MIS 3), culminating at 44.5 ± 8.0 and at 36.6 ± 1.0 ka. Our results indicate that the most extensive advance of the last glacial cycle occurred during MIS 3, and we hypothesize that this was a result of longer and colder winters, as well as increased precipitation delivered by a latitudinal migration of the Southern Westerly Winds belt, highlighting the role of local and regional climate feedbacks in modulating ice mass changes in the southern mid-latitudes.
Fil: Romero, Matias. Consejo Nacional de Investigaciones Científicas y Técnicas. Centro Científico Tecnológico Conicet - Córdoba. Centro de Investigaciones en Ciencias de la Tierra. Universidad Nacional de Córdoba. Facultad de Ciencias Exactas Físicas y Naturales. Centro de Investigaciones en Ciencias de la Tierra; Argentina. University of Wisconsin; Estados Unidos
Fil: Penprase, Shanti B.. University of Minnesota; Estados Unidos
Fil: Van Wyk de Vries, Maximillian S.. University of Minnesota; Estados Unidos. University of Oxford; Reino Unido. University of Liverpool; Reino Unido. University of Nottingham; Estados Unidos. University of Cambridge; Reino Unido
Fil: Wickert, Andrew D.. University of Minnesota; Estados Unidos. Deutsches GeoForschungsZentrum; Alemania
Fil: Jones, Andrew G.. University of Wisconsin; Estados Unidos
Fil: Marcott, Shaun A.. University of Wisconsin; Estados Unidos
Fil: Strelin, Jorge Adrián. Consejo Nacional de Investigaciones Científicas y Técnicas. Centro Científico Tecnológico Conicet - Córdoba. Centro de Investigaciones en Ciencias de la Tierra. Universidad Nacional de Córdoba. Facultad de Ciencias Exactas Físicas y Naturales. Centro de Investigaciones en Ciencias de la Tierra; Argentina. Ministerio de Relaciones Exteriores, Comercio Interno y Culto. Dirección Nacional del Antártico. Instituto Antártico Argentino; Argentina
Fil: Martini, Mateo Antonio. Consejo Nacional de Investigaciones Científicas y Técnicas. Centro Científico Tecnológico Conicet - Córdoba. Centro de Investigaciones en Ciencias de la Tierra. Universidad Nacional de Córdoba. Facultad de Ciencias Exactas Físicas y Naturales. Centro de Investigaciones en Ciencias de la Tierra; Argentina
Fil: Rittenour, Tammy M.. State University of Utah; Estados Unidos
Fil: Brignone, Guido. Universidad Nacional de Córdoba. Facultad de Ciencias Exactas, Físicas y Naturales; Argentina
Fil: Shapley, Mark D.. University of Minnesota; Estados Unidos
Fil: Ito, Emi. University of Minnesota; Estados Unidos
Fil: MacGregor, Kelly R.. Macalester Collage; Estados Unidos
Fil: Caffee, Marc W.. Purdue University; Estados Unidos
Materia
COSMOGENIC DATING
MORAINES
WESTERLIES
PALEOCLIMATE
Nivel de accesibilidad
acceso abierto
Condiciones de uso
https://creativecommons.org/licenses/by/2.5/ar/
Repositorio
CONICET Digital (CONICET)
Institución
Consejo Nacional de Investigaciones Científicas y Técnicas
OAI Identificador
oai:ri.conicet.gov.ar:11336/260914
Acceder
id CONICETDig_aeeab95a05d4179fcdd571c54f0bffc6
oai_identifier_str oai:ri.conicet.gov.ar:11336/260914
network_acronym_str CONICETDig
repository_id_str 3498
network_name_str CONICET Digital (CONICET)
spelling Late Quaternary glacial maxima in southern Patagonia: insights from the Lago Argentino glacier lobeRomero, MatiasPenprase, Shanti B.Van Wyk de Vries, Maximillian S.Wickert, Andrew D.Jones, Andrew G.Marcott, Shaun A.Strelin, Jorge AdriánMartini, Mateo AntonioRittenour, Tammy M.Brignone, GuidoShapley, Mark D.Ito, EmiMacGregor, Kelly R.Caffee, Marc W.COSMOGENIC DATINGMORAINESWESTERLIESPALEOCLIMATEhttps://purl.org/becyt/ford/1.5https://purl.org/becyt/ford/1Determining the timing and extent of Quaternary glaciations around the globe is critical to understanding the drivers behind climate change and glacier fluctuations. Evidence from the southern mid-latitudes indicates that local glacial maxima preceded the global Last Glacial Maximum (LGM), implying that feedbacks in the climate system or ice dynamics played a role beyond the underlying orbital forcings. To shed light on these processes, we investigated the glacial landforms shaped and deposited by the Lago Argentino glacier (50° S), an outlet lobe of the former Patagonian Ice Sheet, in southern Argentina. We mapped geomorphological features on the landscape and dated moraine boulders and outwash sediments using 10Be cosmogenic nuclides and feldspar infrared stimulated luminescence (IRSL) to constrain the chronology of glacial advance and retreat. We report that the Lago Argentino glacier lobe reached more extensive limits prior to the global LGM, advancing during the middle to late Pleistocene between 243–132 ka and during Marine Isotope Stage 3 (MIS 3), culminating at 44.5 ± 8.0 and at 36.6 ± 1.0 ka. Our results indicate that the most extensive advance of the last glacial cycle occurred during MIS 3, and we hypothesize that this was a result of longer and colder winters, as well as increased precipitation delivered by a latitudinal migration of the Southern Westerly Winds belt, highlighting the role of local and regional climate feedbacks in modulating ice mass changes in the southern mid-latitudes.Fil: Romero, Matias. Consejo Nacional de Investigaciones Científicas y Técnicas. Centro Científico Tecnológico Conicet - Córdoba. Centro de Investigaciones en Ciencias de la Tierra. Universidad Nacional de Córdoba. Facultad de Ciencias Exactas Físicas y Naturales. Centro de Investigaciones en Ciencias de la Tierra; Argentina. University of Wisconsin; Estados UnidosFil: Penprase, Shanti B.. University of Minnesota; Estados UnidosFil: Van Wyk de Vries, Maximillian S.. University of Minnesota; Estados Unidos. University of Oxford; Reino Unido. University of Liverpool; Reino Unido. University of Nottingham; Estados Unidos. University of Cambridge; Reino UnidoFil: Wickert, Andrew D.. University of Minnesota; Estados Unidos. Deutsches GeoForschungsZentrum; AlemaniaFil: Jones, Andrew G.. University of Wisconsin; Estados UnidosFil: Marcott, Shaun A.. University of Wisconsin; Estados UnidosFil: Strelin, Jorge Adrián. Consejo Nacional de Investigaciones Científicas y Técnicas. Centro Científico Tecnológico Conicet - Córdoba. Centro de Investigaciones en Ciencias de la Tierra. Universidad Nacional de Córdoba. Facultad de Ciencias Exactas Físicas y Naturales. Centro de Investigaciones en Ciencias de la Tierra; Argentina. Ministerio de Relaciones Exteriores, Comercio Interno y Culto. Dirección Nacional del Antártico. Instituto Antártico Argentino; ArgentinaFil: Martini, Mateo Antonio. Consejo Nacional de Investigaciones Científicas y Técnicas. Centro Científico Tecnológico Conicet - Córdoba. Centro de Investigaciones en Ciencias de la Tierra. Universidad Nacional de Córdoba. Facultad de Ciencias Exactas Físicas y Naturales. Centro de Investigaciones en Ciencias de la Tierra; ArgentinaFil: Rittenour, Tammy M.. State University of Utah; Estados UnidosFil: Brignone, Guido. Universidad Nacional de Córdoba. Facultad de Ciencias Exactas, Físicas y Naturales; ArgentinaFil: Shapley, Mark D.. University of Minnesota; Estados UnidosFil: Ito, Emi. University of Minnesota; Estados UnidosFil: MacGregor, Kelly R.. Macalester Collage; Estados UnidosFil: Caffee, Marc W.. Purdue University; Estados UnidosCopernicus Publications2024-08info:eu-repo/semantics/articleinfo:eu-repo/semantics/publishedVersionhttp://purl.org/coar/resource_type/c_6501info:ar-repo/semantics/articuloapplication/pdfapplication/pdfhttp://hdl.handle.net/11336/260914Romero, Matias; Penprase, Shanti B.; Van Wyk de Vries, Maximillian S.; Wickert, Andrew D.; Jones, Andrew G.; et al.; Late Quaternary glacial maxima in southern Patagonia: insights from the Lago Argentino glacier lobe; Copernicus Publications; Climate of the Past; 20; 8; 8-2024; 1861-18831814-93241814-9332CONICET DigitalCONICETenginfo:eu-repo/semantics/altIdentifier/url/https://cp.copernicus.org/articles/20/1861/2024/info:eu-repo/semantics/altIdentifier/doi/10.5194/cp-20-1861-2024info:eu-repo/semantics/openAccesshttps://creativecommons.org/licenses/by/2.5/ar/reponame:CONICET Digital (CONICET)instname:Consejo Nacional de Investigaciones Científicas y Técnicas2025-09-29T09:33:56Zoai:ri.conicet.gov.ar:11336/260914instacron:CONICETInstitucionalhttp://ri.conicet.gov.ar/Organismo científico-tecnológicoNo correspondehttp://ri.conicet.gov.ar/oai/requestdasensio@conicet.gov.ar; lcarlino@conicet.gov.arArgentinaNo correspondeNo correspondeNo correspondeopendoar:34982025-09-29 09:33:57.075CONICET Digital (CONICET) - Consejo Nacional de Investigaciones Científicas y Técnicasfalse
dc.title.none.fl_str_mv Late Quaternary glacial maxima in southern Patagonia: insights from the Lago Argentino glacier lobe
title Late Quaternary glacial maxima in southern Patagonia: insights from the Lago Argentino glacier lobe
spellingShingle Late Quaternary glacial maxima in southern Patagonia: insights from the Lago Argentino glacier lobe
Romero, Matias
COSMOGENIC DATING
MORAINES
WESTERLIES
PALEOCLIMATE
title_short Late Quaternary glacial maxima in southern Patagonia: insights from the Lago Argentino glacier lobe
title_full Late Quaternary glacial maxima in southern Patagonia: insights from the Lago Argentino glacier lobe
title_fullStr Late Quaternary glacial maxima in southern Patagonia: insights from the Lago Argentino glacier lobe
title_full_unstemmed Late Quaternary glacial maxima in southern Patagonia: insights from the Lago Argentino glacier lobe
title_sort Late Quaternary glacial maxima in southern Patagonia: insights from the Lago Argentino glacier lobe
dc.creator.none.fl_str_mv Romero, Matias
Penprase, Shanti B.
Van Wyk de Vries, Maximillian S.
Wickert, Andrew D.
Jones, Andrew G.
Marcott, Shaun A.
Strelin, Jorge Adrián
Martini, Mateo Antonio
Rittenour, Tammy M.
Brignone, Guido
Shapley, Mark D.
Ito, Emi
MacGregor, Kelly R.
Caffee, Marc W.
author Romero, Matias
author_facet Romero, Matias
Penprase, Shanti B.
Van Wyk de Vries, Maximillian S.
Wickert, Andrew D.
Jones, Andrew G.
Marcott, Shaun A.
Strelin, Jorge Adrián
Martini, Mateo Antonio
Rittenour, Tammy M.
Brignone, Guido
Shapley, Mark D.
Ito, Emi
MacGregor, Kelly R.
Caffee, Marc W.
author_role author
author2 Penprase, Shanti B.
Van Wyk de Vries, Maximillian S.
Wickert, Andrew D.
Jones, Andrew G.
Marcott, Shaun A.
Strelin, Jorge Adrián
Martini, Mateo Antonio
Rittenour, Tammy M.
Brignone, Guido
Shapley, Mark D.
Ito, Emi
MacGregor, Kelly R.
Caffee, Marc W.
author2_role author
author
author
author
author
author
author
author
author
author
author
author
author
dc.subject.none.fl_str_mv COSMOGENIC DATING
MORAINES
WESTERLIES
PALEOCLIMATE
topic COSMOGENIC DATING
MORAINES
WESTERLIES
PALEOCLIMATE
purl_subject.fl_str_mv https://purl.org/becyt/ford/1.5
https://purl.org/becyt/ford/1
dc.description.none.fl_txt_mv Determining the timing and extent of Quaternary glaciations around the globe is critical to understanding the drivers behind climate change and glacier fluctuations. Evidence from the southern mid-latitudes indicates that local glacial maxima preceded the global Last Glacial Maximum (LGM), implying that feedbacks in the climate system or ice dynamics played a role beyond the underlying orbital forcings. To shed light on these processes, we investigated the glacial landforms shaped and deposited by the Lago Argentino glacier (50° S), an outlet lobe of the former Patagonian Ice Sheet, in southern Argentina. We mapped geomorphological features on the landscape and dated moraine boulders and outwash sediments using 10Be cosmogenic nuclides and feldspar infrared stimulated luminescence (IRSL) to constrain the chronology of glacial advance and retreat. We report that the Lago Argentino glacier lobe reached more extensive limits prior to the global LGM, advancing during the middle to late Pleistocene between 243–132 ka and during Marine Isotope Stage 3 (MIS 3), culminating at 44.5 ± 8.0 and at 36.6 ± 1.0 ka. Our results indicate that the most extensive advance of the last glacial cycle occurred during MIS 3, and we hypothesize that this was a result of longer and colder winters, as well as increased precipitation delivered by a latitudinal migration of the Southern Westerly Winds belt, highlighting the role of local and regional climate feedbacks in modulating ice mass changes in the southern mid-latitudes.
Fil: Romero, Matias. Consejo Nacional de Investigaciones Científicas y Técnicas. Centro Científico Tecnológico Conicet - Córdoba. Centro de Investigaciones en Ciencias de la Tierra. Universidad Nacional de Córdoba. Facultad de Ciencias Exactas Físicas y Naturales. Centro de Investigaciones en Ciencias de la Tierra; Argentina. University of Wisconsin; Estados Unidos
Fil: Penprase, Shanti B.. University of Minnesota; Estados Unidos
Fil: Van Wyk de Vries, Maximillian S.. University of Minnesota; Estados Unidos. University of Oxford; Reino Unido. University of Liverpool; Reino Unido. University of Nottingham; Estados Unidos. University of Cambridge; Reino Unido
Fil: Wickert, Andrew D.. University of Minnesota; Estados Unidos. Deutsches GeoForschungsZentrum; Alemania
Fil: Jones, Andrew G.. University of Wisconsin; Estados Unidos
Fil: Marcott, Shaun A.. University of Wisconsin; Estados Unidos
Fil: Strelin, Jorge Adrián. Consejo Nacional de Investigaciones Científicas y Técnicas. Centro Científico Tecnológico Conicet - Córdoba. Centro de Investigaciones en Ciencias de la Tierra. Universidad Nacional de Córdoba. Facultad de Ciencias Exactas Físicas y Naturales. Centro de Investigaciones en Ciencias de la Tierra; Argentina. Ministerio de Relaciones Exteriores, Comercio Interno y Culto. Dirección Nacional del Antártico. Instituto Antártico Argentino; Argentina
Fil: Martini, Mateo Antonio. Consejo Nacional de Investigaciones Científicas y Técnicas. Centro Científico Tecnológico Conicet - Córdoba. Centro de Investigaciones en Ciencias de la Tierra. Universidad Nacional de Córdoba. Facultad de Ciencias Exactas Físicas y Naturales. Centro de Investigaciones en Ciencias de la Tierra; Argentina
Fil: Rittenour, Tammy M.. State University of Utah; Estados Unidos
Fil: Brignone, Guido. Universidad Nacional de Córdoba. Facultad de Ciencias Exactas, Físicas y Naturales; Argentina
Fil: Shapley, Mark D.. University of Minnesota; Estados Unidos
Fil: Ito, Emi. University of Minnesota; Estados Unidos
Fil: MacGregor, Kelly R.. Macalester Collage; Estados Unidos
Fil: Caffee, Marc W.. Purdue University; Estados Unidos
description Determining the timing and extent of Quaternary glaciations around the globe is critical to understanding the drivers behind climate change and glacier fluctuations. Evidence from the southern mid-latitudes indicates that local glacial maxima preceded the global Last Glacial Maximum (LGM), implying that feedbacks in the climate system or ice dynamics played a role beyond the underlying orbital forcings. To shed light on these processes, we investigated the glacial landforms shaped and deposited by the Lago Argentino glacier (50° S), an outlet lobe of the former Patagonian Ice Sheet, in southern Argentina. We mapped geomorphological features on the landscape and dated moraine boulders and outwash sediments using 10Be cosmogenic nuclides and feldspar infrared stimulated luminescence (IRSL) to constrain the chronology of glacial advance and retreat. We report that the Lago Argentino glacier lobe reached more extensive limits prior to the global LGM, advancing during the middle to late Pleistocene between 243–132 ka and during Marine Isotope Stage 3 (MIS 3), culminating at 44.5 ± 8.0 and at 36.6 ± 1.0 ka. Our results indicate that the most extensive advance of the last glacial cycle occurred during MIS 3, and we hypothesize that this was a result of longer and colder winters, as well as increased precipitation delivered by a latitudinal migration of the Southern Westerly Winds belt, highlighting the role of local and regional climate feedbacks in modulating ice mass changes in the southern mid-latitudes.
publishDate 2024
dc.date.none.fl_str_mv 2024-08
dc.type.none.fl_str_mv info:eu-repo/semantics/article
info:eu-repo/semantics/publishedVersion
http://purl.org/coar/resource_type/c_6501
info:ar-repo/semantics/articulo
format article
status_str publishedVersion
dc.identifier.none.fl_str_mv http://hdl.handle.net/11336/260914
Romero, Matias; Penprase, Shanti B.; Van Wyk de Vries, Maximillian S.; Wickert, Andrew D.; Jones, Andrew G.; et al.; Late Quaternary glacial maxima in southern Patagonia: insights from the Lago Argentino glacier lobe; Copernicus Publications; Climate of the Past; 20; 8; 8-2024; 1861-1883
1814-9324
1814-9332
CONICET Digital
CONICET
url http://hdl.handle.net/11336/260914
identifier_str_mv Romero, Matias; Penprase, Shanti B.; Van Wyk de Vries, Maximillian S.; Wickert, Andrew D.; Jones, Andrew G.; et al.; Late Quaternary glacial maxima in southern Patagonia: insights from the Lago Argentino glacier lobe; Copernicus Publications; Climate of the Past; 20; 8; 8-2024; 1861-1883
1814-9324
1814-9332
CONICET Digital
CONICET
dc.language.none.fl_str_mv eng
language eng
dc.relation.none.fl_str_mv info:eu-repo/semantics/altIdentifier/url/https://cp.copernicus.org/articles/20/1861/2024/
info:eu-repo/semantics/altIdentifier/doi/10.5194/cp-20-1861-2024
dc.rights.none.fl_str_mv info:eu-repo/semantics/openAccess
https://creativecommons.org/licenses/by/2.5/ar/
eu_rights_str_mv openAccess
rights_invalid_str_mv https://creativecommons.org/licenses/by/2.5/ar/
dc.format.none.fl_str_mv application/pdf
application/pdf
dc.publisher.none.fl_str_mv Copernicus Publications
publisher.none.fl_str_mv Copernicus Publications
dc.source.none.fl_str_mv reponame:CONICET Digital (CONICET)
instname:Consejo Nacional de Investigaciones Científicas y Técnicas
reponame_str CONICET Digital (CONICET)
collection CONICET Digital (CONICET)
instname_str Consejo Nacional de Investigaciones Científicas y Técnicas
repository.name.fl_str_mv CONICET Digital (CONICET) - Consejo Nacional de Investigaciones Científicas y Técnicas
repository.mail.fl_str_mv dasensio@conicet.gov.ar; lcarlino@conicet.gov.ar
_version_ 1844613047709073408
score 13.070432

Publicaciones similares