The deglaciation of the Americas during the Last Glacial Termination

International audience This paper reviews current understanding of deglaciation in North, Central and South America from the Last Glacial Maximum to the beginning of the Holocene. Together with paleoclimatic and paleoceanographic data, we compare and contrast the pace of deglaciation and the respons...

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Published in:Earth-Science Reviews
Main Authors: Palacios, David, Stokes, Chris, Phillips, Fred, Clague, John, Alcalá-Reygosa, Jesús, Andrés, Nuria, Angel, Isandra, Blard, Pierre-Henri, Briner, Jason, Hall, Brenda, Dahms, Dennis, Hein, Andrew, Jomelli, Vincent, Mark, Bryan, Martini, Mateo, Moreno, Patricio, Riedel, Jon, Sagredo, Esteban, Stansell, Nathan, Vázquez-Selem, Lorenzo, Vuille, Mathias, Ward, Dylan
Other Authors: Universidad Complutense de Madrid = Complutense University of Madrid Madrid (UCM), Durham University, New Mexico Institute of Mining and Technology New Mexico Tech (NMT), Simon Fraser University (SFU.ca), Universidad Nacional Autónoma de México = National Autonomous University of Mexico (UNAM), Universidad Simon Bolivar (USB), Centre de Recherches Pétrographiques et Géochimiques (CRPG), Institut national des sciences de l'Univers (INSU - CNRS)-Université de Lorraine (UL)-Centre National de la Recherche Scientifique (CNRS), Laboratoire de Glaciologie Bruxelles, Université libre de Bruxelles (ULB), University at Buffalo SUNY (SUNY Buffalo), State University of New York (SUNY), University of Maine, University of Northern Iowa (UNI), University of Edinburgh, Laboratoire de géographie physique : Environnements Quaternaires et Actuels (LGP), Université Paris 1 Panthéon-Sorbonne (UP1)-Université Paris-Est Créteil Val-de-Marne - Paris 12 (UPEC UP12)-Centre National de la Recherche Scientifique (CNRS), Ohio State University Columbus (OSU), Universidad de Chile = University of Chile Santiago (UCHILE), Pontificia Universidad Católica de Chile (UC), Consejo Nacional de Investigaciones Científicas y Técnicas Buenos Aires (CONICET), National Park Service, Northern Illinois University, University at Albany SUNY, University of Cincinnati (UC)
Format: Article in Journal/Newspaper
Language:English
Published: HAL CCSD 2020
Subjects:
Online Access:https://hal-cnrs.archives-ouvertes.fr/hal-02627368
https://hal-cnrs.archives-ouvertes.fr/hal-02627368/document
https://hal-cnrs.archives-ouvertes.fr/hal-02627368/file/Palacios%20ESR%202020.pdf
https://doi.org/10.1016/j.earscirev.2020.103113
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record_format openpolar
institution Open Polar
collection Université de Nantes: HAL-UNIV-NANTES
op_collection_id ftunivnantes
language English
topic [SDE]Environmental Sciences
[SDE.MCG]Environmental Sciences/Global Changes
spellingShingle [SDE]Environmental Sciences
[SDE.MCG]Environmental Sciences/Global Changes
Palacios, David
Stokes, Chris
Phillips, Fred
Clague, John
Alcalá-Reygosa, Jesús
Andrés, Nuria
Angel, Isandra
Blard, Pierre-Henri
Briner, Jason
Hall, Brenda
Dahms, Dennis
Hein, Andrew
Jomelli, Vincent
Mark, Bryan
Martini, Mateo
Moreno, Patricio
Riedel, Jon
Sagredo, Esteban
Stansell, Nathan
Vázquez-Selem, Lorenzo
Vuille, Mathias
Ward, Dylan
The deglaciation of the Americas during the Last Glacial Termination
topic_facet [SDE]Environmental Sciences
[SDE.MCG]Environmental Sciences/Global Changes
description International audience This paper reviews current understanding of deglaciation in North, Central and South America from the Last Glacial Maximum to the beginning of the Holocene. Together with paleoclimatic and paleoceanographic data, we compare and contrast the pace of deglaciation and the response of glaciers to major climate events. During the Global Last Glacial Maximum (GLGM, 26.5-19 ka), average temperatures decreased 4°to 8°C in the Americas, but precipitation varied strongly throughout this large region. Many glaciers in North and Central America achieved their maximum extent during the GLGM, whereas others advanced even farther during the subsequent Heinrich Stadial 1 (HS-1). Glaciers in the Andes also expanded during the GLGM, but that advance was not the largest, except on Tierra del Fuego. HS-1 (17.5-14.6 ka) was a time of general glacier thickening and advance throughout most of North and Central America, and in the tropical Andes; however, glaciers in the temperate and subpolar Andes thinned and retreated during this period. During the Bølling-Allerød interstadial (B-A, 14.6-12.9 ka), glaciers retreated throughout North and Central America and, in some cases, completely disappeared. Many glaciers advanced during the Antarctic Cold Reversal (ACR, 14.6-12.9 ka) in the tropical Andes and Patagonia. There were small advances of glaciers in North America, Central America and in northern
author2 Universidad Complutense de Madrid = Complutense University of Madrid Madrid (UCM)
Durham University
New Mexico Institute of Mining and Technology New Mexico Tech (NMT)
Simon Fraser University (SFU.ca)
Universidad Nacional Autónoma de México = National Autonomous University of Mexico (UNAM)
Universidad Simon Bolivar (USB)
Centre de Recherches Pétrographiques et Géochimiques (CRPG)
Institut national des sciences de l'Univers (INSU - CNRS)-Université de Lorraine (UL)-Centre National de la Recherche Scientifique (CNRS)
Laboratoire de Glaciologie Bruxelles
Université libre de Bruxelles (ULB)
University at Buffalo SUNY (SUNY Buffalo)
State University of New York (SUNY)
University of Maine
University of Northern Iowa (UNI)
University of Edinburgh
Laboratoire de géographie physique : Environnements Quaternaires et Actuels (LGP)
Université Paris 1 Panthéon-Sorbonne (UP1)-Université Paris-Est Créteil Val-de-Marne - Paris 12 (UPEC UP12)-Centre National de la Recherche Scientifique (CNRS)
Ohio State University Columbus (OSU)
Universidad de Chile = University of Chile Santiago (UCHILE)
Pontificia Universidad Católica de Chile (UC)
Consejo Nacional de Investigaciones Científicas y Técnicas Buenos Aires (CONICET)
National Park Service
Northern Illinois University
University at Albany SUNY
University of Cincinnati (UC)
format Article in Journal/Newspaper
author Palacios, David
Stokes, Chris
Phillips, Fred
Clague, John
Alcalá-Reygosa, Jesús
Andrés, Nuria
Angel, Isandra
Blard, Pierre-Henri
Briner, Jason
Hall, Brenda
Dahms, Dennis
Hein, Andrew
Jomelli, Vincent
Mark, Bryan
Martini, Mateo
Moreno, Patricio
Riedel, Jon
Sagredo, Esteban
Stansell, Nathan
Vázquez-Selem, Lorenzo
Vuille, Mathias
Ward, Dylan
author_facet Palacios, David
Stokes, Chris
Phillips, Fred
Clague, John
Alcalá-Reygosa, Jesús
Andrés, Nuria
Angel, Isandra
Blard, Pierre-Henri
Briner, Jason
Hall, Brenda
Dahms, Dennis
Hein, Andrew
Jomelli, Vincent
Mark, Bryan
Martini, Mateo
Moreno, Patricio
Riedel, Jon
Sagredo, Esteban
Stansell, Nathan
Vázquez-Selem, Lorenzo
Vuille, Mathias
Ward, Dylan
author_sort Palacios, David
title The deglaciation of the Americas during the Last Glacial Termination
title_short The deglaciation of the Americas during the Last Glacial Termination
title_full The deglaciation of the Americas during the Last Glacial Termination
title_fullStr The deglaciation of the Americas during the Last Glacial Termination
title_full_unstemmed The deglaciation of the Americas during the Last Glacial Termination
title_sort deglaciation of the americas during the last glacial termination
publisher HAL CCSD
publishDate 2020
url https://hal-cnrs.archives-ouvertes.fr/hal-02627368
https://hal-cnrs.archives-ouvertes.fr/hal-02627368/document
https://hal-cnrs.archives-ouvertes.fr/hal-02627368/file/Palacios%20ESR%202020.pdf
https://doi.org/10.1016/j.earscirev.2020.103113
geographic Antarctic
Patagonia
The Antarctic
geographic_facet Antarctic
Patagonia
The Antarctic
genre Antarc*
Antarctic
Tierra del Fuego
genre_facet Antarc*
Antarctic
Tierra del Fuego
op_source ISSN: 0012-8252
Earth-Science Reviews
https://hal-cnrs.archives-ouvertes.fr/hal-02627368
Earth-Science Reviews, 2020, 203, pp.103113. ⟨10.1016/j.earscirev.2020.103113⟩
op_relation info:eu-repo/semantics/altIdentifier/doi/10.1016/j.earscirev.2020.103113
hal-02627368
https://hal-cnrs.archives-ouvertes.fr/hal-02627368
https://hal-cnrs.archives-ouvertes.fr/hal-02627368/document
https://hal-cnrs.archives-ouvertes.fr/hal-02627368/file/Palacios%20ESR%202020.pdf
doi:10.1016/j.earscirev.2020.103113
op_rights info:eu-repo/semantics/OpenAccess
op_doi https://doi.org/10.1016/j.earscirev.2020.103113
container_title Earth-Science Reviews
container_volume 203
container_start_page 103113
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spelling ftunivnantes:oai:HAL:hal-02627368v1 2023-05-15T13:30:51+02:00 The deglaciation of the Americas during the Last Glacial Termination Palacios, David Stokes, Chris Phillips, Fred Clague, John Alcalá-Reygosa, Jesús Andrés, Nuria Angel, Isandra Blard, Pierre-Henri Briner, Jason Hall, Brenda Dahms, Dennis Hein, Andrew Jomelli, Vincent Mark, Bryan Martini, Mateo Moreno, Patricio Riedel, Jon Sagredo, Esteban Stansell, Nathan Vázquez-Selem, Lorenzo Vuille, Mathias Ward, Dylan Universidad Complutense de Madrid = Complutense University of Madrid Madrid (UCM) Durham University New Mexico Institute of Mining and Technology New Mexico Tech (NMT) Simon Fraser University (SFU.ca) Universidad Nacional Autónoma de México = National Autonomous University of Mexico (UNAM) Universidad Simon Bolivar (USB) Centre de Recherches Pétrographiques et Géochimiques (CRPG) Institut national des sciences de l'Univers (INSU - CNRS)-Université de Lorraine (UL)-Centre National de la Recherche Scientifique (CNRS) Laboratoire de Glaciologie Bruxelles Université libre de Bruxelles (ULB) University at Buffalo SUNY (SUNY Buffalo) State University of New York (SUNY) University of Maine University of Northern Iowa (UNI) University of Edinburgh Laboratoire de géographie physique : Environnements Quaternaires et Actuels (LGP) Université Paris 1 Panthéon-Sorbonne (UP1)-Université Paris-Est Créteil Val-de-Marne - Paris 12 (UPEC UP12)-Centre National de la Recherche Scientifique (CNRS) Ohio State University Columbus (OSU) Universidad de Chile = University of Chile Santiago (UCHILE) Pontificia Universidad Católica de Chile (UC) Consejo Nacional de Investigaciones Científicas y Técnicas Buenos Aires (CONICET) National Park Service Northern Illinois University University at Albany SUNY University of Cincinnati (UC) 2020-04 https://hal-cnrs.archives-ouvertes.fr/hal-02627368 https://hal-cnrs.archives-ouvertes.fr/hal-02627368/document https://hal-cnrs.archives-ouvertes.fr/hal-02627368/file/Palacios%20ESR%202020.pdf https://doi.org/10.1016/j.earscirev.2020.103113 en eng HAL CCSD Elsevier info:eu-repo/semantics/altIdentifier/doi/10.1016/j.earscirev.2020.103113 hal-02627368 https://hal-cnrs.archives-ouvertes.fr/hal-02627368 https://hal-cnrs.archives-ouvertes.fr/hal-02627368/document https://hal-cnrs.archives-ouvertes.fr/hal-02627368/file/Palacios%20ESR%202020.pdf doi:10.1016/j.earscirev.2020.103113 info:eu-repo/semantics/OpenAccess ISSN: 0012-8252 Earth-Science Reviews https://hal-cnrs.archives-ouvertes.fr/hal-02627368 Earth-Science Reviews, 2020, 203, pp.103113. ⟨10.1016/j.earscirev.2020.103113⟩ [SDE]Environmental Sciences [SDE.MCG]Environmental Sciences/Global Changes info:eu-repo/semantics/article Journal articles 2020 ftunivnantes https://doi.org/10.1016/j.earscirev.2020.103113 2023-03-08T03:32:46Z International audience This paper reviews current understanding of deglaciation in North, Central and South America from the Last Glacial Maximum to the beginning of the Holocene. Together with paleoclimatic and paleoceanographic data, we compare and contrast the pace of deglaciation and the response of glaciers to major climate events. During the Global Last Glacial Maximum (GLGM, 26.5-19 ka), average temperatures decreased 4°to 8°C in the Americas, but precipitation varied strongly throughout this large region. Many glaciers in North and Central America achieved their maximum extent during the GLGM, whereas others advanced even farther during the subsequent Heinrich Stadial 1 (HS-1). Glaciers in the Andes also expanded during the GLGM, but that advance was not the largest, except on Tierra del Fuego. HS-1 (17.5-14.6 ka) was a time of general glacier thickening and advance throughout most of North and Central America, and in the tropical Andes; however, glaciers in the temperate and subpolar Andes thinned and retreated during this period. During the Bølling-Allerød interstadial (B-A, 14.6-12.9 ka), glaciers retreated throughout North and Central America and, in some cases, completely disappeared. Many glaciers advanced during the Antarctic Cold Reversal (ACR, 14.6-12.9 ka) in the tropical Andes and Patagonia. There were small advances of glaciers in North America, Central America and in northern Article in Journal/Newspaper Antarc* Antarctic Tierra del Fuego Université de Nantes: HAL-UNIV-NANTES Antarctic Patagonia The Antarctic Earth-Science Reviews 203 103113