%0 Journal Article %T The deglaciation of the Americas during the Last Glacial Termination %+ 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) %+ Laboratoire de Glaciologie [Bruxelles] %+ University at Buffalo [SUNY] (SUNY Buffalo) %+ University of Maine %+ University of Northern Iowa (UNI) %+ University of Edinburgh %+ Laboratoire de géographie physique : Environnements Quaternaires et Actuels (LGP) %+ 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) %A Palacios, David %A Stokes, Chris %A Phillips, Fred %A Clague, John %A Alcalá-Reygosa, Jesús %A Andrés, Nuria %A Angel, Isandra %A Blard, Pierre-Henri %A Briner, Jason %A Hall, Brenda %A Dahms, Dennis %A Hein, Andrew %A Jomelli, Vincent %A Mark, Bryan %A Martini, Mateo %A Moreno, Patricio %A Riedel, Jon %A Sagredo, Esteban %A Stansell, Nathan %A Vázquez-Selem, Lorenzo %A Vuille, Mathias %A Ward, Dylan %< avec comité de lecture %@ 0012-8252 %J Earth-Science Reviews %I Elsevier %V 203 %P 103113 %8 2020-04 %D 2020 %R 10.1016/j.earscirev.2020.103113 %Z Environmental Sciences %Z Environmental Sciences/Global ChangesJournal articles %X 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 %G English %2 https://cnrs.hal.science/hal-02627368/document %2 https://cnrs.hal.science/hal-02627368/file/Palacios%20ESR%202020.pdf %L hal-02627368 %U https://cnrs.hal.science/hal-02627368 %~ SDE %~ INSU %~ UNIV-PARIS1 %~ CNRS %~ GIP-BE %~ UPEC %~ LGP %~ UNIV-LORRAINE %~ OTELO-UL %~ CRPG-UL %~ CONDORCET3 %~ CAMPUS-CONDORCET %~ TEST3-HALCNRS