skip to main content
Idioma:
Primo Search
Clear Search Box
Search in: Busca Geral
Busca Avançada
Busca por Índices

The deglaciation of the Americas during the Last Glacial Termination

Palacios, David ; Stokes, Chris R. ; Phillips, Fred M. ; Clague, John J. ; Alcalá-Reygosa, Jesus ; Andrés, Nuria ; Angel, Isandra ; Blard, Pierre-Henri ; Briner, Jason P. ; Hall, Brenda L. ; Dahms, Dennis ; Hein, Andrew S. ; Jomelli, Vincent ; Mark, Bryan G. ; Martini, Mateo A. ; Moreno, Patricio ; Riedel, Jon ; Sagredo, Esteban ; Stansell, Nathan D. ; Vázquez-Selem, Lorenzo ; Vuille, Mathias ; Ward, Dylan J.

Earth-science reviews, 2020-04, Vol.203, p.103113, Article 103113 [Periódico revisado por pares]

Elsevier B.V

Texto completo disponível

Citações Citado por
  • Título:
    The deglaciation of the Americas during the Last Glacial Termination
  • Autor: Palacios, David ; Stokes, Chris R. ; Phillips, Fred M. ; Clague, John J. ; Alcalá-Reygosa, Jesus ; Andrés, Nuria ; Angel, Isandra ; Blard, Pierre-Henri ; Briner, Jason P. ; Hall, Brenda L. ; Dahms, Dennis ; Hein, Andrew S. ; Jomelli, Vincent ; Mark, Bryan G. ; Martini, Mateo A. ; Moreno, Patricio ; Riedel, Jon ; Sagredo, Esteban ; Stansell, Nathan D. ; Vázquez-Selem, Lorenzo ; Vuille, Mathias ; Ward, Dylan J.
  • Assuntos: Americas ; Deglaciation ; Environmental Sciences ; Glacial Chronology ; Global Changes ; Late Pleistocene ; Termination-I
  • É parte de: Earth-science reviews, 2020-04, Vol.203, p.103113, Article 103113
  • Descrição: 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 South America (Venezuela) during the Younger Dryas (12.9-11.7 ka), but glaciers in central and southern South America retreated during this period, except on the Altiplano where advances were driven by an increase in precipitation. Taken together, we suggest that there was a climate compensation effect, or ‘seesaw’, between the hemispheres, which affected not only marine currents and atmospheric circulation, but also the behavior of glaciers. This seesaw is consistent with the opposing behavior of many glaciers in the Northern and Southern Hemispheres.
  • Editor: Elsevier B.V
  • Idioma: Inglês
Links
Voltar para lista de resultados

  • Realização: ABCD-USP USP   Logos de Redes Sociais: Freepik

Buscando em bases de dados remotas. Favor aguardar.