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El último máximo glacial.

Peter U Clark1, Arthur S Dyke, Jeremy D Shakun

  • 1Department of Geosciences, Oregon State University, Corvallis, OR 97331, USA. clarkp@onid.orst.edu

Science (New York, N.Y.)
|August 8, 2009
PubMed
Resumen
Este resumen es generado por máquina.

El Último Máximo Glacial (LGM) se produjo entre hace 33.000 y 19.000 años, impulsado por los cambios climáticos. La deglaciación comenzó hace unos 19.000 años, lo que llevó al aumento del nivel del mar.

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Área de la Ciencia:

  • Paleoclimatología Paleoclimatología
  • Geología Cuaternaria Geología Cuaternaria
  • Glaciología glaciología.

Sus antecedentes:

  • El momento y la extensión del Último Máximo Glacial (LGM) son cruciales para comprender la dinámica climática pasada y el comportamiento de las capas de hielo.
  • Estudios anteriores han proporcionado estimaciones para el tiempo de LGM, pero se necesita una síntesis completa utilizando un gran conjunto de datos.

Objetivo del estudio:

  • Para limitar con precisión el momento de la LGM y la posterior deglaciación utilizando una gran compilación de datos geocronológicos.
  • Investigar la relación entre los forzamientos climáticos y la extensión de la capa de hielo durante el LGM.

Principales métodos:

  • Análisis de las edades 5704 de radiocarbono (14C), berilio-10 (10Be) y helio-3 (3He).
  • El intervalo de datación abarca desde hace 10.000 hasta 50.000 años (10-50 ka).

Principales resultados:

  • Las capas de hielo alcanzaron su extensión máxima entre 33.0 y 26.5 ka en respuesta a la disminución de la insolación del verano del norte, a las temperaturas más frías de la superficie del mar del Pacífico y al menor CO2 atmosférico.
  • Las capas de hielo se mantuvieron cerca de sus posiciones LGM de 26.5 a 19-20 ka.
  • La deglaciación del hemisferio norte se inició alrededor de 19-20 ka, vinculada al aumento de la insolación del verano del norte y el subsiguiente aumento del nivel del mar.
  • La deglaciación de la capa de hielo de la Antártida Occidental comenzó entre 14 y 15 ka, contribuyendo a un aumento significativo del nivel del mar alrededor de 14.5 ka.

Conclusiones:

  • El LGM fue un período dinámico con distintas fases de crecimiento, estabilidad y descomposición de la capa de hielo.
  • Los forzamientos climáticos, en particular los cambios de insolación, jugaron un papel clave en la conducción de LGM y el tiempo de deglaciación.
  • El estudio refina la línea de tiempo del LGM y la desglaciación, mejorando nuestra comprensión de la respuesta del sistema climático de la Tierra al forzamiento.