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Medidas de las elevaciones pasadas de las capas de hielo en el interior de la Antártida Occidental Occidental

Ackert1, Barclay, Borns

  • 1Massachusetts Institute of Technology/Woods Hole Oceanographic Institution Joint Program, MS 25, Clark 419, Department of Marine Chemistry and Geochemistry, Woods Hole Oceanographic Institution, Woods Hole, MA 02543, USA. Department of Geology, State University of New York at Cortland, Cortland, NY 13045, USA. Institute for Quaternary Studies, Department of Computer Science, University of Maine, Orono, ME 04469, USA. Institute of Arctic and Alpine Research, University of Colorado, Boulder, CO 80309, USA. Department of Earth and Environmental Science, University of Pennsylvania, Philadelphia, PA 19104-6316, USA.

Science (New York, N.Y.)
|October 9, 1999
PubMed
Resumen

Las elevaciones superficiales de la capa de hielo de la Antártida Occidental se reconstruyeron utilizando depósitos de morrena. Esta investigación indica una contribución limitada al aumento del nivel del mar en el Holoceno temprano, excluyéndolo como la fuente principal de un gran pulso de agua de deshielo.

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