Geo-Marine Letters

, Volume 22, Issue 2, pp 51–59

No evidence for a Pleistocene collapse of the West Antarctic Ice Sheet from continental margin sediments recovered in the Amundsen Sea

Authors

  • Claus-Dieter Hillenbrand
    • Alfred Wegener Institute for Polar and Marine Research, P.O. Box 120161, 27515 Bremerhaven, Germany
  • Dieter K. Fütterer
    • Alfred Wegener Institute for Polar and Marine Research, P.O. Box 120161, 27515 Bremerhaven, Germany
  • Hannes Grobe
    • Alfred Wegener Institute for Polar and Marine Research, P.O. Box 120161, 27515 Bremerhaven, Germany
  • Thomas Frederichs
    • University of Bremen, Department of Geosciences, P.O. Box 330440, 28334 Bremen, Germany

DOI: 10.1007/s00367-002-0097-7

Cite this article as:
Hillenbrand, C., Fütterer, D.K., Grobe, H. et al. Geo-Mar Lett (2002) 22: 51. doi:10.1007/s00367-002-0097-7

Abstract.

Records of glaciomarine deposition recovered from the West Antarctic continental margin in the Amundsen Sea allow the reconstruction of the behaviour of the West Antarctic Ice Sheet (WAIS) in response to the natural climatic changes of the last 1.8 million years. Contents of gravel-sized and lithogenic components represent the input and redeposition of glaciogenic debris, whereas variations in the proportions of the calcareous sediment fraction reflect palaeoproductivity changes. All proxies, which are regarded as sensitive to a WAIS collapse, changed markedly during the global climatic cycles, but do not confirm a complete disintegration of the WAIS during the Pleistocene.

Ice-rafted debris Glaciomarine sedimentation Pleistocene West Antarctic Ice Sheet Amundsen Sea

Copyright information

© Springer-Verlag 2002