hdl:10013/epic.33041
publisher:10.1016/j.margeo.2009.06.009

Clay mineral provenance of sediments in the southern Bellingshausen Sea reveals drainage changes of the West Antarctic Ice Sheet during the Late Quaternary


Hillenbrand, C.-D., Ehrmann, W., Larter, R. D., Benetti, S., Dowdeswell, J. A., O'Cofaigh, C. O., Graham, A. G. C. and Grobe, Hannes ORCID: https://orcid.org/0000-0002-4133-2218 ;
Contact
Hannes.Grobe [ at ] awi.de

Abstract


Item Type
Article
Authors
Hillenbrand, C.-D., Ehrmann, W., Larter, R. D., Benetti, S., Dowdeswell, J. A., O'Cofaigh, C. O., Graham, A. G. C. and Grobe, Hannes ORCID: https://orcid.org/0000-0002-4133-2218 ;
Divisions
AWI Organizations > Geosciences > Marine Geology and Paleontology
Programs
Helmholtz Research Programs > MARCOPOLI (2004-2008) > POL-MARCOPOLI
Helmholtz Research Programs > MARCOPOLI (2004-2008) > POL6-Earth climate variability since the Pliocene
Publication Status
Published
Eprint ID
19827
DOI 10.1016/j.margeo.2009.06.009

Cite as
Hillenbrand, C. D. , Ehrmann, W. , Larter, R. D. , Benetti, S. , Dowdeswell, J. A. , O'Cofaigh, C. O. , Graham, A. G. C. and Grobe, H. (2009): Clay mineral provenance of sediments in the southern Bellingshausen Sea reveals drainage changes of the West Antarctic Ice Sheet during the Late Quaternary , Marine Geology, 265 (1), pp. 1-18 . doi: 10.1016/j.margeo.2009.06.009


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Research Platforms
Vessels > Polarstern

Campaigns
ANT > XI > 3


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