hdl:10013/epic.37753
publisher:10.1017/S0954102011000320

Provenance changes between recent and glacial-time sediments in the Amundsen Sea embayment, West Antarctica: clay mineral assemblage evidence


Ehrmann, W., Hillenbrand, C.-D., Smith, J. A., Graham, A. G. C., Kuhn, Gerhard ORCID: https://orcid.org/0000-0001-6069-7485 and Larter, R. D. ;
Contact
gerhard.kuhn [ at ] awi.de

Abstract


Item Type
Article
Authors
Ehrmann, W., Hillenbrand, C.-D., Smith, J. A., Graham, A. G. C., Kuhn, Gerhard ORCID: https://orcid.org/0000-0001-6069-7485 and Larter, R. D. ;
Divisions
AWI Organizations > Geosciences > Marine Geology and Paleontology
Programs
Helmholtz Research Programs > PACES I (2009-2013) > TOPIC 3: Lessons from the Past
Helmholtz Research Programs > PACES I (2009-2013) > TOPIC 3: Lessons from the Past > WP 3.1: Past Polar Climate and inter-hemispheric Coupling
Publication Status
Published
Eprint ID
24257
DOI 10.1017/S0954102011000320

Cite as
Ehrmann, W. , Hillenbrand, C. D. , Smith, J. A. , Graham, A. G. C. , Kuhn, G. and Larter, R. D. (2011): Provenance changes between recent and glacial-time sediments in the Amundsen Sea embayment, West Antarctica: clay mineral assemblage evidence , Antarctic Science. . doi: 10.1017/S0954102011000320


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