Short Note: New marine core record of Late Pleistocene glaciation history, Rauer Group, East Antarctica

The evolution of the East Antarctic Ice Sheet (EAIS) during the Late Quaternary is poorly known, partly because some regions, such as the Prydz Bay vicinity, indicate significant variability in the glaciation patterns (e.g. Domack et al. 1998, Zwartz et al. 1998, Hodgson et al. 2005).

Bibliographic Details
Published in:Antarctic Science
Main Authors: Berg, Sonja, Wagner, Bernd, White, Duanne A., Cremer, Holger, Bennike, Ole, Melles, Martin
Format: Article in Journal/Newspaper
Language:English
Published: Cambridge University Press (CUP) 2009
Subjects:
Geology
Ecology, Evolution, Behavior and Systematics
Oceanography
Antarctic
East Antarctica
Prydz Bay
East Antarctic Ice Sheet
Hodgson
Rauer Group
Antarc*
Antarctic Science
Antarctica
Ice Sheet
Online Access:http://dx.doi.org/10.1017/s0954102009001886
https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0954102009001886
Description
Summary:The evolution of the East Antarctic Ice Sheet (EAIS) during the Late Quaternary is poorly known, partly because some regions, such as the Prydz Bay vicinity, indicate significant variability in the glaciation patterns (e.g. Domack et al. 1998, Zwartz et al. 1998, Hodgson et al. 2005).

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