Late Quaternary deglaciation and climate history of the Larsemann Hills (East Antarctica)

The Late Quaternary climate history of the Larsemann Hills has been reconstructed using siliceous microfossils (diatoms, chrysophytes and silicoflagellates) in sediment cores extracted from three isolation lakes. Results show that the western peninsula, Stornes, and offshore islands were ice-covered...

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Bibliographic Details
Published in:Journal of Quaternary Science
Main Authors: Verleyen, Elie, Hodgson, Dominic A., Sabbe, Koen, Vyverman, Wim
Format: Article in Journal/Newspaper
Language:unknown
Published: Wiley 2004
Subjects:
Online Access:http://nora.nerc.ac.uk/id/eprint/12509/
http://onlinelibrary.wiley.com/doi/10.1002/jqs.823/pdf