Holocene depositional environments and surface-level changes at Lake Fryxell, Antarctica

We report on Holocene surface-level variations of Lake Fryxell, Antarctica, as determined from multi-proxy analyses of 18 sediment cores. During this time accumulating sediments were predominantly aeolian sand with algal and carbonate laminae. Based on stratigraphy, mineralogy and diatom assemblages...

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Bibliographic Details
Published in:The Holocene
Main Authors: Whittaker, T. E., Hall, B. L., Hendy, Chris H., Spaulding, S. A.
Format: Article in Journal/Newspaper
Language:English
Published: Sage 2008
Subjects:
Online Access:https://hdl.handle.net/10289/8298
https://doi.org/10.1177/0959683608091797