First characterization and dating of East Antarctic bedrock inclusion form subglacial Lake Vostok accretion ice

The Vostok (East Antarctica, 78°S, 106°E) ice core preserves, below the meteoric ice keeping the climatic memory of the last 420 000 years, ice formed by freezing of subglacial Lake Vostok water. This latter contains some bedrock fragments representing unique samples for the geological investigation...

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Bibliographic Details
Published in:Environmental Chemistry
Main Authors: DELMONTE, BARBARA, MAGGI, VALTER, Petit, J, Basile Doelsch, I, Lipenkov, V
Other Authors: Delmonte, B, Maggi, V
Format: Article in Journal/Newspaper
Language:English
Published: CSIRO PUBLISHING 2004
Subjects:
Antarctica
bedrock topography
bottom lakes
Antarctic
East Antarctica
Lake Vostok
Antarc*
ice core
Ice Sheet
Online Access:http://hdl.handle.net/10281/17861
https://doi.org/10.1071/EN04029
Description
Summary:The Vostok (East Antarctica, 78°S, 106°E) ice core preserves, below the meteoric ice keeping the climatic memory of the last 420 000 years, ice formed by freezing of subglacial Lake Vostok water. This latter contains some bedrock fragments representing unique samples for the geological investigation of the East Antarctic Plateau, covered by ∼2-4km of ice. The first geochemical ( 87 Sr/ 86 Sr versus 143 Nd/ 144 Nd) and mineralogical characterization of these inclusions as well as the dating of one of them (Nd model age on whole-rock sample) has given evidence for a Mid-Proterozoic age of the basement lying below the ice sheet, consistent with recent geophysical data. The geochemical characteristics of bedrock inclusions within the accreted ice zone are markedly different from those of the mineral dust of aeolian origin archived in the uppermost part of the Vostok ice core and originating from deflation of the Southern Hemisphere continents, and easily discriminates between the two contributions. © CSIRO 2004.

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