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Fluctuation history of the interior East Antarctic Ice Sheet since mid-Pliocene

Published online by Cambridge University Press:  10 January 2008

Feixin Huang ,
Xiaohan Liu ,
Ping Kong ,
David Fink ,
Yitai Ju ,
Aimin Fang ,
Liangjun Yu ,
Xiaoli Li  and
Chunguang Na
Feixin Huang*
Affiliation:
Institute of Tibetan Plateau Research, Chinese Academy of Sciences, Beijing, 100085, China
Xiaohan Liu
Affiliation:
Institute of Tibetan Plateau Research, Chinese Academy of Sciences, Beijing, 100085, China
Ping Kong
Affiliation:
Institute of Geology and Geophysics, Chinese Academy of Sciences, Beijing, 100029, China
David Fink
Affiliation:
Australian Nuclear Science and Technology Organisation, Menai, NSW 2234, Australia
Yitai Ju
Affiliation:
Institute of Geology and Geophysics, Chinese Academy of Sciences, Beijing, 100029, China
Aimin Fang
Affiliation:
Institute of Geology and Geophysics, Chinese Academy of Sciences, Beijing, 100029, China
Liangjun Yu
Affiliation:
Institute of Geology and Geophysics, Chinese Academy of Sciences, Beijing, 100029, China
Xiaoli Li
Affiliation:
Institute of Geology and Geophysics, Chinese Academy of Sciences, Beijing, 100029, China
Chunguang Na
Affiliation:
Institute of Geology and Geophysics, Chinese Academy of Sciences, Beijing, 100029, China
*
*[email protected]
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Abstract

Cosmogenic 10Be and 26Al measurements from bedrock exposures in East Antarctica provide indications of how long the rock surface has been free from glacial cover. Samples from the crests of Zakharoff Ridge and Mount Harding, two typical nunataks in the Grove Mountains, show minimum 10Be ages of 2.00 ± 0.22 and 2.30 ± 0.26 Ma, respectively. These ages suggest that the crests were above the ice sheet at least since the Plio–Pleistocene boundary. Adopting a ‘reasonable’ erosion rate of 5–10 cm Ma-1 increases the exposure ages of these two samples to extend into the mid-Pliocene. The bedrock exposure ages steadily decrease with decreasing elevation on the two nunataks, which indicates ~200 m decrease of the ice sheet in the Grove Mountains since mid-Pliocene time. Seven higher elevation samples exhibit a simple exposure history, which indicates that the ice sheet in the Grove Mountains decreased only ~100 m over a period as long as 1–2 Ma. This suggests that the East Antarctic Ice Sheet (EAIS) was relatively stable during the Pliocene warm interval. Five lower elevation samples suggest a complex exposure history, and indicate that the maximum subsequent increase of the EAIS was only 100 m higher than the present ice surface. Considering the uncertainties, their total initial exposure and subsequent burial time could be later than mid-Pliocene, which may not conflict with the stable mid-Pliocene scenario.

Keywords

bedrockcosmogenicexposure ageGrove Mountainsstable
Type
Physical Sciences
Information
Antarctic Science , Volume 20 , Issue 2 , April 2008 , pp. 197 - 203
Copyright
Copyright © Antarctic Science Ltd 2008

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