Do Diatoms beneath the Greenland Ice Sheet Indicate Interglacials Warmer than Present?’
ABSTRACT. Basal sediment debris from the Greenland Ice Sheet was examined with the hope of recovering microfossils that could be used to determine and date changes in ice sheet size through time. Basal debris and debris-laden ice from the lower 18 m of the Camp Century ice core, northwest Greenland,...
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Format: | Text |
Language: | English |
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1985
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Online Access: | http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.565.7433 http://pubs.aina.ucalgary.ca/arctic/Arctic39-4-304.pdf |