In situ cosmogenic 10Be–14C–26Al measurements from recently deglaciated bedrock as a new tool to decipher changes in Greenland Ice Sheet size
Greenland rock cores to trace ice's past melting
Deglaciation of the Greenland and Laurentide ice sheets interrupted by glacier advance during abrupt coolings
Greenland was nearly ice-free for extended periods during the Pleistocene
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