Russian Journal of Earth Sciences
Papers in press
The Late Weichselian Barents-Kara Ice Sheet:
In defense of a maximum reconstruction
M. G. Grosswald
Abstract
Extent of the Late Weichselian glaciation in western Arctic Russia is considered uncertain.
Grosswald’s model suggesting a continuous and long-lived Barents-Kara Ice Sheet centered on the Kara
Sea is questioned by advocates of “restricted” models, including the QUEEN Program members. Based on
sets of radiocarbon dates, they argue for a smaller and "diachronous" glaciation. However, the QUEEN
reconstruction is inconsistent with the record of ice flow across the Kara-Barents divide, as well as with
glacial geology of Kola Peninsula, Late Weichselian climate of the Arctic, Eurasian continental
paleohydrology, and the entire paleogeographic context of northern Eurasia. As for the sets of radiocarbon
dates, they appear erroneous (too old), these dating errors having been due to impeded ventilation of the
Pleistocene Arctic Ocean and to recycling and contamination of the sampled materials. Destructive impacts
of late-glacial ice-sheet surges and Eurasian megafloods upon the glacial sequences would also aggravate
the situation. Thus we (Grosswald and Hughes, 1995, 2002) choose to ignore the dates until these problems
are addressed. The rest of evidence supports extensive and continuous glaciation of the Barents-Kara
continental margin at the LGM. Our reconstructions depict the Barents-Kara Ice Sheet before and after
massive thawing of its bed that allows partial gravitational collapse of the overlying ice.