The last deglaciation of the marine parts of the Eurasian Ice Sheet was driven mainly by oceanic temperature change in the north and by changes in solar insolation in the south, based on a reconstruction of the marine parts of the Eurasian Ice Sheet and Nordic Seas palaeoceanographic data.
- Hans Petter Sejrup
- Berit Oline Hjelstuen
- Alun Hubbard
