The 12 — 21 cm higher
sea level stand during the MWP is likely the highest
sea level since the previous interglacial period 110,000 years ago, and was produced by an
extended period of warming, allowing time for glaciers and thermal expansion to
reach a climatic balance.
These authors postulated an
extended Barents
Sea Ice Sheet, the western part of the huge Eurasian Ice Sheet51, 55, that had reached the shelf edge causing polynya - like open - water conditions (triggered by strong katabatic winds) with phytoplankton and sea ice algae production, subglacial meltwater outflow and the deposition of suspended material on the slope at site PS2138 -
Sea Ice Sheet, the western part of the huge Eurasian Ice Sheet51, 55, that had
reached the shelf edge causing polynya - like open - water conditions (triggered by strong katabatic winds) with phytoplankton and
sea ice algae production, subglacial meltwater outflow and the deposition of suspended material on the slope at site PS2138 -
sea ice algae production, subglacial meltwater outflow and the deposition of suspended material on the slope at site PS2138 - 2.