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The Late-glacial, recorded in both cirques, ispartitioned in three distinct phases (LG1-3): an initial phase of moraine stabilization at 15.5 ± 2.0 ka withsubsequent deglaciation starting at ~14 ka (LG1), followed by a shift to marginal conditions for glaciationat 13.5 ± 2.0 ka (LG2), sustained by large amounts of wind-blown snow, despite regional warming.
The fluvial units preserved directly under the till of the southernmost Saalian ice yield an age of about 150 ka, and enable a correlation of the Drenthe stage to late MIS 6.... Alpes-Maritimes (France) and Liguria (Italy) area contains numerous prehistoric...
more EVOLUTION OF LARGE MAMMAL POPULATIONS IN WEST MEDITERRANEAN EUROPE DURING MIDDLE AND UPPER PLEISTOCENE.