Exact(59)
As OSL ages from the terrace also show a time of deposition during MIS 5a ending at the MIS 5/4 transition, this supports the idea of temperate climatic conditions at the time of deposition.
In this region, V-shaped valleys with broad valley floors are prominent landscape features whose basic shape already existed prior to MIS 2. During MIS 2 the valley bottoms were infilled with fluvially reworked loess, today forming accumulation terraces.
The relative abundance of G. ruber at MIS 21.5 reaches 46%% in the Omma Formation and is higher than during MIS 47, 43, and 31 (Hoiles et al. 2012).
During that period, loess deposition took place during MIS 6/4 and 3. A multiphase pedocomplex that documents progressive climate transition from initially humid to arid conditions, could be placed into MIS 5, although we found striking temporal offset between the phase of most intense soil formation and the Last Interglacial climatic optimum.
The overlying lower pedocomplex experienced a complex genesis in a forest-steppe environment during MIS 9.
On the Swiss Plateau, glacial and glaciofluvial sediments deposited during MIS 2 are widespread.
Cooler, wetter, and more variable climatic conditions during MIS 3 and 2 led to increased channel and floodplain sediment supply.
In central areas of Northeast Siberia, several vegetation shifts from tundra to Dahurian larch forest attest to multiple climatic variations during MIS 3.
These caves are currently at sea level, but during MIS 3 faced an emerged coastal shelf with the shoreline as far as 5 km away at times.
The results indicate that abrupt climate oscillations during MIS 3 contributed to the decline of Neanderthal populations, notably because of habitat fragmentation.
Similar(1)
The fan experienced megaslides in late ∼MIS 6, 9 and during ∼MIS 11 12.
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