The spread of anatomically modern humans (AMH) into Europe occurred when shifts in the
North Atlantic meridional overturning circulation triggered a series of large and abrupt …

While there are numerous hypotheses concerning glacial–interglacial environmental and
climatic regime shifts in the Arctic Ocean, a holistic view on the Northern Hemisphere's late …

The Eurasian ice-sheet complex (EISC) was the third largest ice mass during the Last
Glacial Maximum (LGM), after the Antarctic and North American ice sheets. Despite its …

A reconstruction of Holocene sea ice conditions in the Fram Strait provides insight into the
palaeoenvironmental and palaeoceanographic development of this climate sensitive area …

The last deglaciation was abruptly interrupted by a millennial-scale reversal to glacial
conditions, the Younger Dryas cold event. This cold interval has been connected to a …

Late Quaternary Environmental Change addresses the interaction between human agency
and other environmental factors in the landscapes, particularly of the temperate zone …

We closely compared high-resolution δ13C records of benthic foraminifera Cibicides
wuellerstorfi, a proxy for deep-water ventilation, with the Dansgaard–Oeschger temperature …

High‐resolution sediment cores from the Vøring Plateau, the North Iceland shelf, and the
East Greenland shelf have been studied to investigate the stability of major surface currents …

Two cores from the southwestern shelf and slope of Storfjorden, Svalbard, taken at 389 m
and 1485 m water depth have been analyzed for benthic and planktic foraminifera, oxygen …

At the western continental margin of the Barents Sea, 75° N, hemipelagic sediments provide
a record of Holocene climate change with a time resolution of 10–70 years. Planktic …