The Eurasian ice sheet complex (EISC) was the third largest ice mass during the Last
Glacial Maximum with a span of over 4500 km and responsible for around 20 m of eustatic …

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

We present a new time‐slice reconstruction of the Eurasian ice sheets (British–Irish,
Svalbard–Barents–Kara Seas and Scandinavian) documenting the spatial evolution of these …

Numerous articles have recently reported on gas seepage offshore Svalbard, because the
gas emission from these Arctic sediments was thought to result from gas hydrate …

Rapid sea-level rise caused by the collapse of large ice sheets is a threat to human
societies. In the last deglacial period, the rate of global sea-level rise peaked at more than 4 …

The cryosphere is an important component of global organic contaminant cycles. Snow is an
efficient scavenger of atmospheric organic pollutants while a seasonal snowpack, sea ice …

We present a sea-ice record from northern Greenland covering the past 10,000 years.
Multiyear sea ice reached a minimum between~ 8500 and 6000 years ago, when the limit of …

We synthesize the current understanding of glacier activity on Svalbard from the end of the
Late Pleistocene (12,000 yrs. before present) to the end of the Little Ice Age (c. 1920 AD) …

Data have been compiled from eleven sediment cores from 76° to 80° N on the western
Svalbard slope. The cores are from water depths between 630 and 1880m and show clear …

We compare six high-resolution Holocene, sediment cores along a S–N transect on the
Norwegian–Svalbard continental margin from ca 60° N to 77.4° N, northern North Atlantic …