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 …

Grounding-zone wedges (GZWs) are asymmetric sedimentary depocentres which form
through the rapid accumulation of glacigenic debris along a line-source at the grounding …

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 …

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 …

Glacimarine processes affect about 20% of the global ocean today, and this area expanded
considerably under cyclical full-glacial conditions during the Quaternary (Fig. 1)(Dowdeswell …

A comprehensive inventory of High Arctic cross-shelf troughs is compiled from International
Bathymetric Chart of the Arctic Ocean (IBCAO) bathymetric data (v. 3.0). The location of 75 …

The depositional history of the Storfjorden and Kveithola trough-mouth fans (TMFs) in the
northwestern Barents Sea has been investigated within two coordinated Spanish and Italian …

Abstract The marine-based Barents Sea Ice Sheet covered the polar continental shelf north
of Norway and western Russia during the Last Glacial Maximum. Initial ice sheet retreat …

Mud accumulates on continental shelves under a variety of environmental conditions and
results in a diverse formation of mud depocenters (MDCs). Their three-dimensional …

Our understanding of processes relating to the retreat of marine‐based ice sheets, such as
the West Antarctic Ice Sheet and tidewater‐terminating glaciers in Greenland today, is still …