Uplift and erosion are complex phenomena in terms of their governing processes, precise
timing and exact magnitude. The intricate relationship between different geodynamic …

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 …

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 …

Seafloor methane release due to the thermal dissociation of gas hydrates is pervasive
across the continental margins of the Arctic Ocean. Furthermore, there is increasing …

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 study of contourite drifts is an increasingly used tool for understanding the climate
history of the oceans. In this paper we analyse two contourite drifts along the continental …

Submarine landslides are often characterized by a basal surface of rupture parallel to the
stratigraphy, in which downslope movement is initiated. However, little is known about the …

The values of δ 13 C in benthic foraminifera have been measured in a gas-hydrate-bearing
sediment core collected from an area of active methane venting on the Vestnesa Ridge …

Methane emissions from Arctic continental margins are increasing due to the negative effect
of global warming on ice sheet and permafrost stability, but dynamics and timescales of …

Gas transport through sediments to the seabed and seepage occurs via advection through
pores, faults, and fractures, and as solubility driven gas diffusion. The pore pressure gradient …