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

Multiple ice age cycles spanning the last three million years have fundamentally transformed
the Arctic landscape. The cadence, intensity and pattern of this glacial modification underpin …

Unravelling past, large-scale ocean circulation patterns is crucial for deciphering the long-
term global paleoclimate. Here we apply numerical modelling to reconstruct the detailed …

High-latitude marine sediment archives may contain information about the configuration and
dynamics of former ice sheets, paleoclimate and the intensity of glacial erosion and uplift in …

The Cenozoic pre-glacial development of the southwestern Barents Sea is discussed, with
focus on the early to middle Cenozoic net erosion that was poorly constrained. From 2D and …

Here we present a high-resolution, continuous seismostratigraphic framework that for the
first time, connects the over 1,000 km long western Svalbard-Barents Sea margin and covers …

Here we present the first compilation of sediment volumes, sedimentation rates, and
chronology of Quaternary sediment packages along the entire marine margin of the …

Canyons and other sediment conduits are important components of the deep‐water
environment and are the main pathways for sediment transport from the shelf to the basin …

Sea ice is a critical component in the Arctic and global climate system, yet little is known
about its extent and variability during past warm intervals, such as the Pliocene (5.33–2.58 …

The morphological evolution of the Barents-Kara Shelf is a graphic example of how erosion
and glaciation reshape the Earth's surface. Decades of petroleum exploration sparked …