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 …

In this study, we evaluate the application of shallow (< 2.5 m) cosmogenic depth profiles in
bedrock to constrain long-term ice-burial and erosion histories. Using Markov Chain Monte …

Abstract Marine Isotope Stage (MIS) 4 (ca. 71–57 ka; within the Middle Weichselian
Substage) is considered a significant Pleistocene glaciation, but it remains poorly …

The Greenland Ice Sheet is a key contributor to contemporary global sea level rise, but its
long-term history and response to episodes of warming in Earth's geological past remain …

High-latitude regions store large amounts of carbon trapped by ice sheets, permafrost and
gas hydrates, yet joint evolution of these climate components is poorly understood. Covered …

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 …

We present the first comprehensive geodatabase of glacial cirques on the Iberian Peninsula,
excluding the Pyrenees. A total of 1519 cirques were mapped using Google Earth, guided …

Abstract The Norwegian Sea oceanic basins and prograded margins have developed since
NE Atlantic break-up in the earliest Eocene. Significant amounts of sediments were fed to …

Due to tectonic uplift in the Cenozoic and numerous shelf-wide glaciations during the
Quaternary,∼ 1–2.5 km of sedimentary overburden has been eroded from the Barents Sea …

Glacial groundwater is a conduit for geologic methane release in areas of glacier retreat on
Svalbard, representing a large, climate-sensitive source of the greenhouse gas. Methane …