The evolution and dynamics of the last British–Irish Ice Sheet (BIIS) have hitherto largely
been reconstructed from onshore and shallow marine glacial geological and …

High resolution, multi-proxy records of ice-rafted debris (IRD) flux and provenance in the NE
Atlantic detail the development, variability and decline of marine margins of the last glacial …

Recent intensification of wind-driven upwelling of warm upper circumpolar deep water
(UCDW) has been linked to accelerated melting of West Antarctic ice shelves and glaciers …

Antarctica is one of the most vulnerable regions to climate change on Earth and studying the
past and present responses of this polar marine ecosystem to environmental change is a …

Published studies show that ice rafted debris (IRD) deposition preceding Heinrich (H) events
H1 and H2 in the NE Atlantic was derived from the NW European ice sheets (NWEIS) …

The dissolution of the delicate shells of sea butterflies, or pteropods, has epitomised
discussions regarding ecosystem vulnerability to ocean acidification over the last decade …

Environmental changes associated with the Paleocene–Eocene thermal maximum
(PETM,∼ 56Ma) have not yet been documented in detail from the North Sea Basin. Located …

Explanations of the glacial–interglacial variations in atmospheric pCO2 invoke a significant
role for the deep ocean in the storage of CO2. Deep-ocean density stratification has been …

In aquatic environments, plastic pollution occurs concomitantly with anthropogenic climate
stressors such as ocean acidification. Within the Southern Ocean, Antarctic krill (Euphausia …

Scarred shells of polar pteropod Limacina helicina collected from the Greenland Sea in
June 2012 reveal a history of damage, most likely failed predation, in earlier life stages …