AbstractWhile 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 Quaternary ice-sheet extent and their impact on ocean and sea-ice dynamics remains to be established. Here we aim to provide a step in this direction by presenting an overview of Arctic Ocean glacial history, based on the present state-of-the-art knowledge gained from field work and chronological studies, and with a specific focus on ice-sheet extent and environmental conditions during the Last Glacial Maximum (LGM). The maximum Quaternary extension of ice sheets is discussed and compared to LGM. We bring together recent results from the circum-Arctic cont...
The volume and areal extent of Arctic sea ice is rapidly declining, and to put that decline into per...
Our understanding of how global climatic changes are translated into ice-sheet fluctuations and sea-...
and sediment cores, reflecting the limited access to the these features were caused by the action of...
While there are numerous hypotheses concerning glacial–interglacial environmental and climatic regim...
While there are numerous hypotheses concerning glacial–interglacial environmental and climatic regim...
AbstractWhile there are numerous hypotheses concerning glacial–interglacial environmental and climat...
The hypothesis of floating ice shelves covering the Arctic Ocean during glacial periods was develope...
The hypothesis of floating ice shelves covering the Arctic Ocean during glacial periods was develope...
This paper reviews current knowledge of sedimentation patterns in the Arctic Ocean during the pronou...
Terrestrial and marine geological archives in the Arctic contain information on environmental change...
Terrestrial and marine geological archives in the Arctic contain information on environmental change...
The sediment composition of deep-sea cores from the central Arctic Ocean, the Fram Strait, and the Y...
Over many years there was a general acceptance that thick ice sheets of marine isotope stages 2, 4 a...
The Pechora Sea is optimally located for studying the coalescence of a glacial and periglacial conti...
Arctic sea-ice extent and volume are declining rapidly. Several studies project that the Arctic Ocea...
The volume and areal extent of Arctic sea ice is rapidly declining, and to put that decline into per...
Our understanding of how global climatic changes are translated into ice-sheet fluctuations and sea-...
and sediment cores, reflecting the limited access to the these features were caused by the action of...
While there are numerous hypotheses concerning glacial–interglacial environmental and climatic regim...
While there are numerous hypotheses concerning glacial–interglacial environmental and climatic regim...
AbstractWhile there are numerous hypotheses concerning glacial–interglacial environmental and climat...
The hypothesis of floating ice shelves covering the Arctic Ocean during glacial periods was develope...
The hypothesis of floating ice shelves covering the Arctic Ocean during glacial periods was develope...
This paper reviews current knowledge of sedimentation patterns in the Arctic Ocean during the pronou...
Terrestrial and marine geological archives in the Arctic contain information on environmental change...
Terrestrial and marine geological archives in the Arctic contain information on environmental change...
The sediment composition of deep-sea cores from the central Arctic Ocean, the Fram Strait, and the Y...
Over many years there was a general acceptance that thick ice sheets of marine isotope stages 2, 4 a...
The Pechora Sea is optimally located for studying the coalescence of a glacial and periglacial conti...
Arctic sea-ice extent and volume are declining rapidly. Several studies project that the Arctic Ocea...
The volume and areal extent of Arctic sea ice is rapidly declining, and to put that decline into per...
Our understanding of how global climatic changes are translated into ice-sheet fluctuations and sea-...
and sediment cores, reflecting the limited access to the these features were caused by the action of...