The recent expansion of Atlantic waters into the Arctic Ocean represents undisputable evidence of the rapid changes occurring in this region. Understanding the past variability of this “Atlantification” is thus crucial in providing a longer perspective on the modern Arctic changes. Here, we reconstruct the history of Atlantification along the eastern Fram Strait during the past 800 years using precisely dated paleoceanographic records based on organic biomarkers and benthic foraminiferal data. Our results show rapid changes in water mass properties that com-menced in the early 20th century—several decades before the documented Atlantification by instrumental records. Comparison with regional records suggests a poleward expansion of subtropi...
The last transition from full glacial to current interglacial conditions was accompanied by distinct...
International audienceSea ice is a critical component of the climate system: variations in sea-ice c...
In this paper, we make use of calcium carbonate-bearing sediment sequences in the Arctic-Atlantic ga...
The recent expansion of Atlantic waters into the Arctic Ocean represents undisputable evidence of th...
A sediment core from the West Spitsbergen continental margin was studied to reconstruct climate and ...
EGU2011-2455 The current interglacial has gone through a variety of warmer and colder periods. Cons...
Two high-resolution sediment sequences from the Western Svalbard margin covering the last ca. 10.000...
The paleoceanographic development of the eastern Fram Strait during the transition from the cold Lat...
The transition from last glacial to deglacial and subsequently to modern interglacial climate condit...
A reconstruction of Holocene sea ice conditions in the Fram Strait provides insight into the palaeoe...
The modern polar cryosphere reflects an extreme climate state with profound temperature gradients to...
Oceanic heat transport variations, carried by the northward-flowing Atlantic Water, strongly influen...
Despite the undisputed role of the Arctic Ocean in the modern and Pliocene climate system, the Arcti...
Benthic and planktonic foraminifera, stable isotopes and other geochemical and sedimentological para...
Baffin Bay is a semi-enclosed basin connecting the Arctic Ocean and the western North Atlantic, thus...
The last transition from full glacial to current interglacial conditions was accompanied by distinct...
International audienceSea ice is a critical component of the climate system: variations in sea-ice c...
In this paper, we make use of calcium carbonate-bearing sediment sequences in the Arctic-Atlantic ga...
The recent expansion of Atlantic waters into the Arctic Ocean represents undisputable evidence of th...
A sediment core from the West Spitsbergen continental margin was studied to reconstruct climate and ...
EGU2011-2455 The current interglacial has gone through a variety of warmer and colder periods. Cons...
Two high-resolution sediment sequences from the Western Svalbard margin covering the last ca. 10.000...
The paleoceanographic development of the eastern Fram Strait during the transition from the cold Lat...
The transition from last glacial to deglacial and subsequently to modern interglacial climate condit...
A reconstruction of Holocene sea ice conditions in the Fram Strait provides insight into the palaeoe...
The modern polar cryosphere reflects an extreme climate state with profound temperature gradients to...
Oceanic heat transport variations, carried by the northward-flowing Atlantic Water, strongly influen...
Despite the undisputed role of the Arctic Ocean in the modern and Pliocene climate system, the Arcti...
Benthic and planktonic foraminifera, stable isotopes and other geochemical and sedimentological para...
Baffin Bay is a semi-enclosed basin connecting the Arctic Ocean and the western North Atlantic, thus...
The last transition from full glacial to current interglacial conditions was accompanied by distinct...
International audienceSea ice is a critical component of the climate system: variations in sea-ice c...
In this paper, we make use of calcium carbonate-bearing sediment sequences in the Arctic-Atlantic ga...