Paleoceanographic evolution of the SW Svalbard margin (76°N) since 20,000 14C yr BP

TL;DR: In this article, a first-order thermomechanical ice sheet model was applied to investigate the retreat of the EISC after 23 ka BP, directly extending the work of Patton et al. (2016) who modelled the build-up to its maximum extent.

TL;DR: In this paper, the authors consider the characteristic elements of Arctic fjords and the important dynamical processes and show how the intense seasonality of these regions is reflected in the varying stratification of the Fjords, showing that sea ice has a central role in terms of the fjord salinity which ultimately influences the exchange with oceanic waters.

TL;DR: In this paper, high-resolution mass accumulation rates (MAR) and X-ray fluorescence (XRF) measurements from marine sediment records in the Bay of Biscay (NE Atlantic) have allowed the determination of the timing and the amplitude of the Channel River discharges during glacial stages MIS 10, MIS 8, MIS 6 and MIS 4-2.

TL;DR: In this paper, a five-stage reconstruction of the Late Weichselian deglaciation is proposed, showing that the observed pattern of rapid retreat, with high variability in ice streaming for the marine-based Barents Sea Ice Sheet, is similar to that of the marine based sectors of the late Weichsellian British, Laurentide and West Antarctic Ice Sheets.

TL;DR: In this paper, the influence of Earth's orbital parameters on major ice rafting was examined using deep-sea sediment cores recovered from the Northeast Atlantic Ocean in order to elucidate the influence.

TL;DR: In this article, the authors present records of sea surface temperature from North Atlantic sediments spanning the past 90 kyr which contain a series of rapid temperature oscillations closely matching those in the ice-core record, confirming predictions that the ocean must bear the imprint of the Dansgaard-Oeschger events.

TL;DR: In this article, the authors examine the control of the vertical circulation in the northern seas, and the potential for altering it, by considering the budgets and storage of fresh water in the Arctic Ocean and in the convective regions to the south.

TL;DR: In this paper, the authors present results from a new deep ice core drilled at the summit of the Greenland ice sheet, where the depositional environ-ment and the flow pattern of the ice are close to ideal for core recovery and analysis.