Matthias Forwick

TL;DR: Two sediment cores from the West Spitsbergen area, Euro-Arctic margin, were investigated for paleoceanographic proxies, including benthic and planktonic foraminifera, stable isotopes and ice rafted debris as discussed by the authors.

TL;DR: In this article, the authors used high-resolution swath bathymetry obtained from Van Keulenfjorden and Rindersbukta (inner Van Mijendalen), Spitsbergen, Svalbard, Norway.

TL;DR: In this paper, multi-proxy analyses of two sediment cores from central Isfjorden were used to reconstruct the glacial history in central Spitsbergen during the Late Weichselian and the Holocene, and to relate iceberg rafting and sea-ice rafting to climatic and oceanographic changes in the north Atlantic region.

TL;DR: In this paper, the authors present detailed marine geological and radiocarbon data along three palaeo-ice stream tributary troughs in the western ASE to establish vital information on the timing of deglaciation of the WAIS since the Last Glacial Maximum (LGM).

TL;DR: The presence of IP25 as a proxy for spring sea-ice cover and alkenone-based summer sea-surface temperatures >4 °C that support a seasonal sea- ice cover with an ice-free summer season being predominant during the late Miocene in the central Arctic Ocean is documented.