Varying sediment sources (Hudson Strait, Cumberland Sound, Baffin Bay) to the NW Labrador Sea slope between and during Heinrich events 0 to 4

• Published in: Journal of Quaternary Science
• Main Authors: Andrews, J. T., Barber, D. C., Jennings, A. E., Eberl, D. D., Maclean, B., Kirby, M. E., Stoner, J. S.
• Format: Article in Journal/Newspaper
• Language: English
• Published: Wiley-blackwell 2012
• Subjects: Baffin Bay; detrital carbonate (DC-) events; Heinrich events; Labrador Sea; Laurentide Ice Sheet; Baffin Island; Buff; Cumberland Sound; Hudson; Hudson Strait; Baffin; Ice Sheet
• Online Access: https://archimer.ifremer.fr/doc/00265/37644/35823.pdf; https://doi.org/10.1002/jqs.2535; https://archimer.ifremer.fr/doc/00265/37644/

Core HU97048-007PC was recovered from the continental Labrador Sea slope at a water depth of 945?m, 250?km seaward from the mouth of Cumberland Sound, and 400?km north of Hudson Strait. Cumberland Sound is a structural trough partly floored by Cretaceous mudstones and Paleozoic carbonates. The recor...