A Laurentide outburst flooding event during the last interglacial period

• Published in: Nature Geoscience
• Main Authors: Nicholl, Joseph A. L., Hodell, David A., Naafs, B. David A., Hillaire-Marcel, Claude, Channell, James E. T., Romero, Oscar E.
• Format: Article in Journal/Newspaper
• Language: English
• Published: 2012
• Subjects: 01 - Climate Change and Earth-Ocean Atmosphere Systems; Hudson Bay; Greenland; Hudson; Hudson Strait; Ice Sheet; Labrador Sea
• Online Access: http://eprints.esc.cam.ac.uk/2644/; http://eprints.esc.cam.ac.uk/2644/1/ngeo1622-f1.jpg; http://eprints.esc.cam.ac.uk/2644/2/ngeo1622.pdf; http://www.nature.com/doifinder/10.1038/ngeo1622; https://doi.org/10.1038/ngeo1622

Episodes of ice-sheet disintegration and meltwater release over glacial–interglacial cycles are recorded by discrete layers of detrital sediment in the Labrador Sea1, 2. The most prominent layers reflect the release of iceberg armadas associated with cold Heinrich events3, but the detrital sediment carried by glacial outburst floods from the melting Laurentide Ice Sheet is also preserved4. Here we report an extensive layer of red detrital material in the Labrador Sea that was deposited during the early last interglacial period. We trace the layer through sediment cores collected along the Labrador and Greenland margins of the Labrador Sea. Biomarker data, Ca/Sr ratios and δ18O measurements link the carbonate contained in the red layer to the Palaeozoic bedrock of the Hudson Bay. We conclude that the debris was carried to the Labrador Sea during a glacial outburst flood through the Hudson Strait, analogous to the final Lake Agassiz outburst flood about 8,400 years ago, probably around the time of a last interglacial cold event in the North Atlantic5. We suggest that outburst floods associated with the final collapse of the Laurentide Ice Sheet may have been pervasive features during the early stages of Late Quaternary interglacial periods.