Ice-proximal Labrador Sea Heinrich layers: a sedimentological approach
During Late Pleistocene Heinrich events (H-events), distinct, decimetre- to centimetre-thick layers of ice-rafted debris (IRD) were deposited in the North Atlantic as Heinrich layers (H-layers). These layers are characterized by high detrital carbonate content, low foraminifera content, a high perce...
Published in: | Canadian Journal of Earth Sciences |
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Format: | Article in Journal/Newspaper |
Language: | English |
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Canadian Science Publishing
2016
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Online Access: | http://dx.doi.org/10.1139/cjes-2015-0033 http://www.nrcresearchpress.com/doi/full-xml/10.1139/cjes-2015-0033 http://www.nrcresearchpress.com/doi/pdf/10.1139/cjes-2015-0033 |