Heinrich event 1: An example of dynamical ice-sheet reaction to oceanic changes
Heinrich events, identified as enhanced ice-rafted detritus (IRD) in North Atlantic deep sea sediments (Heinrich, 1988; Hemming, 2004) have classically been attributed to Laurentide ice-sheet (LIS) instabilities (MacAyeal, 1993; Calov et al., 2002; Hulbe et al., 2004) and assumed to lead to importan...
Main Authors: | , , , , , , , , |
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Format: | Article in Journal/Newspaper |
Language: | English |
Published: |
München : European Geopyhsical Union
2011
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Subjects: | |
Online Access: | https://dx.doi.org/10.34657/984 https://oa.tib.eu/renate/handle/123456789/623 |