Abstract
Six layers rich in ice-rafted debris and poor in foraminifera shells have been identified in sediments of last glacial age in the northern Atlantic (Heinrich, 1988; Broecker et al., 1990). Based on their geographic pattern and composition, these layers appear to be debris released during the melting of armadas of icebergs (Bond et al., 1992). Abundant limestone fragments in the ice-rafted debris and the exceptionally high 40K — 40Ar ages for the clay minerals point to Hudson Straits as the launching site. This interpretation is strengthened by the finding by Andrews and Tedesco (1992) of exceptionally thick Heinrich layers in cores from the Labrador Sea.
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References
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© 1993 Springer-Verlag Berlin Heidelberg
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Broecker, W., Bond, G., McManus, J. (1993). Heinrich Events: Triggers of Ocean Circulation Change?. In: Peltier, W.R. (eds) Ice in the Climate System. NATO ASI Series, vol 12. Springer, Berlin, Heidelberg. https://doi.org/10.1007/978-3-642-85016-5_10
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DOI: https://doi.org/10.1007/978-3-642-85016-5_10
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