The Late Quaternary Sedimentary Record of Reykjanes Ridge, North Atlantic

Variability in surface and deep ocean circulation in the North Atlantic is inferred from grain-size characteristics and the composition of terrigenous sediments from a deep-sea core taken on Reykjanes Ridge, south of Iceland. End-member modeling of grain size data shows that deep-ocean circulation i...

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Bibliographic Details
Published in:Radiocarbon
Main Authors: Prins, M A, Troelstra, S R, Kruk, R W, van der Borg, K, de Jong, A F M, Weltje, G J
Format: Article in Journal/Newspaper
Language:English
Published: Cambridge University Press (CUP) 2001
Subjects:
Online Access:http://dx.doi.org/10.1017/s0033822200041606
https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0033822200041606
Description
Summary:Variability in surface and deep ocean circulation in the North Atlantic is inferred from grain-size characteristics and the composition of terrigenous sediments from a deep-sea core taken on Reykjanes Ridge, south of Iceland. End-member modeling of grain size data shows that deep-ocean circulation in this area decreased significantly during periods of maximum iceberg discharge. The episodes of reduced circulation correlate with the cold and abrupt warming phases of the Dansgaard-Oeschger cycles as recognized in the Greenland ice cores.