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The Late Quaternary Sedimentary Record of Reykjanes Ridge, North Atlantic

Published online by Cambridge University Press:  18 July 2016

M A Prins ,
S R Troelstra ,
R W Kruk ,
K van der Borg ,
A F M de Jong  and
G J Weltje
M A Prins*
Affiliation:
Faculty of Earth Sciences, Vrije Universiteit, Amsterdam, the Netherlands
S R Troelstra
Affiliation:
Faculty of Earth Sciences, Vrije Universiteit, Amsterdam, the Netherlands
R W Kruk
Affiliation:
Faculty of Earth Sciences, Vrije Universiteit, Amsterdam, the Netherlands
K van der Borg
Affiliation:
Faculty of Physics and Astronomy, University Utrecht, Utrecht, the Netherlands
A F M de Jong
Affiliation:
Faculty of Physics and Astronomy, University Utrecht, Utrecht, the Netherlands
G J Weltje
Affiliation:
Faculty of Civil Engineering and Applied Geosciences, Delft University of Technology, Delft, the Netherlands
*
Corresponding author. Email: prim@geo.vu.nl.
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Abstract

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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.

Type
II. Our ‘Wet’ Environment
Information
Radiocarbon , Volume 43 , Issue 2B: Proceedings of the 17th International Radiocarbon Conference (Part 2 of 3), Conference Editors: Israel Carmi, Elisabetta Boaretto , 2001 , pp. 939 - 947
Copyright
Copyright © 2001 by the Arizona Board of Regents on behalf of the University of Arizona 

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