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rdiff 03; ac adine from between centennial to millennial scale fluctuations in the flow speed of Iceland-Scotland Overflow Water inferred from granulometric Holocene climate proxy records indicate the presence of responses that may not be present, at least in the same ARTICLE IN PRESS2. Material and...

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Bibliographic Details
Other Authors: The Pennsylvania State University CiteSeerX Archives
Format: Text
Language:English
Subjects:
Giraudeau et al
2000
Bond et al
2001
Haug et al
Haug
Iceland
Online Access:http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.476.1018
http://folk.uib.no/abo007/share/papers/8k/hall_bianchi04.qsr.pdf
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Summary:rdiff 03; ac adine from between centennial to millennial scale fluctuations in the flow speed of Iceland-Scotland Overflow Water inferred from granulometric Holocene climate proxy records indicate the presence of responses that may not be present, at least in the same ARTICLE IN PRESS2. Material and methods Our climate records have been obtained from kasten core NEAP4K recovered from the rapidly deposited sediments of the Bj.orn Drift, northern Iceland Basin $Table 1 available in the online version of this article, doi:10.1016/ j.quascirev.2004.04.004

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