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Nd at the core sites remain roughly constant. Thus, they would require evidence before they can be considered seriously. On the longer term, as explained in the text, there is good evidence that the Pacific end member remained nearly constant on glacial-interglacial time scales, whereas the North Atlantic end member is less well constrained, but current evidence indicates near constancy (15, 18).
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A 35-cm interval in RC11-83, which has an average sedimentation rate through this section of 24 cm/1000 years [a 29-cm interval in RC11-83 (79, 20)], would correspond to a time period of 1450 years.
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45
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Most Nd and carbon isotope measurements in the deglacial and Bølling warming portion of the record were not made on the same sample depths or splits. We therefore conservatively confine our interpretations to lead-lag relationships >150 years or >3 cm of core length.
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This manuscript benefited from discussions with R. Anderson, S. Barker, W. Broecker, H. Elderfield, E. Martin, J. McManus, U. Ninnemann, H. Scher, and A. Tripati; laboratory assistance from D. Zylberberg and comments by anonymous reviewers. This study was supported by NSF grants OCE 98-09253 and OCE 00-96427 to S.L.G. and S.R.H. and ATM03-27722 and OCE99-11637 to R.G.F. Samples used in this project were provided by the Lamont-Doherty Earth Observatory Deep-Sea Sample Repository, supported by the NSF (grant OCE 00-02380) and the Office of Naval Research (grant N00014-02-1-0073). This is LDEO Contribution #6702.
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