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0346940848
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2 by an average of -0.3‰ (41).
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This change represents a 120-m lowering of sea level and the resultant shift of carbonate sedimentation off the continental shelves into deep water, where dissolution is much more extensive. Discussion and details of the glacial carbon cycle boundary conditions are summarized in SOM Text, fig. S3, and table S2.
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0346310790
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note
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This work was supported by NSF (OCE-0117356), Lawrence Livermore National Laboratory (LDRD-97-ERI-009), and the U.S. Department of Energy (W-7405-Eng-48). We thank the ODP Core Repository in Bremen for core sampling; B. Frantz and P. Zermeno for sample preparation assistance; C. Laj, M. Frank, J.-P. Valet, and J. Stoner for providing their data of past geomagentic field intensities; and S. Johnsen for making available the revised GRIPss09sea chronology. This is WHOI contribution no, 11061.
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