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14C ages have been calibrated to calendar years by using the INTCAL98 calibration set and the calibration program CALIB 4.0 [M. Stuiver et al., Radiocarbon 40, 1041 (1998); E. Bard, M. Arnold, B. Hamelin, N. Tisnerat-Laborde, C. Cabioch. Radiocarbon 40, 1085 (1998)], which is distinctly different from the earlier version.
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0342631892
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14C production, and subsidence and uplift. There is no evidence for compaction of these young sediments. Bioturbation is also negligible because of very high sedimentation rates locally. If we take into account that the equatorial ocean siphoning [J. X. Mitrovica and W. R. Peltier, J. Geophys. Res. 96(B12), 20053 (1991)] secondarily decreased the water depth by several meters, our value corresponds well with the generally estimated depth of about - 120 m during LGM and therefore does not indicate a significant effect of hydroisostasy [ K. Fleming et al., Earth Planet. Sci. Lett. 163, 327 (1998)]. Another aspect that is probably important is the effect of gravity field and centrifugal force on the global distribution of newly generated water masses in a scale of meters, as mentioned by W. R. Peltier [Science 265, 195 (1994)].
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14C production, and subsidence and uplift. There is no evidence for compaction of these young sediments. Bioturbation is also negligible because of very high sedimentation rates locally. If we take into account that the equatorial ocean siphoning [J. X. Mitrovica and W. R. Peltier, J. Geophys. Res. 96(B12), 20053 (1991)] secondarily decreased the water depth by several meters, our value corresponds well with the generally estimated depth of about - 120 m during LGM and therefore does not indicate a significant effect of hydroisostasy [ K. Fleming et al., Earth Planet. Sci. Lett. 163, 327 (1998)]. Another aspect that is probably important is the effect of gravity field and centrifugal force on the global distribution of newly generated water masses in a scale of meters, as mentioned by W. R. Peltier [Science 265, 195 (1994)].
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14C production, and subsidence and uplift. There is no evidence for compaction of these young sediments. Bioturbation is also negligible because of very high sedimentation rates locally. If we take into account that the equatorial ocean siphoning [J. X. Mitrovica and W. R. Peltier, J. Geophys. Res. 96(B12), 20053 (1991)] secondarily decreased the water depth by several meters, our value corresponds well with the generally estimated depth of about - 120 m during LGM and therefore does not indicate a significant effect of hydroisostasy [ K. Fleming et al., Earth Planet. Sci. Lett. 163, 327 (1998)]. Another aspect that is probably important is the effect of gravity field and centrifugal force on the global distribution of newly generated water masses in a scale of meters, as mentioned by W. R. Peltier [Science 265, 195 (1994)].
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0343066162
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14C plateau. This works together with the coral startup time and sampling to explain the observed discrepancies.
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35
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0343502068
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note
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Project 03G01115A was supported by the German Ministry of Education and Research. T.H. acknowledges a graduate school stipend funded by the Deutsche Forschungsgemeinschaft. We thank the team from the Leibniz Laboratory in Kiel for support and assistance. We gratefully acknowledge the positive comments by C. D. Woodroffe and two anonymous reviewers.
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