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13C, based on replicate measurements of in-house standard, is ±0.1 and ±0.05‰, respectively.
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0344437698
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note
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3 and analyzed within 6 hours. Measurements of Mg/Ca were made with a Perkin-Elmer Optima 8300 inductively coupled plasma optical emission spectrometer. We used a ratio intensity calibration method. Over the period during which the records at Site 1209 were generated, we observed long-term reproducibility in a liquid consistency standard (interrun precision, 1s, n = 250) to be 0.051, 0.018, and 0.023 mmol/mol for Mg/Ca, Sr/Ca, and Mn/Ca, respectively. During the same period, we observed long-term reproducibility in a foraminiferal consistency standard (interrun precision, 1s, n = 35) to be 0.252, 0.025, and 0.004 mmol/ mol for Mg/Ca, Sr/Ca, and Mn/Ca, respectively. See (43).
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22
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0344869488
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note
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3, was determined by the coulometric method. External precision based on replicates is ±1.5%.
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0344869490
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18O. Currently, the lack of sediment cores or outcrops of this age from the Antarctic margin, however, preclude a more definitive resolution to this issue.
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33
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0344006437
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note
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We thank B. Becker, R. Franks, S. Keller, H Leong and O. Daignieres for technical support, and P. Koch, C. Shellito, L. Sloan, and M. Huber for their comments. The Ocean Drilling Program furnished samples. This research was supported by NSF grants EAR-9814833 and EAR-0120727.
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