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(Table 2) Age determination of sediment core V21-30

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UCI results obtained in the present study have been corrected for isotopic fractionation according to the conventions of Stuiver and Polach (1977), with d13C values measured on prepared graphite using the AMS spectrometer. These can differ from d13C of the original material, if fractionation occurred during sample graphitization or the AMS measurement, and are not shown.
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