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East Pacific Rise

Published online by Cambridge University Press:  18 July 2016

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This study was carried out in cooperation with Steve Emerson of the University of Washington. The purpose was to obtain benthic-planktonic and planktonic-planktonic age differences on hand-picked foraminifera shells. Material was taken from two separate subcores from the primary 50cm2 box core (see Tables 8, 9).

Type
Accelerator Mass Spectrometry Radiocarbon Measurements on Marine Carbonate Samples from Deep Sea Cores and Sediment Traps
Information
Radiocarbon , Volume 30 , Issue 3 , 1988 , pp. 278 - 281
Copyright
Copyright © The American Journal of Science

References

Broecker, W S, Andrée, M, Bonani, G, Mix, A, Klas, M, Wolfli, W and Oeschger, H, ms in preparation, Differences between the radiocarbon ages of coexisting planktonic foraminifera.Google Scholar
Broecker, W S, Andrée, M, Bonani, G, Wolfli, W, Oeschger, H, Klas, M, Mix, A and Curry, W, ms in preparation, The radiocarbon age of deep water in the glacial ocean.Google Scholar
Emerson, S, Stump, C, Grootes, P M, Stuiver, M, Farwell, G W and Schmidt, F H, 1987, Estimates of degradable organic carbon in deep-sea surface sediments from 14C concentrations: Nature, v 329, p 51–53.Google Scholar