Limits on the ventilation rate for the deep ocean over the last 12 000 years

In this paper we present accelerator radiocarbon measurements on hand picked benthic and planktonic foraminifera separated from two deep sea cores raised from the South China Sea. From the benthic-planktonic age differences we are able to place limits on the extent to which the ventilation rate of t...

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Bibliographic Details
Published in:Climate dynamics 1986-09, Vol.1 (1), p.53-62
Main Authors: Andree, M, Oeschger, H, Broecker, W, Beavan, N, Klas, M, Mix, A, Bonani, G, Hofmann, HJ, Suter, M, Woelfli, W, Peng, T-H
Format: Article
Language:English
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Summary:In this paper we present accelerator radiocarbon measurements on hand picked benthic and planktonic foraminifera separated from two deep sea cores raised from the South China Sea. From the benthic-planktonic age differences we are able to place limits on the extent to which the ventilation rate of the deep Pacific Ocean has changed over the last 12 000 years. While much work remains to be done before any definitive answers for the global oceans can be given, these results on cores with sedimentation rates suitably high to avoid major corrections for bioturbation effects suggest that the ventilation rate of the deep Pacific Ocean has remained nearly the same throughout Holocene time. Further, there is no suggestion that the rate was slower during the period of major glacial retreat. These results confirm that the changes in atmospheric super(1) super(4) C/C ratio over the last 10 000 years owe their origin to radiocarbon production rate changes.
ISSN:0930-7575