Ocean ventilation during the last 12,000 years: Hypothesis of counterpoint deep water production-Reference-Cited by-同舟云学术

Ocean ventilation during the last 12,000 years: Hypothesis of counterpoint deep water production

Published:1987-11 Issue:1-2 Volume:78 Page:1-10
ISSN:0025-3227
Container-title:Marine Geology
language:en
Short-container-title:Marine Geology

Author:

Berger W.H

Publisher

Elsevier BV

Subject

Geochemistry and Petrology,Geology,Oceanography

Reference37 articles.

1. 14C measurements on foraminifera of deep-sea core V28–238 and their preliminary interpretation;Andree;Nucl. Instrum. Methods Phys. Res.,1984

2. Accelerator radiocarbon ages on foraminifera separated from deep sea sediments;Andree,1984

3. AMS radiocarbon dates on foraminifera from deep sea sediments;Andree;Radiocarbon,1986

4. Limits on the ventilation rate for the deep ocean over the last 12000 years;Andree;Climate Dyn.,1986

5. Bioturbation effects on abrupt climate changes recorded in deep sea sediments, correlation between δ18O profiles and accelerator 14C dating;Bard,1987

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