Benthic Mixing in Deep Sea Cores as Determined by 14C Dating and its Implications Regarding Climate Stratigraphy and the Fate of Fossil Fuel CO2 1-Reference-Cited by-同舟云学术

Benthic Mixing in Deep Sea Cores as Determined by 14C Dating and its Implications Regarding Climate Stratigraphy and the Fate of Fossil Fuel CO2 1

Published:1977 Issue: Volume: Page:355-373
ISSN:
Container-title:The Fate of Fossil Fuel CO2 in the Oceans
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Author:

Peng T.-H.,Broecker W. S.,Kipphut G.,Shackleton N.

Publisher

Springer US

Link

http://link.springer.com/content/pdf/10.1007/978-1-4899-5016-1_20

Reference25 articles.

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2. Berger, W. H. and G. R. Heath. 1968. Vertical mixing in pelagic sediments. J. Marine Res. 26 (2): 134–143.

3. Broecker, W. S. and E. A. Olson. 1959. Lamont radiocarbon measurements VI. Am. J. Sci. Radiocarbon Suppl. 1: 111–132.

4. Broecker, W. S., K. K. Turekian and B. C. Heezen. 1958. The relation of deep sea sedimentation rates to variations in climate. Am J. Sci. 256: 503–517.

5. Broecker, W. S. and T. Takahashi. 1977. Neutralization of fossil fuel CO 2 by marine calcium carbonate, In: The Fate of Fossil Fuel CO 2, N. R. Andersen and A. Malahoff (Eds.), Plenum, N. Y., (this volume).

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