Evidence for a reduction in the carbonate ion content of the deep sea during the course of the Holocene-Reference-Cited by-同舟云学术

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Evidence for a reduction in the carbonate ion content of the deep sea during the course of the Holocene

Published:1999-12 Issue:6 Volume:14 Page:744-752
ISSN:0883-8305
Container-title:Paleoceanography
language:en
Short-container-title:Paleoceanography

Author:

Broecker Wallace S.,Clark Elizabeth,McCorkle Daniel C.,Peng Tsung-Hung,Hajdas Irena,Bonani Georges

Publisher

American Geophysical Union (AGU)

Subject

Paleontology,Oceanography

Link

http://www.agu.org/journals/pa/v014/i006/1999PA900038/1999PA900038.pdf

Reference9 articles.

1. Effect of deepsea sedimentary calcite preservation on atmospheric CO2 concentration;Archer;Nature,1994

2. CaCO3 size distribution: A paleocarbonate ion proxy;Broecker;Paleoceanography,1999

3. The cause of glacial to interglacial atmospheric CO2 change: A polar alkalinity hypothesis;Broecker;Global Biogeochem. Cycles,1939

4. A search for an early Holocene CaCO3 preservation event;Broecker;Paleoceanography,1993

5. Changes in the distribution of δ13C of deep water ΣCO2 between the last glaciation and the Holocene;Curry;Paleoceanography,1988

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