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

Paleoceanography

Volumn 14, Issue 6, 1999, Pages 744-752

  Broecker, Wallace S ^a   Clark, Elizabeth ^a   McCorkle, Daniel C ^b   Peng, Tsung Hung ^c,e   Hajdas, Irena ^d   Bonani, Georges ^d  

^a Lamont Doherty Earth Observatory of Columbia University   (United States)

^b WOODS HOLE OCEANOGRAPHIC INSTITUTION   (United States)

^c ATLANTIC OCEANOGRAPHIC AND METEOROLOGICAL LABORATORY   (United States)

^d ETH ZURICH   (Switzerland)

^e NOAA EARTH SYSTEM RESEARCH LABORATORY   (United States)

Author keywords

[No Author keywords available]

Indexed keywords

CARBONATE; DEEP SEA; HOLOCENE; PALEOCEANOGRAPHY;

EID: 0033496830     PISSN: 08838305     EISSN: None     Source Type: Journal    
DOI: 10.1029/1999PA900038     Document Type: Article

References (9)

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5. 2 between the last glaciation and the Holocene, Paleoceanography, 3, 317-342, 1988.
6. 2 ice core record from Taylor Dome, Antarctica, Nature, 398, 121-126, 1999.
7. 2 record in the Byrd ice core 50,000-5,000 years BP, Nature, 331, 609-611, 1988.
8. Peterson, L. C., Late Quaternary deep-water paleoceanography of the eastern equatorial Indian Ocean: Evidence from benthic foraminifera, carbonate dissolution, and stable isotopes, Ph.D. thesis, 429 pp., Brown Univ., Providence, R. I., 1984.
9. Sanyal, A., N. G. Hemming, G. N. Hanson, and W. S. Broecker, Evidence for a higher pH in the glacial ocean from boron isotopes in foraminifera, Nature, 373, 234-236, 1995.