Can deep ocean carbonate preservation history inferred from atmospheric pCO2 account for 14C and %CaCO3 profiles on the Ontong-Java Plateau?

Earth and Planetary Science Letters

Volumn 192, Issue 3, 2001, Pages 319-329

  Matsumoto, Katsumi ^a,b,e   Broecker, Wallace S ^a,b   Clark, Elizabeth ^a   McCorkle, Daniel C ^c   Martin, William R ^c   Hajdas, Irka ^d  

^a Department of Earth and Environmental Sciences   (United States)

^b Och Spine at New York Presbyterian Hospitals   (United States)

^c WOODS HOLE OCEANOGRAPHIC INSTITUTION   (United States)

^d ETH ZURICH   (Switzerland)

^e PRINCETON UNIVERSITY   (United States)

Author keywords

Bioturbation; C 14; Deep sea environment; Deglaciation; Ontong Java Plateau; Pacific Ocean; Pb 210; Sediments

Indexed keywords

BIOTURBATION; CARBON DIOXIDE; CARBONATE; DEEP SEA; DEGLACIATION; HOLOCENE; MARINE SEDIMENT;

PACIFIC OCEAN;

EID: 0035172658     PISSN: 0012821X     EISSN: None     Source Type: Journal    
DOI: 10.1016/S0012-821X(01)00412-5     Document Type: Article

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