Glacial-interglacial stability of ocean pH inferred from foraminifer dissolution rates

Nature

Volumn 416, Issue 6876, 2002, Pages 70-73

  Anderson, David M ^a   Archer, David ^b  

^a NOAA EARTH SYSTEM RESEARCH LABORATORY   (United States)

^b UNIVERSITY OF CHICAGO   (United States)

Author keywords

[No Author keywords available]

Indexed keywords

CARBON; CONCENTRATION (PROCESS); DISSOLUTION; OCEANOGRAPHY;

GLACIAL-INTERGLACIAL STABILITY;

PH;

BORON; CALCIUM CARBONATE; CARBON DIOXIDE;

CALCIUM CARBONATE; CARBON CYCLE; DISSOLUTION; FORAMINIFERA; GLACIAL-INTERGLACIAL CYCLE; LAST GLACIAL MAXIMUM; PH;

ARTICLE; ATMOSPHERE; CARBON CYCLE; CIRCULATION; CONCENTRATION PROCESS; DISSOLUTION; FORAMINIFER; ION TRANSPORT; MOLECULAR DYNAMICS; MOLECULAR ECOLOGY; MOLECULAR STABILITY; NONHUMAN; OCEAN ENVIRONMENT; PH MEASUREMENT; PRIORITY JOURNAL; REGULATORY MECHANISM;

ANIMALS; ATLANTIC OCEAN; BORON; CALCIUM CARBONATE; CARBONATES; EUKARYOTIC CELLS; HYDROGEN-ION CONCENTRATION; PACIFIC OCEAN; PLANKTON;

ATLANTIC OCEAN; INDIAN OCEAN; PACIFIC OCEAN;

FORAMINIFERA;

EID: 0037034770     PISSN: 00280836     EISSN: None     Source Type: Journal    
DOI: 10.1038/416070a     Document Type: Article

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