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Fractionation of carbon isotopes by phytoplankton and estimates of ancient CO2levels

Author(s): Katherine H. Freeman , J. M. Hayes

Publication date Created: June 1992

Publication date (Print): June 1992

Journal: Global Biogeochemical Cycles

Publisher: American Geophysical Union (AGU)

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Observational contrains on the global atmospheric co2 budget.

P Tans, I. Fung, T Takahashi (1990)

Observed atmospheric concentrations of CO(2) and data on the partial pressures of CO(2) in surface ocean waters are combined to identify globally significant sources and sinks of CO(2). The atmospheric data are compared with boundary layer concentrations calculated with the transport fields generated by a general circulation model (GCM) for specified source-sink distributions. In the model the observed north-south atmospheric concentration gradient can be maintained only if sinks for CO(2) are greater in the Northern than in the Southern Hemisphere. The observed differences between the partial pressure of CO(2) in the surface waters of the Northern Hemisphere and the atmosphere are too small for the oceans to be the major sink of fossil fuel CO(2). Therefore, a large amount of the CO(2) is apparently absorbed on the continents by terrestrial ecosystems.

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The distribution of 13C of ΣCO2 in the world oceans

P.M. Kroopnick (1985)

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Vertical distribution and isotopic fractionation of living planktonic foraminifera from the Panama Basin

Richard Fairbanks, Marc Sverdlove, Rosemary Free … (1982)

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Author and article information

Journal

Title: Global Biogeochemical Cycles

Abbreviated Title: Global Biogeochem. Cycles

Publisher: American Geophysical Union (AGU)

ISSN: 08866236

Publication date Created: June 1992

Publication date (Print): June 1992

Volume: 6

Issue: 2

Pages: 185-198

Article

DOI: 10.1029/92GB00190

PubMed ID: 11537848

SO-VID: 3a016428-425c-4bbc-bf40-b999b7eb2a9f

Copyright © © 1992

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http://doi.wiley.com/10.1002/tdm_license_1.1

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