Amiotte Suchet, Philippe and Probst, Jean-Luc and Ludwig, Wolfgang Worldwide distribution of continental rock lithology: Implications for the atmospheric/soil CO2 uptake by continental weathering and alkalinity river transport to the oceans. (2003) Global Biogeochemical Cycles, vol. 1 (n°2). pp. 1038-1051.
(Document in English)
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Official URL: http://dx.doi.org/10.1029/2002GB001891
The silicate rock weathering followed by the formation of carbonate rocks in the ocean, transfers CO2 from the atmosphere to the lithosphere. This CO2 uptake plays a major role in the regulation of atmospheric CO2 concentrations at the geologic timescale and is mainly controlled by the chemical properties of rocks. This leads us to develop the first world lithological map with a grid resolution of 1 1. This paper analyzes the spatial distribution of the six main rock types by latitude, continents, and ocean drainage basins and for 49 large river basins. Coupling our digital map with the GEM-CO2 model, we have also calculated the amount of atmospheric/soil CO2 consumed by rock weathering and alkalinity river transport to the ocean. Among all silicate rocks, shales and basalts appear to have a significant influence on the amount of CO2 uptake by chemical weathering
|Additional Information:||Thanks to AGU Publisher. The definitive version is available at http://www.agu.org/pubs/crossref/2003/2002GB001891.shtml|
|Audience (journal):||International peer-reviewed journal|
|Institution:||French research institutions > Institut National de la Recherche Agronomique - INRA (FRANCE)|
French research institutions > Institut de Recherche pour le Développement - IRD (FRANCE)
Université de Toulouse > Université Paul Sabatier-Toulouse III - UPS (FRANCE)
French research institutions > Centre National de la Recherche Scientifique - CNRS (FRANCE)
Other partners > Université de Bourgogne - UB (FRANCE)
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|Deposited By:||Florence Amor|
|Deposited On:||23 Feb 2010 12:04|
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