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Letter
Nature Geoscience 1, 370–374 (1 June 2008) | doi:10.1038/ngeo205
Elevated weathering rates in the Rocky Mountains during the Early Eocene Climatic|[nbsp]|Optimum
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Abstract
During the chemical weathering of silicate minerals, atmospheric carbon dioxide is incorporated into carbonate minerals and buried. As the rate of silicate weathering is thought to increase in response to increasing atmospheric CO2 concentrations, this represents an important negative feedback mechanism.
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