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A framework for predicting global silicate weathering and CO(2) drawdown rates over geologic time-scales
Global silicate weathering drives long-time-scale fluctuations in atmospheric CO(2). While tectonics, climate, and rock-type influence silicate weathering, it is unclear how these factors combine to drive global rates. Here, we explore whether local erosion rates, GCM-derived dust fluxes, temperatur...
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| Hlavní autoři: | , |
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| Médium: | Artigo |
| Jazyk: | Inglês |
| Vydáno: |
National Academy of Sciences
2008
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| Témata: | |
| On-line přístup: | https://ncbi.nlm.nih.gov/pmc/articles/PMC2572559/ https://ncbi.nlm.nih.gov/pubmed/18952842 https://ncbi.nlm.nih.govhttp://dx.doi.org/10.1073/pnas.0801462105 |
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