Direct effects of CO2 and temperature on silicate weathering: Possible implications for climate control
- 1 April 1994
- journal article
- research article
- Published by Elsevier in Geochimica et Cosmochimica Acta
- Vol. 58 (7) , 1853-1856
- https://doi.org/10.1016/0016-7037(94)90543-6
Abstract
No abstract availableThis publication has 25 references indexed in Scilit:
- GEOCARB II; a revised model of atmospheric CO 2 over Phanerozoic timeAmerican Journal of Science, 1994
- Paleozoic Atmospheric CO 2 : Importance of Solar Radiation and Plant EvolutionScience, 1993
- Surface chemistry and silicate dissolution at elevated temperaturesAmerican Journal of Science, 1992
- Olivine dissolution kinetics at near-surface conditionsChemical Geology, 1992
- A model for atmospheric CO 2 over Phanerozoic timeAmerican Journal of Science, 1991
- Kaolinite dissolution at 25 degrees , 60 degrees , and 80 degrees CAmerican Journal of Science, 1990
- Biotic enhancement of weathering and the habitability of EarthNature, 1989
- Feedbacks between weathering and atmospheric CO 2 over the last 100 million yearsAmerican Journal of Science, 1987
- The carbonate-silicate geochemical cycle and its effect on atmospheric carbon dioxide over the past 100 million yearsAmerican Journal of Science, 1983
- Life span of the biosphereNature, 1982