Global climate stabilisation by chemical weathering during the Hirnantian glaciation
Chemical weathering of silicate rocks is a primary drawdown mechanism of atmospheric carbon dioxide. The processes that affect weathering are therefore central in controlling global climate. A temperature-controlled “weathering thermostat” has long been proposed in stabilising long-term climate, but...
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| Fformat: | Journal article |
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European Association of Geochemistry
2017
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