Global climate stabilisation by chemical weathering during the Hirnantian glaciation

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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Bibliografiske detaljer
Main Authors:	von Strandmann, P, Desrochers, A, Murphy, M, Finlay, A, Selby, D, Lenton, T
Format:	Journal article
Udgivet:	European Association of Geochemistry 2017

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