Evidence for rapid weathering response to climatic warming during the Toarcian Oceanic Anoxic Event

Chemical weathering consumes atmospheric carbon dioxide through the breakdown of silicate minerals and is thought to stabilize Earth’s long-term climate. However, the potential influence of silicate weathering on atmospheric pCO(2) levels on geologically short timescales (10(3)–10(5) years) remains...

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Detalhes bibliográficos
Publicado no:Sci Rep
Main Authors: Them, Theodore R., Gill, Benjamin C., Selby, David, Gröcke, Darren R., Friedman, Richard M., Owens, Jeremy D.
Formato: Artigo
Idioma:Inglês
Publicado em: Nature Publishing Group UK 2017
Assuntos:
Article
Acesso em linha:https://ncbi.nlm.nih.gov/pmc/articles/PMC5504049/
https://ncbi.nlm.nih.gov/pubmed/28694487
https://ncbi.nlm.nih.govhttp://dx.doi.org/10.1038/s41598-017-05307-y
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