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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Detalles Bibliográficos
Autores principales: Them, Theodore R., Gill, Benjamin C., Selby, David, Gröcke, Darren R., Friedman, Richard M., Owens, Jeremy D.
Formato: Online Artículo Texto
Lenguaje:English
Publicado: Nature Publishing Group UK 2017
Materias:
Article
Acceso en línea:https://www.ncbi.nlm.nih.gov/pmc/articles/PMC5504049/
https://www.ncbi.nlm.nih.gov/pubmed/28694487
http://dx.doi.org/10.1038/s41598-017-05307-y

Internet

https://www.ncbi.nlm.nih.gov/pmc/articles/PMC5504049/
https://www.ncbi.nlm.nih.gov/pubmed/28694487
http://dx.doi.org/10.1038/s41598-017-05307-y

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