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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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Bibliografske podrobnosti
izdano v:Sci Rep
Main Authors: Them, Theodore R., Gill, Benjamin C., Selby, David, Gröcke, Darren R., Friedman, Richard M., Owens, Jeremy D.
Format: Artigo
Jezik:Inglês
Izdano: Nature Publishing Group UK 2017
Teme:
Online dostop: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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