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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...
Shranjeno v:
| izdano v: | Sci Rep |
|---|---|
| Main Authors: | , , , , , |
| Format: | Artigo |
| Jezik: | Inglês |
| Izdano: |
Nature Publishing Group UK
2017
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| 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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