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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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| Опубликовано в: : | Sci Rep |
|---|---|
| Главные авторы: | , , , , , |
| Формат: | Artigo |
| Язык: | Inglês |
| Опубликовано: |
Nature Publishing Group UK
2017
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| Предметы: | |
| Online-ссылка: | 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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