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Very large release of mostly volcanic carbon during the Paleocene-Eocene Thermal Maximum
Global warming during the Palaeocene-Eocene Thermal Maximum1,2 (PETM, ~56 Ma) is commonly interpreted as being primarily driven by the destabilization of carbon from surficial sedimentary reservoirs such as methane hydrates3. However, the source(s) of carbon remain controversial1,3–5. Resolving this...
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| Publicado en: | Nature |
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| Main Authors: | , , , , , , , , |
| Formato: | Artigo |
| Idioma: | Inglês |
| Publicado: |
2017
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| Assuntos: | |
| Acceso en liña: | https://ncbi.nlm.nih.gov/pmc/articles/PMC5582631/ https://ncbi.nlm.nih.gov/pubmed/28858305 https://ncbi.nlm.nih.govhttp://dx.doi.org/10.1038/nature23646 |
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