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Reconciling early Deccan Traps CO(2) outgassing and pre-KPB global climate
A 2 to 4 °C warming episode, known as the Latest Maastrichtian warming event (LMWE), preceded the Cretaceous–Paleogene boundary (KPB) mass extinction at 66.05 ± 0.08 Ma and has been linked with the onset of voluminous Deccan Traps volcanism. Here, we use direct measurements of melt-inclusion CO(2) c...
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| Vydáno v: | Proc Natl Acad Sci U S A |
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| Hlavní autoři: | , , , , , |
| Médium: | Artigo |
| Jazyk: | Inglês |
| Vydáno: |
National Academy of Sciences
2021
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| Témata: | |
| On-line přístup: | https://ncbi.nlm.nih.gov/pmc/articles/PMC8040825/ https://ncbi.nlm.nih.gov/pubmed/33782114 https://ncbi.nlm.nih.govhttp://dx.doi.org/10.1073/pnas.2007797118 |
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