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Sea level fall during glaciation stabilized atmospheric CO(2) by enhanced volcanic degassing
Paleo-climate records and geodynamic modelling indicate the existence of complex interactions between glacial sea level changes, volcanic degassing and atmospheric CO(2), which may have modulated the climate system’s descent into the last ice age. Between ∼85 and 70 kyr ago, during an interval of de...
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| Publicado no: | Nat Commun |
|---|---|
| Main Authors: | , , , , , , , , |
| Formato: | Artigo |
| Idioma: | Inglês |
| Publicado em: |
Nature Publishing Group
2017
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| Assuntos: | |
| Acesso em linha: | https://ncbi.nlm.nih.gov/pmc/articles/PMC5504290/ https://ncbi.nlm.nih.gov/pubmed/28681844 https://ncbi.nlm.nih.govhttp://dx.doi.org/10.1038/ncomms15867 |
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