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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Detalles Bibliográficos
Autores principales: Hasenclever, Jörg, Knorr, Gregor, Rüpke, Lars H., Köhler, Peter, Morgan, Jason, Garofalo, Kristin, Barker, Stephen, Lohmann, Gerrit, Hall, Ian R.
Formato: Online Artículo Texto
Lenguaje:English
Publicado: Nature Publishing Group 2017
Materias:
Article
Acceso en línea:https://www.ncbi.nlm.nih.gov/pmc/articles/PMC5504290/
https://www.ncbi.nlm.nih.gov/pubmed/28681844
http://dx.doi.org/10.1038/ncomms15867

Internet

https://www.ncbi.nlm.nih.gov/pmc/articles/PMC5504290/
https://www.ncbi.nlm.nih.gov/pubmed/28681844
http://dx.doi.org/10.1038/ncomms15867

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