Middle Eocene greenhouse warming facilitated by diminished weathering feedback
Silicate rock weathering represents a negative feedback mechanism that regulates atmospheric CO2 levels on geological timescales. Here, the authors show that a diminished silicate weathering feedback may have set the stage for greenhouse warming and ocean acidification during the Middle Eocene, ~40...
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Autores principales: | Robin van der Ploeg, David Selby, Margot J. Cramwinckel, Yang Li, Steven M. Bohaty, Jack J. Middelburg, Appy Sluijs |
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Formato: | article |
Lenguaje: | EN |
Publicado: |
Nature Portfolio
2018
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Materias: | |
Acceso en línea: | https://doaj.org/article/7766b14b17574352ae11759b896d0d86 |
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