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Silicate weathering feedback hindered by clay formation
Henehan, M.J. (2023). Silicate weathering feedback hindered by clay formation. Nature Geoscience 16(8): 663-664. https://dx.doi.org/10.1038/s41561-023-01242-y
In: Nature Geoscience. Nature Publishing Group: London. ISSN 1752-0894; e-ISSN 1752-0908, more
Related to:
Krause, A.J.; Sluijs, A.; van der Ploeg, R.; Lenton, T.M.; Pogge von Strandmann, P.A.E. (2023). Enhanced clay formation key in sustaining the Middle Eocene Climatic Optimum. Nature Geoscience 16(8): 730-738. https://dx.doi.org/10.1038/s41561-023-01234-y, more
Peer reviewed article  
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Keyword
    Marine/Coastal
Author  Top 
  • Henehan, M.J.
Abstract
    The chemical weathering of silicate rocks plays a central role in stabilizing our climate through CO2 drawdown. Li isotopic evidence from a prolonged Eocene warming event suggests clay formation may disrupt this feedback on intermediate timescales.
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