Constraints on the Role of Marine Authigenic Clay Formation in Determining Seawater Lithium Isotope Composition

Abstract Silicate weathering reactions generate alkalinity that drives carbonate burial in the ocean, ultimately considered to balance solid‐earth CO2 degassing. Because silicate weathering occurs at a climate dependent rate, it provides a negative feedback on long‐term climate evolution that regula...

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Bibliographic Details
Main Authors: Charlotte Läuchli, Nestor Gaviria‐Lugo, Anne Bernhardt, Hella Wittmann, Dirk Sachse, Mahyar Mohtadi, Andreas Lückge, Patrick J. Frings
Format: Article
Language:English
Published: Wiley 2025-03-01
Series:Geochemistry, Geophysics, Geosystems
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Online Access:https://doi.org/10.1029/2024GC012099
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