An integrated model of mineral weathering and carbon cycling reveals the substantial influence that clay minerals originating from the weathering of magnesium-rich rocks have on Earth’s climate. This research indicates that this clay-forming process contributed to each Palaeozoic glaciation.
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References
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This is a summary of: Murray, J. & Jagoutz, O. Palaeozoic cooling modulated by ophiolite weathering through organic carbon preservation. Nat. Geosci. https://doi.org/10.1038/s41561-023-01342-9 (2023).
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Clay minerals store organic carbon and cool Earth’s climate over millions of years. Nat. Geosci. 17, 8–9 (2024). https://doi.org/10.1038/s41561-023-01353-6
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DOI: https://doi.org/10.1038/s41561-023-01353-6
