Marine clay maturation induces systematic silicon isotope decrease in authigenic clays and pore fluids

Marine silicate alteration exerts a major influence on marine carbon and cation cycles, but has proven difficult to quantify. In this context, silicon isotopes of marine pore fluids became an important tracer. However, poorly constrained silicon isotope signatures of precipitates produced during sil...

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Bibliographic Details
Published in:	Communications earth & environment Vol. 5; no. 1; pp. 573 - 8
Main Authors:	Geilert, Sonja, Frick, Daniel A., Abbott, April N., Löhr, Stefan C.
Format:	Journal Article
Language:	English
Published:	London Nature Publishing Group UK 09-10-2024 Nature Publishing Group Nature Portfolio
Subjects:	704/47/4112 704/47/4113 704/829/827 Aluminum Carbon Carbon cycle Cations Chemical analysis Clay Earth and Environmental Science Earth Sciences Environment Geochemical cycles Iron Isotopes Maturation Potassium oxides Precipitates Seawater Sediments Signatures Silicon Silicon isotopes Smectites Uncertainty analysis Water analysis
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