Marine clay maturation induces systematic silicon isotope decrease in authigenic clays and pore fluids
Abstract 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 d...
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| Автори: | , , , |
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| Формат: | Artigo |
| Мова: | Inglês |
| Опубліковано: |
Nature Portfolio
2024-10-01
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| Серія: | Communications Earth & Environment |
| Онлайн доступ: | https://doi.org/10.1038/s43247-024-01746-4 |
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