Experimental determination of carbonate-associated sulfate δ^(34)S in planktonic foraminifera shells
Understanding the coupling of oxygen, carbon, and sulfur cycles in the past is critical for reconstructing the history of biogeochemical cycles, paleoclimatic variations, and oceanic chemistry. The abundance of sulfur isotopes (δ^(34)S) in sulfate from ancient marine carbonates, or carbonate-associ...
Published in: | Geochemistry, Geophysics, Geosystems |
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Main Authors: | , , , , |
Format: | Article in Journal/Newspaper |
Language: | unknown |
Published: |
American Geophysical Union
2014
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Subjects: | |
Online Access: | https://doi.org/10.1002/2014GC005295 |