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...

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Bibliographic Details
Published in:Geochemistry, Geophysics, Geosystems
Main Authors: Paris, Guillaume, Fehrenbacher, Jennifer S., Sessions, Alex L., Spero, Howard J., Adkins, Jess F.
Format: Article in Journal/Newspaper
Language:unknown
Published: American Geophysical Union 2014
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Online Access:https://doi.org/10.1002/2014GC005295