Pyrite sulfur isotopes reveal glacial−interglacial environmental changes

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Pyrite sulfur isotopes reveal glacial-interglacial environmental changes.

The sulfur biogeochemical cycle plays a key role in regulating Earth's surface redox through diverse abiotic and biological reactions that have distinctive stable isotopic fractionations. As such, variations in the sulfur isotopic composition (δ34S) of sedimentary sulfate and sulfide phases over Earth history can be used to infer substantive changes to the Earth's surface environment, including...

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ژورنال

عنوان ژورنال: Proceedings of the National Academy of Sciences

سال: 2017

ISSN: 0027-8424,1091-6490

DOI: 10.1073/pnas.1618245114