Sulfide oxidation affects the preservation of sulfur isotope signals

Alyssa J. Findlay*, Valeria Boyko, André Pellerin, Khoren Avetisyan, Qingjun Guo, Xi Yang, Alexey Kamyshny

*Corresponding author for this work

Research output: Contribution to journalArticlepeer-review

17 Scopus citations

Abstract

The accumulation of oxygen in Earth's atmosphere and oceans in the late Archean had profound implications for the planet's biogeochemical evolution. Oxygen impacts sulfur cycling through the oxidation of sulfide minerals and the production of sulfate for microbial sulfate reduction (MSR). The isotopic signature of sulfur species preserved in the geologic record is affected by the prevailing biological and chemical processes and can therefore be used to constrain past oxygen and sulfate concentrations. Here, in a study of a late Archean analogue, we find that the sulfur isotopic signature in the water column of a seasonally stratified lake in southern China is influenced by MSR, whereas model results indicate that the isotopic signature of the underlying sediments can be best explained by concurrent sulfate reduction and sulfide oxidation. These data demonstrate that small apparent sulfur isotope fractionations (δ34Ssulfate-AVS = 4.2‰-1.5‰; AVS-acid volatile sulfides) can be caused by dynamic sulfur cycling at millimolar sulfate concentrations. This is in contrast to current interpretations of the isotopic record and indicates that small fractionations do not necessarily indicate very low sulfate or oxygen.

Original languageAmerican English
Pages (from-to)739-743
Number of pages5
JournalGeology
Volume47
Issue number8
DOIs
StatePublished - 1 Aug 2019
Externally publishedYes

Bibliographical note

Publisher Copyright:
© 2019 Geological Society of America.

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