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Journal ArticleDOI

Multiple sulfur isotopes and the evolution of Earth's surface sulfur cycle

David T. Johnston
- 01 May 2011 - 
- Vol. 106, Iss: 1, pp 161-183
TLDR
Canfield et al. as discussed by the authors presented a review of recent works in multiple sulfur isotope geochemistry with a focus on results that inform our understanding of biogeochemical processes and Earth surface evolution.
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This article is published in Earth-Science Reviews.The article was published on 2011-05-01. It has received 318 citations till now. The article focuses on the topics: Isotope geochemistry.

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Citations
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Geochemistry of pyrite from diamictites of the Boolgeeda Iron Formation, Western Australia with implications for the GOE and Paleoproterozoic ice ages

TL;DR: In this paper, a compilation of S-isotope data from pyrite in the Boundary Ridge diamictites analyzed in this study and previous work ( Williford et al., 2011 ) defines multiple δ 34 S vs. δ 33 S arrays, consistent with an origin of detrital pyrites from the underlying Hamersley and Fortescue groups.
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Aspects of the Archean-Proterozoic transition: How the great Huronian Glacial Event was initiated by rift-related uplift and terminated at the rift-drift transition during break-up of Lauroscandia

TL;DR: Mazumder and Eriksson as mentioned in this paper showed that the early Archean-Proterozoic sedimentary record contains evidence of the world's first widespread glacial episodes, which have come to be known as the Huronian Glacial Event.
Journal ArticleDOI

Sulfur isotope characterization of primordial and recycled sources feeding the Samoan mantle plume

TL;DR: In this paper, the relationship between Δ 33 S and radiogenic tungsten, helium and lead isotopes from 7 Samoan basalts (from the islands of Ofu, Vailulu'u and Malumalu) was investigated.

Reconstructing Earth's Surface Oxidation Across The Archean- Proterozoic Transition

TL;DR: In this article, the earliest recorded positive carbon isotope anomaly was found in the Transvaal Supergroup of South Africa, in phase with sulfur isotopes, and the authors linked these environmental perturbations to the Great Oxidation Event (ca. 2.3 Ga).
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Quantification of sulphide oxidation rates in marine sediment

TL;DR: In this paper, the authors present an experimental method to directly determine sulphide oxidation rates in undiluted marine sediment incubations and find that sulphide oxidization rates in the top two centimetres of organic-rich coastal sediments were greater than rates of sulphide production through sulphate reduction.
References
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Book

Geochemistry of Hydrothermal Ore Deposits

TL;DR: In this paper, Skinner et al. discuss the relationship between hydrous alteration and its relationship to hydrous fluid composition in the formation of sulfide-sulfide ores.
Journal ArticleDOI

Sedimentary pyrite formation: An update

TL;DR: In this article, it was shown that organic matter appears to be the major control on pyrite formation in normal (non-euxinic) terrigenous marine sediments where dissolved sulfate and iron minerals are abundant.
Journal ArticleDOI

The age curves of sulfur and oxygen isotopes in marine sulfate and their mutual interpretation

TL;DR: In this article, a model involving symmetrical fluxes is introduced to take advantage of the oxygen data, and the measured δ34S and δ18O correspond to variations in these isotopes in sulfate of the world ocean surface.
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