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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.
About
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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Journal ArticleDOI

Rethinking the Ancient Sulfur Cycle

TL;DR: In this article, the deep-time δ34S record of marine sulfates and sulfides is reviewed in light of recent advances in understanding the sulfur biogeochemical cycle.
Journal ArticleDOI

Influence of sulfate reduction rates on the Phanerozoic sulfur isotope record

TL;DR: Experiments linking the magnitude of fractionations of the multiple sulfur isotopes to the rate of microbial sulfate reduction demonstrate that such fractionations are controlled by the availability of electron donor (organic matter), rather than by the concentration of electron acceptor (sulfate), an environmental constraint that varies among sedimentary burial environments.
Journal ArticleDOI

Rapid oxygenation of Earth’s atmosphere 2.33 billion years ago

TL;DR: The new data suggest that the oxygenation occurred rapidly—within 1 to 10 million years—and was followed by a slower rise in the ocean sulfate inventory, whereas the relationships among GOE, “Snowball Earth” glaciation, and biogeochemical cycling will require further stratigraphic correlation supported with precise chronologies and paleolatitude reconstructions.
Book ChapterDOI

A Post-Genomic View of the Ecophysiology, Catabolism and Biotechnological Relevance of Sulphate-Reducing Prokaryotes

TL;DR: The wealth of publications in this period is a testimony to the large environmental, biogeochemical and technological relevance of these organisms and how much the field has progressed in these years, although many important questions and applications remain to be explored.
Journal ArticleDOI

Anomalous sulphur isotopes in plume lavas reveal deep mantle storage of Archaean crust

TL;DR: Anomalous sulphur isotope signatures indicating mass-independent fractionation (MIF) in olivine-hosted sulphides from 20-million-year-old ocean island basalts from Mangaia, Cook Islands (Polynesia), which have been suggested to sample recycled oceanic crust, suggest that sulphur was subducted into the mantle before 2.45 billion years ago and recycled into theantle source of Mangaia lavas.
References
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Journal ArticleDOI

Morphological and ecological complexity in early eukaryotic ecosystems

TL;DR: It is shown that the cytoskeletal and ecological prerequisites for eukaryotic diversification were already established in eukARYotic microorganisms fossilized nearly 1,500 Myr ago in shales of the early Mesoproterozoic Roper Group in northern Australia.
Journal ArticleDOI

History and applications of mass-independent isotope effects

TL;DR: The discovery of the first chemically produced mass-independent isotope effect in 1983 by Thiemens & Heidenreich opened a broad variety of applications, including physical chemistry studies, atmospheric chemistry, paleoclimatology, biologic primary productivity assessment, Solar System origin and evolution, planetary atmospheres (Mars), and the origin of life in Earth's earliest environment.
Journal ArticleDOI

Late Archean Biospheric Oxygenation and Atmospheric Evolution

TL;DR: The correlation of the time-series sulfur isotope signals in northwestern Australia with equivalent strata from South Africa suggests that changes in the exogenic sulfur cycle recorded in marine sediments were global in scope and were linked to atmospheric evolution.
Journal ArticleDOI

The Early Faint Sun Paradox: Organic Shielding of Ultraviolet-Labile Greenhouse Gases

TL;DR: It is shown that ultraviolet absorption by steady-state amounts of high-altitude organic solids produced from methane photolysis may have shielded ammonia sufficiently that ammonia resupply rates were able to maintain surface temperatures above freezing.
Journal ArticleDOI

Variations in the S33, S34, and S36 contents of meteorites and their relation to chemical and nuclear effects

TL;DR: The isotopic ratios S33/S32, S34/S 32, and S36, S32 of the different forms of sulfur in a number of meteorites have been studied as mentioned in this paper.
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