Explaining the Structure of the Archean Mass-Independent Sulfur Isotope Record

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Pathways for Neoarchean pyrite formation constrained by mass-independent sulfur isotopes

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Neoarchaean seawater sulphate concentrations from sulphur isotopes in massive sulphide ore

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Evidence of magnetic isotope effects during thermochemical sulfate reduction

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Atmospheric sulfur rearrangement 2.7 billion years ago: Evidence for oxygenic photosynthesis

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Production, preservation, and biological processing of mass-independent sulfur isotope fractionation in the Archean surface environment

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Mercury (Hg) mineral evolution: A mineralogical record of supercontinent assembly, changing ocean geochemistry, and the emerging terrestrial biosphere

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Large sulfur isotope fractionations associated with Neoarchean microbial sulfate reduction

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Excitation band dependence of sulfur isotope mass-independent fractionation during photochemistry of sulfur dioxide using broadband light sources

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Archean cherts in banded iron formation: Insight into Neoarchean ocean chemistry and depositional processes

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Neoarchean carbonate–associated sulfate records positive Δ 33 S anomalies

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Episodic concentration of gold to ore grade through Earth's history

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Sulfate-reducing bacteria unearthed: ecological functions of the diverse prokaryotic group in terrestrial environments

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Multiple sulfur isotopes in Paleoarchean barites identify an important role for microbial sulfate reduction in the early marine environment

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SQUID–SIMS is a useful approach to uncover primary signals in the Archean sulfur cycle

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A multiple sulfur and organic carbon isotope record from non-conglomeratic sedimentary rocks of the Mesoarchean Witwatersrand Supergroup, South Africa

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Formation of oxidized sulfur-rich magmas in Neoarchaean subduction zones

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Examining Archean methanotrophy

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Sulfur isotope's signal of nanopyrites enclosed in 2.7 Ga stromatolitic organic remains reveal microbial sulfate reduction

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On the relationship between oxidation state and temperature of volcanic gas emissions

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Reconciling discrepant minor sulfur isotope records of the Great Oxidation Event

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Pyrite in a sulfate-poor Paleoarchean basin was derived predominantly from elemental sulfur: Evidence from 3.2 Ga sediments in the Barberton Greenstone Belt, Kaapvaal Craton

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Methane in the Precambrian atmosphere

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Anoxic continental surface weathering recorded by the 2.95 Ga Denny Dalton Paleosol (Pongola Supergroup, South Africa)

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Large igneous provinces track fluctuations in subaerial exposure of continents across the Archean–Proterozoic transition

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Can organic haze and O2 plumes explain patterns of sulfur mass-independent fractionation during the Archean?

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