ArticleFrontiers in microbiology2019
Formation of Large Native Sulfur Deposits Does Not Require Molecular Oxygen.
Article in Frontiers in microbiology, 2019. The graph could read no effect estimate from its abstract, so it casts no vote on the map. Cited by 6 papers.
What it found
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The abstract states no effect estimate the extractor could read, or names no intervention and outcome on the map, so this paper lights no cell and moves no belief. It is still indexed, cited and linked below.
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Who cites it
6 citing papers in PubMed, 38 citations in OpenAlex.
- Light and polyphosphate kinase 2 cooperatively regulate the production of zero-valent sulfur in a deep-sea bacterium.mSystems · 2025Article
- Generation of zero-valent sulfur from dissimilatory sulfate reduction in sulfate-reducing microorganisms.Proceedings of the National Academy of Sciences of the United States of America · 2023Article
- A deep-sea sulfate-reducing bacterium generates zero-valent sulfur via metabolizing thiosulfate.mLife · 2022Article
- Gene Sets and Mechanisms of Sulfate-Reducing Bacteria Biofilm Formation and Quorum Sensing With Impact on Corrosion.Frontiers in microbiology · 2021Review
- A novel bacterial thiosulfate oxidation pathway provides a new clue about the formation of zero-valent sulfur in deep sea.The ISME journal · 2020Article
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Corrections and comments
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Authors and funding
4 authors at 3 institutions in 3 countries.
Funding
No grant is acknowledged in the PubMed record.
Abstract
Large native (i.e., elemental) sulfur deposits can be part of caprock assemblages found on top of or in lateral position to salt diapirs and as stratabound mineralization in gypsum and anhydrite lithologies. Native sulfur is formed when hydrocarbons come in contact with sulfate minerals in presence of liquid water. The prevailing model for native sulfur formation in such settings is that sulfide produced by sulfate-reducing bacteria is oxidized to zero-valent sulfur in presence of molecular oxygen (O
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Registered trials
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