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Journal Article

Microbial consumption of zero-valence sulfur in marine benthic habitats

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Pjevac,  P.
Department of Molecular Ecology, Max Planck Institute for Marine Microbiology, Max Planck Society;

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Kamyshny,  A.
Department of Biogeochemistry, Max Planck Institute for Marine Microbiology, Max Planck Society;

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Dyksma,  S.
Department of Molecular Ecology, Max Planck Institute for Marine Microbiology, Max Planck Society;

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Mußmann,  M.
Department of Molecular Ecology, Max Planck Institute for Marine Microbiology, Max Planck Society;

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Citation

Pjevac, P., Kamyshny, A., Dyksma, S., & Mußmann, M. (2014). Microbial consumption of zero-valence sulfur in marine benthic habitats. Environmental Microbiology, 16(11 Sp. Iss. SI), 3416-3430.


Cite as: http://hdl.handle.net/21.11116/0000-0001-C4DE-8
Abstract
Zero-valence sulfur (S-0) is a central intermediate in the marine sulfur cycle and forms conspicuous accumulations at sediment surfaces, hydrothermal vents and in oxygen minimum zones. Diverse microorganisms can utilize S-0, but those consuming S-0 in the environment are largely unknown. We identified possible key players in S-0 turnover on native or introduced S-0 in benthic coastal and deep-sea habitats using the 16S ribosomal RNA approach, (in situ) growth experiments and activity measurements. In all habitats, the epsilonproteobacterial Sulfurimonas/Sulfurovum group accounted for a substantial fraction of the microbial community. Deltaproteobacterial Desulfobulbaceae and Desulfuromonadales were also frequently detected, indicating S-0 disproportionation and S-0 respiration under anoxic conditions. Sulfate production from S-0 particles colonized in situ with Sulfurimonas/Sulfurovum suggested that this group oxidized S-0. We also show that the type strain Sulfurimonas denitrificans is able to access cyclooctasulfur (S-8), a metabolic feature not yet demonstrated for sulfur oxidizers. The ability to oxidize S-0, in particular S-8, likely facilitates niche partitioning among sulfur oxidizers in habitats with intense microbial sulfur cycling such as sulfidic sediment surfaces. Our results underscore the previously overlooked but central role of Sulfurimonas/Sulfurovum group for conversion of free S-0 at the seafloor surface.