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Concentration and transport of nitrate by the mat-forming sulphur bacterium Thioploca

MPG-Autoren
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Jørgensen,  Bo Barker
Department of Biogeochemistry, Max Planck Institute for Marine Microbiology, Max Planck Society;

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Huettel,  Markus
Flux Group, Max Planck Institute for Marine Microbiology, Max Planck Society;

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Schulz,  H. D.
Ecophysiology Group, Max Planck Institute for Marine Microbiology, Max Planck Society;

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Canfield,  Donald E.
Department of Biogeochemistry, Max Planck Institute for Marine Microbiology, Max Planck Society;

Forster ,  S.
Department of Biogeochemistry, Max Planck Institute for Marine Microbiology, Max Planck Society;

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Glud,  Ronnie Nohr
Permanent Research Group Microsensor, Max Planck Institute for Marine Microbiology, Max Planck Society;

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Gundersen,  Jens Kristian
Permanent Research Group Microsensor, Max Planck Institute for Marine Microbiology, Max Planck Society;

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Küver,  Jan
Department of Microbiology, Max Planck Institute for Marine Microbiology, Max Planck Society;

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Ramsing,  N.B.
Department of Molecular Ecology, Max Planck Institute for Marine Microbiology, Max Planck Society;

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Teske,  Andreas
Department of Molecular Ecology, Max Planck Institute for Marine Microbiology, Max Planck Society;

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Thamdrup,  B.
Department of Biogeochemistry, Max Planck Institute for Marine Microbiology, Max Planck Society;

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Zitation

Fossing, H., Gallardo, V., Jørgensen, B. B., Huettel, M., Nielsen, L., Schulz, H. D., et al. (1995). Concentration and transport of nitrate by the mat-forming sulphur bacterium Thioploca. Nature, 374(6524), 713-715. doi:10.1038/374713a0.


Zitierlink: https://hdl.handle.net/21.11116/0000-0004-A7D7-D
Zusammenfassung
MARINE species of Thioploca occur over 3,000 km along the continental shelf off Southern Peru and North and Central Chile(1-4). These filamentous bacteria live in bundles surrounded by a common sheath and form thick mats on the sea floor under the oxygen-minimum zone in the upwelling region, at between 40 and 280 m water depth. The metabolism of this marine bacterium(5,6) remained a mystery until long after its discovery(1,7). We report here that Thioploca cells are able to concentrate nitrate to up to 500 mM in a liquid vacuole that occupies >80% of the cell volume. Gliding filaments transport this nitrate 5-10 cm down into the sediment and reduce it, with concomitant oxidation of hydrogen sulphide, thereby coupling the nitrogen and sulphur cycles in the sediment.