Desulfobacter latus

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Desulfobacter latus
Scientific classification
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D. latus
Binomial name
Desulfobacter latus
Widdel 1988

Desulfobacter latus is a sulfate-reducing bacteria, with type strain AcRS2. [1]

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Related Research Articles

Sulfur-reducing bacteria are microorganisms able to reduce elemental sulfur (S0) to hydrogen sulfide (H2S). These microbes use inorganic sulfur compounds as electron acceptors to sustain several activities such as respiration, conserving energy and growth, in absence of oxygen. The final product or these processes, sulfide, has a considerable influence on the chemistry of the environment and, in addition, is used as electron donor for a large variety of microbial metabolisms. Several types of bacteria and many non-methanogenic archaea can reduce sulfur. Microbial sulfur reduction was already shown in early studies, which highlighted the first proof of S0 reduction in a vibrioid bacterium from mud, with sulfur as electron acceptor and H2 as electron donor. The first pure cultured species of sulfur-reducing bacteria, Desulfuromonas acetoxidans, was discovered in 1976 and described by Pfennig Norbert and Biebel Hanno as an anaerobic sulfur-reducing and acetate-oxidizing bacterium, not able to reduce sulfate. Only few taxa are true sulfur-reducing bacteria, using sulfur reduction as the only or main catabolic reaction. Normally, they couple this reaction with the oxidation of acetate, succinate or other organic compounds. In general, sulfate-reducing bacteria are able to use both sulfate and elemental sulfur as electron acceptors. Thanks to its abundancy and thermodynamic stability, sulfate is the most studied electron acceptor for anaerobic respiration that involves sulfur compounds. Elemental sulfur, however, is very abundant and important, especially in deep-sea hydrothermal vents, hot springs and other extreme environments, making its isolation more difficult. Some bacteria – such as Proteus, Campylobacter, Pseudomonas and Salmonella – have the ability to reduce sulfur, but can also use oxygen and other terminal electron acceptors.

Desulfobacter hydrogenophilus is a strictly anaerobic sulfate-reducing bacterium. It was isolated and characterized in 1987 by Friedrich Widdel of the University of Konstanz (Germany). Like most sulfate-reducing bacteria (SRB), D. hydrogenophilus is capable of completely oxidizing organic compounds (specifically acetate, pyruvate and ethanol) to CO2, and therefore plays a key role in biomineralization in anaerobic marine environments. However, unlike many SRB, D. hydrogenophilus is a facultative lithoautotroph, and can grow using H2 as an electron donor and CO2 as a carbon source. D. hydrogenophilus is also unique because it is psychrophilic (and has been shown to grow at temperatures as low as 0 °C or 32 °F). It is also diazotrophic, or capable of fixing nitrogen.

Archaeoglobus profundus is a sulphate-reducing archaea. Archaeoglobus can be found in high-temperature oil fields where it may contribute to oil field souring. A. profundus grows lithotrophically, and while it needs acetate and CO2 for biosynthesis it is heterotrophic.

Gluconacetobacter sacchari is a species of acetic acid bacteria first isolated from the leaf sheath of sugar cane and from the pink sugar-cane mealy bug on sugar cane growing in Queensland and northern New South Wales. The type strain of this species is strain SRI 1794T. It is notable for its production of bacterial cellulose and for being an endophyte in sugar cane.

Desulfobulbus propionicus is a Gram-negative, anaerobic chemoorganotroph. Three separate strains have been identified: 1pr3T, 2pr4, and 3pr10. It is also the first pure culture example of successful disproportionation of elemental sulfur to sulfate and sulfide. Desulfobulbus propionicus has the potential to produce free energy and chemical products.

Desulfomonile tiedjei is a bacterium. It is anaerobic, dehalogenating, sulfate-reducing, Gram-negative, non-motile, non-spore-forming and rod-shaped. Its type strain is DCB-1.

Halobacillus trueperi is a species of bacteria. It is halophilic, gram-positive, heterotrophic and its type strain is DSM 10404T.

Azospirillum halopraeferens is a species of nitrogen-fixing bacteria associated with the roots of Diplachne fusca and black mangrove. It is microaerophilic and its type strain is Au 4.

Synergistes jonesii is a species of bacteria, the type species of its genus. It is a rumen bacterium that degrades toxic pyridinediols including mimosine. It is obligately anaerobic, gram-negative and rod-shaped. It was discovered in 1981 by Raymond J. Jones in Hawaii and Jones' hypothesis was proven in 1986 by himself and R. G. Megarrity.

Acidiphilium cryptum is a species of heterotrophic bacteria, the type species of its genus. It is gram-negative, aerobic, mesophilic and rod-shaped. It does not form endospores and some cells are motile by means of one polar flagellum or two lateral flagella Lhet2 is the type strain.

Desulfobacterium autotrophicum is a mesophilic sulfate-reducing bacterium. Its genome has been sequenced.

Thermodesulforhabdus norvegica is a species of thermophilic sulfate-reducing bacteria, the type and only species of its genus. It is gram-negative, acetate-oxidizing, with type strain A8444.

Gluconacetobacter johannae is a species of acetic acid bacteria first isolated from rhizospheres and rhizoplanes of coffee plants. Its type strain is CFN-Cf55T.

Gluconacetobacter azotocaptans is a species of acetic acid bacteria first isolated from rhizospheres and rhizoplanes of coffee plants. Its type strain is CFN-Ca54T.

Desulfobacter curvatus is a sulfate-reducing bacteria, with type strain AcRM3.

Desulfobacter vibrioformis is a sulfate-reducing bacteria. It is mesophilic, gram-negative, vibrio-shaped, marine and acetate-oxidizing.

Methylophaga sulfidovorans is an obligately methylotrophic, aerobic, dimethylsulfide-oxidizing bacterium. It is Gram-negative, oval, with strain RB-1.

Desulfobacter halotolerans is a halotolerant, acetate-oxidizing, sulfate-reducing bacteria. It is mesophilic and rod-shaped, with type strain GSL-Ac1.

Desulfonatronum thioautotrophicum is a species of haloalkaliphilic sulfate-reducing bacteria. It is able to grow lithotrophically by dismutation of thiosulfate and sulfite.

"CandidatusThiodictyon syntrophicum" is a gram-negative bacterium classified within purple sulfur bacteria (PSB). "Ca. T. syntrophicum" grows best under micro-oxic and low light conditions. There has only been one successful enrichment of "Ca. T. syntrophicum"; "Ca. T. syntrophicum" strain Cad16T.

References

  1. Widdel, F. (1987). "New types of acetate-oxidizing, sulfate-reducing Desulfobacter species, D. hydrogenophilus sp. nov., D. latus sp. nov., and D. curvatus sp. nov". Archives of Microbiology. 148 (4): 286–291. doi:10.1007/BF00456706. ISSN   0302-8933. S2CID   23489467.

Further reading