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Methanogens are microorganisms that produce methane as a metabolic byproduct in hypoxic conditions. They are prokaryotic and belong to the domain Archaea. All known methanogens are members of the archaeal phylum Euryarchaeota. Methanogens are common in wetlands, where they are responsible for marsh gas, and in the digestive tracts of animals such as ruminants and many humans, where they are responsible for the methane content of belching in ruminants and flatulence in humans. In marine sediments, the biological production of methane, also termed methanogenesis, is generally confined to where sulfates are depleted, below the top layers. Moreover, methanogenic archaea populations play an indispensable role in anaerobic wastewater treatments. Others are extremophiles, found in environments such as hot springs and submarine hydrothermal vents as well as in the "solid" rock of Earth's crust, kilometers below the surface.
Horonobe-cho is a town located in Sōya Subprefecture, Hokkaido, Japan. There is a JR train station, Horonobe Station which connects Horonobe-town with other cities in Hokkaido.
Ferroplasma is a genus of Archaea that belong to the family Ferroplasmaceae. Members of the Ferroplasma are typically acidophillic, pleomorphic, irregularly shaped cocci.
Methanosarcina acetivorans is a versatile methane producing microbe which is found in such diverse environments as oil wells, trash dumps, deep-sea hydrothermal vents, and oxygen-depleted sediments beneath kelp beds. Only M. acetivorans and microbes in the genus Methanosarcina use all three known metabolic pathways for methanogenesis. Methanosarcinides, including M. acetivorans, are also the only archaea capable of forming multicellular colonies, and even show cellular differentiation. The genome of M. acetivorans is one of the largest archaeal genomes ever sequenced. Furthermore, one strain of M. acetivorans, M. a. C2A, has been identified to possess an F-type ATPase along with an A-type ATPase.
In biology, syntrophy, synthrophy, or cross-feeding is the phenomenon of one species feeding on the metabolic products of another species to cope up with the energy limitations by electron transfer. In this type of biological interaction, metabolite transfer happens between two or more metabolically diverse microbial species that live in close proximity to each other. The growth of one partner depends on the nutrients, growth factors, or substrates provided by the other partner. Thus, syntrophism can be considered as an obligatory interdependency and a mutualistic metabolism between two different bacterial species.
Thermococcus celer is a Gram-negative, spherical-shaped archaeon of the genus Thermococcus. The discovery of T. celer played an important role in rerooting the tree of life when T. celer was found to be more closely related to methanogenic Archaea than to other phenotypically similar thermophilic species. T. celer was the first archaeon discovered to house a circularized genome. Several type strains of T. celer have been identified: Vu13, ATCC 35543, and DSM 2476.
Methanocaldococcus jannaschii is a thermophilic methanogenic archaean in the class Methanococci. It was the first archaeon to have its complete genome sequenced. The sequencing identified many genes unique to the archaea. Many of the synthesis pathways for methanogenic cofactors were worked out biochemically in this organism, as were several other archaeal-specific metabolic pathways.
Methanothrix soehngenii is a species of methanogenic archaea. Its cells are non-motile, non-spore-forming, rod-shaped and are normally combined end to end in long filaments, surrounded by a sheath-like structure. It is named in honour of N. L. Söhngen.
Methylosphaera hansonii, also called Antarctic budding methanotroph AM6, is a species of psychrophilic, group I methanotrophs, named after microbiologist Richard S. Hanson. It is non-motile, coccoidal in morphology, does not form resting cells, reproduces by constriction, and requires seawater for growth. Its type strain is ACAM 549.
Clostridium uliginosum is a mesophilic bacterium oxidizing acetate in syntrophic association with a hydrogenotrophic methanogenic bacterium. It is a spore-forming, gram-positive, rod-shaped organism, with type strain BST. Its genome has been sequenced.
Methanococcus maripaludis is a species of methanogen. It is anaerobic, weakly motile, non-spore-forming, Gram-negative, and a pleomorphic coccoid-rod averaging 1.2 by 1.6 μm is size. Its genome has been sequenced.
Methanothermobacter marburgensis is a thermophilic and obligately autotrophic archaeon. Its type strain is MarburgT. Its genome has been sequenced.
Methanomethylovorans thermophila is a species of thermophilic, methylotrophic methanogenic microbe. It is Gram-negative, and its type strain is L2FAWT. It was isolated from an anaerobic reactor in a laboratory. Its cells are Gram-negative, non-motile, and coccoid in form. It has been found to use methanol and methyl amines as substrates in the production of methane. It cannot use formiate, carbon dioxide with hydrogen, acetate, dimethyl sulfide, methanethiol, or propanol. As its name suggests, it is a thermophile, with an optimal growth temperature of 50 °C.
Desulfurella acetivorans is a thermophilic acetate-oxidizing sulfur-reducing eubacterium. It is Gram-negative, short rod-shaped, motile, with a single polar flagellum.
Desulfurella multipotens is a thermophilic sulfur-reducing eubacterium. It is 1.5–1.8 by 0.5–0.7 μm in size, Gram-negative, rod-shaped, motile, with a single polar flagellum.
Anaerolinea thermophila is a species of filamentous thermophilic bacteria, the type and only species of its genus. It is Gram-negative, non-spore-forming, with type strain UNI-1T.
Methanothermococcus okinawensis is a thermophilic, methane-producing archaeon first isolated from deep-sea hydrothermal vent on the western Pacific Ocean. Its cells are highly motile, irregular cocci, with a polar bundle of flagella. Its type strain is IH1T. It grows at an optimal temperature of 60–65 °C and pH of 6.7. It is strictly anaerobic and reduces carbon dioxide with hydrogen to produce methane, but it can also use formate. Research studies indicate that it might be able to survive extreme conditions in solar system's other bodies, such as Saturn's moon Enceladus.
Methanobrevibacter oralis is a species of coccobacillary, non-motile, Gram-positive, methane-producing archaeon.
References
- ↑ Zinder, S. H.; Sowers, K. R.; Ferry, J. G. (1985). "NOTES: Methanosarcina thermophila sp. nov., a Thermophilic, Acetotrophic, Methane-Producing Bacterium". International Journal of Systematic Bacteriology. 35 (4): 522–523. doi: 10.1099/00207713-35-4-522 . ISSN 0020-7713.
