Biology:Methanothermococcus okinawensis

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Short description: Species of archaeon

Methanothermococcus okinawensis
Scientific classification
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M. okinawensis
Binomial name
Methanothermococcus okinawensis
Takai et al. 2002

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 (=JCM 11175T =DSM 14208T).[1] 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.[1] Research studies indicate that it might be able to survive extreme conditions in solar system's other bodies, such as Saturn's moon Enceladus.[2]

See also

  • Methanogens

References

  1. 1.0 1.1 Takai, K. (2002). "Methanothermococcus okinawensis sp. nov., a thermophilic, methane-producing archaeon isolated from a Western Pacific deep-sea hydrothermal vent system". International Journal of Systematic and Evolutionary Microbiology 52 (4): 1089–1095. doi:10.1099/ijs.0.02106-0. ISSN 1466-5026. 
  2. Taubner, R.-S. (2018). "Biological methane production under putative Enceladus-like conditions". Nature Communications 9 (748): 748. doi:10.1038/s41467-018-02876-y. PMID 29487311. Bibcode2018NatCo...9..748T. 

Further reading

External links

Wikidata ☰ Q18344108 entry