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Methylacidiphilum fumariolicum is an autotrophic bacterium first described in 2007 growing on volcanic pools near Naples, Italy. It grows in mud at temperatures between 50 °C - 60 °C and an acidic pH of 2–5. It is able to oxidize methane gas. It uses ammonium, nitrate or atmospheric nitrogen as a nitrogen source and fixes carbon dioxide. Due to the presence of a lanthanide dependent methanol dehydrogenase enzyme, its growth is strictly dependent on the abundance of rare-earth metals.

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  • Methylacidiphilum fumariolicum is an autotrophic bacterium first described in 2007 growing on volcanic pools near Naples, Italy. It grows in mud at temperatures between 50 °C - 60 °C and an acidic pH of 2–5. It is able to oxidize methane gas. It uses ammonium, nitrate or atmospheric nitrogen as a nitrogen source and fixes carbon dioxide. Due to the presence of a lanthanide dependent methanol dehydrogenase enzyme, its growth is strictly dependent on the abundance of rare-earth metals. No biotic interactions between M. fumariolicum and other organisms are known, probably due to the extreme environment the bacteria needs in order to grow. (en)
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  • Methylacidiphilum fumariolicum (en)
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  • H. Op den Camp, et al 2007 (en)
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  • Unclassified (en)
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  • Methylacidiphilum (en)
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  • M. fumariolicum (en)
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  • Methylacidiphilum fumariolicum is an autotrophic bacterium first described in 2007 growing on volcanic pools near Naples, Italy. It grows in mud at temperatures between 50 °C - 60 °C and an acidic pH of 2–5. It is able to oxidize methane gas. It uses ammonium, nitrate or atmospheric nitrogen as a nitrogen source and fixes carbon dioxide. Due to the presence of a lanthanide dependent methanol dehydrogenase enzyme, its growth is strictly dependent on the abundance of rare-earth metals. (en)
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  • Methylacidiphilum fumariolicum (en)
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