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|a Discovery of a novel methanogen prevalent in thawing permafrost |h [electronic resource]. |
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|a [S.l.] : |b Macmillan Publishers Limited, |c 2014. |
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|a Nature Communications. |
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|a Please contact the owning institution for licensing and permissions. It is the user's responsibility to ensure use does not violate any third party rights. |
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|a Thawing permafrost promotes microbial degradation of cryo-sequestered and new carbon
leading to the biogenic production of methane, creating a positive feedback to climate change.
Here we determine microbial community composition along a permafrost thaw gradient in
northern Sweden. Partially thawed sites were frequently dominated by a single archaeal
phylotype, Candidatus ‘Methanoflorens stordalenmirensis’ gen. nov. sp. nov., belonging to the
uncultivated lineage ‘Rice Cluster II’ (Candidatus ‘Methanoflorentaceae’ fam. nov.). Metagenomic
sequencing led to the recovery of its near-complete genome, revealing the genes
necessary for hydrogenotrophic methanogenesis. These genes are highly expressed and
methane carbon isotope data are consistent with hydrogenotrophic production of methane in
the partially thawed site. In addition to permafrost wetlands, ‘Methanoflorentaceae’ are
widespread in high methane-flux habitats suggesting that this lineage is both prevalent and
a major contributor to global methane production. In thawing permafrost, Candidatus
‘M. stordalenmirensis’ appears to be a key mediator of methane-based positive feedback to
climate warming. |
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|a Electronic reproduction. |c Florida International University, |d 2015. |f (dpSobek) |n Mode of access: World Wide Web. |n System requirements: Internet connectivity; Web browser software. |
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|a Nathan C. VerBerkmoes. |
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|a dpSobek |c Sea Level Rise |
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|u http://dpanther.fiu.edu/dpService/dpPurlService/purl/FI15052502/00001 |y Click here for full text |
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|a http://dpanther.fiu.edu/sobek/content/FI/15/05/25/02/00001/FI15052502_thm.jpg |