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dc.contributor.authorCoolen, Marco J. L.  Concept link
dc.contributor.authorOrsi, William D.  Concept link
dc.date.accessioned2015-05-12T19:06:35Z
dc.date.available2015-05-12T19:06:35Z
dc.date.issued2015-03-16
dc.identifier.citationFrontiers in Microbiology 6 (2015): 197en_US
dc.identifier.urihttps://hdl.handle.net/1912/7281
dc.description© The Author(s), 2015. This article is distributed under the terms of the Creative Commons Attribution License. The definitive version was published in Frontiers in Microbiology 6 (2015): 197, doi:10.3389/fmicb.2015.00197.en_US
dc.description.abstractThawing of permafrost soils is expected to stimulate microbial decomposition and respiration of sequestered carbon. This could, in turn, increase atmospheric concentrations of greenhouse gasses, such as carbon dioxide and methane, and create a positive feedback to climate warming. Recent metagenomic studies suggest that permafrost has a large metabolic potential for carbon processing, including pathways for fermentation and methanogenesis. Here, we performed a pilot study using ultrahigh throughput Illumina HiSeq sequencing of reverse transcribed messenger RNA to obtain a detailed overview of active metabolic pathways and responsible organisms in up to 70 cm deep permafrost soils at a moist acidic tundra location in Arctic Alaska. The transcriptional response of the permafrost microbial community was compared before and after 11 days of thaw. In general, the transcriptional profile under frozen conditions suggests a dominance of stress responses, survival strategies, and maintenance processes, whereas upon thaw a rapid enzymatic response to decomposing soil organic matter (SOM) was observed. Bacteroidetes, Firmicutes, ascomycete fungi, and methanogens were responsible for largest transcriptional response upon thaw. Transcripts indicative of heterotrophic methanogenic pathways utilizing acetate, methanol, and methylamine were found predominantly in the permafrost table after thaw. Furthermore, transcripts involved in acetogenesis were expressed exclusively after thaw suggesting that acetogenic bacteria are a potential source of acetate for acetoclastic methanogenesis in freshly thawed permafrost. Metatranscriptomics is shown here to be a useful approach for inferring the activity of permafrost microbes that has potential to improve our understanding of permafrost SOM bioavailability and biogeochemical mechanisms contributing to greenhouse gas emissions as a result of permafrost thaw.en_US
dc.description.sponsorshipThis work was fostered by grants from WHOI's Arctic Research Initiative to MJLC and AS, as well as a Center for Dark Energy Biosphere Investigations (CDEBI) grant OCE-0939564 to WDO.en_US
dc.format.mimetypeapplication/pdf
dc.format.mimetypeapplication/msword
dc.language.isoen_USen_US
dc.publisherFrontiers Mediaen_US
dc.relation.urihttps://doi.org/10.3389/fmicb.2015.00197
dc.rightsAttribution 4.0 International*
dc.rights.urihttp://creativecommons.org/licenses/by/4.0/
dc.titleThe transcriptional response of microbial communities in thawing Alaskan permafrost soilsen_US
dc.typeArticleen_US
dc.identifier.doi10.3389/fmicb.2015.00197


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Attribution 4.0 International
Except where otherwise noted, this item's license is described as Attribution 4.0 International