Denitrifiers, nitrogen-fixing bacteria and N₂O soil gas flux in high Arctic ice-wedge polygon cryosols

Climate warming and subsequent permafrost thaw may result in organic carbon and nutrient stores being metabolized by microbial communities, resulting in a positive feedback loop of greenhouse gas (GHG) soil emissions. As the third most important GHG, understanding nitrous oxide (N₂O) flux in Arctic...

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Bibliographic Details
Published in:FEMS Microbiology Ecology
Main Authors: Altshuler, Ianina, Ronholm, Jennifer, Layton, Alice, Onstott, Tullis C., Greer, Charles W., Whyte, Lyle G.
Format: Article in Journal/Newspaper
Language:English
Published: Oxford 2019
Subjects:
Ice
Online Access:https://doi.org/10.1093/femsec/fiz049
https://nrc-publications.canada.ca/eng/view/object/?id=700d5bf8-1750-4b4b-88f8-746e97d338f1
https://nrc-publications.canada.ca/fra/voir/objet/?id=700d5bf8-1750-4b4b-88f8-746e97d338f1
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Summary:Climate warming and subsequent permafrost thaw may result in organic carbon and nutrient stores being metabolized by microbial communities, resulting in a positive feedback loop of greenhouse gas (GHG) soil emissions. As the third most important GHG, understanding nitrous oxide (N₂O) flux in Arctic mineral ice-wedge polygon cryosols and its relationship to the active microbial community is potentially a key parameter for understanding future GHG emissions and climatic warming potential. In the present study, metatranscriptomic analyses of active layer Arctic cryosols, at a representative ice-wedge polygon site, identified active nitrogen-fixing and denitrifying bacteria that included members of Rhizobiaceae, Nostocaceae, Cyanothecaceae, Rhodobacteraceae, Burkholderiaceae, Chloroflexaceae, Azotobacteraceae and Ectothiorhodospiraceae. Unique microbial assemblages with higher proportion of Rhodobacteriales and Rhocyclales were identified by targeted functional gene sequencing at locations with higher (P = 0.053) N₂O emissions in the wetter trough soils compared with the dryer polygon interior soils. This coincided with a higher relative abundance of the denitrification nirS gene and higher nitrate/nitrite concentrations in trough soils. The elevated N₂O flux observed from wetter trough soils compared with drier polygon interior soils is concerning from a climate warming perspective, since the Arctic is predicted to become warmer and wetter. Peer reviewed: Yes NRC publication: Yes