Ed R C Hornibrook
Substantial high-affinity methanotroph populations in Andisols effect high rates of atmospheric methane oxidation
Hornibrook, Ed R C; Maxfield, Pete J.; Evershed, Richard P.
Authors
Pete Maxfield Pete.Maxfield@uwe.ac.uk
Senior Lecturer in Environmental Chemistry
Richard P. Evershed
Abstract
Methanotrophic bacteria in soils derived from volcanic ash (Andisols) were characterized via time series 13C-phospholipid fatty acid (PLFA) labelling. Three Andisols were incubated under 2 ppmv 13CH 4 for up to 18 weeks, thus enabling high-affinity methanotrophs to be selectively characterized and quantified. PLFA profiles from all soils were broadly similar, but the magnitude of the high-affinity methanotrophic populations determined through 13C-PLFA-stable isotope probing displayed sizeable differences. Substantial incorporation of 13C indicated very large high-affinity methanotrophic populations in two of the soils. Such high values are far in excess (10×) of those observed for a range of mineral soils incubated under similar conditions (Bull et al., 2000; Maxfield et al., 2006; 2008a, b). Two of the three Andisols studied also displayed high but variable CH 4 oxidation rates ranging from 0.03 to 1.58 nmolCH 4 g -1 d.wt. h -1. These findings suggest that Andisols, a previously unstudied soil class with respect to high-affinity methanotrophic bacteria, may oxidize significant amounts of atmospheric methane despite their low areal coverage globally. © 2009 Society for Applied Microbiology and Blackwell Publishing Ltd.
Journal Article Type | Article |
---|---|
Publication Date | Oct 1, 2009 |
Journal | Environmental Microbiology Reports |
Electronic ISSN | 1758-2229 |
Publisher | Wiley |
Peer Reviewed | Peer Reviewed |
Volume | 1 |
Issue | 5 |
Pages | 450-456 |
DOI | https://doi.org/10.1111/j.1758-2229.2009.00071.x |
Keywords | Andisols, atmospheric methane oxidation, methanotroph populations |
Public URL | https://uwe-repository.worktribe.com/output/991957 |
Publisher URL | http://dx.doi.org/10.1111/j.1758-2229.2009.00071.x |
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