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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

Ed R C Hornibrook

Profile image of Pete Maxfield

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