Impact of land management practices on high-affinity methanotrophic bacterial populations: evidence from long-term sites at Rothamsted

A - Papers appearing in refereed journals

Maxfield, P. J., Brennand, E. L., Powlson, D. S. and Evershed, R. P. 2011. Impact of land management practices on high-affinity methanotrophic bacterial populations: evidence from long-term sites at Rothamsted. European Journal of Soil Science. 62 (1), pp. 56-68. https://doi.org/10.1111/j.1365-2389.2010.01339.x

AuthorsMaxfield, P. J., Brennand, E. L., Powlson, D. S. and Evershed, R. P.
Abstract

The impacts of land-use change and long-term agricultural practices on the bacterial and methanotrophic biomass in the soils comprising the Classical Experiments at Rothamsted Research were investigated by using 13CH(4) phospholipid fatty acid stable isotope probing (PLFA SIP). Nine sites were studied, including six arable plots, two regenerated woodlands and a regenerated grassland. The regenerating sites had all been in arable cropping for at least 200 years (and probably much longer) before commencing regeneration approximately 120 years ago. Six sites were plots within the Broadbalk Wheat Experiment, which had been cultivated, and on which winter wheat was grown annually for 163 years with different fertilizer and manure treatments; the field had been in arable cropping for at least 200 years previously. Triplicate soil samples were incubated under 2 ppmv 13CH(4) for up to 100 days. Extraction and 13C-PLFA analysis revealed that overall methanotrophic biomass was smaller in the Rothamsted soils compared with the other mineral soils studied to date, as indicated by poor 13C incorporation. High-affinity methanotrophs similar to known type II methanotrophs were most abundant in all of the soils studied, except in two plots receiving farmyard manure (FYM and FYM + N). Manuring resulted in a shift to a population similar to known type I methanotrophs. Methanotrophic biomass was elevated in soils that had received the largest input of N fertilizer, though without detectable differences in CH(4) oxidation rates, indicating the potential mediation of atmospheric CH(4) oxidation by non-methanotrophs, which are most likely to be nitrifying bacteria.

KeywordsSoil Science
Year of Publication2011
JournalEuropean Journal of Soil Science
Journal citation62 (1), pp. 56-68
Digital Object Identifier (DOI)https://doi.org/10.1111/j.1365-2389.2010.01339.x
Open accessPublished as non-open access
FunderBiotechnology and Biological Sciences Research Council
Funder project or codeSEF
Maintaining soil resilience and function for sustainable land management
Carbon, nutrient and energy flows through the soil microbial biomass and soil ecosystem functioning
ISSN13510754
1351-0754
PublisherWiley

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