Journal
SOIL BIOLOGY & BIOCHEMISTRY
Volume 36, Issue 9, Pages 1431-1441Publisher
PERGAMON-ELSEVIER SCIENCE LTD
DOI: 10.1016/j.soilbio.2004.03.008
Keywords
microbial community; denitrification; denitrifying activities; N(2)O; nosZT-RFLP
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We examined denitrifying bacteria from wet soils and creek sediment in an agroecosystem in Oregon, USA that received inputs of nitrogen (N) fertilizer. Our objective was to determine the variation in denitrifying community composition and activities across three adjacent habitats: a fertilized agricultural field planted to perennial ryegrass, a naturally vegetated riparian area, and creek sediment. Using C(2)H(2) inhibition, denitrifying enzyme and N(2)O-reductase activities were determined in short-term incubations of anaerobic slurries. A key gene in the denitrification pathway, N(2)O reductase (nosZ), served as a marker for denitrifiers. Mean denitrifying enzyme activity (DEA) was similar among habitats, ranging from 0.5 to 1.8 mug N g(-1) dry soil h(-1). However, the ratio of N(2)O production, without C2H2, to DEA was substantially higher in riparian soil (0.64 +/- 0.02; mean +/- standard error, n = 12) than in agricultural soil (0.19 +/- 0.02) or creek sediment (0.32 +/- 0.03). Mean N(2)O-reductase activity ranged from 0.5 to 3.2 mug N g(-1) dry soil h(-1), with greater activity in agricultural soil than in riparian soil. Denitrifying community composition differed significantly among habitats based on nosZ terminal-restriction fragment length polymorphisms. The creek sediment community was unique. Communities in the agricultural and riparian soil were more closely related but distinct. A number of unique nosZ genotypes were detected in creek sediment. Sequences of nosZ obtained from riparian soil were closely related to nosZ from Bradyrhizobium japonicum. Although nosZ distribution and N(2)O-reductase activity differed among habitats, relationships between activity and community composition appeared uncoupled across the agroecosystem. (C) 2004 Elsevier Ltd. All rights reserved.
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