Abstract

Abstract. Denitrification is an anaerobic respiration process that is the primary contributor of the nitrous oxide (N2O) produced from grassland soils. Our objective was to gain insight into the relationships between denitrifier community size, structure, and activity for a range of pasture soils. We collected 10 dairy pasture soils with contrasting soil textures, drainage classes, management strategies (effluent irrigation or non-irrigation), and geographic locations in New Zealand, and measured their physicochemical characteristics. We measured denitrifier abundance by quantitative polymerase chain reaction (qPCR) and assessed denitrifier diversity and community structure by terminal restriction fragment length polymorphism (T-RFLP) of the nitrite reductase (nirS, nirK) and N2O reductase (nosZ) genes. We quantified denitrifier enzyme activity (DEA) using an acetylene inhibition technique. We investigated whether varied soil conditions lead to different denitrifier communities in soils, and if so, whether they are associated with different denitrification activities and are likely to generate different N2O emissions. Differences in the physicochemical characteristics of the soils were driven mainly by soil mineralogy and the management practices of the farms. We found that nirS and nirK communities were strongly structured along gradients of soil water and phosphorus (P) contents. By contrast, the size and structure of the nosZ community was unrelated to any of the measured soil characteristics. In soils with high water content, the richnesses and abundances of nirS, nirK, and nosZ genes were all significantly positively correlated with DEA. Our data suggest that management strategies to limit N2O emissions through denitrification are likely to be most important for dairy farms on fertile or allophanic soils during wetter periods. Finally, our data suggest that new techniques that would selectively target nirS denitrifiers may be the most effective for limiting N2O emissions through denitrification across a wide range of soil types.

Highlights

  • Nitrous oxide (N2O) is a potent greenhouse gas that is produced as an intermediate product of biological nitrogen conversions in soils (Stevens et al, 1997)

  • We found that axes 1 and 3 of the principal component analysis (PCA) were not significantly correlated with denitrifier enzyme activity (DEA) or microbial biomass carbon (MBC)

  • We found that the % FC soil water content (SWC) and a gradient in mineral-N form accounted for the greatest variation in soil physicochemical characteristics and that key microbial parameters for denitrification, such as MBC and DEA, were significantly positively correlated with higher soil nitric oxide (NO)−3 –N

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Summary

Introduction

Nitrous oxide (N2O) is a potent greenhouse gas that is produced as an intermediate product of biological nitrogen conversions in soils (Stevens et al, 1997). It is the major global contributor to N2O production in grassland soils (Saggar et al, 2013) and is responsible for a significant fraction of agricultural greenhouse gas emissions (IPCC, 2014). Denitrification is mediated by the action of four enzymes: NO−3 reductase (NAR), NO−2 reductase (NIR), nitric oxide (NO) reductase (NOR), and N2O reductase (N2OR) (Zumft, 1997), which are encoded by the nar/nap, nir, nor, and nos genes, respectively. Diverse bacteria, archaea (Philippot et al, 2007; Tiedje, 1994; Ishii et al, 2010), and eukaryotes (Zumft, 1997) are known to harbour two or more denitrification enzymes.

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