Quantification of Nitrogen Reductase and Nitrite Reductase Genes in Soil of Thinned and Clear-Cut Douglas-Fir Stands by Using Real-Time PCR

The abundance of nifH, nirS, and nirK gene fragments involved in nitrogen (N) fixation and denitrification in thinned second-growth Douglas-fir (Pseudotsuga menziesii subsp. menziesii Mirb.] Franco) forest soil was investigated by using quantitative real-time PCR. Prokaryotic N cycling is an important aspect of N availability in forest soil. The abundance of universal nifH, Azotobacter sp.-specific nifH (nifH-g1), nirS, and nirK gene fragments in unthinned control and 30, 90, and 100% thinning treatments were compared at two long-term research sites on Vancouver Island, Canada. The soil was analyzed for organic matter (OM), total carbon (C), total N, NH₄-N, NO₃-N, and phosphorus (P). The soil horizon accounted for the greatest variation in nutrient status, followed by the site location. The 30% thinning treatment was associated with significantly greater nifH-g1 abundance than the control treatment in one site; at the same site, nirS in the mineral soil horizon was significantly reduced by thinning. The abundance of nirS genes significantly correlated with the abundance of nirK genes. In addition, significant correlations were observed between nifH-g1 abundance and C and N in the organic horizon and between nirS and nirK and N in the mineral horizon. Overall, no clear influence of tree thinning on nifH, nirS, and nirK was observed. However, soil OM, C, and N were found to significantly influence N-cycling gene abundance.Nitrogen (N) is a limiting nutrient in most Douglas-fir (Pseudotsuga menziesii subsp. menziesii Mirb.] Franco) forest ecosystems. Understanding the links between forest management and forest ecosystem function, including the cycling of N, is of paramount importance to researchers and forest managers. Management practices such as thinning and clear-cutting can alter the soil microbial community, potentially altering the rate and amount of net N addition or loss to the forest floor. Clear-cutting alters the functional diversity of soil microorganisms and alters soil characteristics (temperature, pH, moisture, and nutrient status). Thinning and clear-cutting can increase nitrification, denitrification, and leaching of N in soil, all of which can reduce the available N (2, 13, 22, 41, 47). Clear-cutting in Douglas-fir forests can also remove associated gene pools of diazotrophic microorganisms (46). It is not yet well understood how clear-cutting or thinning affects the abundance of N-cycling microorganisms. We focus on two populations of N-cycling microorganisms: diazotrophs, which biologically fix N₂ gas to ammonia, and denitrifiers, which reduce N oxides and result in the release of N-containing gasses.Fixation of N by diazotrophic microorganisms is the primary source of N addition to undisturbed, unfertilized forest soil ecosystems (9, 39). The diazotrophic community is most often studied in situ using the marker gene for nitrogenase reductase (nifH); the diversity and abundance of diazotrophic microorganisms as determined by nifH characterization may be used as an indicator of overall soil ecological health. Diazotrophs can be symbiotic, associated (e.g., with a specific plant or fungal biomass), or free-living in the soil. Endophytic diazotrophs fix ∼100 times more N than free-living strains (9). Free-living diazotrophs such as Azotobacter vinelandii and A. chroococcum may fix between 0 and 60 kg of N ha⁻¹ year⁻¹ (9) and, because of a relative dearth of endophytic interactions in coniferous forests, free-living diazotrophs can be an important source of N in these soils. Cultural studies have shown that free-living diazotrophs improve the establishment of mycorrhizae and conifer seedlings, with relative activity fluctuating according to season, site aspect, and moisture conditions (11). Fixed-N inputs act as a catalyst for interlinked N-cycling events, e.g., fungal decomposition of woody debris and organic material (28). Nitrogen fixation in temperate forest soil is directly related to the amounts of soil organic matter (17). However, it is unclear how nifH gene abundance relates to the amount of total carbon (C) and organic matter (OM) and N in forest soil. It is also unknown how common silvicultural practices (e.g., clear-cutting and thinning) affect diazotrophic abundance or how diazotrophic abundance may in turn affect cycling of soil nutrients.The reduction of inorganic N oxides by denitrifying microorganisms can cause N loss from forest soil ecosystems, as well as the release of greenhouse gases into the atmosphere. The loss of N from temperate forest soil as N₂O has been reported as ranging from 0.2 to 7.0 kg ha⁻¹ year⁻¹, depending largely on soil nitrogen status, soil moisture, and temperature (57). Robertson and Tiedje (44) state that soil N loss in coniferous ecosystems due to denitrification is regulated by nitrification potential (e.g., nitrate levels) in the soil, and while not considered a major N loss component following clear-cutting, this loss is generally of the same magnitude as the N loss due to leaching. Denitrification is primarily studied using molecular approaches by monitoring several genes in the denitrification pathway: cytochrome cd₁-containing nitrite reductase (nirS), Cu-containing nitrite reductase (nirK), nitrous oxide reductase (nosZ), and membrane-bound nitrate reductase A (narG). The nirS and nirK genes were the denitrification genes used in the present study. Studies demonstrating (i) that the nirS gene is more diverse than nirK in soil and (ii) the domination of the nirK population by a relatively reduced number of clones have been published (42, 45). However, recent meta-analysis of studies involving nirK and nirS has shown that both communities tend to be phylogenetically clustered in undisturbed soils (23).To compare the effects of silvicultural practices on the abundance of diazotrophs and denitrifiers, we used quantitative real-time PCR (qPCR) assays to quantify nifH, nirS, and nirK genes in soil. This method can be used to quantify target sequences in environmental samples. Several qPCR protocols for the analysis of functional gene abundance in soil have been developed for N-cycling genes, including nifH, ammonia monooxygenase (amoA), nirK, nirS, nosZ, and narG (21, 24, 31, 38, 43, 54, 55). The objectives of the present study were (i) to quantify nifH, nirS, and nirK; (ii) to compare the effects of thinning and clear-cutting in Douglas-fir stands on the abundance of total diazotrophs, free-living diazotrophs, and denitrifiers; and (iii) to elucidate the relationships between N-cycling genes and nutrient abundance in forest soils.