Molecular diversity of nitrogen-fixing bacteria associated with Chrysopogon zizanioides (L.) Roberty (vetiver), an essential oil producer plant

The essential oil produced by vetiver can vary in amount and composition depending on the bacterial community associated with its roots. Some of these bacteria could also promote plant growth by fixing nitrogen. This study aimed to analyze the diversity of diazotrophic bacteria tightly associated with roots of different vetiver genotypes. nifH-based PCR-denaturing gradient gel electrophoresis (DGGE) and clone libraries were used. DGGE profiles obtained from bulk and rhizosphere soils and root DNA amplified with nifH primers showed that samples from rhizosphere soil and root were separated at 68% similarity. Twelve bands were excised from the DGGE and sequenced. High similarity with nifH sequences of Bradyrhizobium sp., Pseudacidovorax sp. and Xanthobacter sp. was observed. Moreover, three nifH clone libraries were generated using polF/polR-primers from root DNA samples obtained from vetiver genotypes UFS-VET001, UFS-VET003 and UFS-VET004. In UFS-VET001, 24.2% of 95 clones were affiliated with sequences of Mesorhizobium loti while in UFS-VET003 41.5% of 89 clones were affiliated with Sphingomonas azotifigens, and in UFS-VET004 36.4% of 85 clones were affiliated with Klebsiella pneumoniae. The data obtained can be used to guide the isolation of diazotrophic bacteria, which may contribute to plant growth promotion and improvement of the production of essential oil in vetiver.     

Comparative study of endophytic and endophytic diazotrophic bacterial communities across rice landraces grown in the highlands of northern Thailand

Communities of bacterial endophytes within the rice landraces cultivated in the highlands of northern Thailand were studied using fingerprinting data of 16S rRNA and nifH genes profiling by polymerase chain reaction–denaturing gradient gel electrophoresis. The bacterial communities’ richness, diversity index, evenness, and stability were varied depending on the plant tissues, stages of growth, and rice cultivars. These indices for the endophytic diazotrophic bacteria within the landrace rice Bue Wah Bo were significantly the lowest. The endophytic bacteria revealed greater diversity by cluster analysis with seven clusters compared to the endophytic diazotrophic bacteria (three clusters). Principal component analysis suggested that the endophytic bacteria showed that the community structures across the rice landraces had a higher stability than those of the endophytic diazotrophic bacteria. Uncultured bacteria were found dominantly in both bacterial communities, while higher generic varieties were observed in the endophytic diazotrophic bacterial community. These differences in bacterial communities might be influenced either by genetic variation in the rice landraces or the rice cultivation system, where the nitrogen input affects the endophytic diazotrophic bacterial community.     

Prevalence of Betaproteobacterial Sequences in <Emphasis Type="Italic">nifH</Emphasis> Gene Pools Associated with Roots of Modern Rice Cultivars

The diversity and function of nitrogen-fixing bacteria colonizing rice roots are not well understood. A field experiment was conducted to determine the diversity of diazotrophic communities associated with roots of modern rice cultivars using culture-independent molecular analyses of nitrogenase gene (nifH) fragments. Experimental treatments included four modern rice cultivars (Oryza sativa, one Indica, one Japonica and two hybrid rice varieties) and three levels (0, 50, and 100 kg N ha⁻¹) of N (urea) fertilizer application. Cloning and sequencing of 103 partial nifH genes showed that a diverse community of diazotrophs was associated with rice roots. However, the nifH gene fragments belonging to betaproteobacteria were dominant, accounting for nearly half of nifH sequences analyzed across the clone libraries. Most of them were similar to nifH fragments retrieved from wild rice and Kallar grass, with Azoarcus spp. being the closest cultured relatives. Alphaproteobacteria were also detected, but their relative abundance in the nifH gene pools was dramatically decreased with N fertilizer application. In addition, a high fraction of nifH gene pools was affiliated with methylotrophs and methane oxidizers. The sequence analysis was consistent with the terminal restriction fragment-length polymorphism (T-RFLP) fingerprinting of the nifH gene fragments, which showed three of four dominant terminal restriction fragments were mainly related to betaproteobacteria based on in silico digestion of nifH sequences. T-RFLP analyses also revealed that the effects of N fertilizer on the nifH gene diversity retrieved from roots varied according to rice cultivars. In summary, the present study revealed the prevalence of betaproteobacterial sequences among the proteobacteria associated with roots of modern rice cultivars. This group of diazotrophs appeared less sensitive to N fertilizer application than diazotrophic alphaproteobacteria. Furthermore, methylotrophs may also play a role in nitrogen fixation on rice roots. However, it must be noted that due to the potential bias of polymerase chain reaction protocol, the significance of non-proteobacterial diazotrophs such as Firmicutes and anaerobic bacteria is possibly underestimated.     

Vertical distribution of diazotrophic bacterial community associated with temperature and oxygen gradients in a subtropical reservoir

Nitrogen-fixing microorganisms play important roles in the structure and function of aquatic ecosystems. However, the diversity and distribution of diazotrophic bacteria along the lake depth continuum are so far poorly understood. In this study, we investigated the dynamic variations of diazotrophs in a subtropical deep reservoir during the stratified period. We applied an in-depth biomolecular approach (DGGE, clone libraries, and quantitative real-time PCR) to explore the nitrogenase (nifH) gene diversity and abundance. The diazotrophic community shifted between the oxic/anoxic interface and the nifH diversity increased with depth. The Cyanobacteria, affiliated to the toxic bloom-forming Cylindrospermopsis raciborskii, were the dominant diazotrophic cluster in the surface waters, whereas diazotrophic Alphaproteobacteria were dominant in the bottom waters. The relationships between microbial and environmental factors clearly demonstrated that the temperature gradient and the oxygen concentration affect the heterogeneity of the diazotrophic community, thereby influencing the entire aquatic nitrogen cycle.     

Diazotrophic Community Structure and Function in Two Successional Stages of Biological Soil Crusts from the Colorado Plateau and Chihuahuan Desert

The objective of this study was to characterize the community structure and activity of N₂-fixing microorganisms in mature and poorly developed biological soil crusts from both the Colorado Plateau and Chihuahuan Desert. Nitrogenase activity was approximately 10 and 2.5 times higher in mature crusts than in poorly developed crusts at the Colorado Plateau site and Chihuahuan Desert site, respectively. Analysis of nifH sequences by clone sequencing and the terminal restriction fragment length polymorphism technique indicated that the crust diazotrophic community was 80 to 90% heterocystous cyanobacteria most closely related to Nostoc spp. and that the composition of N₂-fixing species did not vary significantly between the poorly developed and mature crusts at either site. In contrast, the abundance of nifH sequences was approximately 7.5 times greater (per microgram of total DNA) in mature crusts than in poorly developed crusts at a given site as measured by quantitative PCR. 16S rRNA gene clone sequencing and microscopic analysis of the cyanobacterial community within both crust types demonstrated a transition from a Microcoleus vaginatus-dominated, poorly developed crust to mature crusts harboring a greater percentage of Nostoc and Scytonema spp. We hypothesize that ecological factors, such as soil instability and water stress, may constrain the growth of N₂-fixing microorganisms at our study sites and that the transition to a mature, nitrogen-producing crust initially requires bioengineering of the surface microenvironment by Microcoleus vaginatus.     

Coral-associated nitrogen fixation rates and diazotrophic diversity on a nutrient-replete equatorial reef

The role of diazotrophs in coral physiology and reef biogeochemistry remains poorly understood, in part because N₂ fixation rates and diazotrophic community composition have only been jointly analyzed in the tissue of one tropical coral species. We performed field-based ¹⁵N₂ tracer incubations during nutrient-replete conditions to measure diazotroph-derived nitrogen (DDN) assimilation into three species of scleractinian coral (Pocillopora acuta, Goniopora columna, Platygyra sinensis). Using multi-marker metabarcoding (16S rRNA, nifH, 18S rRNA), we analyzed DNA- and RNA-based communities in coral tissue and skeleton. Despite low N₂ fixation rates, DDN assimilation supplied up to 6% of the holobiont’s N demand. Active coral-associated diazotrophs were chiefly Cluster I (aerobes or facultative anaerobes), suggesting that oxygen may control coral-associated diazotrophy. Highest N₂ fixation rates were observed in the endolithic community (0.20 µg N cm⁻² per day). While the diazotrophic community was similar between the tissue and skeleton, RNA:DNA ratios indicate potential differences in relative diazotrophic activity between these compartments. In Pocillopora, DDN was found in endolithic, host, and symbiont compartments, while diazotrophic nifH sequences were only observed in the endolithic layer, suggesting a possible DDN exchange between the endolithic community and the overlying coral tissue. Our findings demonstrate that coral-associated diazotrophy is significant, even in nutrient-rich waters, and suggest that endolithic microbes are major contributors to coral nitrogen cycling on reefs.Subject terms: Microbial ecology, Biogeochemistry, Stable isotope analysis     

Changes in Nitrogen-Fixing and Ammonia-Oxidizing Bacterial Communities in Soil of a Mixed Conifer Forest after Wildfire

This study was undertaken to examine the effects of forest fire on two important groups of N-cycling bacteria in soil, the nitrogen-fixing and ammonia-oxidizing bacteria. Sequence and terminal restriction fragment length polymorphism (T-RFLP) analysis of nifH and amoA PCR amplicons was performed on DNA samples from unburned, moderately burned, and severely burned soils of a mixed conifer forest. PCR results indicated that the soil biomass and proportion of nitrogen-fixing and ammonia-oxidizing species was less in soil from the fire-impacted sites than from the unburned sites. The number of dominant nifH sequence types was greater in fire-impacted soils, and nifH sequences that were most closely related to those from the spore-forming taxa Clostridium and Paenibacillus were more abundant in the burned soils. In T-RFLP patterns of the ammonia-oxidizing community, terminal restriction fragments (TRFs) representing amoA cluster 1, 2, or 4 Nitrosospira spp. were dominant (80 to 90%) in unburned soils, while TRFs representing amoA cluster 3A Nitrosospira spp. dominated (65 to 95%) in fire-impacted soils. The dominance of amoA cluster 3A Nitrosospira spp. sequence types was positively correlated with soil pH (5.6 to 7.5) and NH₃-N levels (0.002 to 0.976 ppm), both of which were higher in burned soils. The decreased microbial biomass and shift in nitrogen-fixing and ammonia-oxidizing communities were still evident in fire-impacted soils collected 14 months after the fire.     

Genetic Diversity of nifH Gene Sequences in Paenibacillus azotofixans Strains and Soil Samples Analyzed by Denaturing Gradient Gel Electrophoresis of PCR-Amplified Gene Fragments

The diversity of dinitrogenase reductase gene (nifH) fragments in Paenibacillus azotofixans strains was investigated by using molecular methods. The partial nifH gene sequences of eight P. azotofixans strains, as well as one strain each of the close relatives Paenibacillus durum, Paenibacillus polymyxa, and Paenibacillus macerans, were amplified by PCR by using degenerate primers and were characterized by DNA sequencing. We found that there are two nifH sequence clusters, designated clusters I and II, in P. azotofixans. The data further indicated that there was sequence divergence among the nifH genes of P. azotofixans strains at the DNA level. However, the gene products were more conserved at the protein level. Phylogenetic analysis showed that all nifH cluster II sequences were similar to the alternative (anf) nitrogenase sequence. A nested PCR assay for the detection of nifH (cluster I) of P. azotofixans was developed by using the degenerate primers as outer primers and two specific primers, designed on the basis of the sequence information obtained, as inner primers. The specificity of the inner primers was tested with several diazotrophic bacteria, and PCR revealed that these primers are specific for the P. azotofixans nifH gene. A GC clamp was attached to one inner primer, and a denaturing gradient gel electrophoresis (DGGE) protocol was developed to study the genetic diversity of this region of nifH in P. azotofixans strains, as well as in soil and rhizosphere samples. The results revealed sequence heterogeneity among different nifH genes. Moreover, nifH is probably a multicopy gene in P. azotofixans. Both similarities and differences were detected in the P. azotofixans nifH DGGE profiles generated with soil and rhizosphere DNAs. The DGGE assay developed here is reproducible and provides a rapid way to assess the intraspecific genetic diversity of an important functional gene in pure cultures, as well as in environmental samples.     

The roots of the halophyte Salicornia brachiata are a source of new halotolerant diazotrophic bacteria with plant growth-promoting potential

Soil salinity is the major cause limiting plant productivity worldwide. Nitrogen-fixing bacteria were enriched and characterised from roots of Salicornia brachiata, an extreme halophyte which has substantial economic value as a bioresource of diverse and valuable products. Nitrogen-free semisolid NFb medium with malate as carbon source and up to 4% NaCl were used for enrichment and isolation of diazotrophic bacteria. The isolates were tested for plant growth-promoting traits and 16S rRNA, nifH and acdS genes were analysed. For selected strains, plant growth-promoting activities were tested in axenically grown Salicornia seedlings at different NaCl concentrations (0–0.5M). New halotolerant diazotrophic bacteria were isolated from roots of S. brachiata. The isolates were identified as Brachybacterium saurashtrense sp. nov., Zhihengliuella sp., Brevibacterium casei, Haererehalobacter sp., Halomonas sp., Vibrio sp., Cronobacter sakazakii, Pseudomonas spp., Rhizobium radiobacter, and Mesorhizobium sp. Nitrogen fixation as well as plant growth-promoting traits such as indole acetic acid (IAA) production, phosphate solubilisation, and 1-aminocyclopropane-1-carboxylic acid (ACC) deaminase activity were demonstrated. For Brachybacterium saurashtrense and Pseudomonas sp., significant plant growth-promoting activities were observed in Salicornia in salt stress conditions. Salicornia brachiata is a useful source of new halotolerant diazotrophic bacteria with plant growth-promoting potential.     

Biodiversity of diazotrophic bacteria within the soil, root and stem of field-grown maize

Recent studies suggest a high diversity of diazotrophic bacteria in maize. However, none of these works have been based on a sufficient number of samples to provide reasonable quantitative estimates of diazotrophic bacterial diversity. Here we present the use of molecular tools and statistical inference to assess diazotrophic bacterial diversity within rhizosphere soils, roots and stems of field grown maize. DNA was isolated from the latter collected from six maize growing regions within the southern most state in Brazil, Rio Grande do Sul. Using conserved primers, nifH Cluster I gene fragments were amplified from each of the three zones, and the products cloned and sequenced. The majority of the sequences were classified within the Proteobacteria with the α-proteobacteria and β-proteobacteria being the most abundant in the rhizosphere soil and stem samples. The γ-proteobacteria were most abundant in rhizosphere soils, less so in roots, and least in the stem samples. According to three different diversity measures, the rhizosphere soil samples possessed greater diazotrophic bacterial diversity than the roots and stems of the maize plants. Only two genera, Azospirillum and Azotobacter, were found in virtually all samples at an abundance of over 1% of the total nifH sequences obtained. Other genera were largely restricted to soil (Methylocystis, Beijerinckia, Geobacter, Rhodovulum, Methylobacterium, Gluconacetobacter, Methylocella, and Delftia), roots (Dechloromonas), or stems (Methylosinus, Raoultella, and Rhizobium). Three genera, Herbaspirillum, Ideonella, and Klebsiella, appeared to dominate in the interior of the plant but were much rarer in soil.     

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.     

Abundance and Genetic Diversity of nifH Gene Sequences in Anthropogenically Affected Brazilian Mangrove Sediments

Although mangroves represent ecosystems of global importance, the genetic diversity and abundance of functional genes that are key to their functioning scarcely have been explored. Here, we present a survey based on the nifH gene across transects of sediments of two mangrove systems located along the coast line of São Paulo state (Brazil) which differed by degree of disturbance, i.e., an oil-spill-affected and an unaffected mangrove. The diazotrophic communities were assessed by denaturing gradient gel electrophoresis (DGGE), quantitative PCR (qPCR), and clone libraries. The nifH gene abundance was similar across the two mangrove sediment systems, as evidenced by qPCR. However, the nifH-based PCR-DGGE profiles revealed clear differences between the mangroves. Moreover, shifts in the nifH gene diversities were noted along the land-sea transect within the previously oiled mangrove. The nifH gene diversity depicted the presence of nitrogen-fixing bacteria affiliated with a wide range of taxa, encompassing members of the Alphaproteobacteria, Betaproteobacteria, Gammaproteobacteria, Firmicutes, and also a group of anaerobic sulfate-reducing bacteria. We also detected a unique mangrove-specific cluster of sequences denoted Mgv-nifH. Our results indicate that nitrogen-fixing bacterial guilds can be partially endemic to mangroves, and these communities are modulated by oil contamination, which has important implications for conservation strategies.     

Analysis of the diversity of diazotrophic bacteria in peat soil by cloning of the <Emphasis Type="Italic">nifH</Emphasis> gene

The diversity of nitrogen-fixing microorganisms in the soil of an oligotrophic Sphagnum peat bog was studied by molecular cloning of fragments of the nifH gene encoding one of the main components of the nitrogenase complex. The fragments were amplified from the DNA isolated from the peat samples collected at the same site in January (library I) and November (library II), 2005. Analysis of the nifH sequence libraries revealed high diversity of diazotrophic bacteria in peat soil: the first library consisted of 237 clones and 55 unique sequence types, the second one included 171 clones and 52 sequence types. Comparison of the two clone libraries showed that the composition and population structure of the nitrogen-fixing community depended greatly on the sampling time; they shared only 11 phylotypes. The sequences of representatives of the class Alphaproteobacteria prevailed in both libraries (27% and 57% of clones in libraries I and II, respectively). Representatives of the classes Deltaproteobacteria and Chlorobea were minor components of library I (6% and 7% of clones, respectively), whereas they prevailed in library II (18% and 24% of clones, respectively). Members of the class Chloroflexi were present only in library I, while members of the classes Bacilli, Clostridia, and Methanomicrobia were present only in library II. Our studies demonstrated that, for complete evaluation of the diversity of natural nitrogen-fixing communities, nifH libraries should consist of at least 200–300 clones.     

Comparison of nifH Gene Pools in Soils and Soil Microenvironments with Contrasting Properties

The similarities and differences in the structures of the nifH gene pools of six different soils (Montrond, LCSA-p, Vernon, Dombes, LCSA-c, and Thysse Kaymor) and five soil fractions extracted from LCSA-c were studied. Bacterial DNA was directly extracted from the soils, and a region of the nifH gene was amplified by PCR and analyzed by restriction. Soils were selected on the basis of differences in soil management, plant cover, and major physicochemical properties. Microenvironments differed on the basis of the sizes of the constituent particles and the organic carbon and clay contents. Restriction profiles were subjected to principal-component analysis. We showed that the composition of the diazotrophic communities varied both on a large scale (among soils) and on a microscale (among microenvironments in LCSA-c soil). Soil management seemed to be the major parameter influencing differences in the nifH gene pool structure among soils by controlling inorganic nitrogen content and its variation. However, physicochemical parameters (texture and total C and N contents) were found to correlate with differences among nifH gene pools on a microscale. We hypothesize that the observed nifH genetic structures resulted from the adaptation to fluctuating conditions (cultivated soil, forest soil, coarse fractions) or constant conditions (permanent pasture soil, fine fractions). We attempted to identify a specific band within the profile of the clay fraction by cloning and sequencing it and comparing it with the gene databases. Unexpectedly, the nifH sequences of the dominant bacteria were most similar to sequences of unidentified marine eubacteria.     

Genetic diversity and symbiotic evolution of rhizobia from root nodules of Coronilla varia

Ninety symbiotic rhizobial isolates from root nodules of Coronilla varia growing in the Shaanxi province of China were characterized. Combined with the results of RFLP patterns, six genotypes were defined among the rhizobial strains and they were divided into three genomic genera. These included Mesorhizobium sp., M. alhagi, M. amorphae, M. metallidurans/M. gobiense as the dominant group (86.7%), and Rhizobium yanglingense and Agrobacterium tumefaciens as the minor groups, according to analysis of the corresponding 16S rRNA, nodC and nifH genes. Five nodC types, which mainly grouped into the Mesorhizobium genus, were obtained from all the isolates examined, implying that nodC genes probably occurred from the native habitat through lateral transfer and long-term adaptation, finally evolving toward M. alhagi. Four different nifH types, displaying obvious differences compared to those of 16S rRNA and nodC, implied that possible lateral transfer of the symbiotic genes occurred between different genera. The association between soil components and the genetic diversity of the rhizobial population demonstrated that combined genotypes were positively correlated with the pH of soil samples.     

小麦-甘薯轮作长期增施有机肥对碱性土壤固氮菌群落结构及多样性的影响

生物固氮为农业生态系统提供天然的氮素来源,探究长期增施有机肥对土壤固氮菌群落的影响,为合理增施有机肥和维持土壤固氮微生物群落多样性提供科学依据。选取小麦-甘薯轮作中连续37a不施肥对照(CK)、单施化肥(NPK)、化肥+有机肥(NPKM)处理的甘薯季碱性土壤样品为研究对象。采用Illumina MiSeq高通量测序技术,研究土壤固氮菌群落的组成、多样性及其与土壤特性的关系。结果表明:与对照和单施化肥相比,长期增施有机肥降低土壤固氮菌群落丰富度和多样性,且丰富度与土壤pH显著正相关,与有机碳、全氮和有效养分(硝态氮、有效磷和速效钾)显著负相关。主坐标分析表明长期施肥显著改变土壤固氮菌群落结构,与对照相比,增施有机肥比单施化肥对固氮菌群落结构的影响更大。冗余分析表明土壤有机碳和速效钾是影响固氮菌群落结构改变最主要的因素。长期增施有机肥显著降低变形菌门、蓝藻菌门、Beta-变形菌和固氮弧菌属的相对丰度,显著增加硝化螺旋菌门、酸杆菌门和硝化螺菌属的相对丰度,这与土壤pH、有机碳和有效养分显著相关。因此,在碱性土壤上长期增施有机肥对固氮菌群落结构的改变更大,对群落多样性的抑制作用更强。