转cry1 Ac/cpti基因水稻对土壤氨氧化细菌群落组成和丰度的影响

【背景】氨氧化细菌是驱动硝化作用的关键微生物,其群落多样性变化对土壤氮素转化具有重要意义。转基因作物可能通过根系分泌物和植株残体组成的改变对土壤微生物群落产生影响。【方法】本研究通过田间定位试验,利用特异引物进行PCR-DGGE（聚合酶链反应—变性梯度凝胶电泳）和荧光定量PCR,分析了种植转cry1 Ac/cpti双价抗虫基因水稻第3、4年土壤中氨氧化细菌群落组成和丰度的变化。【结果】水稻各生育期（分蘖期、齐穗期和成熟期）内,转cry1 Ac/cpti基因杂交稻Ⅱ优科丰8号（GM）的土壤氨氧化细菌16S rRNA基因群落组成、多样性指数与其对应的非转基因杂交稻Ⅱ优明恢86（CK）间均没有显著差异;以DGGE条带为基础的氨氧化细菌群落组成的冗余分析（RDA）显示,GM和CK的土壤氨氧化细菌群落组成只与水稻生育期存在显著相关性（P=0.002和0.018）;同时,水稻各生育期内土壤氨氧化细菌16S rRNA基因丰度在GM和CK间也没有显著差异,但均随水稻生长而变化且在齐穗期达到最高（P〈0.05）。【结论与意义】稻田土壤氨氧化细菌的群落组成与丰度在水稻不同生育期存在差异,但在转cry1 Ac/cpti基因水稻和非转基因水稻间没有显著差异,即一定时期内种植转cry1 Ac/cpti抗虫基因水稻不会影响土壤氨氧化细菌的群落组成和丰度。     

内蒙古呼伦贝尔草原土壤氨氧化细菌多样性及群落结构

采用聚合酶链式反应-变性梯度凝胶电泳技术及扩增产物序列分析方法,研究了呼伦贝尔5种草地类型(线叶菊草原、贝加尔针茅草原、羊草草原、大针茅草原、克氏针茅草原)土壤氨氧化细菌多样性及群落结构特征.研究表明:不同草地类型间土壤氨氧化细菌群落结构组成差异显著,相似性均低于50%.线叶菊草原土壤氨氧化细菌群落多样性最高,其次是贝加尔针茅草原、羊草草原和克氏针茅草原,大针茅草原最低.5种草地类型土壤氨氧化细菌均以Nitrosospira cluster 3为优势种群,此外还发现有Nitrosospira cluster 1、2、4和Nitrosomonas.线叶菊草原土壤氨氧化细菌群落组成较其他草地类型复杂,而羊草草原和大针茅草原群落组成较简单.经相关性分析,土壤含水量、土壤全氮、有机碳、土壤C/N与土壤氨氧化细菌群落多样性显著正相关(P<0.05).     

Abundance and community composition of ammonia-oxidizing archaea and bacteria in two different zones of Lake Taihu

The abundance and community composition of ammonia-oxidizing archaea and ammonia-oxidizing bacteria in the surface sediments of 2 different zones (Meiliang Bay and Eastern Lake Taihu) of Lake Taihu were investigated using real-time quantitative polymerase chain reaction and clone libraries. The amoA gene copy numbers in the surface sediment of Meiliang Bay ranged from 4.91?× 10(5) to 8.65?× 10(6) copies/g dry sediment for the archaeal amoA gene and from 3.74?× 10(4) to 3.86?× 10(5) copies/g dry sediment for the bacterial amoA gene, which were significantly higher than those of Eastern Lake Taihu (P?< 0.05). Concentrations of ammonia (NH(4)(+)), total nitrogen, organic matter, and pH of the sediments exhibited significantly negative correlations with the abundance of ammonia-oxidizing archaea or ammonia-oxidizing bacteria (P?< 0.05 or P?< 0.01, respectively). The potential nitrification rates show remarkable correlations with the copy numbers of the archaeal amoA gene. Diversity of the archaeal amoA gene in Eastern Lake Taihu was significantly higher than that of Meiliang Bay, whereas the bacterial amoA gene diversity was comparable for the 2 lake zones. The data obtained in this study would be useful to elucidate the role of ammonia-oxidizing archaea and ammonia-oxidizing bacteria in the nitrogen cycle of freshwater ecosystems.     

Impact of Collimonas bacteria on community composition of soil fungi

The genus Collimonas consists of soil bacteria that have the potential to grow at the expense of living fungal hyphae. However, the consequences of this mycophagous ability for soil fungi are unknown. Here we report on the development of fungal communities after introduction of collimonads in a soil that had a low abundance of indigenous collimonads. Development of fungal communities was stimulated by addition of cellulose or by introducing plants ( Plantago lanceolata ). Community composition of total fungi in soil and rhizosphere and of arbuscular mycorrhizal fungi in roots was examined by PCR-DGGE. The introduction of collimonads altered the composition of all fungal communities studied but had no effects on fungal biomass increase, cellulose degrading activity or plant performance. The most likely explanation for these results is that differences in sensitivity of fungal species to the presence of collimonads result in competitive replacement of species. The lab and greenhouse experiments were complemented with a field experiment. Mesh bags containing sterile sand with or without collimonads were buried in an ex-arable field and a forest. The presence of collimonads had an effect on the composition of fungi invading these bags in the ex-arable site but not in the forest site.     

Community composition of ammonia-oxidizing bacteria and archaea in rice field soil as affected by nitrogen fertilization

Little information is available on the ecology of ammonia-oxidizing bacteria (AOB) and archaea (AOA) in flooded rice soils. Consequently, a microcosm experiment was conducted to determine the effect of nitrogen fertilizer on the composition of AOB and AOA communities in rice soil by using molecular analyses of ammonia monooxygenase gene (amoA) fragments. Experimental treatments included three levels of N (urea) fertilizer, i.e. 50, 100 and 150 mg N kg⁻¹ soil. Soil samples were operationally divided into four fractions: surface soil, bulk soil deep layer, rhizosphere and washed root material. NH₄⁺-N was the dominant form of N in soil porewater and increased with N fertilization. Cloning and sequencing of amoA gene fragments showed that the AOB community in the rice soil consisted of three major groups, i.e. Nitrosomonas communis cluster, Nitrosospira cluster 3a and cluster 3b. The sequences related to Nitrosomonas were predominant. There was a clear effect of N fertilizer and soil depth on AOB community composition based on terminal restriction fragment length polymorphism fingerprinting. Nitrosomonas appeared to be more abundant in the potentially oxic or micro-oxic fractions, including surface soil, rhizosphere and washed root material, than the deep layer of anoxic bulk soil. Furthermore, Nitrosomonas increased relatively in the partially oxic fractions and that of Nitrosospira decreased with the increasing application of N fertilizer. However, AOA community composition remained unchanged according to the denaturing gradient gel electrophoresis analyses.     

Ammonia biofiltration and community analysis of ammonia-oxidizing bacteria in biofilters

Biological removal of ammonia was investigated using compost and sludge as packing materials in laboratory-scale biofilters. The aim of this study is to characterize the composition of ammonia-oxidizing bacteria (AOB) in two biofilters designed to remove ammonia. Experimental tests and measurements included analysis of removal efficiency and metabolic products. The inlet concentration of ammonia applied was 20–100 mg m⁻³. Removal efficiencies of BFC and BFS were in the range of 97–99% and 95–99%, respectively. Periodic analysis of the biofilter packing materials showed ammonia was removed from air stream by nitrification and by the improved absorption of NH₃ in the resultant acidity. Nitrate was the dominant product of NH₃ transformation. Changes in the composition of AOB were examined by using nested PCR, denaturing gradient gel electrophoresis (DGGE) and sequencing of DGGE bands. DGGE analysis of biofilter samples revealed that shifts in the community structure of AOB were observed in the experiment; however, the idle phase did not cause the structural shift of AOB. Phylogenetic analysis revealed the population of AOB showed Nitrosospira sp. remains the predominant population in BFC, while Nitrosomonas sp. is the predominant population in BFS.     

Abundance and composition of ammonia-oxidizing bacteria and ammonia-oxidizing archaea communities of an alkaline sandy loam

The abundance and composition of soil ammonia-oxidizing bacteria (AOB) and ammonia-oxidizing archaea (AOA) communities under different long-term (17 years) fertilization practices were investigated using real-time polymerase chain reaction and denaturing gradient gel electrophoresis (DGGE). A sandy loam with pH (H(2)O) ranging from 8.3 to 8.7 was sampled in years 2006 and 2007, including seven fertilization treatments of control without fertilizers (CK), those with combinations of fertilizer nitrogen (N), phosphorus (P) and potassium (K): NP, NK, PK and NPK, half chemical fertilizers NPK plus half organic manure (1/2OMN) and organic manure (OM). The highest bacterial amoA gene copy numbers were found in those treatments receiving N fertilizer. The archaeal amoA gene copy numbers ranging from 1.54 x 10(7) to 4.25 x 10(7) per gram of dry soil were significantly higher than those of bacterial amoA genes, ranging from 1.24 x 10(5) to 2.79 x 10(6) per gram of dry soil, which indicated a potential role of AOA in nitrification. Ammonia-oxidizing bacteria abundance had significant correlations with soil pH and potential nitrification rates. Denaturing gradient gel electrophoresis patterns revealed that the fertilization resulted in an obvious change of the AOB community, while no significant change of the AOA community was observed among different treatments. Phylogenetic analysis showed a dominance of Nitrosospira-like sequences, while three bands were affiliated with the Nitrosomonas genus. All AOA sequences fell within cluster S (soil origin) and cluster M (marine and sediment origin). These results suggest that long-term fertilization had a significant impact on AOB abundance and composition, while minimal on AOA in the alkaline soil.     

Quantitative analyses of the abundance and composition of ammonia-oxidizing bacteria and ammonia-oxidizing archaea of a Chinese upland red soil under long-term fertilization practices

The abundance and composition of soil ammonia-oxidizing bacteria (AOB) and ammonia-oxidizing archaea (AOA) were investigated by using quantitative real-time polymerase chain reaction, cloning and sequencing approaches based on amoA genes. The soil, classified as agri-udic ferrosols with pH (H(2)O) ranging from 3.7 to 6.0, was sampled in summer and winter from long-term field experimental plots which had received 16 years continuous fertilization treatments, including fallow (CK0), control without fertilizers (CK) and those with combinations of fertilizer nitrogen (N), phosphorus (P) and potassium (K): N, NP, NK, PK, NPK and NPK plus organic manure (OM). Population sizes of AOB and AOA changed greatly in response to the different fertilization treatments. The NPK + OM treatment had the highest copy numbers of AOB and AOA amoA genes among the treatments that received mineral fertilizers, whereas the lowest copy numbers were recorded in the N treatment. Ammonia-oxidizing archaea were more abundant than AOB in all the corresponding treatments, with AOA to AOB ratios ranging from 1.02 to 12.36. Significant positive correlations were observed among the population sizes of AOB and AOA, soil pH and potential nitrification rates, indicating that both AOB and AOA played an important role in ammonia oxidation in the soil. Phylogenetic analyses of the amoA gene fragments showed that all AOB sequences from different treatments were affiliated with Nitrosospira or Nitrosospira-like species and grouped into cluster 3, and little difference in AOB community composition was recorded among different treatments. All AOA sequences fell within cluster S (soil origin) and cluster M (marine and sediment origin). Cluster M dominated exclusively in the N, NP, NK and PK treatments, indicating a pronounced difference in the community composition of AOA in response to the long-term fertilization treatments. These findings could be fundamental to improve our understanding of the importance of both AOB and AOA in the cycling of nitrogen and other nutrients in terrestrial ecosystems.     

Quantification of ammonia-oxidizing bacteria in arable soil by real-time PCR

Real-time PCR was used to quantify populations of ammonia-oxidizing bacteria representing the beta subdivision of the class Proteobacteria in samples of arable soil, both nitrogen fertilized and unfertilized, from Mellby, Sweden. Primers and probes targeting a 16S ribosomal DNA region of the ammonia-oxidizing bacteria were designed and used. In the fertilized soil there were approximately 6.2 x 10(7) ammonia-oxidizing bacteria per g of soil, three times more than the number of bacteria in the unfertilized soil. The lytic efficiency of bead beating in these soils was investigated by using populations of free or loosely attached bacteria, bacteria tightly bound to particles, and bacteria in nonfractionated samples. The shapes of the curves generated in these tests showed that the concentration of template DNA released at various times remained constant after 10 to 100 s of bead beating.     

秸秆覆盖免耕对土壤氮素转化细菌区系的影响

不同耕作方法影响土壤N素转化细菌的组成和数量.多年连续秸秆覆盖免耕试验结果表明,好氧固氮菌和厌氧固氮菌数量在铁茬处理土壤中较少,而在免耕与翻耕土壤中较多,免耕厌氧固氮菌数量明显地高于翻耕和铁茬,而铁茬最低,这种趋势特别在0～0.1m和0.1～0.2m土层中表现明显.土壤反硝化细菌的数量在表层土壤中较少,三种耕作方法相差较小,但在0.1～0.2m,0.2～0.3m土层中,翻耕反硝化细菌数量比免耕和铁茬多,而铁茬最少.不同耕作方法间氨氧化细菌数量相差不明显,免耕土壤中氨氧化细菌数量较高,动态变化趋势不规则.0～0.1m土层中免耕亚硝酸氧化细菌数量高于翻耕和铁茬,0.1～0.2m土层免耕与翻耕亚硝酸氧化菌数较多,而铁茬较少.     

Effects of nitrobenzene contamination and of bioaugmentation on nitrification and ammonia-oxidizing bacteria in soil

Bioaugmentation of nitrobenzene-contaminated soil was performed by inoculation with Pseudomonas putida ZWL73, which can grow on nitrobenzene as carbon and nitrogen sources and release free ammonium from the aromatic ring via a partial-reductive pathway. Removal of nitrobenzene was effectively enhanced with concurrent accumulation of ammonium in the bioaugmented soil. Moreover, the negative impact of nitrobenzene contamination on culturable bacterial types and soil nitrification was reduced by strain ZWL73. Changes in the community structure of ammonia-oxidizing bacteria, determined by denaturing gradient gel electrophoresis, were associated with changes in environmental factors in nitrobenzene-contaminated soil, including concentrations of nitrobenzene, ammonium, nitrite and nitrate, but their influence was attenuated in the bioaugmented soil. Overall, P. putida ZWL73 shows promising abilities for effective removal of nitrobenzene and for attenuating the negative effects of nitrobenzene contamination on soil functioning.     

Influence of soil pollution on the composition of a microbial community

The abundance dynamics and composition of indigenous soil microbial communities were studied in soils polluted with naphthalene, dioctyl phthalate, diesel fuel, and crude oil. DGGE analysis of the 16S rRNA genes amplified from the total soil DNA revealed that the bacterial community of uncontaminated soil was more diverse and included no dominant species. In the soil samples polluted with the crude oil, diesel fuel, or dioctyl phthalate, Pseudomonas became the dominant bacteria since the third day of the experiment. In the soil polluted with naphthalene, two genera of bacteria (Pseudomonas and Paenibacillus) were dominant in population on the third day of the experiment, while on the 21th day of the experiment Arthrobacter became dominant. During the experiment, the average number of indigenous bacterial degraders increased approximately by two orders of magnitude. While the key genes of naphthalene catabolism, nahAc and nahH, were not detected in the pristine soil, they were found in a significant amount on the third day after naphthalene addition. Three degrader strains harboring the plasmids of naphthalene biodegradation (IncP-9 group) were isolated on the third day from the soil polluted with naphthalene. Two of these plasmids, although isolated from various degraders, were shown to be identical.     

三种利用方式对羊草草原土壤氨氧化细菌群落结构的影响

本文以内蒙古呼伦贝尔羊草草原为研究对象,利用聚合酶链式反应－变性梯度凝胶电泳(PCR－DGGE)技术及扩增产物序列分析方法比较研究了刈割、放牧和围栏封育三种利用方式对羊草草原土壤氨氧化细菌多样性和系统发育的影响,结果表明：羊草草原土壤中氨氧化细菌的优势类群为亚硝化螺旋菌属和亚硝化单孢菌属的细菌,分别占氨氧化细菌总数的72.4%和28.6%,Cluster 4和Cluster 6在各个样地中均为优势类群但所占比例不同,放牧样地中氨氧化细菌的多样性最高,逐步回归分析的结果表明,影响多样性指数的关键理化因子是土壤硝态氮含量。放牧样地中脲酶活性和硝化率都显著高于其他两种利用方式,其中,脲酶活性与土壤硝态氮和全磷含量表现出极显著的相关性,与速效磷含量表现出显著相关性;而硝化率仅与硝态氮含量表现出显著相关性。不同利用方式土壤氨氧化细菌群落与土壤理化因子的典范对应分析结果表明铵态氮的含量对氨氧化细菌群落的影响显著。     

Effect of coupled reduced irrigation and nitrogen fertilizer on soil mite community composition in a wheat field

Groundwater and nitrogen fertilizer overuse severely threatens crop productions; thus, current ecological agriculture requires low irrigation and nitrogen fertilizer inputs. The effects of combined reduced irrigation and nitrogen fertilizer addition on soil organism (e.g., mite) community and biodiversity remain poorly understood. We analyzed soil mite community composition, wheat grain yield, and soil characteristics in a 10‐year manipulation experiment with two levels of irrigation (reduced and conventional irrigation) and five nitrogen fertilizer levels (0, 70, 140, 210, and 280 kg N/ha). Reduced irrigation (20% reduction, from 280 to 220 mm) and nitrogen fertilizer (25% reduction, from 280 to 210 kg N/ha) addition did not significantly influence soil mite community and wheat yield. The relative abundances of fungivores and predators showed negative quadratic relationships with wheat yield, while that of plant parasites showed a positive relationship. The relationships between soil mite trophic groups and wheat yield revealed that we can evaluate the impacts of reduced irrigation and nitrogen fertilizer addition from the perspective of soil fauna. Soil mite community composition was altered by soil abiotic factors prior to reduced irrigation and nitrogen fertilizer addition. Overall, moderate reductions of irrigation and nitrogen fertilizer may not threaten to soil mite community and diversity or decrease crop production; in contrast, such reductions will benefit mite community development and the sustainable agriculture.     

亚高山/高山森林土壤有机层氨氧化细菌和氨氧化古菌丰度特征

为了解季节性冻融作用对川西亚高山/高山地区土壤氨氧化微生物群落的影响,采用qPCR技术,以氨单加氧酶基因的α亚基(amoA)为标记,在生长阶段、冻结阶段、融化阶段中的9个关键时期调查了该地区不同森林群落：岷江冷杉(Abies faxoniana)原始林(PF)、岷江冷杉(A. faxoniana)和红桦(Betula albosinensis)混交林(MF)、岷江冷杉次生林(SF)土壤有机层的氨氧化细菌(ammonia-oxidizing bacteria, AOB)和氨氧化古菌(ammonia-oxidizing archaea, AOA)丰度的特征。结果表明,三个森林群落土壤有机层中都具有相当数量的氨氧化细菌和古菌,均表现出从生长阶段至冻结阶段显著降低,在冻结阶段最低,但冻结阶段后显著增加,在融化阶段为全年最高的趋势。土壤氨氧化微生物类群结构(AOA/AOB)受负积温影响明显。冻结后期三个森林群落土壤负积温最大时,AOA数量明显高于AOB,但其他关键时期土壤氨氧化微生物类群结构与群落类型密切相关。高海拔的PF群落土壤有机层表现为AOA>AOB(冻结初期除外),低海拔的SF群落中表现为AOB>AOA(冻结后期除外),而MF群落则仅在融冻期和生长季节末期表现为AOB>AOA。这些结果为认识亚高山/高山森林及其相似区域的生态过程提供了一定的科学依据。     

Effects of nitrite on ammonia-oxidizing activity and gene regulation in three ammonia-oxidizing bacteria

Nitrite is the highly toxic end product of ammonia oxidation that accumulates in the absence of a nitrite-consuming process and is inhibitory to nitrifying and other bacteria. The effects of nitrite on ammonia oxidation rates and regulation of a common gene set were compared in three ammonia-oxidizing bacteria (AOB) to determine whether responses to this toxic metabolite were uniform. Mid-exponential-phase cells of Nitrosomonas europaea ATCC 19718, Nitrosospira multiformis ATCC 25196, and Nitrosomonas eutropha C-91 were incubated for 6 h in mineral medium supplemented with 0, 10, or 20 mM NaNO(2) . The rates of ammonia oxidation (nitrite production) decreased significantly only in NaNO(2) -supplemented incubations of N. eutropha; no significant effect on the rates was observed for N. europaea or N. multiformis. The levels of norB (nitric oxide reductases), cytL (cytochrome P460), and cytS (cytochrome c'-β) mRNA were unaffected by nitrite in all strains. The levels of nirK (nitrite reductase) mRNA increased only in N. europaea in response to nitrite (10 and 20 mM). Nitrite (20 mM) significantly reduced the mRNA levels of amoA (ammonia monooxygenase) in N. multiformis and norS (nitric oxide reductase) in the two Nitrosomonas spp. Differences in response to nitrite indicated nonuniform adaptive and regulatory strategies of AOB, even between closely related species.