富营养化城市湖泊武汉东湖沉积物微生物群体结构及空间变化研究(英文)北大核心CSCD

【目的】城市湖泊沉积物中的微生物群体是富营养环境生物修复的重要因素。本研究拟对中型富营养化湖泊——武汉东湖沉积物细菌群体结构及空间变化规律进行研究。加深对富营养湖泊微生物群体结构的理解,并为城市湖泊的保护和污染控制提供参考。【方法】采用16S r RNA基因RFLP分析和序列分析技术获得细菌群体系统发育信息。采用PCoA法分析武汉东湖沉积物细菌群体内以及与其它湖泊沉积物细菌群体间的相似性。采用CCA法分析环境因素对细菌群体的影响。【结果】武汉东湖沉积物细菌群体包含13个门和2个未知种群。PCoA分析进一步表明来自东湖3个子湖的细菌群体与其它地域富营养化湖泊的微生物种群结构相似,并区别于重度富营养化子湖庙湖的细菌群体。在庙湖中,我们发现了Thermogymnomonas类古菌的含量显著偏高。CCA分析表明细菌的分布与沉积物中碳、氮和磷元素的含量显著相关。【结论】本研究进一步确证了环境因素对细菌群体组成和分布的调节作用,加深了对富营养水体微生物群体结构的理解,并为城市湖泊的保护和污染控制提供了参考。     

富营养化城市湖泊武汉东湖沉积物微生物群体结构及空间变化研究（英文）

【目的】城市湖泊沉积物中的微生物群体是富营养环境生物修复的重要因素。本研究拟对中型富营养化湖泊——武汉东湖沉积物细菌群体结构及空间变化规律进行研究。加深对富营养湖泊微生物群体结构的理解,并为城市湖泊的保护和污染控制提供参考。【方法】采用16S r RNA基因RFLP分析和序列分析技术获得细菌群体系统发育信息。采用PCoA法分析武汉东湖沉积物细菌群体内以及与其它湖泊沉积物细菌群体间的相似性。采用CCA法分析环境因素对细菌群体的影响。【结果】武汉东湖沉积物细菌群体包含13个门和2个未知种群。PCoA分析进一步表明来自东湖3个子湖的细菌群体与其它地域富营养化湖泊的微生物种群结构相似,并区别于重度富营养化子湖庙湖的细菌群体。在庙湖中,我们发现了Thermogymnomonas类古菌的含量显著偏高。CCA分析表明细菌的分布与沉积物中碳、氮和磷元素的含量显著相关。【结论】本研究进一步确证了环境因素对细菌群体组成和分布的调节作用,加深了对富营养水体微生物群体结构的理解,并为城市湖泊的保护和污染控制提供了参考。     

长江口外低氧区及其邻近海域表层沉积物反硝化微生物多样性和分布特征

【目的】微生物参与的反硝化是河口区氮损失的主要途径。【方法】本研究采用Illumina MiSeq测序方法,研究了长江口外低氧区及其邻近海域表层沉积物中nirS型和nirK型反硝化微生物群落的多样性和分布特征。【结果】样品共检测到346个nirS Operational Taxonomic Units和267个nirK Operational TaxonomicUnits,根据采样地的环境特征及nirS型和nirK型反硝化微生物群落聚类分析结果将所有OperationalTaxonomicUnits划分为低氧区、南部区域及外部深水区,其中外部深水区的样品nirS功能基因的多样性最高。各实验样地优势Operational Taxonomic Units在系统进化关系上可分为多个不同的簇。此次发现的所有优势OperationalTaxonomicUnits均属于未被培养的菌群,其中部分Operational Taxonomic Units还是首次被发现。此外还发现nirS功能基因对低氧区的环境适应性更好。【结论】我们的研究结果表明广泛存在的反硝化微生物在河口沉积物的氮循环中发挥重要作用。     

九龙江河口区nirS型反硝化细菌多样性及系统发育学分析

【目的】结合16S rRNA基因克隆文库和nirS基因克隆文库的分析,揭示九龙江河口区nirS型反硝化细菌多样性。【方法】选取九龙江河口区一富营养化采样点,分别采集水样及沉积物样品,进行理化因子的测定并提取细菌总DNA。以水样DNA构建16S rRNA基因克隆文库,以沉积物DNA构建nirS基因克隆文库,分析微生物群落结构的多样性并构建系统发育树。【结果】从16S rRNA基因克隆文库中获得86条有效序列,按97%的序列相似性划分为53个OTU,分别属于Proteobacteria门、Planctomycetes门、Bacteroidetes门、Actinobacteria门、Firmicutes门和Chloroflexi门。其中属于Proteobacteria门OTU的克隆子占克隆数的62.9%,是最优势的类群,分属于Alphaproteobacteria、Betaproteobacteria、Gammaproteobacteria和Deltaproteobacteria纲等。从nirS基因克隆文库中获得190条有效序列,翻译为氨基酸序列后,按82%的序列相似性划分为60个OTU,并定位到属的水平。其中Proteobacteria门是最优势的类群,占文库克隆子总数的71.6%,包括Alphaproteobacteria纲(5.8%)、Betaproteobacteria纲(49.0%)和Gammaproteobacteria纲(16.9%)。nirS基因克隆文库中丰度最高的OTU与GenBank中的一株可培养反硝化菌Thauera sp. R-26906具有100%的序列相似性。【结论】九龙江河口区的微生物以及亚硝酸盐还原酶基因(nirS)具有丰富的多样性。大部分NirS序列在GenBank中的最相似序列来源于河口、海湾等相似的环境。     

干湿交替对生物滞留系统中氮素功能微生物群落的影响

【目的】为探究生物滞留系统干湿交替下环境因子对氮素功能微生物群落的影响。【方法】应用高通量测序技术(Illumina MiSeq PE300),并以amoA和nirS功能基因为分子标记,对无植物型和植物型生物滞留系统在干湿交替下不同土壤空间位置(种植层、淹没层)的硝化和反硝化细菌的多样性和群落结构进行研究,并对微生物群落与环境因子的相互关系进行相关性分析。【结果】微生物种群的功能基因存在显著的空间差异,相比淹没层,种植层的功能细菌更丰富。种植层的OTUs高于淹没层,而进水再湿润促使两种功能基因在种植层和淹没层的OTUs占比差异性增大。群落组成分析表明,amoA型硝化细菌和nirS型反硝化细菌的优势细菌门均为变形菌门(Proteobacteria)。虽然植物根系对氮素功能微生物的多样性指数影响不显著,但在属水平上,植物系统种植层的反硝化菌群种类高于淹没层,而无植物系统则刚好相反。CCA/RDA分析表明,土壤空间位置是影响硝化和反硝化菌群结构的最重要环境因子。【结论】本研究证实干湿交替运行下生物滞留系统中的氮素功能微生物群落受土壤空间位置、水分含量和植物根系的共同调控,其机制有待进一步研究。     

青藏高原淡水湖普莫雍错和盐水湖阿翁错湖底沉积物中细菌群落的垂直分布

【目的】湖泊沉积物中存储着大量独特的微生物,这些微生物在湖泊生态系统生物地球化学循环中扮演着非常重要的角色。然而,很少有研究报道微生物群落在湖泊沉积物中的垂直分布。本文比较研究青藏高原淡水湖普莫雍错和盐水湖阿翁错沉积物在不同深度下细菌的丰度和群落结构。【方法】利用定量PCR(q PCR)和变性梯度凝胶电泳(DGGE)技术分别测定细菌群落的丰度与群落结构。【结果】定量PCR结果显示,湖泊沉积物中细菌丰度均随深度增加而降低,盐水湖阿翁错和淡水湖普莫雍错的细菌丰度分别从1011数量级降到108数量级,从1012数量级降到1010数量级。在相对应的沉积物层,淡水湖沉积物的细菌丰度比盐水湖高1-2个数量级。变性梯度凝胶电泳(DGGE)指纹图谱的分析表明,淡水湖沉积物细菌群落的DGGE条带数(丰富度)显著高于盐水湖(P=0.014);淡水与盐水湖泊沉积物细菌群落结构明显不同,同时在同一湖泊沉积物中上层(0-6 cm)和下层(7-20 cm)细菌群落结构也呈明显分异。系统发育分析表明,盐水湖阿翁错沉积物特有菌门为Gamma-变形菌、拟杆菌门、蓝细菌和栖热菌门,而淡水湖普莫雍错沉积物中特有菌门为Delta-和Beta-变形菌、酸杆菌和绿弯菌门。【结论】青藏高原淡水与盐水湖泊沉积物细菌丰度与群落结构具有明显的差异;同时,细菌群落结构在沉积物的不同深度也表现出差异。这些结果可为进一步阐明青藏高原湖泊生态系统中微生物对气候环境变化的响应提供科学依据。     

氮肥对小麦田土壤nirS型反硝化细菌多样性的影响

摘要：【目的】研究施用无机氮肥对小麦田土壤nirS型反硝化细菌多样性的影响。【方法】通过构建反硝化细菌亚硝酸盐还原酶nirS基因克隆文库,采用限制性片段长度多态性（Restriction Fragment Length Polymorphism, RFLP）技术分析了施氮肥处理和不施氮肥处理土壤中nirS型反硝化细菌的多样性。【结果】两种处理各自分别得到了27个可操作分类单元（Operational Taxa Units, OTUs）,其中有9个OTUs在两个处理中相同。虽然两种处理中 nirS反硝化细菌的香农-威纳指数,Simpon指数,丰富度指数,均匀度指数相近,但是土壤的OTU类型发生了很大变化。通过对施氮肥处理nirS文库中11个代表性nirS克隆子的序列分析,有10个克隆子与数据库中的nirS序列的相似度在73％～95％之间,有1个序列在数据库中找不到相似序列。【结论】施氮肥在短期内显著改变了土壤中nirS型反硝化细菌群落结构的构成。     

克拉玛依油田石油污染土壤细菌群落结构与环境因子的关系

【目的】以16S rRNA为分子标记,探讨克拉玛依油田石油污染土壤中细菌群落多样性和系统发育,并分析环境因子对群落分布的影响,为生物降解石油污染物提供理论基础。【方法】在克拉玛依油田分别采集深度为5、20、50 cm的石油污染土壤样品,测定环境参数;提取石油污染土壤细菌群落基因组DNA,分别构建3个土层细菌16S rRNA基因文库,利用限制性片段长度多态性分析(Restriction fragment length polymorphisms RFLP)技术初步分群,确定各文库中的代表菌株并测定16S rRNA基因序列;利用软件Biodap计算各群落多样性和丰富度指数,以Neighbor-Joining法构建3个土层细菌的系统发育树;运用软件CANOCO 4.5结合不同样品环境因子的差异进行典型对应分析(CCA),并探讨了环境因子对细菌多样性的影响。【结果】环境参数结果表明20 cm土层总磷(TP)、总氮(TN)含量最低,50 cm含量最高;5 cm土层中有机碳(TOC)含量最高,50 cm含量最低。基于16S rRNA序列的生物多样性和物种丰富度指数表明20 cm土层生物多样性和丰富度指数较高,而50 cm土层各项指数均较低。各土层供试序列RFLP聚类分析表明,克拉玛依油田石油污染土壤细菌种群具有丰富的多样性。Neighbor-Joining构建的系统发育分析表明,石油污染土壤被分为5个类群(I–V),分别为变形菌门(Proteobacteria)、放线菌门(Actinobacteria)、厚壁菌门(Firmicute)、拟杆菌门(Bacteroidetes)、浮霉状菌门(Planctomycetes),其中群Ⅰ占78.57%,广泛分布于不同的生态环境;其中来自5 cm土层代表菌的69.23%分布于群Ⅰ。CCA分析结果显示TN、TP和TOC对大部分细菌影响较大;TOC含量对Pseudomonas影响明显。【结论】克拉玛依油田石油污染土壤细菌群落具有丰富的多样性;环境因子是影响石油污染土壤细菌群落空间分布的重要因素。     

牛场肥水灌溉对土壤nirK、nirS型反硝化微生物群落结构的影响

以徐水县梁家营长期定位施肥试验田为研究对象,利用末端限制性片段长度多态性(T-RFLP)分析和克隆文库构建,研究了5种施肥处理(清水灌溉CK、无机肥灌溉CF、牛场肥水不同浓度、不同次数灌溉T4、T5和T11)下土壤中nirK、nirS型反硝化细菌群落多样性及其群落结构的演变。结果表明,不同施肥处理下nirK、nirS型反硝化细菌群落多样性无显著差异,但群落结构却有明显变化:nirK型反硝化细菌群落结构既受施肥种类又受施肥量影响,优势种群尤其对施肥种类和施肥量响应显著;nirS型反硝化细菌则主要受施肥种类影响,施肥量影响微弱。牛场肥水处理和无机肥处理分别促进和抑制不同的nirS型反硝化细菌,群落主成分受无机肥促进、牛场肥水抑制。系统发育分析结果表明,土壤中nirK型反硝化细菌主要与假单胞菌属(Pseudomonas)、产碱杆菌属(Alcaligenes)和根瘤菌属(Rhizobium)的反硝化细菌具有较近的亲缘关系;nirS型反硝化细菌主要与劳尔氏菌(Ralstonia)和红长命菌属(Rubrivivax)有较近的亲缘关系。试验土壤中反硝化微生物多与目前已报道的好氧反硝化细菌亲缘关系较近,这可能与微生物分析取自表层土有关。     

东太平洋多金属结核区两个站位深海沉积物细菌多样性北大核心CSCD

【目的】为了解东太平洋中国多金属结核勘探合同区西区2个站位(WBC1305和WBC1316A)深海沉积物细菌群多样性。【方法】直接提取环境样品总基因组,通过PCR和TA克隆策略构建了2个站位6个层次16S r RNA基因文库,对2个站位沉积物表层泥样中细菌多样性和群落结构特征进行分析,并通过构建系统发育树,进行系统发育学分析。【结果】2个站位6个文库共获得有效克隆533个,其中472个克隆包括α-变形菌纲、β-变形菌纲、γ-变形菌纲、δ-变形菌纲、浮霉菌门、酸杆菌门、硝化螺旋菌门、放线菌门、绿弯菌门、厚壁菌门、拟杆菌门、迷踪菌门、芽单胞菌门、Hydrogenedentes、Chlorobi和Nitrospinae16个细菌类群,而另外61个克隆为不可分类细菌类群。【结论】结果表明γ-变形菌纲和厚壁菌门分别是WBC1305和WBC1316A站位的优势种群;WBC1316A站位细菌群落结构更加丰富和复杂。     

东湖通道工程对沿线底泥细菌群落结构和多样性的影响

为调查东湖通道工程对沿线底泥细菌群落结构和多样性可能造成的影响, 随着隧道施工的进程, 在东湖通道沿线的3个湖区中的19个采样点进行了3次采样, 通过PCR-DGGE结合分子克隆技术, 分析了细菌群落的群落结构及多样性。3批样品共检出细菌类群分别为5门18属、6门17属、5门11属。在门水平上, 底泥中的优势菌是变形菌门, 但其在总量中的比例随施工进程逐渐下降, 依次为86%、80.6%和43.9%。在属水平上, 施工初期的优势菌是埃希氏杆菌属, 施工后期却是Steroidobacter。通道施工初期, 汤菱湖、郭郑湖的湖心区域在属水平上的群落结构相似性较高, 与团湖差异显著; 接近施工区样点与远离施工区样点的底泥细菌群落存在显著差异; 因施工形成的临时封闭水域与敞水区除均有埃希氏杆菌属外, 其他菌属类群差异显著。施工后期的汤菱湖、郭郑湖及团湖的湖心区的底泥微生物群落结构趋于相似; 接近施工区样点与远离施工区样点的底泥细菌群落差异不显著; 封闭区和敞水区有相似的细菌群落结构。施工期间, 细菌群落的多样性指数的最高点都有出现在靠近施工区的位置。各批次样点的Simpson_1-D指数、Shannon_H指数、Margalef指数, 均随着施工进程而逐渐增加。因此, 东湖通道修建对通道沿线近距离的底泥细菌的群落结构和多样性产生了较显著的影响, 这种影响是暂时性还是持续性的, 尚需通道完工回填后的长期评估。研究将为进一步探讨通道修建等人为强干扰活动对浅水湖泊的可能环境影响和制定合理的生态修复策略提供理论基础和数据支撑。     

Communities of nirS-type denitrifiers in the water column of the oxygen minimum zone in the eastern South Pacific

The major sites of water column denitrification in the ocean are oxygen minimum zones (OMZ), such as one in the eastern South Pacific (ESP). To understand the structure of denitrifying communities in the OMZ off Chile, denitrifier communities at two sites in the Chilean OMZ (Antofagasta and Iquique) and at different water depths were explored by terminal restriction fragment length polymorphism analysis and cloning of polymerase chain reaction (PCR)-amplified nirS genes. NirS is a functional marker gene for denitrification encoding cytochrome cd1-containing nitrite reductase, which catalyses the reduction of nitrite to nitric oxide, the key step in denitrification. Major differences were found between communities from the two geographic locations. Shifts in community structure occurred along a biogeochemical gradient at Antofagasta. Canonical correspondence analysis indicated that O2, NO3-, NO2- and depth were important environmental factors governing these communities along the biogeochemical gradient in the water column. Phylogenetic analysis grouped the majority of clones from the ESP in distinct clusters of genes from presumably novel and yet uncultivated denitrifers. These nirS clusters were distantly related to those found in the water column of the Arabian Sea but the phylogenetic distance was even higher compared with environmental sequences from marine sediments or any other habitat. This finding suggests similar environmental conditions trigger the development of denitrifiers with related nirS genotypes despite large geographic distances.     

Diversity of nitrite reductase (nirK and nirS) gene fragments in forested upland and wetland soils

The genetic heterogeneity of nitrite reductase gene (nirK and nirS) fragments from denitrifying prokaryotes in forested upland and marsh soil was investigated using molecular methods. nirK gene fragments could be amplified from both soils, whereas nirS gene fragments could be amplified only from the marsh soil. PCR products were cloned and screened by restriction fragment length polymorphism (RFLP), and representative fragments were sequenced. The diversity of nirK clones was lower than the diversity of nirS clones. Among the 54 distinct nirK RFLP patterns identified in the two soils, only one pattern was found in both soils and in each soil two dominant groups comprised >35% of all clones. No dominance and few redundant patterns were seen among the nirS clones. Phylogenetic analysis of deduced amino acids grouped the nirK sequences into five major clusters, with one cluster encompassing most marsh clones and all upland clones. Only a few of the nirK clone sequences branched with those of known denitrifying bacteria. The nirS clones formed two major clusters with several subclusters, but all nirS clones showed less than 80% identity to nirS sequences from known denitrifying bacteria. Overall, the data indicated that the denitrifying communities in the two soils have many members and that the soils have a high richness of different nir genes, especially of the nirS gene, most of which have not yet been found in cultivated denitrifiers.     

Community structure of denitrifiers, bacteria, and archaea along redox gradients in Pacific Northwest marine sediments by terminal restriction fragment length polymorphism analysis of amplified nitrite reductase (nirS) and 16S rRNA genes

Steep vertical gradients of oxidants (O(2) and NO(3)(-)) in Puget Sound and Washington continental margin sediments indicate that aerobic respiration and denitrification occur within the top few millimeters to centimeters. To systematically explore the underlying communities of denitrifiers, Bacteria, and Archaea along redox gradients at distant geographic locations, nitrite reductase (nirS) genes and bacterial and archaeal 16S rRNA genes (rDNAs) were PCR amplified and analyzed by terminal restriction fragment length polymorphism (T-RFLP) analysis. The suitablility of T-RFLP analysis for investigating communities of nirS-containing denitrifiers was established by the correspondence of dominant terminal restriction fragments (T-RFs) of nirS to computer-simulated T-RFs of nirS clones. These clones belonged to clusters II, III, and IV from the same cores and were analyzed in a previous study (G. Braker, J. Zhou, L. Wu, A. H. Devol, and J. M. Tiedje, Appl. Environ. Microbiol. 66:2096-2104, 2000). T-RFLP analysis of nirS and bacterial rDNA revealed a high level of functional and phylogenetic diversity, whereas the level of diversity of Archaea was lower. A comparison of T-RFLPs based on the presence or absence of T-RFs and correspondence analysis based on the frequencies and heights of T-RFs allowed us to group sediment samples according to the sampling location and thus clearly distinguish Puget Sound and the Washington margin populations. However, changes in community structure within sediment core sections during the transition from aerobic to anaerobic conditions were minor. Thus, within the top layers of marine sediments, redox gradients seem to result from the differential metabolic activities of populations of similar communities, probably through mixing by marine invertebrates rather than from the development of distinct communities.     

The incidence of nirS and nirK and their genetic heterogeneity in cultivated denitrifiers

Gene sequence analysis of nirS and nirK, both encoding nitrite reductases, was performed on cultivated denitrifiers to assess their incidence in different bacterial taxa and their taxonomical value. Almost half of the 227 investigated denitrifying strains did not render an nir amplicon with any of five previously described primers. NirK and nirS were found to be prevalent in Alphaproteobacteria and Betaproteobacteria, respectively, nirK was detected in the Firmicutes and Bacteroidetes and nirS and nirK with equal frequency in the Gammaproteobacteria. These observations deviated from the hitherto reported incidence of nir genes in bacterial taxa. NirS gene phylogeny was congruent with the 16S rRNA gene phylogeny on family or genus level, although some strains did group within clusters of other bacterial classes. Phylogenetic nirK gene sequence analysis was incongruent with the 16S rRNA gene phylogeny. NirK sequences were also found to be significantly more similar to nirK sequences from the same habitat than to nirK sequences retrieved from highly related taxa. This study supports the hypothesis that horizontal gene transfer events of denitrification genes have occurred and underlines that denitrification genes should not be linked with organism diversity of denitrifiers in cultivation-independent studies.     

Vertical distribution of nitrite reductase genes (nir S) in continental margin sediments of the Gulf of Mexico

Marine sediments account for up to 66% of the loss of nitrogen load to coastal areas. Sedimentary denitrification is the main sink for fixed nitrogen in the global nitrogen budget, and thus it is important to understand the structure and composition of denitrifying communities. To understand the structure and composition of denitrifying communities, the diversity of nitrite reductase (nirS) genes from sediments along the Gulf of Mexico was examined using a PCR-based cloning approach. Sediments were collected at three different depths (0-0.5, 4-5 and 19-21 cm). Geochemical analysis revealed decreasing nitrate and oxygen concentrations with increasing sediment depth. This trend coincided with the decrease in diversity of denitrifying bacteria. LIBSHUFF analysis indicated that the clone library in the shallowest sediment (depth, 0-0.5 cm) was significantly different from that in the deepest sediment (depth, 19-21 cm), and that the deeper sediments (depths of 4-5 and 19-21 cm) were significantly similar. Community structural shifts were evident between the shallowest (oxic zone) and deepest (anoxic zone) sediments. Community changes within the deepest sediments were more subtle, with the presence of different nirS clone sequences gradually becoming dominant or, alternatively, decreasing with depth. The changes in community structure at this depth are possibly driven by nutrient availability, with lower quality sources of carbon and energy leading to the disappearance of nirS sequences common in the top layer. The majority of recovered nirS sequences were phylogenetically divergent relative to known denitrifying bacteria in the database.     

Vertical profiles of water and sediment denitrifiers in two plateau freshwater lakes

The present study investigated the abundance, richness, diversity, and community composition of denitrifiers (based on nirS and nosZ genes) in the stratified water columns and sediments in eutrophic Dianchi Lake and mesotrophic Erhai Lake using quantitative PCR assay and high-throughput sequencing analysis. Both nirS- and nosZ denitrifiers were detected in waters of these two lakes. Surface water showed higher nosZ gene density than bottom water, and Dianchi Lake waters had larger nirS gene abundance than Erhai Lake waters. The abundance of sediment nirS- and nosZ denitrifiers in Dianchi Lake was larger than that in Erhai Lake. nirS richness and diversity and nosZ richness tended to increase with increasing sediment layer depth in both lakes. The distinct structure difference of sediment nirS- and nosZ denitrifier communities was found between in Dianchi Lake and Erhai Lake. These two lakes also differed greatly in water denitrifier community structure. Moreover, phylogenetic analysis indicated the presence of several different groups of nirS- or nosZ denitrifiers in both lakes. The novel nirS denitrifiers were abundant in both Dianchi Lake and Erhai Lake, while most of the obtained nosZ sequences could be affiliated with known genera.