基于高通量绝对定量测序解析岗南水库微生物群落的时空分布特征及关键驱动因素

为了探究水源水库微生物群落时空演变特征及其环境驱动因子,采用高通量绝对定量测序技术,结合数据分析了相对定量和绝对定量对岗南水库微生物群落演变和驱动因子的影响.结果表明,基于绝对定量的微生物群落α-多样性呈现出明显的季节差异(p＜0.05),基于相对定量的微生物群落α-多样性没有差异;绝对定量的微生物群落a-多样性高于相...     

蠡河底泥中反硝化复合菌群富集及菌群结构研究

从无锡市滨湖区蠡河底泥中富集培养反硝化复合菌群,研究其在不同富集培养阶段TN、NO-3-N、NO-2-N、NH+4-N和COD动态变化,分析反硝化过程中气体释放总量、释放速率和成分,通过构建全长16S r DNA克隆文库研究其菌落结构.结果表明,反硝化复合菌群富集在阶段4时脱氮效果最佳,仅在9 h内,330 mg·L-1的TN负荷下,TN去除率达90.9%,NO-3-N去除率达100%,中间产物NO-2-N和NH+4-N积累量最少,分别为3.39 mg·L-1和16.64 mg·L-1,COD去除率达85%;释放气体260m L,气体主要成分为N2,同时还有少量的CH4和CO2等.富集培养反硝化复合菌群细菌属于Pseudomonadaceae科和Rhodocyclaceae科,为Proteobacteria门,OUT丰度分别为57.8%和31.6%,Pseudomonadaceae科是优势类群.     

渤海排污口邻近海域异养细菌的组成与分布

对渤海4个重点监测排污口（北塘、大蒲河、弥河和虞河）邻近海域异养细菌的组成和分布进行了调查研究。结果表明,分离到的各排污口邻近海域的细菌隶属于变形菌门（Proteobacteria）、厚壁菌门（Firmicutes）、放线菌门（Acti-nobacteria）和拟杆菌门（Bacteroidetes）4个细菌类群,其中变形菌门的细菌最丰富。各排污口的优势菌有所不同,北塘、弥河2个采样点的优势菌分别为Bacillus sp．、Pseudoalteromonas sp．,大蒲河采样点的优势菌为Vibrio sp．和Oceanospirillum sp．,虞河采样点的优势菌为 Shewanella sp．和 Bacillus sp．。多维尺度分析表明,北塘和虞河采样点的细菌种群特征较相近,细菌种群分布特征可能与排污口的海洋环境有一定的相关性。     

Screening and degrading characteristics and community structure of a high molecular weight polycyclic aromatic hydrocarbon-degrading bacterial consortium from contaminated soil

Inoculation with effcient microbes had been proved to be the most important way for the bioremediation of polluted environments. For the treatment of abandoned site of Beijing Coking Chemical Plant contaminated with high level of high-molecular-weight polycyclic aromatic hydrocarbons(HMW-PAHs) ,a bacterial consortium capable of degrading HMW-PAHs,designated 1-18-1,was enriched and screened from HMW-PAHs contaminated soil.Its degrading ability was analyzed by high performance liquid chromatography(HPLC) ,and the community structure was investigated by construction and analyses of the 16S rRNA gene clone libraries(A,B and F) at different transfers.The results indicated that 1-18-1 was able to utilize pyrene,fluoranthene and benzoapyrene as sole carbon and energy source for growth.The degradation rate of pyrene and fluoranthene reached 82.8%and 96.2%after incubation for 8 days at 30°C,respectively;while the degradation rate of benzoapyrene was only 65.1%after incubation for 28 days at 30°C. Totally,108,100 and 100 valid clones were randomly selected and sequenced from the libraries A,B,and F.Phylogenetic analyses showed that all the clones could be divided into 5 groups,Bacteroidetes,α-Proteobacteria,Actinobacteria,β-Proteobacteria andγ-Proteobacteria.Sequence similarity analyses showed total 39 operational taxonomic units(OTUs) in the libraries.The predominant bacterial groups wereα-Proteobacteria(19 OTUs,48.7%) ,γ-Proteobacteria(9 OTUs,23.1%) andβ-Proteobacteria(8 OTUs,20.5%) . During the transfer process,the proportions ofα-Proteobacteria andβ-Proteobacteria increased greatly(from 47%to 93%) ,while γ-Proteobacteria decreased from 32%(library A) to 6%(library F) ;and Bacteroidetes group disappeared in libraries B and F.     

实时荧光定量PCR法快速测定水中微囊藻

以铜绿微囊藻（Microcystis aeruginosa）16S rRNA基因片段为靶序列设计一对特异性引物,采用Real-time PCR法,对铜绿微囊藻进行定性、定量检测。试验表明,仅含铜绿微囊藻DNA模板的样品有特异性扩增,扩增产物熔解曲线平稳,峰尖且窄,熔解温度为（87±1）℃。以重组质粒pMD-18T-16S为标准品,检测区间为1．1×102 copies/mL～1．1×108 copies/mL,所得标准曲线符合制备实时定量PCR标准曲线的要求,对标准品进行测定,方法检出限为11 copies/mL。用该标准曲线对实验室培养获得的铜绿微囊藻DNA样品进行定量检测,与显微镜计数结果基本一致。     

典型岩溶土壤微生物丰度与多样性及其对碳循环的指示意义

探讨土壤微生物指标的变化规律,用于揭示其在岩溶土壤碳循环中的指示意义.以桂林岩溶试验场洼地、坡地和垭口这3种岩溶地貌形态下的剖面(0~10、10~20、20~30cm)土壤为研究对象,采用聚合酶链式反应-变性梯度凝胶电泳(PCRDGGE)和荧光定量PCR相结合的方法,分析这个典型岩溶土壤剖面中的微生物多样性和丰度变化.数据显示,16S rRNA最高丰度出现在洼地,为1.32×1011拷贝·g-1,而18S rRNA最高丰度出现在垭口,为1.12×1010拷贝·g-1;洼地和垭口剖面的16S rRNA丰度随着深度的增加而降低,3种岩溶地貌形态的18S rRNA丰度均随着剖面深度的增加而降低,与土壤有机碳质量分数的变化趋势一致.但是,在3种岩溶地貌形态中,3个16S rRNA和6个18S rRNA的多样性指数均随土壤剖面深度的增加而增大.由于16S rRNA和18S rRNA的多样性与丰度和土壤有机碳之间总体上表现出相反的变化趋势,说明微生物丰度指标在土壤碳循环中的指示意义比微生物多样性指数更重要.     

垃圾填埋场细菌种群空间分布及组成多样性研究

采用PCR-DGGE技术对垃圾填埋场细菌种群垂直分布及组成多样性进行了研究．结果表明：垃圾填埋场细菌种群组成波动较大,某些种群对环境因子的变化十分敏感．在填埋年龄已达3a的取样点,细菌种群的多样性随着垃圾填埋深度的增加而呈现“多—少—多”的变化趋势。各种群间相对密度也呈现由不均一到均一的变化规律,部分层次优势种和非优势种发生较大变化．填埋深度4．0m至6．25m左右的区域是填埋场微生物区系组成发生变化的过渡区,该区域细菌种群的多样性较小,亲缘关系相差比较大的种交叉在一起,具有明显的过渡特征．从时间因素来看,填埋场同层次微生物群落组成随时间延长,种群构成趋于稳定．表层垃圾1～2a内,细菌种群处于交替更叠的阶段,日趋发育成熟．8．25m以下层次的细菌种群主要受填埋深度影响,与填埋时间关系较小。     

Alga-lysing bioreactor and dominant bacteria strain

Alga-lysing bacteria have been paid much attention to in recent years. In this study, the alga-lysing strain P05 which was isolated from an immobilizing biosystem was immobilized by coke and elastic filler, forming two biological reactors. The removal efficiencies of algae, NH4^＋-N and organic matter using the two reactors were studied. The results showed that strain P05 was an ideal algal-lysing bacteria strain because it was easy to be immobilized by coke and elastic filler which are of cheap, low biodegradability and the simple immobilization procedure. After 7 d filming, the biological film could be formed and the reactors were used to treat the eutrophic water. These two reactors were of stability and high effect with low cost and easy operation. The optimal hydraulic retention time （HRT） of each reactor was 4 h. The algae removal rates were 80.38% and 82.1% （in term of Chl-α） of coke reactor and filler reactor, respectively. And that of NH4^＋-N were 52.3% and 52.7%. The removal rates of CODMn were 39.03% and 39.64%. The strain P05 was identified as Bacillus sp. by PCR amplification of the 16S rRNA gene, BLAST analysis, and comparison with sequences in the GenBank nucleotide database.     

细菌群落结构对水体富营养化的响应

于2005年2月在太湖不同营养水平湖区采集水样,寞接提取水样的总DNA,以细菌16SrDNA通用引物进行V3区PCR扩增,产物经DGGE(变性凝胶梯度电泳)分离后,获得水体细菌群落的16SrDNA指纹图谱;并运用FDC(表面荧光直接计数)方法对细菌丰度进行了测定.结果表明,水体中细菌的群落结构随着水体富营养化程度的改变产生明显变化,细菌数量呈现随水体营养水平增加而上升的趋势,营养水平较低的湖心区细菌数量仅为2.87×106 cells·mL-1,超富营养化的五里湖区水体中.细菌数量高达5.92×106cells·mL-1;细菌群落多样性随水体营养水平增加呈现显著的下降趋势,在超富营养化的1#、2#采样位点,细菌DGGE主要条带数量仅为23条,在沉水植物丰富区(贡湖湾)细菌DGGE主要条带数量达33条.PCA(主成分分析)的聚类结果表明,太湖水体中不同营养水平下的细菌群落多样性可大致归为3种类型,超富营养化的五里湖区水体细菌群落结构与梅粱湾及汞湖湾存在明显不同,可以大体归为超富营养类型、藻型湖区及草型湖区类型3种.此结果反映了水体富营养化过程中,由于营养物质的增加,促进了某些类群微生物的大量繁殖,水体中微生物的生物量显著增加;生态环境条件的恶化,造成了微生物多样性的下降,这可能导致原本稳定的水生态系统脆弱化.     

地下水波动带中细菌群落结构与水质响应关系

为揭示地下水波动带中细菌群落结构特征及其与地下水环境相互作用关系,选取哈尔滨市第一水源地作为研究区,采集地下水样品以及波动带不同深度（0~5m非饱和带和6~50m饱和带）含水介质样品,分别用于水化学分析和16S rRNA细菌高通量测序,依托冗余分析定量表述地下水质参数与细菌群落相关性.水化学分析结果显示,研究区地下水主要污染物为Fe、Mn、NH₄⁺和有机质,Fe、Mn超标与研究区特定地质背景有关,NH₄⁺和有机质主要来源于人类活动.微生物分析结果显示,非饱和带和饱和带的细菌群落结构差异性显著,非饱和带细菌群落丰度和多样性显著高于饱和带,Proteobacteria、Bacteroidetes、Actinobacteria、Firmicutes和Acidobacteria为研究区优势门,在非饱和带和饱和带的累积相对丰度分别为82.89%和98.64%.冗余分析（RDA）结果显示,门水平上非饱和带中与水质演化强相关的细菌类群是Bacteroidetes、Proteobacteria、Actinobacteria、Verrucomicrobia,贡献率分别为15%、14.8%、8.9%和5.2%;饱和带中对地下水质演化起主要作用的类群为Bacteroidetes、Acidobacteria、Actinobacteria和Firmicutes,贡献率分别为38.4%、19.0%、10.8%和9.1%.属水平上非饱和带中的Pseudomonas和饱和带中的Flavobacterium对Fe、Mn、NH₄⁺生物转化起主导作用.本研究为揭示地下水波动带中生物地球化学作用对地下水环境的影响提供了科学依据,对地下水污染修复具有重要的意义.