溴代阻燃剂污染底泥与未污染底泥中细菌群落结构之比较分析

【目的】通过免培养的分子生物学方法,比较受溴代阻燃剂污染严重的河流底泥和与未污染水库底泥中细菌多样性差异,解析二者间细菌群落结构,为污染河流的治理与生物修复提供相关的理论依据。【方法】从中国贵屿溴代阻燃剂污染区练江底泥样品和未污染水库底泥样品中分别提取微生物总DNA,用细菌通用引物27F和1500R扩增16S rRNA基因,构建16S rRNA基因文库。用HhaⅠ和HinfⅠ2种限制性内切酶对克隆子进行扩增产物rDNA的限制性酶切分析(ARDRA),挑取不同的操作分类单元OUT中的克隆进行测序并构建系统发育树,比较代表克隆子的基本分类类群和生物多样性构成。【结果】未污染水库底泥中细菌群落组成主要包括变形细菌门(Proteobacteria)的α、β、γ和δ4个亚门、浮霉菌门(Planctomycetes)、酸杆菌门(Acidobacteria)、放线菌门(Actinobacteria)、绿弯菌门(Chloroflexi)、疣微菌门(Verrucomicrobia)和厚壁菌门(Firmicutes)。优势菌是酸杆菌,占文库克隆的30.2%。污染河流底泥中细菌群落组成包括变形细菌门(Proteobacteria)的α、β、δ和ε4个亚门、浮霉菌门(Planctomycetes)、绿菌门或拟杆菌门(Chlorobi orBacteroidetes)、酸杆菌门(Acidobacteria)、放线菌门(Actinobacteria)、绿弯菌门(Chloroflexi)、待定菌群candidatedivision OP01、candidate division OP08和candidate division WS3的相似菌。优势菌是ε-变形细菌和绿弯菌,占文库克隆的44.9%。【结论】受溴代阻燃剂污染河流底泥中的细菌群落具有较高水平的多样性,与未污染底泥有显著区别,主要体现在ε-变形细菌和绿弯菌在细菌群落中具有优势地位。这种优势种群的改变可能与污染物的过度富集具有一定的相关性,对于我们进一步探索和了解溴代阻燃剂的微生物修复具有一定的指导意义。     

乌梁素海湖滨湿地细菌群落结构多样性

【目的】了解乌梁素海湖滨湿地水陆过渡带细菌群落结构及多样性变化,探讨富营养化湖泊湿地基质条件对细菌群落结构的影响。【方法】应用变性梯度凝胶电泳(PCR-DGGE)技术,分析和比较了依陆向分布的4个水陆过渡带样点的湿地细菌群落结构多样性,采用典型对应分析(CCA)探讨了湿地基质因子对细菌多样性的影响。【结果】DGGE图谱显示依湖泊水体沉积物(S-1)→湖滨芦苇沼泽沉积物(S-2)→湖滨碱蓬盐化草甸土壤(S-3)→岸上白刺荒漠土壤(S-4),4个样点的条带数依次减少,对应菌群结构及多样性变化显著;多样性指数分析结果显示,Shannon-Wiener指数(H)、均匀度(E)、丰富度(S)以及Simpson指数(DS)均显示依陆向分布逐步下降的规律,即:S-1S-2S-3S-4。序列比对结果显示,沉积物及土壤细菌分属于变形菌门(78.6%)、酸杆菌门(7.1%)、拟杆菌门(14.3%)这3个细菌类群,优势菌门为变形菌门,而变形菌门又分为5个亚群,其中ε变形菌纲为优势亚群;CCA结果表明,图中各条带对应物种的分布受铵态氮、总氮、有机碳、水溶盐总量、氯离子以及钾离子影响最大。【结论】乌梁素海富营养化湖泊的水陆过渡带湿地细菌群落结构存在较大差异,富营养化相关基质因子对细菌多样性影响较大。这为研究富营养化湖泊湿地水陆过渡带的细菌结构多样性及空间异质性提供了科学依据。     

宁夏第三排水沟底泥细菌群落结构特征和空间分布

【背景】微生物对环境有指示作用,微生物群落组成是水环境的研究热点之一。【目的】探究宁夏第三排水沟底泥细菌群落结构及空间分布。【方法】在底泥理化性质分析的基础上,采用MiSeq PE300测序平台对沟道及主要支流共11个采样点的表层底泥细菌进行16S rRNA基因扩增子测序。【结果】三排底泥呈弱碱性,底泥有机碳、全氮、全磷、氨氮和硝态氮等理化指标存在空间差异。平罗县段底泥有机碳、全氮和全磷均低于贺兰县和惠农区;下游惠农区段底泥细菌的物种丰富度和多样性明显高于上游贺兰县段,十二分沟与干流差异较明显。三排底泥优势细菌菌门为变形菌门(Proteobacteria,24.41%–44.40%)、绿弯菌门(Chloroflexi,5.46%-17.55%)、放线菌门(Actinobacteria,9.12%–21.21%)、拟杆菌门(Bacteroidetes,6.96%–13.10%)、热脱硫杆菌门(Thermodesulfobacteria,3.40%-12.20%)、厚壁菌门(Firmicutes,3.31%–14.61%)和酸杆菌门(Acidobacteria, 2.00%-9.77%)。...     

五大连池不同火山喷发沉积物的细菌群落多样性研究

【目的】揭示五大连池火山区的细菌多样性。【方法】运用Illumina Miseq高通量测序技术解析五大连池不同火山喷发沉积物中细菌的群落组成和分布规律。【结果】五大连池火山区沉积物中的细菌主要包含厚壁菌门(Firmicutes)、变形菌门(Proteobacteria)、疣微菌门(Verrucomicrobia)、酸杆菌门(Acidobacteria)、绿弯菌门(Chloroflexi)、放线菌门(Actinobacteria)等23个细菌门类,其中,厚壁菌门、变形菌门丰度较高,芽孢杆菌属(Bacillus)为绝对优势菌群。另外,由于火山物质的同源性,导致各沉积物中细菌的代谢通路多与C、N、S、Fe等元素的生化循环相关,群落结构及功能具有一定程度的相似性。但由于各研究区域在沉积组分、环境因素及地质演化进程上的差异,致使芽孢杆菌属、地杆菌属(Geobacter)、酸杆菌属(Acidobacterium)、嘉利翁氏菌属(Gallionella)、Blastocatella等部分种群在不同火山沉积物中呈现差异化分布,具有典型的地域适应特性。【结论】五大连池火山沉积物中含有较为丰富的细菌资源,为今后挖掘功能性种质及进一步探讨微生物群落与火山环境之间的关系提供基础数据。     

鄱阳湖湖泊细菌群落组成及结构——以松门山为例

于2011年5月在鄱阳湖——松门山湖区采集底泥与表层水样,分别提取了表层水体浮游和底泥微生物基因组DNA,利用454高通量测序技术对细菌的16S rRNA基因进行了序列测定,分析了湖泊底泥细菌、水体浮游细菌群落结构特征。结果显示:底泥细菌OTUs(Operational Taxonomic Units)为1454,表层水体浮游细菌OTUs为269;底泥细菌群落比表层水体更加多样化,底泥细菌的物种数大大多于表层水体。同时,底泥细菌群落与表层浮游细菌群落结构存在显著差异。物种分类显示鄱阳湖底泥细菌种类隶属于20门,228属,其中优势种群为δ-变形菌纲(Deltaproteobacteria)、β-变形菌纲(Betaproteobacteria)和疣微菌门(Verrucomicrobia);表层水体浮游细菌隶属于13门116属,优势种群为β-变形菌纲、拟杆菌门(Bacteroidetes)和放线菌门(Actinobacteria)。结果进一步揭示,无论是浮游细菌群落还是沉积物细菌群落,优势细菌种群的基因型多样性更高。     

海南海口温泉真菌、细菌多样性及其环境影响因素分析

【目的】海南海口含有丰富的温泉资源,对温泉微生物多样性进行研究,有助于进一步开发和利用海南温泉微生物资源。【方法】本文采用Illumina Hi Seq高通量测序技术对海口3个温泉[海甸岛荣域温泉(S1)、火山口开心农场温泉(S2)和西海岸海长流温泉(S3)]水样中微生物ITS序列和16Sr RNA基因V3-V4区进行测序及生物信息学分析,探究海口市3个不同区域的温泉真菌多样性与细菌多样性。【结果】(1)α多样性分析表明,真菌群落中,S3(29)S1(29)S2,而在细菌群落中,S2(29)S1(29)S3。β多样性分析表明,3个温泉真菌群落和细菌群落组成差异皆显著。(2)分类分析表明,温泉真菌群落优势菌门为子囊菌门(Ascomycota)和担子菌门(Basidiomycota),细菌群落优势菌门为变形菌门(Proteobacteria)、拟杆菌门(Bacteroidetes)、Thermi、硝化螺旋菌门(Nitrospirae)、绿菌门(Chlorobi)、厚壁菌门(Firmicutes)、绿弯菌门(Chloroflexi)、放线菌门(Actinobacteria)。(3) CCA (Canonical correspondence analysis)分析表明,3个温泉的真菌群落主要影响因子是温度,细菌群落主要影响因子是总磷。【结论】海南省海口市温泉中含有丰富的微生物资源,其微生物群落组成受多种环境因子影响,且影响真菌和细菌的主要环境因子不同。     

乌梁素海富营养化湖泊湖滨湿地过渡带细菌群落结构的高通量分析

摘要:【目的】揭示乌梁素海富营养化湖泊湖滨湿地沉积物与土壤过渡带细菌群落的组成、丰度以及多样性变化,结合土壤理化因子探讨其对细菌群落结构的影响。【方法】采用湿地土壤总DNA提取方法提取沉积物和土壤总DNA,对细菌群落的16S rRNA 基因的V1-V3区进行高通量测序,分析各样品中细菌群落结构的组成、丰度以及多样性指标;土壤理化性质采用标准方法测定,分析其对细菌群落结构的驱动作用。【结果】富营养化湖泊湖滨湿地水陆过渡带的芦苇沼泽沉积物、碱蓬群落盐碱化土壤和白刺群落荒漠化土壤中,细菌群落组成和各类群细菌的相对丰度差异较大,门水平上的细菌类群主要有Proteobacteria、Bacteroidetes、Chloroflexi、Actinobacteria、Planctomycetes和Gemmatimonadetes,细菌群落多样性指数随陆向分布依次在增高,门水平上Proteobacteria和属水平上Sulfurimonas对湖泊退化演化敏感;环境因子最佳子集为总磷、水溶盐总量和铵态氮的组合对整个细菌群落结构的影响最为明显,相关系数最高(R=0.8857),Mantel检验结果表明这种相关关系为显著相关(P=0.037)。【结论】乌梁素海富营养化湖泊湖滨湿地过渡带细菌群落结构差异较大,Sulfurimonas属在乌梁素海富营养化湖泊沉积物的生物地球化学循环中扮演着重要的角色,应在以后的研究中得到更多的关注。     

大水面放养水葫芦对富营养化湖泊水体可培养细菌群落结构的影响

【目的】了解大水面放养水葫芦对富营养化湖泊水体可培养细菌群落结构和多样性的影响。【方法】采用稀释平板法,分别对云南滇池紫根水葫芦放养区(ZW)、野生型普通水葫芦放养区(PW)、未放养水葫芦对照区(CK)水体中细菌进行分离,并对其16S r RNA序列进行分析。【结果】分别从ZW、PW、CK 3种水体分离得到54、49、40株菌落形态差异的细菌,Shannon-Wiener多样性指数分别为3.17、3.07、2.73,细菌数量分别为1.35×107、8.35×106、2.70×106 CFU/L。16S r RNA序列分析表明,ZW、PW、CK 3种水体可培养细菌主要包括变形菌门α亚群(Alphaproteobacteria,35.1%、32.4%和40%)、放线菌门(Actinobacteria,18.9%、32.4%和20%)、变形菌门β亚群(Betaproteobacteria,13.5%、5.9%和16.0%)、变形菌门γ亚群(Gammaproteobacteria,13.5%、14.6%和12.0%)、拟杆菌门(Bacteroidetes,13.5%、8.8%和8.0%)和厚壁菌门(Firmicutes,2.7%、5.9%和4.0%)。在属的水平上,3种水体仅有鞘氨醇盒菌属(Sphingopyxis)、红细菌属(Rhodobacter)、黄色杆菌属(Xanthobacter)、新鞘脂菌属(Novosphingobium)、鞘氨醇单胞菌属(Sphingomonas)、假单胞菌属(Pseudomonas)、微杆菌属(Microbacterium)、链霉菌属(Steptomyces)、黄杆菌属(Flavobacterium)、芽孢杆菌属(Bacillus)等10个属的细菌为共有菌属。【结论】大水面放养水葫芦提高了富营养化湖泊水体中可培养细菌的多样性,改变了细菌的群落结构。     

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。     

新疆艾比湖湿地博乐河入口处土壤细菌多样性分析

【目的】了解新疆艾比湖湿地国家级自然保护区非培养土壤细菌群落组成及多样性。【方法】采用非培养法直接从湿地土壤提取总DNA进行16S r RNA基因扩增,构建细菌16S r RNA基因克隆文库。使用MspⅠ和AfaⅠ限制性内切酶对阳性克隆进行16S r RNA基因扩增片段的限制性酶切分析(Amplified r DNA restriction analysis,ARDRA),挑取具有不同双酶切图谱的克隆进行测序,序列比对并构建16S r RNA基因系统发育树。【结果】从土壤细菌的16S r RNA基因文库中随机挑取75个不同谱型的克隆子,共得到58个OTUs,系统发育归类为8个细菌类群:绿弯菌门(Chloroflexi)、蓝藻门(Cyanobacteria)、变形菌门(Proteobacteria)、厚壁菌门(Firmicutes)、放线菌门(Actinobacteria)、拟杆菌门(Bacteroidetes)、疣微菌门(Verrucomicrob)和芽单胞菌门(Gemmatimonadetes)。其中,变形菌门为第一优势菌群,拟杆菌门为第二优势菌群,两者约占总克隆的65%。【结论】艾比湖湿地博乐河入口处土壤细菌多样性丰富,且存在一定数量的潜在微生物新种。     

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。     

Current status and future tendency of lake eutrophication in China

Current trophic status and trend of Chinese freshwater lakes were investigated in this study. The results showed that all lakes studied were commonly undergoing the eutrophication process, water quality decreased and lake's ecosystem is being declined. Most of the urban lakes are facing serious eutrophication. Many medium-sized lakes are in metrophic or eutrophic status, some local water are even approaching the hypertrophic level. The famous five freshwater lakes in China have entered into eutrophication in the condition of higher nutrient load. Lake Taihu, Hongze and Caohu are already in eutrophic state. Eutrophic lakes are mainly distributed in the middle and lower reaches of Yangtze River and Yungui plateau. Lake eutrophication developed rapidly. Among the 34 lakes studied in 1970's, most of lakes were in the mesotrophic status,mesotrophic water area accounted for 91.8%. With the nine year of 1978-1987 the area percentage of oligotrophic lakes decreased from 3.2% to 0.53%, and that of eutrophic lakes increased from 5.0% to 55.01%. Recent data showed 57.5% lakes were in eutrophic and hypertrophic status of the 40 surveyed lakes.Eutrophic trend of Lake Taihu, Chaohu and Xuanwu in the region of the middle and lower reaches of Yangtze River was predicated using the ecological stress model. The results showed that in 2008 Lake Taihu, Chaohu and Xuanwu might be of eutrophication, eutrophication and hypertrophication, respectively if no control measurement is taken. Provided the pollution water treatment rate is 60% in 2030, approximately 30 billion ton pollution water would still be discharged directly in the lakes. Therefore, in 2030 the urban lakes in China might be eutrophication or hypertrophication, and most of the medium-sized lakes at the urban-rural fringe might be in eutrophication or hypertrophication. The famous five biggest freshwater lakes in China might be eutrophication if control countermeasures are taken as now.Lake eutrophication has become a serious environmental problem in China. Based on the domestic and foreign experiences of the eutrophic control technologies, both nutrient pollution control and lake ecological restoration should be carried out and this may be the guidance for the eutrophic control of lakes in China.     

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.

     

海水富营养化对海洋细菌影响的研究进展

综述了海水富营养化对海洋细菌影响的研究进展。随着海水富营养化程度的增加,海洋细菌数量或生物量增加;反硝化细菌、大肠菌群尤其是厌氧性的硫酸盐还原菌和产甲烷菌等典型细菌生理群数量增加;浮游细菌群落结构随富营养化递增趋于简单,物种多样性降低;富营养化也明显导致细菌群落正常功能活性的紊乱。海水富营养化对细菌群落的结构和功能有着深远的影响。     

Bacterial Diversity in Shallow Oligotrophic Marine Benthos and Overlying Waters: Effects of Virus Infection,Containment, and Nutrient Enrichment

Little is known of the factors shaping sediment bacterial communities, despite their high abundance and reports of high diversity. Two factors hypothesized to shape bacterial communities in the water column are nutrient (resource) availability and virus infection. The role these factors play in benthic bacterial diversity was assessed in oligotrophic carbonate–based sediments of Florida Bay (USA). Sediment–water mesocosm enclosures were made from 1-m diameter clear polycarbonate cylinders which were pushed into sediments to 201 cm sediment depth enclosing 80 L of water. Mesocosms were amended each day for 14 d with 10 µM NH ₄ ⁺ and 1 µM PO ₄ ^3– . In a second experiment, viruses from a benthic flocculent layer were concentrated and added back to flocculent layer samples which were collected near the mesocosm enclosures. Photosynthesis by microalgae in virus-amended incubations was monitored by pulse-amplitude modulated (PAM) fluorescence. In both experiments, bacterial diversity was estimated using automated rRNA intergenic spacer analysis (ARISA), a high-resolution fingerprinting approach. Initial sediment bacterial operational taxonomic unit (OTU) richness (236 ± 3) was higher than in the water column (148 ± 9), where an OTU was detectable when its amplified DNA represented >0.09% of the total amplified DNA. Effects on bacterial diversity and operational taxonomic unit (OTU) richness in nutrient-amended mesocosms may have been masked by the effects of containment, which stimulated OTU richness in the water column, but depressed OTU richness and diversity in sediments. Nutrient addition significantly elevated virus abundance and the ratio of viruses to bacteria (p < 0.05 for both) in the sediments, concomitant with elevated bacterial diversity. However, water column bacterial diversity (in unamended controls) was not affected by nutrient amendments, which may be due to rapid nutrient uptake by sediment organisms or adsorption of P to carbonate sediments. Addition of live viruses to benthic flocculent layer samples increased bacterial OTU diversity and richness compared with heat-killed controls; however, cluster analyses showed that the community structure in the virus-amended mesocosms varied greatly between replicates. Despite the strong effects upon eubacterial communities, photosynthesis of co-occurring protists and cyanobacteria was not significantly altered by the presence of virus concentrates. This study supports the hypothesis that nutrient availability plays a key role in shaping sediment bacterial communities, and also that viruses may regulate the abundance of the dominant competitors and allow less dominant organisms to maintain or increase their abundance in a community due to decreased competition for resources.     

Bacterial Diversity and Geochemical Profiles in Sediments from Eutrophic Azorean Lakes

In the Azores, the advanced trophic state of the lakes requires a fast intervention to achieve the good ecological status prescribed by the Water Framework Directive. Despite the considerable effort made to describe the phytoplankton growing on the water column, the lack of information regarding the microbial processes in sediments is still high. Thus, for the successful implementation of internal management actions, the present work explored the relationships between geochemical profiles and dominant members of the bacterial community in sediments from eutrophic Azorean lakes. Lake Azul geochemical profiles were quite homogeneous for all parameters, while in lake Furnas the total iron profile presented a peak below the aerobic layer. For lake Verde, the concentrations of all studied parameters (20 ± 2% loss-on-ignition; 2.10 ± 0.08 mg g^?1 total phosphorus; 1.31 ± 0.50 mg g^?1 total nitrogen; 8.06 ± 0.13 mg g^?1 total iron) in the uppermost sediment layer were approximately two times higher than the ones in sediments from other lakes, decreasing with sediment depth. The higher amounts of phosphorus and organic matter in lake Verde suggested a higher internal contribution of phosphorus to eutrophication. The dominant members of the sediment bacterial community, investigated by denaturing gradient gel electrophoresis, were mostly affiliated to Proteobacteria phylum (Alpha-, Delta-, and Gamma-subclasses), group Bacteroidetes/Chlorobi and phylum Chloroflexi. The Cyanobacteria phylum was solely detected in sediments from lake Verde and lake Furnas that presented the highest amounts of nitrogen and phosphorus both in the water column and sediments, while the other phyla were detected in sediments from the three studied lakes. In conclusion, management measurers to achieve the good ecological status until 2015 should be distinct for the different lakes taking into account the relative magnitude of the nutrient sources and the bacterial diversity in sediments.     

Bacterial communities in the sediments of Dianchi Lake, a partitioned eutrophic waterbody in China

Bacteria play an important role in the decomposition and cycling of a variety of compounds in freshwater aquatic environments, particularly nutrient-rich eutrophic lakes. A unique Chinese eutrophic lake--Dianchi--was selected for study because it has two separate and distinct basins, Caohai with higher organic carbon levels and Waihai with lower organic carbon levels. Sediment bacterial communities were studied in the two basins using samples collected in each season from June 2010 to March 2011. Barcoded pyrosequencing based on the 16 S rRNA gene found that certain common phyla, Proteobacteria, Bacteroidetes, Firmicutes and Chloroflexi, were dominant in the sediments from both basins. However, from the class to genus level, the dominant bacterial groups found in the sediments were distinct between the two basins. Correlation analysis revealed that, among the environmental parameters examined, total organic carbon (TOC) accounted for the greatest proportion of variability in bacterial community. Interestingly, study results suggest that increasing allochthonous organic carbon could enhance bacterial diversity and biomass in the sediment. In addition, analysis of function genes (amoA and nosZ) demonstrated that ammonia-oxidizing bacteria (AOB) were dominant in sediments, with 99% belonging to Nitrosomonas. Denitrifying bacteria were comparatively diverse and were associated with some cultivatable bacteria.     

Comparing sediment bacterial communities in the macrophyte-dominated and algae-dominated areas of eutrophic Lake Taihu, China

Bacterial community structure and the effects of several environmental factors on bacterial community distribution were investigated in the sediment of the macrophyte-dominated and algae-dominated areas in a large, shallow, eutrophic freshwater lake (Lake Taihu, China). Surface sediment samples were collected at 6 sampling sites (3 sites from each of the 2 areas) on 15 February and 15 August 2009. Based on cluster analysis of the DGGE banding patterns, there were significant seasonal variations in the structure of the sediment bacterial community in the macrophyte- and algae-dominated areas, and site-specific variation within an area and between 2 areas. However, there were no significant between-area variations due to the large within-area variation. Analysis of DNA sequences showed that there were differences in the species composition of the sediment bacteria between the macrophyte- and algae-dominated area clone libraries. In the macrophyte-dominated area library, the bacterial community was dominated by Deltaproteobacteria, Verrucomicrobia, Acidobacteria, Bacteroidetes, Gammaproteobacteria, and Betaproteobacteria. OP10 was found in the library of this area but not in the algae-dominated area library. The algae-dominated area library was dominated by Betaproteobacteria, Deltaproteobacteria, Gammaproteobacteria, and Acidobacteria. Cyanobacteria, Alphaproteobacteria, and Planctomycetes were found in this area library but not in the macrophyte-dominated area library. Canonical correspondence analysis demonstrated that total phosphorus and water temperature were the dominant environmental factors affecting bacterial community composition in the sediment.     

Current status and future tendency of lake eutrophication in China

Current trophic status and trend of Chinese freshwater lakes were investigated in this study. The results showed that all lakes studied were commonly undergoing the eutrophica-tion process, water quality decreased and lake's ecosystem is being declined. Most of the urban lakes are facing serious eutrophication. Many medium-sized lakes are in metrophic or eutrophic status, some local water are even approaching the hypertrophic level. The famous five freshwater lakes in China have entered into eutrophication in the condition of higher nutrient load. Lake Taihu, Hongze and Caohu are already in eutrophic state. Eutrophic lakes are mainly distributed in the middle and lower reaches of Yangtze River and Yungui plateau. Lake eutrophication developed rapidly. Among the 34 lakes studied in 1970's, most of lakes were in the mesotrophic status, mesotrophic water area accounted for 91.8%. With the nine year of 1978-1987 the area percentage of oligotrophic lakes decreased from 3.2% to 0.53%, and that of eutrophic lakes increased from 5.0% to 55.01%. Recent data showed 57.5% lakes were in eutrophic and hyper trophic status of the 40 surveyed lakes. Eutrophic trend of Lake Taihu, Chaohu and Xuanwu in the region of the middle and lower reaches of Yangtze River was predicated using the ecological stress model. The results showed that in 2008 Lake Taihu, Chaohu and Xuanwu might be of eutrophication, eutrophication and hypertrophication, respectively if no control measurement is taken. Provided the pollution water treatment rate is 60% in 2030, approximately 30 billion ton pollution water would still be discharged directly in the lakes. Therefore, in 2030 the urban lakes in China might be eutrophication or hypertrophication, and most of the medium-sized lakes at the urban-rural fringe might be in eutrophication or hypertrophication. The famous five biggest freshwater lakes in China might be eutrophication if control countermeasures are taken as now. Lake eutrophication has become a serious environmental problem in China. Based on the domestic and foreign experiences of the eutrophic control technologies, both nutrient pollution control and lake ecological restoration should be carried out and this may be the guidance for the eutrophic control of lakes in China.     

新疆天山北坡不同盐湖微生物菌群结构及其影响因子

新疆分布的众多湖泊由于干旱气候成盐作用强烈,近半数已演化到盐湖发展阶段,不同盐湖中也因此蕴含着丰富的耐盐及嗜盐微生物资源。为更好的掌握新疆盐湖微生物资源分布规律及对环境因子变化的响应规律,利用高通量测序技术对新疆天山北坡5个不同演化阶段盐湖湖底沉积物中细菌、古菌多样性和菌群结构及其主要驱动因子进行研究,探讨盐湖演化过程中原核微生物群落结构变化规律。分别采集5个盐湖湖底沉积物样本,进行理化因子测试与细菌和古菌16S rRNA扩增子测序分析,比较不同盐湖理化性质和原核微生物菌群差异,并对原核微生物丰度与环境因子进行关联分析。实验结果表明：5个盐湖湖底沉积物总盐和Na⁺含量顺序为：巴里坤湖 > 伊吾湖 > 艾比湖 > 盐湖 > 柴窝堡湖,除艾比湖外其他四个盐湖沉积物均呈碱性。Alpha多样性结果显示5个盐湖细菌richness、chao1、ACE和shannon丰富度指数均大于古菌相应丰富度指数,不同盐湖细菌丰富度指数差异较大,古菌丰富度指数差异相对较小。从5个盐湖湖底沉积物中共检测获得细菌58门、68纲、138目、253科和560属,古菌4门、8纲、12目、21科和60属,细菌以变形菌门为主,古菌以广古菌门为主。不同盐湖细菌和古菌优势属种类均不相同,巴里坤湖主要是一些嗜盐和耐盐细菌属,而伊吾湖主要是嗜盐和耐盐古菌属,PCoA分析结果也表明不同盐湖微生物在OTUs水平有其独特菌群结构类型。RDA和Bioenv分析结果表明,盐湖湖底沉积物中微生物菌群群落结构主要受Na⁺和总盐（TS）浓度的影响,对细菌菌群结构影响较大,而古菌菌群结构可能受多种理化因子共同调节。此外,盐湖特殊卤水成分会对微生物群落结构产生重大影响。