南海南部陆坡表层沉积物细菌和古菌多样性

从南海南部陆坡表层沉积物中扩增了细菌和古菌16S rDNA序列,并对克隆子文库进行系统发育分析.细菌序列以变形杆菌(Proteobacteria)居多,其次是浮霉菌(Planctomycete)、酸杆菌(Acidobacteria)和candidate division OP10,另外还有少量铁还原杆菌(Deferrobacteres)、candidate division OP3、OP11、OP8、TM6、疣微菌(Verrucomicrobia)和螺旋体(Spirochaetes).古菌序列分别来自泉古生菌(Crenarchaeota)和广古生菌(Euryarchaeota),以Marine Benthic Group B(MBGB)、MarineCrenarchaeotic Group Ⅰ(MGⅠ)、Marine Benthic Group D(MBGD)和South African Gold Mine Euryarchaeotic Group(SAGMEG)为主.少量序列为C3、甲烷杆菌(Methanobacteriales)和Novel Euryarchaeotic Group(NEG).结果表明海底表层沉积物中有丰富多样的微生物群落.     

南海北部表层沉积物中原核微生物多样性

[目的]为研究南海北部沉积物原核微生物的多样性和群落结构.[方法]从南海北部XSCS13站位表层沉积物中扩增古菌和细菌的16S rDNA并构建文库,随机挑出阳性克隆子进行测序,选出所有的OTU构建系统进化树,进行系统发育学分析.[结果]多数克隆子来自于未培养原核微生物,沉积物中的古菌分属3大门类:泉古菌(Crenarchaeota)、奇古菌(Thaumarchaeota)和广古菌(Euryarchaeota),其中泉古菌(Crenarchaeota)为主要门类,占71％;广古菌(Euryarchaeota)最少,只有3个克隆子.泉古菌(Crenarchaeota)又以MG Ⅰ为主要类群,占61％.细菌多样性明显高于古菌,共9个门类:变形杆菌(Proteobacteria)(32.6％)、疣微菌(Verrucomicrobia)(3.0％)、拟杆菌门(Bacteroidete)(5.2％)、酸杆菌(Acidobacteria)(4.4％)、绿弯菌(Chloroflexi)(6.0％)、厚壁菌(Firmicute)(3.7％)、浮霉菌(Planctomycete)(5.2％)、芽单胞菌(Gemmatimonadete)(11.1％)、放线细菌(Actinobacteria)(4.4％).变形杆菌为优势类群(包括α-Proteobacteria、γy-Proteobacteria和δ-Proteobacteria 3个亚群),其中γ-Proteobacteria是Proteobacteria中的优势种群,占54.5％.另外所有原核微生物总共有超过50％的克隆子与硫酸盐的还原以及甲烷的形成相关.[结论]结果表明南海北部XSCS13站位表层沉积物中原核微生物的多样性非常丰富,其中蕴含大量未知的微生物资源;另外古菌和细菌群落结构表明该位点可能处于富含甲烷的冷泉活动区.     

南海北部陆坡神狐海域HS-PC500 岩心微生物多样性

[目的]本文研究南海北部陆坡神狐HS-PC500重力活塞岩心沉积物中微生物多样性.[方法]使用吖啶橙染色法计数沉积物中微生物丰度;提取沉积物微生物总DNA,使用特异性引物扩增古菌及细菌16SrRNA基因序列;对克隆文库进行系统发育分析.[结果]系统发育分析显示表层PC500-l(0-5 cm below sea floor,bsf)古菌以C3为主要类群,占该层总序列的25.6%;中层PC500-6(350-355 cm bsf)和底层PC500-11(790-795 cm bsf)古菌以Marine Benthic Group(MBG)-B为主要类群,分别占该层总序列的48.1%和38.9%.另有部分克隆序列属于MBG-A、Miscellaneous Crenarchaeotic Group(MCG)、Thermoprotei、NGC、Halobacteriales、MBG-E、South African Gold Mine Euryarchaeotic Group(SAGMEG).表层细菌以变形菌(Proteobacteria)为主要类群,占该层文库的38.3%.中层和底层细菌以绿弯菌(Choloflexi)和JS1为主要类群,分别占该层文库的28.1%、29.2%和39%、24.7%.另有部分克隆序列属于硝化螺旋菌(Nitrospirae)、放线菌(Actinobacteria)、酸杆菌(Acidobacteria)、OP8、螺旋体菌(Spirochaetes)、TM6、脱铁杆菌(Deferribacteres)、浮霉菌(Plantomycete).[结论]结果显示,HS-PC500岩心微生物丰度与甲烷浓度变化相吻合;微生物丰度较低可能与较低的总有机碳量有关;微生物多样性较高,并且随深度的增加群落结构变化明显;岩心中有关硫酸盐还原的微生物类群占优势,说明微生物的硫代谢在该海区沉积物的物质循环过程中占有重要地位.     

海南东寨港红树林不同植被土壤微生物群落结构比较

【目的】比较不同植被下红树林土壤细菌和古菌的多样性及群落结构,认识红树林土壤微生物资源多样性。【方法】直接提取红树林土壤总DNA,采用细菌通用引物27F/1492R和古菌通用引物Arch21F/Arch958R进行PCR扩增,构建细菌和古菌16S rRNA基因文库,对海南东寨港自然保护区秋茄林、无瓣海桑林和无红树林裸滩土壤的细菌和古菌多样性和群落结构进行分析和比较。【结果】3种土壤样品的细菌类群包括变形细菌门(Proteobacteria)等16个类群,其中变形细菌门(Proteobacteria)与绿屈挠菌门(Chloroflexi)是优势类群;古菌包括6个嗜泉古菌界(Crenarchaeota)类群和7个广域古菌界(Euryarchaeota)类群,分别以Marine Benthic Group C、Marine Benthic Group D为优势类群。多样性指数(H’)和物种丰富度指数(Schao1)表明,本地种秋茄林下土壤细菌和古菌的多样性指数最高,外来种无瓣海桑显著低于秋茄林,甚至明显低于相邻无红树林裸滩沉积物;不同植被下土壤细菌和古菌群落结构存在显著差异,秋茄林土壤微生物群落结构和无红树林裸滩沉积物更相似。【结论】红树林土壤微生物类群丰富,不同植被下土壤细菌和古菌多样性和群落结构存在显著差异。     

中国南海北部陆坡沉积物古菌多样性及丰度分析

【目的】海洋沉积物中的古菌在全球生物地球化学循环中充当重要的角色,深入了解沉积物中古菌群落的结构及功能特征是探究海洋沉积物中古菌参与生物地球化学循环和生态学功能的基础。【方法】采用高通量测序技术,分别对南海北部陆坡不同海域(东部,西部和神狐海域的7个站位)沉积物中古菌16SrRNA基因进行Illumina Mi Seq测序。【结果】中国南海北部陆坡沉积物中古菌的主要门类是Bathyarchaeota、Thermoplasmata、Woesearchaeota(DHVEG-6)、Thaumarchaeota(Marine Group I)、Lokiarchaeota和Marine Hydrothermal Vent Group(MHVG),还存在少量的AK8、Marine Benthic Group A和Terrestrial Hot Spring Crenarchaeota Group(THSCG)等。在潜在水合物区沉积物中还发现了甲烷代谢相关古菌(Anaerobic methanotrophic archaea,ANME)类群,主要为ANME-1、ANME-2ab和ANME-2c等。甲烷代谢古菌的分布特征也从甲烷代谢保守功能基因mcr A(Methyl coenzyme-Mreductase A)的扩增中得到了验证。利用定量PCR对南海沉积物中的细菌、古菌的16SrRNA基因和mcrA基因进行了定量,发现细菌16SrRNA基因拷贝数为10~5-10~7 copies/g(湿重),古菌16SrRNA基因拷贝数为10~5-10~6 copies/g(湿重),潜在水合物区mcrA基因拷贝数为10~3-10~5 copies/g(湿重)。【结论】揭示了中国南海北部陆坡沉积物中具有丰富的微生物资源,其中古菌种类多样且丰度较高,同时发现冷泉特征古菌群落,为深入认识和理解南海沉积物中微生物丰度和古菌多样性,以及解析古菌地球化学功能奠定基础。     

污水处理活性污泥微生物群落多样性研究

为研究污水处理活性污泥微生物多样性,提取了活性污泥宏基因组DNA,并采用细菌通用引物27F和1492R扩增了上海污泥厂活性污泥细菌16S rDNA片段,构建了细菌16S rDNA克隆文库,并对该文库中的微生物群落进行了分析。共获得200条高质量序列并建立系统发育树,结果显示活性污泥主要的细菌类群为变形菌门(Proteobacteria)(91.9%)、厚壁菌门(Firmicures)(4.6%)、拟杆菌门(Bacteroidetes)(2%)、绿弯菌门(Chloroflexi)(0.5%)、硝化螺菌门(Nitrospirae)(1%)。其中,明显的优势菌群为Alcaligenes feacalis(55%)、Pseudomonas aeruginosa(12.8%)和Stenotrophomonas(12.8%),优势菌的产酶能力在活性污泥中显示生态修复功能菌的作用。     

洋山深水港海域表层海水中古菌多样性特点

利用DGGE、定量PCR以及16S rRNA基因克隆文库技术对洋山深水港海域表层海水中的古菌多样性组成进行了调查和分析。通过Quantity One软件分析不同样品的DGGE图谱,发现洋山深水港3个不同海域(小洋山港口区、大洋山港口区、中间航道)的古菌群落多样性组成不存在明显的区别;利用定量PCR的方法对3个不同样品中的古菌16S rRNA基因拷贝进行计数,发现3个不同海域的古菌16S rRNA基因拷贝数的数量关系为:大洋山海域((1.69±0.19)×10~6copies/mL)中间航道((2.17±0.20)×10~6copies/mL)小洋山港口区((2.42±0.22)×10~6copies/mL),这说明洋山深水港3个不同海域的古菌群落组成是一致的,只是在数量上略有差异,为对该海域古菌的更深入调查研究提供了便利和数据基础。洋山深水港海域表层海水的古菌16S rRNA基因文库分析表明,古菌由三大门类组成:广古菌门(Euryarchaeota)、泉古菌门(Crenarchaeota)和奇古菌门(Thaumarchaeota)。广古菌门所占比例约为26.8%,泉古菌门约为33.0%,奇古菌门约为40.2%。广古菌门含有2个类群,分别是Mathanobacteriales(10.3%)和Marine GroupⅡ(16.5%);泉古菌门含有1个类群,为Unidentified Crenarchaeotic Group(33.0%);奇古菌门含有1个类群,为Marine GroupⅠ(40.2%)。结果显示,Mathanobacteriales类群和Marine GroupⅡ类群的比例失调,这可能预示着洋山深水港海域存在油污污染及外来微生物物种入侵的风险。     

大庆聚驱后油藏微生物群落结构分析

目的:进一步研究大庆聚驱后油藏微生物种类.方法:应用T-RFLP方法比较系统地分析比较了聚驱后油藏微生物多样性,分析了与采油功能相关的主要微生物组成,初步研究了聚驱后油藏微生物分布特点及规律.结果:利用聚驱后油藏细菌群落16S rDNA构建克隆文库,共挑取了49个阳性克隆,T-RFLP分型结果,共出现21个不同类型.所得的序列在Genbank中比对的结果表明细菌克隆可分为5个类群,分属于变形杆菌、拟杆菌、脱铁杆菌、厚壁菌以及未确定分类的类群;同时构建了聚驱后油藏古菌群落16S rDNA的克隆文库,共挑取了48个阳性克隆,根据T-RF分型结果共有5个类群,构建的古菌克隆文库的12个阳性克隆分属5个不同的类群,这些克隆和产甲烷菌亲缘关系很近.结论:该研究为大庆油田本源微生物采油技术的应用提供了可靠的理论依据.     

沙颍河下游城市黑臭内河沉积物微生物群落季节变化特征

为了研究沙颍河下游城市黑臭内河不同季节沉积物微生物群落特征,对安徽省阜阳市黑臭内河中清河、七渔河表层沉积物进行16S rDNA高通量测序。结果发现:黑臭河流中沉积物的微生物多样性指数均不高,但是表现出一定的变化规律,即春季>冬季≥夏季>秋季;通过冗余性分析发现微生物多样性受季节与沉积物pH影响较显著。分析沉积物门水平上的微生物群落结构发现,季节、温度、TN及SOM对微生物影响较大。变形杆菌、厚壁菌门、绿弯菌门、疣微菌门、拟杆菌门和放线菌门等优势菌门的相对丰度在季节水平上存在差异,春季厚壁菌门、绿弯菌门、放线菌门和酸杆菌门相对丰度较高,其中绿弯菌门和酸杆菌门是已知指示污染的微生物,变形杆菌门相对较少。秋季疣微菌门与拟杆菌门相对丰度显著减小,变形杆菌门相对其他季节显著增加。样品中共发现16个硫酸盐还原菌(SRB)菌属,其中Desulfoprunum是丰度最高的菌属。春季沉积物中SRB的类群最多,相对丰度最大;硫酸盐还原菌群与SO42-、TN、SOM、Cl–等呈显著正相关。上述结果为营养盐控制时机的选择从而有效避免河流中黑臭物质的产生提供了一定参考。     

新疆泥火山细菌遗传多样性

为了解新疆乌苏泥火山细菌多样性,从泥火山泥浆样品中直接提取总DNA,构建了含150个有效转化子的泥火山细菌16S rDNA基因文库,转化子经菌液PCR及HaeⅢ酶切后获得16个不同带型,克隆测序结果表明,其分属于16个不同的分类单元.一部分序列与已知细菌类群的16S rDNA序列相似性较高,归属变形菌门(Proteobacteria),厚壁菌门(Firmicutes),梭杆菌门(Fusobacteria),放线菌门(Actinobacteria);另外一部分序列与已知细菌类群的16S rDNA序列同源性较低,可能代表新的分类单位.研究结果显示,泥火山环境中微生物种群丰富,值得进一步研究.     

Microbial diversity in surface sediments of the Xisha Trough, the South China Sea

Microbial communities were obtained from the surface sediments of the Xisha Trough using the culture-independent technique. The characteristics of the 16S rDNA gene amplified from the sediments indicated that archaeal clones could be grouped into Euryarchaeota and Crenarchaeota, respectively. Two archaeal groups, Marine Crenarchaeotic GroupI and Terrestrial Miscellaneous Euryarchaeotal Group, were the most dominant archaeal 16S rDNA gene components in the sediments. The remaining components were related to the members of Marine Benthic Group B, Marine Benthic Group A, Marine Benthic Group D, Novel Euryarchaeotic Group and C3. The bacterial clones exhibited greater diversity than the archaeal clones with the 16S rDNA gene sequences from the members of Proteobacteria, Planctomycetes, Actinobacteria, Firmicutes, Chloroflexi, Acidobacteria, candidate division OP8, Bacterioidetes/Chlorobi and Verrucomicrobia. Most of these lineages represented uncultured microorganisms. The result suggests that a vast amount of microbial resource in the surface sediments of the South China Sea has not been known.     

Community Structure of Archaea from Deep-Sea Sediments of the South China Sea

Using the archaeal 16S rRNA gene, we determined the community structures of archaea of subseafloor sediments (～9-11 m below seafloor) from two geographically distant cores (MD05-2896, south, water depth 1,657 m; MD05-2902, north, water depth 3,697 m) in the South China Sea. Euryarchaeota accounted for 61.4% of total archaeal clone libraries at MD05-2896 and 56.2% at MD05-2902. At both locations, the Euryarchaeota-related sequences were dominated by Marine Benthic Group D, Terrestrial Miscellaneous Eryarchaeotal Group, and South African GoldMine Euryarchaeotal Group; the Crenarchaeota-related sequences were dominated by Marine Benthic Group B, Marine Group I, pSL12, and C3. The community structure showed no significant difference with depth at each location, suggesting the lack of stratification of archaeal populations in the deep-sea marine sediments in the South China Sea. On the other hand, the community structure is significantly different between the two sites, which may be related to geographical difference in the South China Sea.     

Profile of Microbial Community Structure and Presence of Endolithic Microorganisms Inside a Deep-Sea Rock

Microbial community structure in the depth profile of a deep-sea sedimentary rock collected from the Sanriku Escarpment in the Japan Trench at a depth of 6337 m were analyzed using enrichment culture methods and culture-independent molecular phylo-genetic techniques. The rock was subsampled at four depths (S1 to S4; from the surface to the inside), and carbon concentrations and colony-forming units (CFU) were determined under several culture conditions. Terminal-restriction fragment length polymorphism (T-RFLP) analysis of PCR-amplified 16S rRNA gene (rDNA) sequences indicated that a shift in bacterial and archaeal ribotype structures occurred in the sections at different depths from the surface. rDNA clone analysis revealed a significant change in microbial rDNA community structure. Bacterial community rDNA in sections S1 to S3 consisted of typical marine bacteria mainly members of the f and n -subclass of Proteobacteria, while the inner most section, S4, contained rDNA signatures for the g -subclass of Proteobacteria and the High G + C Gram-Positive Group. Major archaeal rDNA clones shifted from Marine Group I (S1) to Thermococcales (S2-S4). The changes in bacterial and archaeal rDNA community structure indicated the possible infiltration of seawater and microorganisms into the rock and strongly suggested the isolation of endolithic microbial communities over the geological history of the rock.     

High 16S rDNA bacterial diversity in glacial meltwater lake sediment,Bratina Island,Antarctica

The microbial diversity in maritime meltwater pond sediments from Bratina Island, Ross Sea, Antarctica was investigated by 16S rDNA-dependent molecular phylogeny. Investigations of the vertical distribution, phylogenetic composition, and spatial variability of Bacteria and Archaea in the sediment were carried out. Results revealed the presence of a highly diverse bacterial population and a significantly depth-related composition. Assessment of 173 partial 16S rDNA clones analyzed by amplified rDNA restriction analysis (ARDRA) using tetrameric restriction enzymes (HinP1I 5'G/CGC3'and Msp I. 5'C/CGG3', BioLabs) revealed 153 different bacterial OTUs (operational taxonomic units). However, only seven archaeal OTUs were detected, indicating low archaeal diversity. Based on ARDRA results, 30 bacterial clones were selected for sequencing and the sequenced clones fell into seven major lineages of the domain Bacteria; the alpha, gamma, and delta subdivisions of Proteobacteria, the Cytophaga-Flavobacterium-Bacteroides, the Spirochaetaceae, and the Actinobacteria. All of the archaeal clones sequenced belonged to the group Crenarchaeota and phylogenetic analysis revealed close relationships with members of the deep-branching Group 1 Marine Archaea.     

Archaeal communities associated with shallow to deep subseafloor sediments of the New Caledonia Basin

The distribution of the archaeal communities in deep subseafloor sediments [0–36 m below the seafloor (mbsf)] from the New Caledonia and Fairway Basins was investigated using DNA- and RNA-derived 16S rRNA clone libraries, functional genes and denaturing gradient gel electrophoresis (DGGE). A new method, Co-Migration DGGE (CM-DGGE), was developed to access selectively the active archaeal diversity. Prokaryotic cell abundances at the open-ocean sites were on average ∼3.5 times lower than at a site under terrestrial influence. The sediment surface archaeal community (0–1.5 mbsf) was characterized by active Marine Group 1 (MG-1) Archaea that co-occurred with ammonia monooxygenase gene ( amoA ) sequences affiliated to a group of uncultured sedimentary Crenarchaeota . However, the anoxic subsurface methane-poor sediments (below 1.5 mbsf) were dominated by less active archaeal communities, such as the Thermoplasmatales , Marine Benthic Group D and other lineages probably involved in the methane cycle ( Methanosarcinales , ANME-2 and DSAG/MBG-B). Moreover, the archaeal diversity of some sediment layers was restricted to only one lineage (Uncultured Euryarchaeota , DHVE6, MBG-B, MG-1 and SAGMEG). Sequences forming two clusters within the Thermococcales order were also present in these cold subseafloor sediments, suggesting that these uncultured putative thermophilic archaeal communities might have originated from a different environment. This study shows a transition between surface and subsurface sediment archaeal communities.     

Characterization of Archaeal Community in Contaminated and Uncontaminated Surface Stream Sediments

Archaeal communities from mercury and uranium-contaminated freshwater stream sediments were characterized and compared to archaeal communities present in an uncontaminated stream located in the vicinity of Oak Ridge, TN, USA. The distribution of the Archaea was determined by pyrosequencing analysis of the V4 region of 16S rRNA amplified from 12 streambed surface sediments. Crenarchaeota comprised 76% of the 1,670 archaeal sequences and the remaining 24% were from Euryarchaeota. Phylogenetic analysis further classified the Crenarchaeota as a Freshwater Group, Miscellaneous Crenarchaeota group, Group I3, Rice Cluster VI and IV, Marine Group I and Marine Benthic Group B; and the Euryarchaeota into Methanomicrobiales, Methanosarcinales, Methanobacteriales, Rice Cluster III, Marine Benthic Group D, Deep Sea Hydrothermal Vent Euryarchaeota 1 and Eury 5. All groups were previously described. Both hydrogen- and acetate-dependent methanogens were found in all samples. Most of the groups (with 60% of the sequences) described in this study were not similar to any cultivated isolates, making it difficult to discern their function in the freshwater microbial community. A significant decrease in the number of sequences, as well as in the diversity of archaeal communities was found in the contaminated sites. The Marine Group I, including the ammonia oxidizer Nitrosopumilus maritimus, was the dominant group in both mercury and uranium/nitrate-contaminated sites. The uranium-contaminated site also contained a high concentration of nitrate, thus Marine Group I may play a role in nitrogen cycle.     

Anaerobic oxidation of methane at different temperature regimes in Guaymas Basin hydrothermal sediments

Anaerobic oxidation of methane (AOM) was investigated in hydrothermal sediments of Guaymas Basin based on δ¹³C signatures of CH₄, dissolved inorganic carbon and porewater concentration profiles of CH₄ and sulfate. Cool, warm and hot in-situ temperature regimes (15–20 °C, 30–35 °C and 70–95 °C) were selected from hydrothermal locations in Guaymas Basin to compare AOM geochemistry and 16S ribosomal RNA (rRNA), mcrA and dsrAB genes of the microbial communities. 16S rRNA gene clone libraries from the cool and hot AOM cores yielded similar archaeal types such as Miscellaneous Crenarchaeotal Group, Thermoproteales and anaerobic methane-oxidizing archaea (ANME)-1; some of the ANME-1 archaea formed a separate 16S rRNA lineage that at present seems to be limited to Guaymas Basin. Congruent results were obtained by mcrA gene analysis. The warm AOM core, chemically distinct by lower porewater sulfide concentrations, hosted a different archaeal community dominated by the two deep subsurface archaeal lineages Marine Benthic Group D and Marine Benthic Group B, and by members of the Methanosarcinales including ANME-2 archaea. This distinct composition of the methane-cycling archaeal community in the warm AOM core was confirmed by mcrA gene analysis. Functional genes of sulfate-reducing bacteria and archaea, dsrAB, showed more overlap between all cores, regardless of the core temperature. 16S rRNA gene clone libraries with Euryarchaeota-specific primers detected members of the Archaeoglobus clade in the cool and hot cores. A V6-tag high-throughput sequencing survey generally supported the clone library results while providing high-resolution detail on archaeal and bacterial community structure. These results indicate that AOM and the responsible archaeal communities persist over a wide temperature range.