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Impact of redox-stratification on the diversity and distribution of bacterial communities in sandy reef sediments in a microcosm

机译:氧化还原分层对沙质礁沉积物中细菌群落多样性和分布的影响

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摘要

Relationships between microbial communities and geochemical environments are important in marine microbial ecology and biogeochemistry.Although biogeochemical redox stratification has been well documented in marine sediments,its impact on microbial communities remains largely unknown.In this study,we applied denaturing gradient gel electrophoresis (DGGE) and clone library construction to investigate the diversity and stratification of bacterial communities in redox-stratified sandy reef sediments in a microcosm.A total of 88 Operational Taxonomic Units (OTU) were identified from 16S rRNA clone libraries constructed from sandy reef sediments in a laboratory microcosm.They were members of nine phyla and three candidate divisions,including Proteobacteria (Alpha-,Beta-,Gamma-,Delta-,and Epsilonproteobacteria),Actinobacteria,Acidobacteria,Bacteroidetes,Chloroflexi,Cyanobacteria,Firmicutes,Verrucomicrobia,Spirochaetes,and the candidate divisions WS3,SO31 and AO19.The vast majority of these phylotypes are related to clone sequences from other marine sediments,but OTUs of Epsilonproteobacteria and WS3 are reported for the first time from permeable marine sediments.Several other OTUs are potential new bacterial phylotypes because of their low similarity with reference sequences.Results from the 16S rRNA,gene clone sequence analyses suggested that bacterial communities exhibit clear stratification across large redox gradients in these sediments,with the highest diversity found in the anoxic layer (15-25 mm) and the least diversity in the suboxic layer (3-5 mm).Analysis of the nosZ,and amoA gene libraries also indicated the stratification of denitrifiers and nitrifiers,with their highest diversity being in the anoxic and oxic sediment layers,respectively.These results indicated that redox-stratification can affect the distribution of bacterial communities in sandy reef sediments.
机译:在海洋微生物生态学和生物地球化学中,微生物群落与地球化学环境之间的关系非常重要。尽管海洋沉积物中已充分记录了生物地球化学氧化还原分层,但其对微生物群落的影响仍然未知。在本研究中,我们应用了变性梯度凝胶电泳(DGGE)克隆库的构建,以调查在一个微观世界中氧化还原分层的沙礁沉积物中细菌群落的多样性和分层。从实验室缩影中由沙礁沉积物中构建的16S rRNA克隆文库中鉴定出总共88个操作分类单位(OTU)它们是9个门和3个候选类的成员,包括Proteobacteria(Alpha,Beta,Gamma,Delta和Epsilon变形杆菌),Actinobacteria,Acidobacteria,Bacteroidetes,Chloroflexi,Cyanobacteria,Firmicutes,Verrucomicrobia,Spirochaetes等WS3,SO31和AO19部门。菌型与其他海洋沉积物的克隆序列有关,但首次报道了渗透性海洋沉积物中的Epsilon变形杆菌和WS3的OTU。由于其他OTU与参考序列的相似性较低,其他几种OTU也是潜在的新细菌系统型.16S rRNA的结果基因克隆序列分析表明,在这些沉积物中,细菌群落在较大的氧化还原梯度上表现出清晰的分层,其中缺氧层的多样性最高(15-25 mm),亚缺氧层的多样性最低(3-5 mm)。对nosZ和amoA基因库的分析也表明反硝化剂和硝化剂的分层,其最高的多样性分别在缺氧和含氧沉积物层中。这些结果表明氧化还原分层可影响沙礁中细菌群落的分布。沉积物。

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  • 来源
    《中国海洋湖沼学报(英文版)》 |2011年第6期|1209-1223|共15页
  • 作者单位

    State Key Laboratory of Crop Biology, College of Life Sciences, Shandong Agricultural University, Tai'an 271000, China;

    Department of Oceanography, University of Hawaii, 1000 Pope Road, Honolulu, Hawaii 96822, USA;

    Department of Oceanography, University of Hawaii, 1000 Pope Road, Honolulu, Hawaii 96822, USA;

    Department of Oceanography, University of Hawaii, 1000 Pope Road, Honolulu, Hawaii 96822, USA;

    Department of Oceanography, University of Hawaii, 1000 Pope Road, Honolulu, Hawaii 96822, USA;

    Shenzhen Engineering Laboratory for Algal Biofuel Technology Development and Application, School of Environment and Energy, Peking University Shenzhen Graduate School, Shenzhen 518055, China;

  • 收录信息 中国科学引文数据库(CSCD);中国科技论文与引文数据库(CSTPCD);
  • 原文格式 PDF
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