DNA extractions from deep subseafloor sediments: novel cryogenic-mill-based procedure and comparison to existing protocols

Extracting DNA from deep subsurface sediments is challenging given the complexity of sediments types, low biomasses, resting structures (spores, cysts) frequently encountered in deep sediments, and the potential presence of enzymatic inhibitors. Promising results for cell lysis efficiency were recently obtained by use of a cryogenic mill (Lipp et al., 2008). These findings encouraged us to devise a DNA extraction protocol using this tool. Thirteen procedures involving a combination of grinding in liquid nitrogen (for various durations and beating rates) with different chemical solutions (phenol, chloroform, SDS, sarkosyl, proteinase, GTC), or with use of DNA recovery kits (MagExtractor®) were compared. Effective DNA extraction was evaluated in terms of cell lysis efficiency, DNA extraction efficiency, DNA yield and determination of prokaryotic diversity. Results were compared to those obtained by standard protocols: the FastDNA®SPIN kit for soil and the Zhou protocol. For most sediment types grinding in a cryogenic mill at a low beating rate in combination with direct phenol-chloroform extraction resulted in much higher DNA yields than those obtained using classical procedures. In general (except for clay-rich sediments), this procedure provided high-quality crude extracts for direct downstream nested-PCR, from cell numbers as low as 1.1 × 10⁶ cells/cm³. This procedure is simple, rapid, low-cost, and could be used with minor modifications for large-scale DNA extractions for a variety of experimental goals.     

Biogeography of Rhizobium radiobacter and distribution of associated temperate phages in deep subseafloor sediments

Bacteriophages might be the main ‘predators'' in the marine deep subsurface and probably have a major impact on indigenous microbial communities. To identify their function within this habitat, we have determined their abundance and distribution along the sediment columns of two continental margin and two open ocean sites that were recovered during Leg 201 of the Ocean Drilling Program. For all investigated sites, viral abundance followed the total cell numbers with a virus-to-cell ratio between 1 and 10 in the upper 100 mbsf (meters below seafloor). An increasing ratio of about 20 in deeper layers indicated an ongoing viral production in up to 11 Ma old sediments. We have used Rhizobium radiobacter as the most frequently isolated organism from the deep subsurface with a high in situ abundance to identify the frequency of associated rhizobiophages. In this study, 16S rRNA gene copies of R. radiobacter accounted for up to 5.6% of total bacterial 16S rRNA genes (average: 0.75%) as detected by quantitative PCR. A distinctive distribution was identified for R. radiobacter as indicated by a site-specific arrangement of genetically similar populations. Whole genome information of rhizobiophage RR1-A was used to generate a primer system for quantitative PCR specifically targeting the prophage antirepressor gene, indicative for temperate phages. The quantification of this gene within various sediment horizons showed a contribution of temperate phages of up to 14.3% to the total viral abundance. Thus, the high amount of temperate phages within the sediments and among all investigated isolates indicates that lysogeny is the main viral proliferation mode in deep subsurface populations.     

Methanogen and bacterial diversity and distribution in deep gas hydrate sediments from the Cascadia Margin as revealed by 16S rRNA molecular analysis

The microbial community of a deep (to 234 m below the sea floor) sediment gas hydrate deposit (Cascadia Margin Ocean Drilling Program Site 889/890, Leg 146) was analysed for the first time by molecular genetic techniques. Both bacterial and methanogen diversity were determined by phylogenetic analysis of ribosomal DNA sequences. High molecular mass DNA, indicative of active bacteria, was present in all of the samples. Ribosomal RNA genes were amplified from extracted DNA extracted from sediment using bacteria, and methanogen specific PCR primers, the latter designed in this study. Phylogenetic analysis of approximately 400 bacterial clones demonstrated that 96% were members of the Proteobacteria. These clones were affiliated with the alpha, beta and gamma subdivisions, with Caulobacter (Zymomonas group), Ralstonia and Pseudomonas phylotypes predominating. The methanogen clones were of low diversity and clustered in three sub-groups. Two of these sub-groups (contained 96% of the 400 clones) were closely related to Methanosarcina mazeii, while the third sub-group clustered in the Methanobacteriales. This analysis of a deep sediment gas hydrate environment shows a bacteria and methanogen community of limited diversity and confirms that the gas hydrate zone is biogeochemically active. These results are consistent with the presence of bacterial populations capable of methanogenesis throughout the core, and suggest that the methane hydrate at this site is at least partially biogenic in origin.     

Prokaryotic community composition and biogeochemical processes in deep subseafloor sediments from the Peru Margin

The community compositions of Bacteria and Archaea were investigated in deep, sub-seafloor sediments from the highly productive Peru Margin (ODP Leg 201, sites 1228 and 1229, c. 25 km apart) down to nearly 200 m below the seafloor using taxonomic (16S rRNA) and functional (mcrA and dsrA) gene markers. Bacterial and archaeal groups identified from clone libraries of 16S rRNA gene sequences at site 1229 agreed well with sequences amplified from bands excised from denaturing gradient gel electrophoresis (DGGE) depth profiles, with the exception of the Miscellaneous Crenarchaeotic Group (MCG). This suggested that the prokaryotic community at site 1228, obtained from DGGE profiling alone, was reliable. Sites were dominated by Bacteria in the Gammaproteobacteria, Chloroflexi (green non-sulphur bacteria) and Archaea in the MCG and South African Gold Mine Euryarchaeotic Group, although community composition changed with depth. The candidate division JS1 was present throughout both sites but was not dominant. The populations identified in the Peru Margin sediments consisted mainly of prokaryotes found in other deep subsurface sediments, and were more similar to communities from the Sea of Okhotsk (pelagic clays) than to those from the low organic carbon Nankai Trough sediments. Despite broad similarities in the prokaryotic community at the two sites, there were some differences, as well as differences in activity and geochemistry. Methanogens (mcrA) within the Methanosarcinales and Methanobacteriales were only found at site 1229 (4 depths analysed), whereas sulphate-reducing prokaryotes (dsrA) were only found at site 1228 (one depth), and these terminal-oxidizing prokaryotes may represent an active community component present at low abundance. This study clearly demonstrates that the deep subsurface sediments of the Peru Margin have a large diverse and metabolically active prokaryotic population.     

Phylogenetic diversity and activity of aerobic heterotrophic bacteria from a hypersaline oil-polluted microbial mat

The diversity and function of aerobic heterotrophic bacteria (AHB) in cyanobacterial mats have been largely overlooked. We used culture-dependent and molecular techniques to explore the species diversity, degradative capacities and functional guilds of AHB in the photic layer (2mm) of an oil-polluted microbial mat from Saudi Arabia. Enrichment isolation was carried out at different salinities (5% and 12%) and temperatures (28 and 45 degrees C) and on various substrates (acetate, glycolate, Spirulina extract and crude oils). Counts of most probable number showed a numerical abundance of AHB in the range of 1.15-8.13x10(6) cellsg(-1) and suggested the presence of halotolerant and thermotolerant populations. Most of the 16S rRNA sequences of the obtained clones and isolates were phylogenetically affiliated to the groups Gammaproteobacteria, Bacteriodetes and Alphaproteobacteria. Groups like Deltaproteobacteria, Verrucomicrobia, Planctomycetes, Spirochaetes, Acidobacteria and Deinococcus-Thermus were only detected by cloning. The strains isolated on acetate and glycolate belonged to the genera Marinobacter, Halomonas, Roseobacter and Rhodobacter whereas the strains enriched on crude oil belonged to Marinobacter and Alcanivorax. Members of the Bacteriodetes group were only enriched on Spirulina extract indicating their specialization in the degradation of cyanobacterial dead cells. The substrate spectra of representative strains showed the ability of all AHB to metabolize cyanobacterial photosynthetic and fermentation products. However, the unique in situ conditions of the mat apparently favored the enrichment of versatile strains that grew on both the cyanobacterial exudates and the hydrocarbons. We conclude that AHB in cyanobacterial mats represent a diverse community that plays an important role in carbon-cycling within microbial mats.     

Vertical distribution and diversity of bacteria and archaea in sulfide and methane-rich cold seep sediments located at the base of the Florida Escarpment

The bacterial and archaeal communities of the sediments at the base of the Florida Escarpment (Gulf of Mexico, USA) were investigated using molecular phylogenetic analysis. The total microbial community DNA of each of three vertical zones (top, middle and bottom) of a sediment core was extracted and the 16S rRNA genes were amplified by PCR, cloned and sequenced. Shannon–Weaver Diversity measures of bacteria were high in all three zones. For the archaea, diversity was generally low, but increased with depth. The archaeal clonal libraries were dominated by representatives of four groups of organisms involved in the anaerobic oxidation of methane (ANME groups). Phylogenetic analysis of bacteria suggests the dominance of -proteobacteria in the top zone, the -, - and -proteobacteria in the middle zone and the -proteobacteria in the bottom zone of the core. Members of the Cytophaga–Flexibacter–Bacteroidetes group, the Chloroflexi/green non-sulfur bacteria, the Gram+ (Firmicutes), the Planctomyces, candidate division WS3 and Fusobacterium were also detected. Our data suggest that the community structure and diversity of microorganisms can shift greatly within small vertical distances, possibly in response to changes in the physical and chemical conditions.     

Analysis of DGGE profiles to explore the relationship between prokaryotic community composition and biogeochemical processes in deep subseafloor sediments from the Peru Margin

The aim of this work was to relate depth profiles of prokaryotic community composition with geochemical processes in the deep subseafloor biosphere at two shallow-water sites on the Peru Margin in the Pacific Ocean (ODP Leg 201, sites 1228 and 1229). Principal component analysis of denaturing gradient gel electrophoresis banding patterns of deep-sediment Bacteria, Archaea, Euryarchaeota and the novel candidate division JS1, followed by multiple regression, showed strong relationships with prokaryotic activity and geochemistry (R(2)=55-100%). Further correlation analysis, at one site, between the principal components from the community composition profiles for Bacteria and 12 other variables quantitatively confirmed their relationship with activity and geochemistry, which had previously only been implied. Comparison with previously published cell counts enumerated by fluorescent in situ hybridization with rRNA-targeted probes confirmed that these denaturing gradient gel electrophoresis profiles described an active prokaryotic community.     

渤海沉积物产脂肪酶细菌的筛选及其多样性分析

【目的】从渤海沉积物中分离筛选产脂肪酶细菌,分析其物种多样性,增加人们对渤海生态系统中产脂肪酶菌多样性的认识,获取高效产脂肪酶菌株,为海洋产脂肪酶微生物的挖掘提供菌群资源。【方法】分别将8个渤海沉积物样品梯度稀释涂布至吐温-80筛选平板和三丁酸甘油酯筛选平板,选择性分离产脂肪酶细菌;分析基于16SrRNA基因序列的系统发育关系,揭示这些细菌的分类地位和遗传多样性;利用对硝基苯酚法测定胞外脂肪酶活性,筛选出高效产脂肪酶菌株。【结果】从8个渤海沉积物样品中分离获得51株产脂肪酶细菌,这些菌株隶属于Bacteroidetes、Proteobacteria和Firmicutes三个门的8个属,其中Pseudoalteromonas(35.2%)、Marinobacter(23.5%)和Sulfitobacter(17.6%)是优势菌群;脂肪酶酶活性实验表明所有测定菌株都能够分泌脂肪酶,菌株70623分泌的脂肪酶酶活最高,为42.4 U/m L。【结论】渤海沉积物中可培养产脂肪酶细菌类群较为丰富,Pseudoalteromonas、Marinobacter和Sulfitobacter菌株是优势菌群,测定菌株所产胞外脂肪酶能力不同,获得了一株高效产脂肪酶菌株Marinobacter sp.70623。     

Phylogenetic diversity of nitrogen-fixing bacteria in mangrove sediments assessed by PCR-denaturing gradient gel electrophoresis

Culture-independent PCR–denaturing gradient gel electrophoresis (DGGE) was employed to assess the composition of diazotroph species from the sediments of three mangrove ecosystem sites in Sanya, Hainan Island, China. A strategy of removing humic acids prior to DNA extraction was conducted, then total community DNA was extracted using the soil DNA kit successfully for nifH PCR amplification, which simplified the current procedure and resulted in good DGGE profiles. The results revealed a novel nitrogen-fixing bacterial profile and fundamental diazotrophic biodiversity in mangrove sediments, as reflected by the numerous bands present DGGE patterns. Canonical correspondence analysis (CCA) revealed that the sediments organic carbon concentration and available soil potassium accounted for a significant amount of the variability in the nitrogen-fixing bacterial community composition. The predominant DGGE bands were sequenced, yielding 31 different nifH sequences, which were used in phylogenetic reconstructions. Most sequences were from Proteobacteria, e.g. α, γ, β, δ-subdivisions, and characterized by sequences of members of genera Azotobacter, Desulfuromonas, Sphingomonas, Geobacter, Pseudomonas, Bradyrhizobium and Derxia. These results significantly expand our knowledge of the nitrogen-fixing bacterial diversity of the mangrove environment.     

深部生物圈古菌的研究进展与展望

古菌作为深部生物圈中常见的原核生物,广泛分布于各类海洋沉积生境中,在沉积物生物地球化学循环中发挥着重要作用.由于不同的古菌类群对环境条件存在生理适应性差异,它们分别在近岸沿海和开阔大洋沉积物中构成了厌氧微生物生态系统和好氧微生物生态系统.本文通过对近岸与远洋、沉积物与上覆水体两个不同维度的古菌群落结构进行比较,以及对出...     

玛珥湖好氧不产氧光合细菌pufM基因DNA和mRNA的定量及多样性分析

【目的】湖光岩玛珥湖是一类特殊的火山口湖,它完全封闭,地质年代久远,尚未受人类活动的剧烈影响,孕育着丰富而特殊的微生物种群。好氧不产氧光合细菌(AAPB)是以其在有氧情况下能行使光合功能而定义的一类专性异养细菌,其生理生态特征独特,进化年代久远,在水生生态系统的上层水体中广泛分布。目前,AAPB在玛珥湖水体中是否有分布仍是未知。【方法】构建和比较夏季湖水1 m、5 m、12 m三个水层的总DNA和总RNA的AAPB光合中心合成的关键基因pufM的6个克隆文库,并结合定量PCR技术,分析了不同水层AAPB的分布、系统发育多样性及其在总细菌中的比重。【结果】6个文库覆盖率和稀释曲线显示样本初步揭示了各水层优势AAPB类群的多样性。BLAST核苷酸同源性介于80%93%;多样性指数表明,湖光岩表层和底层多样性相当,中间层最低,总RNA的多样性高于总DNA。系统发育分析结果表明,OTU21 24所含的序列(占总序列的49.43%)与β-变形细菌的进化距离最接近,是湖光岩玛珥湖的优势AAPB菌群。定量PCR结果显示1 m水层中AAPB在总细菌中的比重最高,可达38.06%;而5 m水层中AAPB所占的比重最低,仅为0.85%;12 m为9.54%。【结论】湖光岩玛珥湖孕育着丰富而多样的AAPB类群。     

西南印度洋中脊深海沉积物砷抗性菌的富集分离与多样性分析

[目的]为了筛选深海砷抗性菌,了解印度洋中脊深海沉积物砷抗性菌的多样性情况.[方法]通过砷富集培养,筛选出砷抗性菌;通过变性梯度凝胶电泳(DGGE)分析与构建16S rDNA克隆文库法两种手段分析了富集物中砷抗性菌的多样性.利用兼并引物PCR,从抗性菌株中克隆与砷抗性相关的基因.[结果]共筛选到8株砷抗性菌,分别属于y-proteobacteria的5个不同的属.其中,菌株AS-I1-3的抗性最高,可以在26×10-3 mol/L三价砷存在的情况下生长,该菌株的16S rDNA序列与菌株Pseudoalteromonas tetraodoni IAM同源性最高(100%).DGGE分析显示,该菌是富集物中的最优势菌,其次是盐单胞菌(Halomonas)和海杆菌(Marinobacter).16S rDNA克隆文库分析结果进一步证明,与菌株AS-I1-3序列相同的克隆子占整个克隆文库的72.5%;而与菌株AS-I1-5(Halomonas meridiana,100%)和菌株Mn-I1-6(Marinobacter vinifirmus,99%)序相同的克隆子分别占10%和7.5%.然而,利用兼并引物PCR,仅能从2株非优势菌中克隆到了与砷抗性相关的基因,表明菌群中的优势抗性菌可能有其他的抗性机制.[结论]在深海环境中存在着多种砷抗性菌,其中Pseudoalteromonas属的菌株是该富集条件下的砷抗性优势菌.这些砷抗性菌在大洋环境砷元素的生物地球化学循环中的作用有待进一步研究.     

Enumeration of aerobic faecal flora in healthy and diseased individuals

Studies on aerobic bacterial flora of faecal samples from healthy and diarrhoeal patients of different age groups were carried out. Giardia cysts were observed in the faecal sample of both the diarrhoeal patients. Organisms were cultivated on non-specific as well as specific enrichment media. Based on morphological, physiological and biochemical characteristics, organisms were identified to genus level. Irrespective of the age, a sharp decrease in the population of Lactobacilli, Proteus, Aeromonas, Yersinia, Micrococci and Escherichia coli with concomitant increase in the population of Klebsiella were observed in the diseased individuals when compared with the healthy ones. Significant differences were observed in the population of spore-forming Bacillus and Staphylococcus when both the diseased individuals were compared. Absence of Enterococcus and Providencia both in the child and adult diseased individuals were quite significant. Association of Candida, Pseudomonas and other aerobic spore formers only with the adult individuals confirmed some of the earlier observations. The presence of Gram-positive Diplococci and unidentified Gram-negative cocci in the healthy child were quite significant. It was therefore, evident that the alteration of resident flora was associated with the disease.     

泥浸汁对太湖沉积物中的好氧可培养细菌多样性的影响

【目的】研究添加泥浸汁与否对太湖沉积物中可培养细菌的影响。【方法】采用R2A培养基和添加泥浸汁R2A培养基对沉积物中细菌进行分离培养,16S r RNA基因系统发育分析比较种群结构。【结果】培养基中添加泥浸汁,可使可培养细菌的种类数量增加到1.6倍。16S r RNA基因序列分析表明,培养的优势细菌类群存在明显差别。R2A培养基上生长的细菌主要为厚壁菌门(52%)、放线菌门(24%)、变形菌门(20%)和拟杆菌门(4%),其中大部分细菌与芽孢杆菌属、假单胞菌属、节杆菌属等关系密切;而添加泥浸汁的R2A培养基上生长的细菌则主要为变形菌门(40%)、放线菌门(35%)、厚壁菌门(22.5%)和拟杆菌门(2.5%),与鞘脂单胞菌属、芽孢杆菌属、副球菌属、节杆菌属等关系密切。【结论】添加泥浸汁原始营养因子可提高沉积物中可培养细菌的多样性,提高菌种可培养效率。     

海岸带沉积物中氮循环功能微生物多样性

海岸带生境类型多样,环境梯度明显,是研究微生物多样性、群落结构与功能关系及调控机制的天然实验场.沉积物是海岸带环境中营养盐再生与转化发生的重要场所,其中多种微生物类群在氮素循环过程中扮演重要角色.本文重点介绍海岸带沉积物中固氮菌、氨氧化菌、厌氧氨氧化菌、反硝化与硝酸盐铵化微生物的基于16SrRNA基因的物种多样性和基于关键酶基因nifH、amoA、narG、nirS、nirK、nosZ、nrfA、hzo、hzs等的功能多样性;总结了在海岸带特有生境(如河口、潮间带、海草藻床、红树林、盐沼、珊瑚礁、浅海等)及污染胁迫、生物扰动等条件下各功能类群的群落组成特征及时空变化规律,并提出今后需要重点关注新的培养技术和方法的开发,以进一步提高微生物的可培养性,将单细胞基因组测序与分析技术、DNA和RNA结合起来研究,以全面了解氮循环微生物多样性、参与介导硝酸盐铵化过程的微生物多样性等方面.     

Psychrotrophic amylolytic bacteria from deep sea sediment of Prydz Bay, Antarctic: diversity and characterization of amylases

Seventeen psychrotrophic bacteria with cold-adaptive amylolytic, lipolytic or proteolytic activity were isolated from deep sea sediment of Prydz Bay, Antarctic. They were affiliated with γ-Proteobacteria (12 strains) and gram-positive bacteria (5 strains) as determined by 16S rDNA sequencing. The amylase-producing strains belonged to genus Pseudomonas, Rhodococcus, and Nocardiopsis. Two Pseudomonas strains, 7193 and 7197, which showed highest amylolytic activity were chosen for further study. The optimal temperatures for their growth and amylase-producing were between 15 and 20°C. Both of the purified amylases showed highest activity at 40°C and pH 9.0, and retained 50% activity at 5°C. The SDS-PAGE and zymogram activity staining showed that the molecular mass of strain 7193 and 7197 amylases were about 60 and 50 kDa respectively. The Pseudomonas sp. 7193 amylase hydrolyzed soluble starch into glucose, maltose, maltotriose, and maltotetraose, indicating that it had both activities of α-amylase and glucoamylase. The product hydrolyzed by Pseudomonas sp. 7197 amylase was meltotetraose.