宏基因组学分析揭示深古菌Bathyarchaeota B242的代谢特征

【背景】海洋沉积物中蕴含着丰富的微生物资源,估算约2.9×1029个细胞,与海水中的微生物总量相当。但是由于缺少可培养物,大部分的微生物缺乏生理特征、代谢方式以及生态功能的相关研究。深古菌(Bathyarchaeota)是一类典型的未培养微生物,在全球海洋沉积物中普遍存在,并且具有很高的丰度。【目的】对深古菌代谢潜能及其在海洋沉积物中发挥的生态功能进行更加深入的研究。【方法】应用宏基因组学的技术手段,对采集自瓜伊马斯盆地的深海热液沉积物样本进行了分析,获得了一个接近完整的深古菌基因组Bathyarchaeota B242。【结果】对Bathyarchaeota B242基因组的分析发现,其具有以降解蛋白质和多种碳水化合物为主的异养代谢途径,同时还具有通过还原型乙酰辅酶A途径实现的自养途径。【结论】同时具有自养和异养代谢途径对Bathyarchaeota B242适应低物质能量供给环境下的生存起到重要作用。     

光照对深海热液喷口周围可培养微生物的生长影响

研究采用析因实验设计,探讨了光照和培养温度对深海热液喷口周围可培养微生物生长繁殖的影响。样品培养10天后。对培养液中蛔菌量进行显微计数,实验数据用SFSS11．0统计软件中的方差分析程序进行处理。统计结果显示：在标准大气压下,在33℃、50℃和65℃三个实验温度中,当温度为33℃时,光照培养液中细茼浓度约为暗培养液中的3．5倍;而在50℃和65℃的培养液中其细菌浓度均比暗培养液中的要低。研究结果为进一步荻取、认识与开发利用深海喷口周围细菌贵源打下了基础。     

深海热液区化能自养菌Caminibacter profundus氢酶及其对H2的响应特点

化能自养菌中的氢酶在深海热液区生态系统的物质和能量转化中具有重要作用。以Caminibacter profundus为研究对象,通过设计PCR引物,克隆编码膜结合的类型I NiFe-氢酶大亚基基因序列hynL并进行生物信息学分析;研究hynL相对表达、甲基紫晶(MV)还原氢酶活性以及菌株生长对H2浓度变化的响应特点。结果表明,从C.profundus克隆获得864 bp的hynL基因片段,其编码的氨基端序列与Lebetimonas acidiphila的相似性为99%,与热液区化能自养的Epsilonproteobacteria D类群的类型I NiFe氢酶大亚基属同一分支。hynL相对表达量和MV还原的氢酶活性分别于12 h和24 h达到最高,此时菌体处于指数生长期;hynL相对表达量和MV还原的氢酶活性和菌株生长的最适H2浓度均为60%。提示C.profundus通过调控hynL的表达,响应环境中H2浓度的变化,以影响菌株能量代谢的催化过程和生长繁殖。     

光照对深海热液喷口周围可培养微生物的生长影响

研究采用析因实验设计,探讨了光照和培养温度对深海热液喷口周围可培养微生物生长繁殖的影响。样品培养10天后,对培养液中细菌量进行显微计数,实验数据用SPSS11.0统计软件中的方差分析程序进行处理。统计结果显示:在标准大气压下,在33℃、50℃和65℃三个实验温度中,当温度为33℃时,光照培养液中细菌浓度约为暗培养液中的3.5倍;而在50℃和65℃的培养液中其细菌浓度均比暗培养液中的要低。研究结果为进一步获取、认识与开发利用深海喷口周围细菌资源打下了基础。     

劳盆地深海热液喷口沉积物中细菌多样性研究

采用PCR-RFLP技术调查了劳盆地深海热液喷口两位点沉积物中的细菌多样性。结果表明, 在劳盆地深海热液喷口沉积物环境中细菌多样性十分丰富, 样品DY1中发现6个细菌类群, DY2中则存在4个细菌类群, 其中Gammaproteobacteria细菌亚群和Epsilonproteobacteria细菌亚群在两文库中均占据最大比例, 为沉积物样品中的优势菌群。另外, 在克隆文库中还发现了一些与数据库中的已知序列同源性较低的类群, 从而说明劳盆地深海热液喷口沉积物中存在特有的微生物种属。     

宏基因组学及其在口腔微生物研究中的应用

宏基因组是指环境中所有微生物的遗传物质总和。宏基因组学技术可以最大限度地利用环境中的微生物资源,受到了国内外微生物研究者的重点关注。口腔中寄居着大量的微生物群落,以往对口腔疾病微生物的研究大多局限于单纯的细菌培养技术,然而,由于培养技术的局限性,部分微生物很难或根本不能培养,宏基因组学技术打破了这一局限性,帮助人类发掘更丰富的口腔微生物资源。最近,以宏基因组学测序为基础的研究描绘出了口腔生态系统的图谱,越来越多的实验证明口腔微生物组在各种口腔疾病甚至全身系统性疾病中的重要作用。同时,这也为基于人类微生物组的诊断和治疗开辟了新的途径。本综述旨在说明宏基因组学是研究人类口腔疾病及全身疾病相关微生物的得力工具,而且具有广阔的发展前景,同时也讨论了宏基因组学在应用中有待克服的局限性。     

基于宏基因组学分析湘西腊肉的细菌多样性

目的 解析湘西成熟腊肉制品中微生物群落结构和种群丰度。 方法 采集湖南慈利县、辰溪县和古丈县3个样地成熟腊肉样品,提取样品细菌总DNA,利用454焦磷酸高通量测序法进行测序,并进行生物信息学分析。 结果 从慈利腊肉获得10 449条优质序列,聚类得到132个OTUs,注释为8个菌门,鉴定出82个属;其中变形菌门为主要细菌类群,占比90.1%;葡萄球菌属为优势菌属,占比47.6%。辰溪腊肉获得10 719条优质序列,聚类得到70个OTUs,归入5个菌门,37个菌属,变形菌门占比54.2%,为优势菌门;葡萄球菌属为第一大菌属,占比65.5%。古丈腊肉获得15 577条优质序列,聚类得到97个OTUs,分属于9个菌门,52个菌属,其中厚壁菌门占比84.5%,为最丰富的类群;葡萄球菌属为优势属,占比71.1%。3地区腊肉样品群落多样性高低依次为辰溪>慈利>古丈,湘西成熟腊肉中优势细菌类群为葡萄球菌,其次为鞘氨醇单胞菌和嗜冷杆菌。鞘氨醇单胞菌在腊肉样品中作为优势菌群为首次报道。 结论 湘西成熟腊肉中蕴含着丰富的微生物类群,鞘氨醇单胞菌可能与湘西腊肉独特风味形成有一定关联。     

基于宏基因组学的野生鸟类肠道菌群研究现状

肠道微生物对鸟类宿主至关重要,宏基因组学技术是研究野生鸟类肠道菌群的重要手段,且研究方法已较为成熟。本文对宏基因组技术在野生鸟类肠道菌群的发展现状进行了总结,并结合其在野生鸟类肠道微生物领域中的具体应用,对野生鸟类肠道微生物的组成、影响因素及肠道微生物功能进行了梳理,以期为野生鸟类尤其是濒危鸟类的保护研究提供新的方向,进一步推动宏基因组学在野生鸟类肠道菌群研究中的应用。     

基于宏基因组学的卤醇脱卤酶筛选

环境中的多数有机卤化物具有高毒性和低可降解性,卤醇脱卤酶可以催化邻卤醇进行分子内亲和取代生成相应的环氧化物,在消除有机卤化物的污染方面具有十分重要的作用.此外,在催化环氧化物和邻卤醇之间的转化反应中卤醇脱卤酶具有很高的立体选择性,因而在手性药物合成方面也有广阔的应用前景.宏基因组是生境中全部微小生物遗传物质的总和,极大地扩展了微生物资源的利用空间.本文介绍了卤醇脱卤酶的特性及利用宏基因组方法筛选新的卤醇脱卤酶的两种方法及各自的优缺点.     

宏基因组测序分析东寨港红树林淤泥和水体微生物的多样性

为深入了解海南东寨港红树林生态系统微生物多样性及其在氮、磷、硫等代谢循环中的功能特点,本研究采用宏基因组测序,从物种注释与丰度、群落功能及多样性指数等角度,分析红树林淤泥和水体生境中微生物群落结构及生态功能的特异性。结果显示,在淤泥中检测到53个门、909个属的微生物类群,有3个占比超过1%的优势门类,其中变形杆菌门为83.78%,处于绝对优势,其下的12个优势属全部来自变形杆菌门;不动杆菌属是聚磷微生物的主要类群,其在淤泥中含量是水体的107.7倍,硫氧化单胞菌属、脱硫杆菌属是硫化物代谢的主要菌属,主要存在于淤泥生境当中。在水体中检测到64个门、1 522个属,包括13个优势门类、7个优势属;Nitrospinae和硝化螺旋菌门是亚硝酸盐氧化代谢的关键类群,两者在水体中占比分别是淤泥中的28.1倍和6.8倍。多样性评估得知,水体样品中的Shannon Wiener指数和Simpson指数均高于淤泥样品,两样品在属分类学单元上的Simpson指数趋近于1,表明红树林生态系统具有非常高的微生物多样性,水体生境的微生物多样性高于淤泥;亚硝酸盐的微生物代谢循环主要发生在水体生境中,微生物对磷的富集作用和硫化合物的氧化还原代谢主要发生在淤泥生境中。本研究有助于认识东寨港红树林湿地生境中的微生物资源状况,为保护红树林生态系统和开发利用其中的微生物资源提供依据。     

DNA base composition and genome size of the prokaryotic symbiont in Riftia pachyptila (Pogonophora)

Abstract It has been proposed that Riftia pachyptila , a pogonophoran tube worm abundant at hydrothermal deep sea vents, metabolizes solely via a chemoautotrophic symbiosiols. The symbionts resemble sulfur oxidizing bacteria and form the specific 'trophosome' tissue. Samples of DNA purified from trophosome and vestimentum (muscle) tissues of R. pachyptila were comparatively characterized by thermal denaturation studies, and by analysis of renaturation kinetics. The results show that the great majority of trophosome DNA is homogeneous and prokaryotic with a base ratio of approx. 58 mol% G + C. Its genome size (genetic complexity) is typical of free-living bacteria. Approx. 5% of trophosome DNA appears to be invertebrate DNA equivalent to that found in the vestimentum tissue which lacks symbionts.     

Microbial Distribution in a Hydrothermal Plume of the Southwest Indian Ridge

Hydrothermal plumes are widely distributed throughout the global spreading ridges, yet few of them are microbiologically explored. The ultraslow-spreading ridges, recently recognized as a unique, new class of mid-ocean-ridge system, have provided surprises and new insights in hydrothermal system research. A suite of water column samples including both hydrothermal plume samples and ambient seawater were collected at different depths from the ultraslow-spreading Southwest Indian Ridge (SWIR) in 2010. We use molecular approaches such as clone libraries, denaturing gradient gel electrophoresis (DGGE) and quantitative PCR to determine microbial community compositions and their spatial variability within the hydrothermal plume and seawater. Phylogenetic analysis showed that plume samples were mainly dominated by members of α-Proteobacteria and γ-Proteobacteria and members of marine group I group within the Crenarchaeota. Within the hydrothermal plume, archaeal populations were spatially homogeneous, while bacterial compositions were heterogeneous and remarkably distinct at different depths. Moreover, several lineages, closely related to known Mn(II) oxidizers were found to be abundant and even predominant within the plume bacterial communities. DGGE band patterns showed that there was no significant difference in microbial compositions between the samples of hydrothermal plume and ambient seawater. Taken together, we inferred that microbial communities in the SWIR hydrothermal plumes were sourced from ambient seawater rather than from seafloor vent-derived niches. This is the first report on the characteristics of microbial community structures in hydrothermal plume and ambient seawater in the Southwest Indian Ridge.     

Novel uncultured Epsilonproteobacteria dominate a filamentous sulphur mat from the 13 degrees N hydrothermal vent field, East Pacific Rise

Rapid growth of microbial sulphur mats have repeatedly been observed during oceanographic cruises to various deep-sea hydrothermal vent sites. The microorganisms involved in the mat formation have not been phylogenetically characterized, although the production of morphologically similar sulphur filaments by a Arcobacter strain coastal marine has been documented. An in situ collector deployed for 5 days at the 13 degrees N deep-sea hydrothermal vent site on the East Pacific Rise (EPR) was rapidly colonized by a filamentous microbial mat. Microscopic and chemical analyses revealed that the mat consisted of a network of microorganisms embedded in a mucous sulphur-rich matrix. Molecular surveys based on 16S rRNA gene and aclB genes placed all the environmental clone sequences within the Epsilonproteobacteria. Although few 16S rRNA gene sequences were affiliated with that of cultured organisms, the majority was related to uncultured representatives of the Arcobacter group (< or = 95% sequence similarity). A probe designed to target all of the identified lineages hybridized with more than 95% of the mat community. Simultaneous hybridizations with the latter probe and a probe specific to Arcobacter spp. confirmed the numerical dominance of Arcobacter-like bacteria. This study provides the first example of the prevalence and ecological significance of free-living Arcobacter at deep-sea hydrothermal vents.     

An extremely thermophilic Methanococcus from a deep sea hydrothermal vent and its plasmid

An extremely thermophilic methanogen was isolated from a hydrothermal vent core sample from Guaymas Basin, Gulf of California, at a depth of 2003 m. The isolate, designated strain AG86, was a coccoid autotroph using H₂-CO₂ as energy and carbon source with a growth temperature range of 48 to 92°C, optimum, 85°C. AG86 required NaCl and Mg²⁺ and trace amounts of selenite and tungstate. Vitamins were not required. However, yeast extract, Casamino acids and Trypticase stimulated growth significantly. When grown in the presence of these stimulants and at the optimal growth temperature and pH 6.5, the minimum doubling time was 20 min. Cells were fragile and readily lysed by detergents. The mol% G+C was 33%. These results and partial 16S rRNA sequencing indicated that AG86 belonged to the genus Methanococcus and closely resembled Methanococcus jannaschii. Tests for extrachromosomal DNA revealed a plasmid in AG86 and two plasmids in M. jannaschii. Different patterns were obtained from restriction endonuclease digestion of the three plasmids, and no homology was observed with DNA-DNA hybridization.Abbreviations CCC DNA covalently close circular DNA - DM defined marine medium - G+C Guanine plus cytosine - MPN most probable number     

The influence of ultramafic rocks on microbial communities at the Logatchev hydrothermal field, located 15 degrees N on the Mid-Atlantic Ridge

The ultramafic-hosted Logatchev hydrothermal field (LHF) on the Mid-Atlantic Ridge is characterized by high hydrogen and methane contents in the subseafloor, which support a specialized microbial community of phylogenetically diverse, hydrogen-oxidizing chemolithoautotrophs. We compared the prokaryotic communities of three sites located in the LHF and encountered a predominance of archaeal sequences affiliated with methanogenic Methanococcales at all three. However, the bacterial composition varied in accordance with differences in fluid chemistry between the three sites investigated. An increase in hydrogen seemed to coincide with the diversification of hydrogen-oxidizing bacteria. This might indicate that the host rock indirectly selects this specific group of bacteria. However, next to hydrogen availability further factors are evident (e.g. mixing of hot reduced hydrothermal fluids with cold oxygenated seawater), which have a significant impact on the distribution of microorganisms.     

Did shifting seawater sulfate concentrations drive the evolution of deep-sea methane-seep ecosystems?

The origin and evolution of the faunas inhabiting deep-sea hydrothermal vents and methane seeps have been debated for decades. These faunas rely on a local source of sulfide and other reduced chemicals for nutrition, which spawned the hypothesis that their evolutionary history is independent from that of photosynthesis-based food chains and instead driven by extinction events caused by deep-sea anoxia. Here I use the fossil record of seep molluscs to show that trends in body size, relative abundance and epifaunal/infaunal ratios track current estimates of seawater sulfate concentrations through the last 150 Myr. Furthermore, the two main faunal turnovers during this time interval coincide with major changes in seawater sulfate concentrations. Because sulfide at seeps originates mostly from seawater sulfate, variations in sulfate concentrations should directly affect the base of the food chain of this ecosystem and are thus the likely driver of the observed macroecologic and evolutionary patterns. The results imply that the methane-seep fauna evolved largely independently from developments and mass extinctions affecting the photosynthesis-based biosphere and add to the growing body of evidence that the chemical evolution of the oceans had a major impact on the evolution of marine life.     

Evidence for phylogenetic congruence among sulfur-oxidizing chemoautotrophic bacterial endosymbionts and their bivalve hosts

Sulfur-oxidizing chemoautotrophic (thioautotrophic) bacteria are now known to occur as endosymbionts in phylogenetically diverse bivalve hosts found in a wide variety of marine environments. The evolutionary origins of these symbioses, however, have remained obscure. Comparative 16S rRNA sequence analysis was used to investigate whether thioautotrophic endosymbionts are monophyletic or polyphyletic in origin and to assess whether phylogenetic relationships inferred among these symbionts reflect those inferred among their hosts. 16S rRNA gene sequences determined for endosymbionts from nine newly examined bivalve species from three families (Vesicomyidae, Lucinidae, and Solemyidae) were compared with previously published 16S rRNA sequences of thioautotrophic symbionts and free-living bacteria. Distance and parsimony methods were used to infer phylogenetic relationships among these bacteria. All newly examined symbionts fall within the gamma subdivision of the Proteobacteria, in clusters containing previously examined symbiotic thioautotrophs. The closest free-living relatives of these symbionts are bacteria of the genus Thiomicrospira. Symbionts of the bivalve superfamily Lucinacea and the family Vesicomyidae each form distinct monophyletic lineages which are strongly supported by bootstrap analysis, demonstrating that host phylogenies inferred from morphological and fossil evidence are congruent with phylogenies inferred for their respective symbionts by molecular sequence analysis. The observed congruence between host and symbiont phylogenies indicates shared evolutionary history of hosts and symbiont lineages and suggests an ancient origin for these symbioses. Correspondence to: D.L. Distel