基于宏基因组学重建来自深海热液喷口的Epsilonproteobacteria基因组及其代谢分析

【背景】非致病性Epsilonproteobacteria广泛存在于全球各种不同的自然环境中,特别是一些极端生境如深海热液喷口,并且经常在微生物群落中作为优势物种被发现。然而,由于现阶段培养技术的限制,仅有为数不多的深海热液Epsilonproteobacteria被分离培养,极大限制了对其生理特征、代谢方式以及生态功能的深入认识。【目的】研究深海热液未培养Epsilonproteobacteria的进化地位、代谢潜能及其在原位生态系统中可能发挥的作用。【方法】基于宏基因组学Binning的方法,从采集自东太平洋海隆深海热液烟囱体样本中构建4个高质量的Epsilonproteobacteria基因组Bin225、Bin51、Bin54和Bin189,并进行了系统发育和代谢途径的分析。【结果】Bin189在系统发育树上相对独立于其他所有已知的Epsilonproteobacteria类群,而其余3个重构基因组都与Nitratiruptor sp. SB155-2具有较近的亲缘关系。在代谢潜能方面,所有的基因组除了都含有sqr硫氧化和rTCA碳固定途径的基因以外,也同时具有脂多糖输出转运子和多种分泌系统。Bin189显示出与其它基因组显著不同的代谢特征,其中还检测到与有机物和氨基酸转运相关的功能基因。而其他的3个基因组均具有完整的反硝化途径的功能基因,其中2个还具有Sox系统、氢化酶和鞭毛移动系统。【结论】Bin189可能是一种新发现的深海热液兼性化能营养型Epsilonproteobacteria,推测其余的3个类群能够利用硫化物和氢气作为能源进行化能自养生长。考虑到它们多样的代谢潜能,这些Epsilonproteobacteria类群很可能在深海热液微生物群落的形成发展和地球化学元素循环中发挥重要作用。     

The chitin secreting system from deep sea hydrothermal vent worms

Summary— Deep-sea hydrothermal vent worms livé in tubes made of giant β-chitin crystallites (50 nm in diameter, several μm in length) embedded in a protein matrix. These chitin cyrstallites form a liquid-crystal-like structure differing from the wellknown cholesteric arrangement of classical chitin-protein systems. Furthermore, and in contrast with the latter systems, the vestimentiferan chitin-protein systems are produced by goatskin-shaped glands. Rod-shaped elements in the lumen of these glands were identified by DCTEM and Au-WGA labeling and freeze fracture as chitin crystallites. The main characteristics of these “chitin secreting glands” are described.     

Thermosipho japonicus sp. nov., an extremely thermophilic bacterium isolated from a deep-sea hydrothermal vent in Japan

A novel barophilic, extremely thermophilic bacterium was isolated from a deep-sea hydrothermal vent chimney at the Iheya Basin, in the Okinawa area, Japan. The cells were found to be rod shaped and surrounded by a sheath-like outer structure; the organism did not possess flagella and was not motile. Growth was observed between 45° and 80°C (optimum, 72°C, 45 min doubling time), pH 5.3 and 9.3 (optimum, pH 7.2–7.6), 6.6 and 79 g/l sea salts (optimum, 40 g/l), and 0.1 and 60 MPa (optimum, 20 MPa). Strain IHB1 was found to be a strictly anaerobic chemoorganotroph capable of utilizing yeast extract and proteinaceous substrates such as peptone and tryptone. Elemental sulfur or thiosulfate acted as electron acceptors improving growth. The isolate was able to utilize casein as a sole carbon and energy source in the presence of thiosulfate. The G + C content of the genomic DNA was 31.4 mol%. Phylogenetic analysis based on 16S rDNA sequences and DNA–DNA hybridization analysis indicated that the isolate is closely related to Thermosipho africanus; however, it represents a species distinct from the previously described members of the genus Thermosipho. On the basis of the physiological and molecular properties, we propose that the new isolate represents a new species, which we name Thermosipho japonicus sp. nov. (type strain: IHB1; JCM10495). Received: May 26, 1999 / Accepted: August 7, 1999     

Marinitoga lauensis sp. nov., a novel deep-sea hydrothermal vent thermophilic anaerobic heterotroph with a prophage

A novel moderately thermophilic, heterotrophic anaerobe, designated strain LG1^T, was isolated from the Mariner deep-sea hydrothermal vent field along the Eastern Lau Spreading Center and Valu Fa Ridge. Cells of strain LG1^T were motile rods, occurring singly or in pairs, 0.6 μm in width and 1.2 μm in length. The strain LG1^T grew between 40 and 70 °C (optimum 50–55 °C), at a pH between 5 and 8 (optimum pH 6.5) and with 7.5–50 g L⁻¹ NaCl (optimum 30 g L⁻¹). Sulfur, cystine and thiosulfate were reduced to sulfide, and cell yield was improved in the presence of cystine. Strain LG1^T was an organotroph able to use a variety of organic compounds. Phylogenetic analysis based on 16S rRNA gene sequence comparisons indicated that strain LG1^T was affiliated to the genus Marinitoga within the order Petrotogales. It shared 95.34–96.31% 16S rRNA gene sequence similarity with strains of other Marinitoga species, and is most closely related to Marinitoga okinawensis. Genome analysis revealed the presence of a prophage sharing high sequence homology with the viruses MPV1, MCV1 and MCV2 hosted by Marinitoga strains. Based on the data from the phylogenetic analyses and the physiological properties of the novel isolate, we propose that strain LG1^T is a representative of a novel species, for which the name Marinitoga lauensis sp. nov. is proposed; the type strain is LG1^T (=DSM 106824 = JCM 32613).     

一株深海热液口嗜热芽孢杆菌SY27F代谢产物活性的研究

【目的】对一株来源于深海热液口嗜热芽孢杆菌的次生代谢产物进行抑菌活性和抗肿瘤活性的初步研究。【方法】采用纸片法和微量肉汤稀释法检测嗜热芽孢杆菌SY27F次生代谢产物的抑菌活性,采用CCK-8法测定其次生代谢产物的抗肿瘤活性。【结果】抑菌实验表明,嗜热芽孢杆菌代谢产物对大肠杆菌、金黄色葡萄球菌均有抑菌作用,其最低抑菌浓度分别为1.56 mg/mL和3.13 mg/mL;细胞实验表明,其代谢产物对肿瘤细胞A549、HepG2、HeLa、MCF-7均有一定的抑制作用,其半致死浓度分别为0.390、0.451、0.704、1.105 mg/mL;与人肝肿瘤细胞(HepG2)相比,其对人正常肝细胞(L02)表现出良好的生物相容性。【结论】嗜热芽孢杆菌SY27F次生代谢产物具有一定的抑菌和抗肿瘤活性,可为寻找新型抑菌抗肿瘤活性物质提供优质资源。     

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。     

Complete genome sequence of Thermovibrio ammonificans HB-1T,a thermophilic,chemolithoautotrophic bacterium isolated from a deep-sea hydrothermal vent

Thermovibrio ammonificans type strain HB-1^T is a thermophilic (T_opt: 75°C), strictly anaerobic, chemolithoautotrophic bacterium that was isolated from an active, high temperature deep-sea hydrothermal vent on the East Pacific Rise. This organism grows on mineral salts medium in the presence of CO₂/H₂, using NO₃^- or S⁰ as electron acceptors, which are reduced to ammonium or hydrogen sulfide, respectively. T. ammonificans is one of only three species within the genus Thermovibrio, a member of the family Desulfurobacteriaceae, and it forms a deep branch within the phylum Aquificae. Here we report the main features of the genome of T. ammonificans strain HB-1^T (DSM 15698^T).     

Genetic diversity and connectivity of deep‐sea hydrothermal vent metapopulations

Deep‐sea hydrothermal vents provide ephemeral habitats for animal communities that depend on chemosynthetic primary production. Sporadic volcanic and tectonic events destroy local vent fields and create new ones. Ongoing dispersal and cycles of extirpation and colonization affect the levels and distribution of genetic diversity in vent metapopulations. Several species exhibit evidence for stepping‐stone dispersal along relatively linear, oceanic, ridge axes. Other species exhibit very high rates of gene flow, although natural barriers associated with variation in depth, deep‐ocean currents, and lateral offsets of ridge axes often subdivide populations. Various degrees of impedance to dispersal across such boundaries are products of species‐specific life histories and behaviours. Though unrelated to the size of a species range, levels of genetic diversity appear to correspond with the number of active vent localities that a species occupies within its range. Pioneer species that rapidly colonize nascent vents tend to be less subdivided and more diverse genetically than species that are slow to establish colonies at vents. Understanding the diversity and connectivity of vent metapopulations provides essential information for designing deep‐sea preserves in regions that are under consideration for submarine mining of precious metals.     

Description of a new family,new genus,and two new species of deep‐sea Forcipulatacea (Asteroidea), including the first known sea star from hydrothermal vent habitats

Based on a phylogenetic analysis of undescribed taxa within the Forcipulatacea, a new family of deep‐sea forcipulatacean starfishes, Paulasteriidae fam. nov., is described from deep‐sea settings. Paulasterias tyleri gen. et sp. nov. was observed at recently documented hydrothermal vents on the East Scotia Ridge, Southern Ocean. A second species, Paulasterias mcclaini gen. et sp. nov. was observed in deep‐sea settings in the North Pacific, more distant from hydrothermal vents. Both species are multi‐armed (with between six and eight arms), with a fleshy body wall, and a poorly developed or absent adoral carina. Here, we include discussions of pedicellariae morphology, feeding biology, and classification. © 2015 The Linnean Society of London     

Comparison of thermophilic methanogens from submarine hydrothermal vents

An extremely thermophilic methanogen was isolated from hydrothermal vent sediment (80°–120° C) collected from the Guaymas Basin, Gulf of California, at a depth of approximately 2000 m. The isolate was a characteristic member of the genus Methanococcus based on its coccoid morphology, ability to produce methane from CO₂ and H₂, and DNA base composition (31.4 mol% G+C); it is distinguished from previously described extremely thermophilic vent methanogens by its ability to grow and produce methane from formate and in the composition of membrane lipids. The temperature range for growth was 48°–94° C (optimum near 85° C); the pH optimum was 6.0. The isolate grew autotrophically but was stimulated by selenium and growth nutrients supplied by yeast extract and trypticase. Extracted polar lipids consisted primarily of diphytanyl glycerol diether (62%), macrocyclic glycerol diether (15.3%), and dibiphytanyl glycerol tetraether (11.8%). Neutral lipids were dominated by a series of C₃₀ isoprenoids; in addition, a novel series of C₃₅ isoprenoids were detected. The isolate appears to be a close relative of the previously described Methanococcus jannaschii, isolated from the East Pacific Rise hydrothermal vent system. From the frequency of isolation, it appears that extremely thermophilic methanococci are the predominant representatives of the methanogenic archaebacteria occurring at deep sea hydrothermal vents.     

Lebetimonas natsushimae sp. nov., a novel strictly anaerobic,moderately thermophilic chemoautotroph isolated from a deep-sea hydrothermal vent polychaete nest in the Mid-Okinawa Trough

A moderately thermophilic, strictly anaerobic, chemoautotrophic bacterium, designated strain HS1857^T, was isolated from a deep-sea hydrothermal vent at the Noho site in the Mid-Okinawa Trough. Strain HS1857^T grew between 35 and 63 °C (optimum 55 °C), in the presence of 10–55 g l^?1 NaCl (optimum 25 g l^?1), and pH 5.5–7.1 (optimum 6.4). Growth occurred with molecular hydrogen as the electron donor and elemental sulfur, nitrate, or selenate as the electron acceptors. Formate could serve as an alternative electron donor with nitrate as an electron acceptor. During growth with nitrate as the electron acceptor, strain HS1857^T produced ammonium and formed a biofilm. CO₂ was utilized as the sole carbon source. The G + C content of the genomic DNA was 33.2 mol%. Phylogenetic analysis of the 16S rRNA gene sequence indicated that strain HS1857^T is a member of the order Nautiliales, showing a sequence similarity of 95.0% with Lebetimonas acidiphila Pd55^T. The fatty acid composition was similar to that of L. acidiphila, which was dominated by C_18:0 (47.0%) and C_18:1 (23.7%). Based on the genomic, chemotaxonomic, phenotypic characteristics, the name Lebetimonas natsushimae sp. nov., is proposed. The type strain is HS1857^T (= NBRC 112478^T = DSM 104102^T).     

Halomonas profundus sp. nov., a new PHA-producing bacterium isolated from a deep-sea hydrothermal vent shrimp

Aims:  The objective of the present work was to describe a new deep-sea, aerobic, mesophilic and heterotrophic bacterium, referenced as strain AT1214, able to produce polyhydroxyalkanoates (PHAs) under laboratory conditions. This bacterium was isolated from a shrimp collected nearby a hydrothermal vent located on the Mid-Atlantic Ridge. Methods and Results:  This micro-organism, on the basis of the phenotypical features and genotypic investigations, can be clearly assigned to the Halomonas genus and the name of Halomonas profundus is proposed. Optimal growth occurred between 32 and 37°C at a pH between 8 and 9 and at ionic strength between 20 and 30 g l⁻¹ of sea salts. The G + C content of DNA was 58·6%. This bacterium produced PHAs of poly(3-hydroxybutyrate) and poly(3-hydroxybutyrate-co-3-hydroxyvalerate) from different carbon sources. Conclusions:  The bacterium H. profundus produces PHA of 3HB and 3HV monomers from different carbon sources. Significance and Impact of the Study:  PHAs share physical and material properties that suggest them for application in various areas, and are considered as an alternative to nonbiodegradable plastics produced from fossil oils. In this study, we describe a new bacteria isolated from a deep-sea hydrothermal vent with the capability to produce polyesters of biotechnological interest.     

Development and characterization of 12 microsatellite markers from the deep-sea hydrothermal vent siboglinid Riftia pachyptila

Ecological processes at deep‐sea hydrothermal vents on fast‐spreading mid‐ocean ridges are punctuated by frequent physical disturbance, often accompanied by a high occurrence of population turnover. To persist through local extinction events, sessile invertebrate species living in these geologically and chemically dynamic habitats depend on larval dispersal. We characterized 12 polymorphic microsatellite loci from one such species, the siboglinid tubeworm Riftia pachyptila. All loci conformed to Hardy–Weinberg expectations without linkage (mean H_E = 0.9405, mean N_A = 20.25). These microsatellites are being employed in the investigation of spatial and temporal population genetic structure in the eastern Pacific Ocean.     

Draft genome sequence of Caminibacter mediatlanticus strain TB-2, an epsilonproteobacterium isolated from a deep-sea hydrothermal vent

Caminibacter mediatlanticus strain TB-2(T) [1], is a thermophilic, anaerobic, chemolithoautotrophic bacterium, isolated from the walls of an active deep-sea hydrothermal vent chimney on the Mid-Atlantic Ridge and the type strain of the species. C. mediatlanticus is a Gram-negative member of the Epsilonproteobacteria (order Nautiliales) that grows chemolithoautotrophically with H(2) as the energy source and CO(2) as the carbon source. Nitrate or sulfur is used as the terminal electron acceptor, with resulting production of ammonium and hydrogen sulfide, respectively. In view of the widespread distribution, importance and physiological characteristics of thermophilic Epsilonproteobacteria in deep-sea geothermal environments, it is likely that these organisms provide a relevant contribution to both primary productivity and the biogeochemical cycling of carbon, nitrogen and sulfur at hydrothermal vents. Here we report the main features of the genome of C. mediatlanticus strain TB-2(T).     

Molecular characteristics of the tubeworm, Ridgeia piscesae, from the deep-sea hydrothermal vent

Ridgeia piscesae, living around the extremely harsh hydrothermal vent in deep sea, is an ideal model for studying the adaptative mechanism to extreme environment. For insights of its molecular characteristics, a cDNA library of R. piscesae was constructed. A total of 879 expressed sequence tags (ESTs) were sequenced and 199 genes were identified for the first time. They were found to be involved in basal metabolism, adaptation and defense, or signal transduction. Among them, we found 23 various chitin-binding proteins, which are the major component of the chitinous tube that prevents the tubeworms from predators and surrounding extreme environment. Additionally, high polymorphism also exists in other genes, such as myohemerythrin, lysozyme. The gene-expression profile might help to further understand the molecular basis of tubeworm physiology. It will also lay a good foundation for functional studies on the adaptation to extreme environments.     

Chitinase gene diversity at a deep sea station of the east Pacific nodule province

The Pacific nodule province covered about 4.5 million km² in the east tropical Pacific with an abundance of polymetallic nodules at the seafloor. In view of the environmental protection and resource preservation, the survey of biodiversity was important during the reconnaissance and exploitation in this area. As one of the important component of the deep sea ecosystem, the microbial community in the Pacific nodule province was still largely unknown. The chitinolytic bacteria diversity in deep-sea sediment of a station within the Pacific nodule province was examined by molecular technology. A total of 18 chitinase genes were detected by a set of degenerate PCR primer specific for chiA gene fragment of family 18 chitinase. Most of them belonged to the Serratia-like chitinase. Eight genes had different amino acid sequences in the conserved motif, encompassing the catalytic site among the ChiA protein of family 18 glycosyl hydrolases, and clustered in an independent clade on the phylygenetic tree.