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1.
WEI Manman ZHANG Rubing WANG Yuguang JI Houguo ZHENG Ji CHEN Xinhu ZHOU Hongbo 《海洋学报(英文版)》2013,32(2):42-51
The aim of this study is to investigate microbial structures and diversities in five active hydrothermal fields’ sediments along the Eastern Lau Spreading Centre (ELSC) in the Lau Basin (southwest Pacific). Microbial communities were surveyed by denatured gradient gel electrophoresis (DGGE) and clone library analysis of 16S rRNA genes. The differences in microbial community structures among sediment samples from the five deep-sea hydrothermal sites were revealed by DGGE profiles. Cluster analysis of DGGE profiles separated the five hydrothermal samples into two groups. Four different 16S rRNA gene clone libraries, representing two selected hydrothermal samples (19-4TVG8 and 19-4TVG11), were constructed. Twenty-three and 32 phylotypes were identified from 166 and 160 bacterial clones respectively, including Proteobacteria, Bacteroidetes, Firmicutes, Nitrospirae and Planctomycetes. The phylum Proteobacteria is dominant in both bacterial libraries with a predominance of Gamma-Proteobacteria. A total of 31 and 25 phylotypes were obtained from 160 and 130 archaeal clones respectively, including Miscellaneous Crenarchaeotic Group, Marine Group Ⅰ and Ⅲ, Marine Benthic Group E, Terrestrial Hot Spring Crenarchaeota and Deep-sea Hydrothermal Vent Euryarchaeota. These results show a variety of clones related to those involved in sulfur cycling, suggesting that the cycling and utilization of sulfur compounds may extensively occur in the Lau Basin deep-sea hydrothermal ecosystem. 相似文献
2.
TAO Chunhui WU Guanghai DENG Xianming QIU Zhongyan HAN Chenhu LONG Yanmei 《海洋学报(英文版)》2013,32(8):85-88
The 26th Chinese COMRA (China Ocean Mineral Resources Research & Development Association) cruise was an important cruise. The Carlsberg Ridge (CR) of the Northwest Indian Ocean and the North Atlantic Ridge (NAR), in which less investigation has been carried out for hydrothermal activities, were investigated and studied during the first two legs of the 26th COMRA cruise. During the first leg, we found one hydrothermal activity field located in the CR at 3.5 -3.8 N on the Northwest Indian Ocean Ridge (NWIR), and sampled seafloor polymetallic sulfide deposits where only abnormalities were found before. During the second leg, we found a new hydrothermal anomaly field located in the NAR at 4 -7 N. The discovery of two hydrothermal and anomaly fields filled in the gap of hydrothermal investigation and study in the corresponding regions for China. 相似文献
3.
CO2 fixation pathway of Caminibacter profundus, a chemolithoautotrophic -Proteobacteria from deep-sea hydrothermal vent, was determined and characterized by genetic and enzymatic analyses. Gene expression of key enzymes for CO2 fixation in response to salinity, pH and O2 in Medium 829 were also investigated. The results demonstrate that C. profundus contained aclB, porA and oorA, the genes encoding key enzymes of reductive tricarboxylic acid (rTCA) cycle. However, genes fragments of cbbL and cbbM encoding key enzyme of Calvin cycle were not recovered. Key enzymatic activities of ATP citrate lyase (ACL), pyruvate: ferredoxin oxidoreductase (POR) and 2-oxoglutarate: ferredoxin oxidoreductase (OOR) were also present in C. profundus. The combination of genetic and enzymatic analyses confirm that C. profundus adopted rTCA cycle for carbon assimilation. The results of aclB and oorA relative expressions of C. profundus demonstrate that the ranges of environmental factors for high genes expression were sea salt 3.0%-5.0% (optimum 3.0%), pH 5.0-6.5(optimum pH 6.5), anaerobic to microaerobic conditions (optimum 1.0% O2 ). Gene expression patterns under different conditions show similar patterns with bacterial growth, revealing that key rTCA cycle genes provided molecular basis for bacterial growth and propagation. Our results suggest that C. profundus could regulate key genes of rTCA cycle for carbon assimilation and energy metabolism in response to environmental fluctuations in hydrothermal vent. 相似文献
4.
MU Chunhu BAO Zhenmin CHEN Gang HU Jingjie HAO Lujiang QI Zizhong LI Guangxue 《海洋学报(英文版)》2005,24(3):114-121
Diversity of bacteria was studied in deep-sea sediments from the Shikoku Basin in the Northwest Pacific Ocean by PCR, RFLP and sequence analysis of 16S rDNA and comparing with Genbank database. Based on the RFLP profile generated, 77 clones from the 16S rDNA library were divided into 27 types. Phylogenetic analysis showed that the 27 independent clones fell into four groups: Proteobacteria (62.96%), Chloroflexi (14.81%), Planctomycetes (14.81%) and Acidobacteria (7.41%). Among all sequenced clones, 6 were related to the sulfur or sulfate metabolism bacteria and the results also demonstrated that some bacteria in deep-sea sediments had relation to matter-energy circulation. 相似文献
5.
The ultraslow-spreading Southwest Indian Ridge(SWIR) to the east of the Melville fracture zone is characterized by very low melt supply and intensive tectonic activity. Due to its weak thermal budget and extremely slow spreading rate, the easternmost SWIR was considered to be devoid of hydrothermal activity until the discovery of the inactive Mt. Jourdanne hydrothermal field(27°51′S, 63°56′E) in 1998. During the COMRA DY115-20 cruise in2009, two additional hydrothermal fields(i.e., the Tiancheng(27°51′S, 63°55′E) and Tianzuo(27°57′S, 63°32′E)fields) were discovered. Further detailed investigations of these two hydrothermal sites were conducted by Chinese manned submersible Jiaolong in 2014–2015. The Tiancheng filed can be characterized as a lowtemperature(up to 13.2°C) diffuse flow hydrothermal field, and is hosted by fractured basalts with hydrothermal fauna widespread on the seafloor. The Tianzuo hydrothermal field is an inactive sulfide field, which is hosted by ultramafic rocks and controlled by detachment fault. The discovery of the three hydrothermal fields around Segment #11 which receives more melt than the regional average, provided evidence for local enhanced magmatism providing heat source to drive hydrothermal circulation. We further imply that hydrothermal activity and sulfide deposits may be rather promising along the easternmost SWIR. 相似文献
6.
The diversity of modular polyketide synthase (PKS) genes in sediments of Ardley Island in Antarctica, was studied by restriction fragment length polymorphism (RFLP) analysis. Phylogenetic analysis of 14 amino acid (AA) sequences indicates that the identified ketosynthase (KS) domains were clustered with those from diverse bacterial groups, including Cyanobacteria, γ-Proteobacteria, Actinobacteria, Firmicutes, and some unidentified microorganisms from marine sponge, bryozoan and other environmental samples. ... 相似文献
7.
Shengyi Mao Hongxiang Guan Lihua Liu Xiqiu Han Xueping Chen Juan Yu Yongge Sun Yejian Wang 《海洋学报(英文版)》2021,40(8):53-64
Hydrothermal venting has a profound effect on the chemical and biological properties of local and distal seawater and sediments. In this study, lipid biomarkers were analyzed to examine the potential influence of hydrothermal activity on the fate of organic matter(OM) in surface sediments around Tianxiu Hydrothermal Field in the Carlsberg Ridge(CR), Northwest Indian Ocean. By comparing the biomarker distributions of the samples with that of other typical hydrothermal sediments in the mid ocean ridge, it is shown that the location of the samples is not affected by the hydrothermal activity. The relatively low abundances of terrestrial n-alkyl lipids and riverine1,15-C32 diol suggested a minor contribution of terrigenous OM to the study area. The bacteria contributed predominantly to sedimentary marine OM; however, other marine source organisms, e.g., eukaryotes(i.e.,phytoplankton and fungi) could not be completely neglected. The marine-originated biomarkers showed significantly variable distributions between the two sediments, suggesting different dynamic physical and biogeochemical processes controlling the fate of marine OM. This study identified various diagnostic biomarkers(5,5-diethyl alkanes, diols and β-OH FAs), which may have significant environmental implications for future works in this region. 相似文献
8.
A sediment core MD05-2902 was collected from the deep-sea basin of the Xisha Trough. The vertical distribution and diversity of bacteria in the core was investigated through ten sub-sampling with an interval of 1 m using bacterial 16 S rRNA gene as a phylogenetic bio-marker. Eighteen phylogenetic groups were identified from 16 S rRNA gene clone libraries. The dominant bacterial groups were JS1, Planctomycetes and Chloroflexi, which accounted for 30.6%, 16.6%, and 15.6% of bacterial clones in the libraries, respectively. In order to reveal the relationship between biotic and abiotic data, a nonmetric multidimensional scaling analysis was performed. The result revealed that the δ15N, δ13C, total organic carbon and total organic nitrogen possibly influenced the bacterial community structure. This study expanded our knowledge of the biogeochemical cycling in the Xisha Trough sediment. 相似文献
9.
To understand the source and nature of the ore-forming fluids of the Edmond hydrothermal field on the Central Indian Ridge, we studied the He-Ar isotope composition and fluid inclusions of the hydrothermal precipitates.Our results show that the sulfide samples contain noble gases He, Ne, Kr, and Xe with their abundances in between those of air-saturated water(ASW) and mid-ocean ridge basalt(MORB). The ~3He/~4He ratio varies from1.3 to 8.7 R_a(n=10, average: 5.1 R_a), whereas the ~(40)Ar/~(36) Ar ratio is from 285.3 to 314.7(n=10, average: 294.8). These results suggest that the He was derived from a mixture of MORB with variable amounts of seawater, but the Ar in the ore-forming fluids trapped in the sulfides is predominantly derived from seawater. The fluid inclusions of barite have a wide range of homogenization temperatures and salinities varying from 163°C to 260°C and 2.6 wt%to 8.5 wt% Na Cl equiv., respectively. It is suggested that the ore-forming fluids were produced by phase separation, which agreed with the present-day vent fluid study. 相似文献
10.
Massive sulfide precipitates found in the Southwest Indian Ridge(SWIR) 49.6°E hydrothermal field are enriched in gold.Here,the mineralogy and mineral chemistry of these massive sulfides to constrain the process of gold precipitation were studied.Sulfide samples in this field include lowertemperature Zn-rich sulfides and relative higher-temperature Fe-rich sulfides.Zn-rich sulfides are dominated by sphalerite-pyrite-chalcopyrite assemblages,with concentrations of gold ranging from 9.08 to 17.0 μg/g.Fe-rich sulfides consist mainly of pyrite-marcasite-isocubanite assemblages,with gold concentrations from 2.17 to 3.79 μg/g.The significant enrichment in gold within the lowertemperature Zn-rich sulfides and the effective separation of Zn and Fe in hydrothermal precipitates at the surface of this field are here interpreted to reflect the strong temperature dependence of gold transportation and deposition within the sulfides.In Zn-rich samples,large amounts of isolated native gold grains were identified.They were found mainly as inclusions up to 8 μm in diameter,occupying porous cavities in sphalerite or in the elevated iron content rim of sphalerite.The fineness of the gold ranged from 810 to 830.Unlike previously published results on other hydrothermal fields,these data show a low gold fineness values in SWIR 49.6°E.The FeS content of sphalerite associated with gold grains ranged from 3.2 mole % to 18.9 mole %.This was higher than in other fields,indicating that the sulfur activity is relatively low during the gold precipitation process and that sulfur activity may be one of the main factors affecting gold fineness in the SWIR 49.6°E hydrothermal field.Evidence regarding gold fineness and sulfur activity suggests that gold was quite likely transported as AuHS0 rather than as a Au(HS)-2 complex. 相似文献
11.
近来的研究表明，一些所谓的环球或环极地分布的广布种实际上包含着一些局限性分布的隐存种，物种多样性可能被低估。本文采用形态学和DNA条形码技术相结合的方式，对印度洋和西北太平洋海域的龟螺属(Cavolinia)和小龟螺属(Diacavolinia)的种类进行了分类学研究和物种鉴定。结果表明，线粒体16S rRNA基因数据不支持小龟螺属形态种的划分，分布于西北太平洋的D. grayi、D. vanutrechti、D. pacifica、D. elegans、D. angulosa等多个形态种可能属同一个种，即长吻小龟螺(D. longirostris)。COI基因数据也不支持钩龟螺(C. uncinata)亚种和变形的划分。许多形态特征不能作为种或种下分类单元的区分依据。钩龟螺、球龟螺(C. globulosa)和长吻小龟螺在COI系统树中均形成2个地理支系，其内部可能存在隐存种。西北太平洋海域长吻小龟螺的核基因组中存在线粒体假基因，对DNA条形码分析产生严重干扰。 相似文献
12.
自20世纪70年代以来,现代海底热液活动调查研究一直是地球科学领域研究的热点和焦点.中国大洋19航次第Ⅰ、Ⅱ航段于2007年3月在西南印度洋脊首次发现的海底热液活动区,为IODP在超慢速扩张洋脊热液活动区进一步的调查和研究创造了条件.为了能够更深入地开展该热液区的地质地球物理、矿产资源和生物多样性调查研究,笔者建议应在该区域开展IODP钻探研究,以便对热液活动区硫化物矿体、基岩及深部物质的三维分布和结构物质组成,热液流体与岩石、沉积物相互作用关系,以及热液循环、热及物质通量和成矿机制、成矿物质来源演化关系等方面得到更深入的认识,进而探索地球深部极端环境下的微生物生命现象. 相似文献
13.
Shingo Kato Kurt Hara Hiroko Kasai Takashi Teramura Michinari Sunamura Jun-ichiro Ishibashi Takeshi Kakegawa Toshiro Yamanaka Hiroyuki Kimura Katsumi Marumo Tetsuro Urabe Akihiko Yamagishi 《Deep Sea Research Part I: Oceanographic Research Papers》2009,56(10):1844-1855
Spatial distribution, diversity, and composition of bacterial communities within the shallow sub-seafloor at the deep-sea hydrothermal field of the Suiyo Seamount, Izu-Bonin Arc, Western Pacific Ocean, were investigated. Fluids were sampled from four boreholes in this area. Each borehole was located near or away from active vents, the distance ranging 2–40 m from active vents. In addition, fluids discharging from a natural vent and ambient seawater were sampled in this area. We extracted DNA from each sample, amplified bacterial 16S rRNA genes by PCR, cloned the PCR products and sequenced. The total number of clones analyzed was 348. Most of the detected phylotypes were affiliated with the phylum Proteobacteria, of which the detection frequency in each clone library ranged from 84.6% to 100%. The bacterial community diversity and composition were different between hydrothermal fluids and seawater, between fluids from the boreholes and the vent, and even among fluids from each borehole. The relative abundances of the phylotypes related to Thiomicrospira, Methylobacterium and Sphingomonas were significantly different among fluids from each borehole. The phylotypes related to Thiomicrospira and Alcanivorax were detected in all of the boreholes and vent samples. Our findings provide insights into bacterial communities in the shallow sub-seafloor environments at active deep-sea hydrothermal vent fields. 相似文献
14.
热液喷口附近的羽状流中存在明显的化学及浊度异常，通过探测这些异常可判断是否存在热液喷口及确定喷口的具体位置。本文研制了一款可用于探测热液喷口的多通道化学传感器，该传感器具有体积小、精度高的特点，且可在4000米深海中进行工作。该化学传感器共配备五个全固态电极，一个为参比电极，其余四个为离子选择性电极，并且可根据所测量的化学离子进行更换。本文基于该化学传感器共进行了两组实验。在第一组浅海试验中，化学传感器集成了pH，Eh，CO32-和SO42-电极，在浅海海域中测量对应化学量，结果表明该化学传感器可在实际应用中获得高精度、稳定的测量数据。第二组实验为深海热液探测，装配了pH，Eh，CO32-和H2S电极的化学传感器在西南印度洋中脊区域的29次测线中投入使用，共获得有效数据27组。通过对测量所得到的化学量进行分析，本文提出了一种确定热液喷口的化学异常探测方法，若某时间段内Eh和H2S的电势降低，而pH和CO32-的电势上升则可判定存在化学异常。利用该方法对27组有效数据进行分析，共发现5个潜在的热液喷口。实验结果表明，该化学传感器可有效地探测由热液引起的化学异常，适用于实际热液探测中。 相似文献
15.
海底热液活动调查研究是深海进入、深海探测和深海开发的切入点之一。近十年来，中国在西太平洋弧后盆地、东太平洋海隆、大西洋洋中脊和印度洋脊，发现了一批新的海底热液活动区，围绕着热液活动区的硫化物、流体、热液柱、生物等热液产物开展了调查研究，构建了海底热液地质学，提出了热液活动、冷泉及天然气水合物的同源异汇假说，出版了《海底热液地质学》、《现代海底热液硫化物成矿地质学》、《现代海底热液活动》、《东太平洋海隆热液地质》专著，获得了一批调查研究成果。未来，聚焦海底热液活动的深部过程及其资源环境效应关键问题，发展海底热液活动探测技术，拓展极地海底热液活动调查研究新领域，围绕烟囱体、热液柱、含金属沉积物、流体以及热液区生物等热液产物，开展深入、系统的调查研究工作，无疑将推动海底热液地质学取得新的进展。 相似文献
16.
好氧不产氧光合(AAP)细菌因其具有利用溶解性有机物及光能的能力,在海洋碳循环及能量流动中发挥着重要的作用。该类细菌广泛分布在海洋环境中,其在不同生境中的多样性已被调查。但到目前为止,人们对于高纬度地区好氧不产氧光合细菌的认识还较为缺乏。有鉴于此,本研究基于编码光反应复合物上一个色素结合蛋白亚基的pufM基因,对北极王湾及南极乔治王岛近岸水体中夏季好氧不产氧光合细菌的多样性进行了检测。针对2个王湾站位和2个南极麦克斯维尔湾站位构建了4个pufM基因克隆文库,获得674个阳性克隆子。北极克隆子全部由α-变形细菌组成,而南极克隆子则包括α-变形细菌及β-变形细菌。来源于类似红细菌科的pufM基因在所有样品中皆占据优势。此外,与一株滴状亚硫酸盐杆菌中质粒编码的pufM基因存在亲缘关系的序列,在南、北极样品中均占优势。结果表明海洋环境中的pufM基因存在跨极甚至是环球分布。与此同时,南、北极序列之间的差异,也表明了极地地方种的存在。这些结果显示,作为好氧不产氧光合细菌的红细菌科在两极的近岸水体中具有重要的地位。 相似文献
17.
During the Dives Nos. 409, 410, 480 and 481 of the Japanese submersible Shinkai 2000, conducted on June 10 and 11, 1989 and on May 16 and 17, 1990, several hydrothermal vents and prosperous vent associated
biological communities were found on the northern slope of the Iheya Ridge in the Mid-Okinawa Trough (27°32.5′ N, 126°58.5′
E: depth 1,400 m). The first site we found, the “Calyptogena Site”, was characterized by a relatively thick blanket of sediments, pleated and/or laminated lava flows, with occasional
lobate pillows and white and yellow stains. Although no remarkable shimmering water and thermal anomalies were detected during
the observations, the extraordinarily dense community must be related to hydrothermal activities. The community was dominated
by the giant white clam, Calyptogena okutanii, in biomass, and by Neolepas-type primitive scalpellids and slender vestimentiferan tube-worms in number. The second site, the “Pyramid Site”, situated
only 200 m northward from the Calyptogena Site has typical clear smokers emitting hot water over 200°C, and is characterized by a hard substratum of volcanic rocks
and hydrothermal slabs. No noteworthy succession was perceived at the Calyptogena Site over a year. Many of the vent members occurred at both sites. However, Calyptogena okutanii, which were confined to the sediment bottom, Neolepas spp. and larger vestimentiferan tube-worms were found to thrive only at the Calyptogena Site, being only minor elements in the Pyramid Site. The global distribution of several groups of organisms is discussed
preliminarily in zoogeographical terms based on comparison with other submersible missions and surveys done by surface vessels.
This revised version was published online in August 2006 with corrections to the Cover Date. 相似文献
18.
One strain of unicellular greenish algae embedded by mucilage was successfully isolated from equatorial area in the Indian Ocean. Microscopic observation, ultrastructure features and genetic identification confirmed that the strain was closely related to Cyanothece sp., which was a cyanobacteria species with great ecological significance.Cells were solitary with oval or bacilliform shapes. Diameters of this strain were relatively small, ranging from 2.5 to 6.5 μm on average. Ultrastructure of cells was simple. Thylakoids were arranged parietal and keritomized content were observed in the thylakoid region. Various electron-transparent granules with low electron-dense region as well as cyanophycin or glycogen granules-like organelle and carbonxysomes were also observed. For pigment composition, the dominant pigments were chlorophyll a, β-Carotene, Zeaxanthin and an unknown pigment, contributing 23.8%, 26.1%, 14.7% and 15.7% to total pigments respectively. The phylogenetic analysis of16 S rRNA gene and nif H gene confirmed that Strain EIO409 was closely related with Cyanothece sp.. 相似文献
19.
曾胤新 《海洋学报(英文版)》2019,38(8):64-71
Dimethylsulfoniopropionate(DMSP) is mainly produced by marine phytoplankton as an osmolyte, antioxidant,predator deterrent, or cryoprotectant. DMSP is also an important carbon and sulfur source for marine bacteria.Bacteria may metabolize DMSP via the demethylation pathway involving the DMSP demethylase gene(dmdA) or the cleavage pathway involving several different DMSP lyase genes. Most DMSP released into seawater is degraded by bacteria via demethylation. To test a hypothesis that the high gene frequency of dmdA among major marine taxa results in part from horizontal gene transfer(HGT) events, a total of thirty-one bacterial strains were isolated from Arctic Kongsfjorden seawater in this study. Analysis of 16S rRNA gene sequences showed that,except for strains BSw22118, BSw22131 and BSw22132 belonging to the genera Colwellia, Pseudomonas and Glaciecola, respectively, all bacteria fell into the genus Pseudoalteromonas. DmdA genes were detected in five distantly related bacterial strains, including four Arctic strains(Pseudoalteromonas sp. BSw22112, Colwellia sp.BSw22118, Pseudomonas sp. BSw22131 and Glaciecola sp. BSw22132) and one Antarctic strain(Roseicitreum antarcticum ZS2–28). Their dmdA genes showed significant similarities(97.7%–98.3%) to that of Ruegeria pomeroyi DSS–3, which was originally isolated from temperate coastal seawater. In addition, the sequence of the gene transfer agent(GTA) capsid protein gene(g5) detected in Antarctic strain ZS2–28 exhibited a genetically closely related to that of Ruegeria pomeroyi DSS–3. Among the five tested strains, only Pseudomonas sp. BSw22131 could grow using DMSP as the sole carbon source. The results of this study support the hypothesis of HGT for dmdA among taxonomically heterogeneous bacterioplankton, and suggest a wide distribution of functional gene(i.e., dmdA) in global marine environments. 相似文献
20.
cGAS(cyclic GMP-AMP synthase)基因是近几年来新发现的先天免疫中一个新型的信号分子。作者基于大黄鱼(Larimichthys crocea)基因组信息,用cDNA末端快速扩增(RACE)技术在鳃组织中克隆鉴定了cGAS基因cDNA全长序列:包含1个231 bp的5′端-非翻译区(5′-UTR)、207 bp的3′-UTR和1 488 bp的开放阅读框(ORF),命名为Lc-cGAS-like X1。该基因编码1个由495个氨基酸残基组成的多肽,预测的分子量(Mw)大小为56.57kDa,理论等电点(pI)为9.45;序列分析表明其预测的蛋白无信号肽,第115～431位氨基酸序列为Mab-21功能域,第470～492位氨基酸序列为跨膜结构域。基因组全长3 153 bp,包含8个外显子和7个内含子,所有内含子的剪切特点都符合GT-AG规则。同源比对结果显示:Lc-cGAS-likeX1与鱼类cGAS的相似性大于66%,与高等脊椎动物的相似性较低。系统进化分析表明Lc-cGAS-like X1与鱼类cGAS聚成一支。荧光定量PCR(qPCR)检测显示Lc-cGAS基因(X1/X2两种剪切体)在大黄鱼9种组织中均有表达,其中在鳃中的表达量最高;刺激隐核虫感染后,大黄鱼免疫器官头肾中Lc-cGASmRNA分别在刺激隐核虫幼虫感染阶段和滋养体脱落阶段出现了极显著上调(P0.01);解毒器官肝脏中分别在滋养体脱落阶段和细菌感染阶段出现极显著上调变化(P0.01)。本研究结果暗示大黄鱼cGAS基因参与了大黄鱼感染刺激隐核虫的免疫防御过程,为进一步了解鱼类cGAS基因的多样化功能提供参考。 相似文献