Incidence and Diversity of Microorganisms within the Walls of an Active Deep-Sea Sulfide Chimney

A large, intact sulfide chimney, designated Finn, was recovered from the Mothra Vent Field on the Juan de Fuca Ridge in 1998. Finn was venting 302°C fluids on the seafloor and contained complex mineralogical zones surrounding a large open central conduit. Examination of microorganisms within these zones, followed by community analysis with oligonucleotide probes, showed that there were variations in the abundance and diversity of eubacteria and archaea from the exterior to the interior of the chimney. The microbial abundance based upon epifluorescence microscopy and quantitative fatty acid analyses varied from >10⁸ cells/g of sulfide 2 to 10 cm within the chimney wall to <10⁵ cells/g in interior zones. Direct microscopic observation indicated that microorganisms were attached to mineral surfaces throughout the structure. Whole-cell hybridization results revealed that there was a transition from a mixed community of eubacteria and archaea near the cool exterior of the chimney to primarily archaea near the warm interior. Archaeal diversity was examined in three zones of Finn by cloning and sequencing of the 16S rRNA gene. The majority of sequences from the exterior of the chimney were related to marine group I of the Crenarchaeota and uncultured Euryarchaeota from benthic marine environments. In contrast, clone libraries from interior regions of the chimney contained sequences closely related to methanogens, Thermococcales, and Archaeoglobales, in addition to uncultured crenarchaeal phylotypes obtained from deep subsurface sites. These observations of microbial communities within an active hydrothermal chimney provide insight into the microbial ecology within such structures and may facilitate follow-up exploration into expanding the known upper temperature limits of life.     

Biosignatures in chimney structures and sediment from the Loki’s Castle low-temperature hydrothermal vent field at the Arctic Mid-Ocean Ridge

We investigated microbial life preserved in a hydrothermally inactive silica–barite chimney in comparison with an active barite chimney and sediment from the Loki’s Castle low-temperature venting area at the Arctic Mid-Ocean Ridge (AMOR) using lipid biomarkers. Carbon and sulfur isotopes were used to constrain possible metabolic pathways. Multiple sulfur (δ³⁴S, ?³³S) isotopes on barite over a cross section of the extinct chimney range between 21.1 and 22.5 ‰ in δ³⁴S, and between 0.020 and 0.034 ‰ in Δ³³S, indicating direct precipitation from seawater. Biomarker distributions within two discrete zones of this silica–barite chimney indicate a considerable difference in abundance and diversity of microorganisms from the chimney exterior to the interior. Lipids in the active and inactive chimney barite and sediment were dominated by a range of ¹³C-depleted unsaturated and branched fatty acids with δ¹³C values between ?39.7 and ?26.7 ‰, indicating the presence of sulfur-oxidizing and sulfate-reducing bacteria. The majority of lipids (99.5 %) in the extinct chimney interior that experienced high temperatures were of archaeal origin. Unusual glycerol monoalkyl glycerol tetraethers (GMGT) with 0–4 rings were the dominant compounds suggesting the presence of mainly (hyper-) thermophilic archaea. Isoprenoid hydrocarbons with δ¹³C values as low as ?46 ‰ also indicated the presence of methanogens and possibly methanotrophs.     

Microbial diversity of Loki's Castle black smokers at the Arctic Mid‐Ocean Ridge

Hydrothermal vent systems harbor rich microbial communities ranging from aerobic mesophiles to anaerobic hyperthermophiles. Among these, members of the archaeal domain are prevalent in microbial communities in the most extreme environments, partly because of their temperature‐resistant and robust membrane lipids. In this study, we use geochemical and molecular microbiological methods to investigate the microbial diversity in black smoker chimneys from the newly discovered Loki's Castle hydrothermal vent field on the Arctic Mid‐Ocean Ridge (AMOR) with vent fluid temperatures of 310–320 °C and pH of 5.5. Archaeal glycerol dialkyl glycerol tetraether lipids (GDGTs) and H‐shaped GDGTs with 0–4 cyclopentane moieties were dominant in all sulfide samples and are most likely derived from both (hyper)thermophilic Euryarchaeota and Crenarchaeota. Crenarchaeol has been detected in low abundances in samples derived from the chimney exterior indicating the presence of Thaumarchaeota at lower ambient temperatures. Aquificales and members of the Epsilonproteobacteria were the dominant bacterial groups detected. Our observations based on the analysis of 16S rRNA genes and biomarker lipid analysis provide insight into microbial communities thriving within the porous sulfide structures of active and inactive deep‐sea hydrothermal vents. Microbial cycling of sulfur, hydrogen, and methane by archaea in the chimney interior and bacteria in the chimney exterior may be the prevailing biogeochemical processes in this system.     

云南热带户用沼气池的原核生物群落结构研究

【目的】揭示云南热带农村户用沼气池中的原核生物(细菌和古菌)的群落结构特征。【方法】采用16S r RNA基因克隆文库技术对云南(北)热带代表性气候区的户用沼气池中的原核生物(细菌和古菌)多样性进行研究。【结果】得到细菌330条有效序列,划分为108个OTUs,文库覆盖度为81.5%;古菌有效序列185条,划分为17个OTUs,文库覆盖度为97.8%。通过Gen Bank数据库进行相似性比对与系统发育分析,结果表明:大部分细菌为未知细菌(Unclassified bacteria,占24.19%),优势细菌类群归属拟杆菌门(Bacteroidetes,占23.58%)、绿弯菌门(Chloroflexi,占21.46%)、厚壁菌门(Firmicutes,占13.91%)和变形菌门(Proteobacteria,占8.74%);古菌主要的优势类群为乙酸盐营养型的甲烷八叠球菌目(Methanosarcinales)的鬃毛甲烷菌属(Methanosaeta,占76.75%);此外还检测到少量未培养的泉古菌门细菌(Crenarchaeota,占9.19%)。【结论】云南(北)热带代表性气候区的农村户用沼气池中的微生物种类十分丰富,不同微生物种类的丰度存在明显差异,并存在明显优势种群,且细菌比古菌具有更丰富的多样性。     

Lipid Biomarkers Reveal Microbial Communities in Hydrothermal Chimney Structures from the 49.6°E Hydrothermal Vent Field at the Southwest Indian Ocean Ridge

Lipid biomarkers were investigated to reveal the microbial life preserved in sulfide and Si-rich chimney from the 49.6°E hydrothermal vent field. In sulfide chimney, iso-/anteiso-fatty acids and H-shaped glycerol dialkyl glycerol tetraethers are the main microbial biomarkers. In Si-rich chimney, monounsaturated fatty acids (C16:1n7, C18:1n7) are the main bacterial biomarkers detected, and crenarchaeol and its isomer are relatively abundant (up to 25% of glycerol dialkyl glycerol tetraethers) archaeol biomarkers. Composition of lipid biomarkers reveals the diversity of microbial communities in different types of chimney structures. Sulfate-reducing bacteria and hyperthermophilic archaea were considered to be the majority microbial life in sulfide chimney, and sulfur-oxidizing bacteria were abundant in Si-rich chimney while archaea in Si-rich chimney and mainly attributed to Thaumarchaeota, which were predominately ammonia oxidizers. Our result suggested that fluid temperature and gaseous components could be the main constraints for the diversity of microbial communities in hydrothermal chimney structures in 49.6°E hydrothermal vent field.     

Characterization of eubacterial and archaeal community diversity in the pit mud of Chinese Luzhou-flavor liquor by nested PCR–DGGE

The aim of this study was to investigate and compare the microbial community structures of eubacteria and archaea in the pit mud of Chinese Luzhou-flavor liquor from the wall (C_w) and bottom (C_b) of cellar through nested PCR–denaturing gradient gel electrophoresis (DGGE). The Shannon–Wiener index (H) calculated from the DGGE profiles showed that the community diversities of eubacteria and archaea in samples from C_b were almost higher than that from C_w. In addition, cluster analysis of the DGGE profiles revealed that some differences were found in the microbial community structure in samples from different locations. The closely relative microorganisms of all eubacterial 16S rRNA gene sequences fell into four phyla (Firmicutes, Proteobacteria, Bacteroidetes and Actinobacteria), including 12 genera and 2 uncultured eubacteria. Moreover, 37.1 % eubacteria were affiliated with Clostridium. Particularly, genus Acinetobacter was absent in all samples from C_b but present in all samples from C_w. The closely relative microorganisms of all archaeal 16S rRNA gene sequences fell into four genera, which included Methanobrevibacter, Methanoculleus, Methanobacterium and Methanosaeta, while the dominant archaea in samples from C_w and C_b were similar. Results presented in this study provide further understanding of the spatial differences in microbial community structure in the pit mud, and is of great importance for the production and quality improvement of Luzhou-flavor liquor.     

Relative abundance and diversity of ammonia-oxidizing archaea and bacteria in the San Francisco Bay estuary

Ammonia oxidation in marine and estuarine sediments plays a pivotal role in the cycling and removal of nitrogen. Recent reports have shown that the newly discovered ammonia-oxidizing archaea can be both abundant and diverse in aquatic and terrestrial ecosystems. In this study, we examined the abundance and diversity of ammonia-oxidizing archaea (AOA) and betaproteobacteria (beta-AOB) across physicochemical gradients in San Francisco Bay--the largest estuary on the west coast of the USA. In contrast to reports that AOA are far more abundant than beta-AOB in both terrestrial and marine systems, our quantitative PCR estimates indicated that beta-AOB amoA (encoding ammonia monooxygenase subunit A) copy numbers were greater than AOA amoA in most of the estuary. Ammonia-oxidizing archaea were only more pervasive than beta-AOB in the low-salinity region of the estuary. Both AOA and beta-AOB communities exhibited distinct spatial structure within the estuary. AOA amoA sequences from the north part of the estuary formed a large and distinct low-salinity phylogenetic group. The majority of the beta-AOB sequences were closely related to other marine/estuarine Nitrosomonas-like and Nitrosospira-like sequences. Both ammonia-oxidizer community composition and abundance were strongly correlated with salinity. Ammonia-oxidizing enrichment cultures contained AOA and beta-AOB amoA sequences with high similarity to environmental sequences. Overall, this study significantly enhances our understanding of estuarine ammonia-oxidizing microbial communities and highlights the environmental conditions and niches under which different AOA and beta-AOB phylotypes may thrive.     

南海Formosa冷泉区沉积物微生物多样性与分布规律研究

【目的】当前对全球冷泉生态系统微生物生态学研究显示，冷泉生态系统中主要微生物类群为参与甲烷代谢的微生物，它们的分布差异与所处冷泉区生物地球化学环境密切相关。但在冷泉区内也存在环境因子截然不同的生境，尚缺乏比较冷泉区内小尺度生境间微生物多样性和分布规律的研究。本研究旨在分析南海Formosa冷泉区内不同生境间微生物多样性差异，完善和理解不同环境因子对冷泉内微生物群落结构的影响。【方法】对采集自南海Formosa冷泉区不同生境(黑色菌席区、白色菌席区和碳酸盐岩区)沉积物样本中古菌和细菌16S rRNA基因进行测序，结合环境因子，比较微生物多样性差异，分析环境因子对微生物分布的影响。【结果】发现在Formosa冷泉内的不同生境中，甲烷厌氧氧化古菌(anaerobic methanotrophic archaea,ANME)是主要古菌类群，占古菌总体相对丰度超过70%；在菌席区ANME-1b和ANME-2a/b是主要ANME亚群，碳酸盐岩区则是ANME-1b。硫酸盐还原菌(sulfate-reducing bacteria,SRB)和硫氧化菌(sulfur-oxidizing bacteria...     

Exploration and isolation of novel thermophiles in frozen enrichment cultures derived from a terrestrial acidic hot spring

An isolation strategy, exploring novel microorganisms in frozen enrichment cultures (ENFE), which uses a combination of enrichment culture and 16S rRNA gene clone analysis, was evaluated for isolating uncultured thermophiles from a terrestrial acidic hot spring. The procedure comprised (a) multiple enrichment cultures under various conditions, (b) cryostorage of all enrichments, (c) microbial community analyses of the enrichments using 16S rRNA gene sequences, and (d) purification of microorganisms from enrichments containing previously uncultured microorganisms. The enrichments were performed under a total of 36 conditions, and 16 of these enrichments yielded positive microbial growth with the detection of three previously uncultured archaea. Two of the three previously uncultured archaea, strains HS-1 and HS-3, were successfully isolated. Strain HS-1 and HS-3 represented a novel lineage of the order Sulfolobales and novel species of the genus Sulfolobus, respectively. Although innovative isolation methods play strategic roles in isolating previously uncultured microorganisms, the ENFE strategy showed potential for characterizing and isolating such microorganisms using conventional media and techniques.     

Comparison of an inactive submarine spring with an active nearshore anchialine spring in Florida

Jewfish Sink is a former anchialine karst feature located in the Gulf of Mexico off the coast of West Central Florida. Freshwater flowed from the feature until 1962 and it is now an anoxic marine basin. The current biodiversity within Jewfish Sink was examined in terms of Bacteria, Archaea, and Eukaryota using a combination of 16S and 18S ribosomal RNA analysis from environmental samples. Analysis of 16S rRNA sequences from microbial mats in the anoxic zones revealed a broad diversity of bacteria (265 clones) and archaea (392 clones), many of which had previously been identified in anoxic environmental samples and are likely to be involved with sulfur, nitrogen, and methane metabolism. Sequence analysis of 785 18S clones revealed that fungi and dinoflagellate sequences dominate the eukaryote sequences. Because Jewfish Sink water is anoxic and high in sulfide, we investigated the effect of Jewfish Sink on the nearby shallow benthic environment. We compared the shallow benthic macrofauna near Jewfish Sink with that near Crystal Beach Spring, an active submarine spring. We found significantly greater species richness, abundance, and diversity of benthic fauna near the Jewfish Sink site than near Crystal Beach Spring. This comparison suggests that greater submarine groundwater discharge in an area with active submarine springs is a significant factor reducing the richness and diversity of the benthic community structure in the nearshore, shallow marine environment.     

Geochemical Influence on Diversity and Microbial Processes in High Temperature Oil Reservoirs

The diversity of thermophilic microbial assemblages detected within two neighboring high temperature petroleum formations was shown to closely parallel the different geochemical regimes existing in each. A high percentage of archaeal 16S rRNA gene sequences, related to thermophilic aceticlastic and hydrogenotrophic methanogens, were detected in the natural gas producing Rincon Formation. In contrast, rRNA gene libraries from the highly sulfidogenic Monterey Formation contained primarily sulfur-utilizing and fermentative archaea and bacteria. In addition to the variations in microbial community structure, microbial activities measured in microcosm experiments using high temperature production fluids from oil-bearing formations also demonstrated fundamental differences in the terminal respiratory and redox processes. Provided with the same suite of basic energy substrates, production fluids from the South Elwood Rincon Formation actively generated methane, while thermophilic microflora within the Monterey production fluids were dominated by hydrogen sulfide producing microorganisms. In both cases, molecular hydrogen appeared to play a central role in the stimulation of carbon and sulfur cycling in these systems. In methanogenic production fluids, the addition of sulfur compounds induced a rapid shift in the terminal electron accepting process, stimulating hydrogen sulfide formation and illustrating the metabolic versatility of the subsurface thermophilic assemblage. The high similarity between microbial community structure and activity corresponding with the prevalent geochemical conditions observed in deep subsurface petroleum reservoirs suggests that the resident microflora have adapted to the subsurface physicochemical conditions and may actively influence the geochemical environment in situ.     

Novel groups of Gammaproteobacteria catalyse sulfur oxidation and carbon fixation in a coastal, intertidal sediment

The oxidation of hydrogen sulfide is essential to sulfur cycling in marine habitats. However, the role of microbial sulfur oxidation in marine sediments and the microorganisms involved are largely unknown, except for the filamentous, mat‐forming bacteria. In this study we explored the diversity, abundance and activity of sulfur‐oxidizing prokaryotes (SOP) in sulfidic intertidal sediments using 16S rRNA and functional gene sequence analyses, fluorescence in situ hybridization (FISH) and microautoradiography. The 16S rRNA gene analysis revealed that distinct clades of uncultured Gammaproteobacteria are important SOP in the tidal sediments. This was supported by the dominance of gammaproteobacterial sequences in clone libraries of genes encoding the reverse dissimilatory sulfite reductase (rDSR) and the adenosine phosphosulfate reductase (APR). Numerous sequences of all three genes grouped with uncultured autotrophic SOP. Accordingly, Gammaproteobacteria accounted for 40–70% of all ¹⁴CO₂‐incorporating cells in surface sediments as shown by microautoradiography. Furthermore, phylogenetic analysis of all three genes consistently suggested a discrete population of SOP that was most closely related to the sulfur‐oxidizing endosymbionts of the tubeworm Oligobrachia spp. FISH showed that members of this population (WS‐Gam209 group) were abundant, reaching up to 1.3 × 10⁸ cells ml^?1 (4.6% of all cells). Approximately 25% of this population incorporated CO₂, consistent with a chemolithoautotrophic metabolism most likely based on sulfur oxidation. Thus, we hypothesize that novel, gammaproteobacterial SOP attached to sediment particles may play a more important role for sulfide removal and primary production in marine sediments than previously assumed.     

Microbial community of reduced pockmark sediments (Gdansk Deep,Baltic Sea)

The microbial community of reduced pockmark sediments in the Russian sector of the Gdansk Deep, Baltic Sea, was investigated by molecular biological techniques. Fluorescent in situ hybridization was used to determine the numbers of eubacteria, archaea, and sulfate-reducing bacteria. Eubacteria were found to predominate in the upper 10 cm of the sediment (up to 5.3 × 10⁹ cells/g wet sediment), while the number of archaea increased in the 10- to 30-cm layers (up to 2.8 × 10⁹ cells/g wet sediment, which is higher than the number of eubacteria in the same horizons). Analysis of 16S rRNA gene fragments revealed members of the following phyla: Proteobacteria, Chloroflexi, Firmicutes, Planctomycetales, and high-G + C gram-positive bacteria. Sulfate-reducing bacteria (SRBs) of the families Syntrophaceae, Desulfuromonadaceae, and Actinobacteria of the genera Kocuria and Rothia were the predominant groups. Molecular probes were used to determine predominance of Desulfovibrionales in the SRB enrichment cultures obtained from different horizons of pockmark sediments. Three archaeal phylotypes were revealed, belonging to Euryarchaeota. One of these fell into the group of uncultured methanotrophic archaea (ANME-1a), while the other two were most closely related to uncultured methanogens.     

Microbial diversity of extant stromatolites in the hypersaline marine environment of Shark Bay, Australia

Stromatolites have been present on Earth, at various levels of distribution and diversity, for more than 3 billion years. Today, the best examples of stromatolites forming in hypersaline marine environments are in Hamelin Pool at Shark Bay, Western Australia. Despite their evolutionary significance, little is known about their associated microbial communities. Using a polyphasic approach of culture-dependent and culture-independent methods, we report the discovery of a wide range of microorganisms associated with these biosedimentary structures. There are no comparable reports combining these methodologies in the survey of cyanobacteria, bacteria, and archaea in marine stromatolites. The community was characterized by organisms of the cyanobacterial genera Synechococcus, Xenococcus, Microcoleus, Leptolyngbya, Plectonema, Symploca, Cyanothece, Pleurocapsa and Nostoc. We also report the discovery of potentially free-living Prochloron. The other eubacterial isolates and clones clustered into seven phylogenetic groups: OP9, OP10, Marine A group, Proteobacteria, Low G+C Gram-positive, Planctomycetes and Acidobacteria. We also demonstrate the presence of sequences corresponding to members of halophilic archaea of the divisions Euryarchaeota and Crenarchaeota and methanogenic archaea of the order Methanosarcinales. This is the first report of such archaeal diversity from this environment. This study provides a better understanding of the microbial community associated with these living rocks.     

水圈微生物：推动地球重要元素循环的隐形巨人

正生活在水圈环境中的微生物数量巨大、遗传与代谢方式极为多样,它们驱动着地球上重要元素的循环。水圈微生物研究已经成为生命科学与地球科学的研究热点。国家自然科学基金委员会于2017年启动了"水圈微生物驱动地球元素循环的机制"重大研究计划(简称"水圈微生物"计划)。"水圈微生物"计划拟选择典型水圈生境,通过多学科交叉研究,借助新技术、新方法,揭示水圈微生物在物种、群落和生态水平驱动碳氮硫循环的机制及其环境响应,     

单细胞稳定同位素标记技术在固氮微生物中的应用研究

生物固氮是指固氮微生物将大气中氮气还原为生物可利用氨的过程,是环境中新氮的主要来源,调控初级生产力并影响氮储库的收支平衡。由于环境中大部分固氮微生物不可纯培养,不依赖培养且具有高空间分辨率水平的单细胞技术,成为研究固氮微生物的有力手段。~(15)N_2稳定同位素标记技术,以微生物对~(15)N的同化量或速率为依据,是表征微生物固氮活性的最直接手段。本文对~(15)N_2稳定同位素标记结合两种单细胞技术,即纳米二次离子质谱(Nano SIMS)和单细胞拉曼光谱,用于固氮微生物研究的最新进展进行了综述,内容包括揭示环境中高活性固氮微生物、空间分布、与其他生物的共生关系、细胞生理状态等,并进一步对近期发展的基于单细胞拉曼光谱的固氮微生物研究进行了展望。     

土壤中甲烷厌氧氧化菌多样性的分子检测

甲烷厌氧氧化作用是减少海洋底泥甲烷释放的重要生物地球化学过程,然而在陆地生态系统中甲烷厌氧氧化作用及其功能菌群的生态功能仍然不确定。对甲烷厌氧氧化菌多样性的研究可为减少甲烷排放提供重要科学依据。与传统的分离培养方法比较,分子检测方法是一种更为快速和高效的研究手段,可直接和全面的反映参与甲烷厌氧氧化作用的功能微生物。以DNA分子标记物为研究对象,重点探讨三类主要的分子标记基因,即16S rRNA,mcr A和pmo A,所采用的相关探针和引物信息,同时从定性和定量两个角度综述土壤甲烷厌氧氧化菌的多样性研究的主要进展,最后提出厌氧甲烷氧化菌多样性研究中存在的一些问题和相应的解决思路。     

Metagenomics: Concept,methodology, ecological inference and recent advances

Microorganisms constitute two third of the Earth's biological diversity. As many as 99% of the microorganisms present in certain environments cannot be cultured by standard techniques. Culture-independent methods are required to understand the genetic diversity, population structure and ecological roles of the majority of organisms. Metagenomics is the genomic analysis of microorganisms by direct extraction and cloning of DNA from their natural environment. Protocols have been developed to capture unexplored microbial diversity to overcome the existing barriers in estimation of diversity. New screening methods have been designed to select specific functional genes within metagenomic libraries to detect novel biocatalysts as well as bioactive molecules applicable to mankind. To study the complete gene or operon clusters, various vectors including cosmid, fosmid or bacterial artificial chromosomes are being developed. Bioinformatics tools and databases have added much to the study of microbial diversity. This review describes the various methodologies and tools developed to understand the biology of uncultured microbes including bacteria, archaea and viruses through metagenomic analysis.     

The Diversity of Archaea and Bacteria in Association with the Roots of Zea mays L.

The diversity of bacteria and archaea associating on the surface and interior of maize roots (Zea mays L.) was investigated. A bacterial 16S rDNA primer was designed to amplify bacterial sequences directly from maize roots by PCR to the exclusion of eukaryotic and chloroplast DNA. The mitochondrial sequence from maize was easily separated from the PCR-amplified bacterial sequences by size fractionation. The culturable component of the bacterial community was also assessed, reflecting a community composition different from that of the clone library. The phylogenetic overlap between organisms obtained by cultivation and those identified by direct PCR amplification of 16S rDNA was 48%. Only 4 bacterial divisions were found in the culture collection, which represented 27 phylotypes, whereas 6 divisions were identified in the clonal analysis, comprising 74 phylotypes, including a member of the OP10 candidate division originally described as a novel division level lineage in a Yellowstone hot spring. The predominant group in the culture collection was the actinobacteria and within the clone library, the a-proteobacteria predominated. The population of maize-associated proteobacteria resembled the proteobacterial population of a typical soil community within which resided a subset of specific plant-associated bacteria, such as Rhizobium- and Herbaspirillum-related phylotypes. The representation of phylotypes within other divisions (OP10 and Acidobacterium) suggests that maize roots support a distinct bacterial community. The diversity within the archaeal domain was low. Of the 50 clones screened, 6 unique sequence types were identified, and 5 of these were highly related to each other (sharing 98% sequence identity). The archaeal sequences clustered with good bootstrap support near Marine group I (crenarchaea) and with Marine group II (euryarchaea) uncultured archaea. The results suggest that maize supports a diverse root-associated microbial community composed of species that for the first time have been described as inhabitants of a plant-root environment.     

Bacterial and archaeal phylotypes associated with distinct mineralogical layers of a white smoker spire from a deep-sea hydrothermal vent site (9 degrees N, East Pacific Rise)

A diffusely venting chimney spire from the East Pacific Rise (9 degrees N) was analysed by petrographic thin sectioning and 16S rRNA gene cloning and sequencing in parallel, to correlate microbial community composition with mineralogy and inferred in situ conditions within the chimney mineral matrix. Both approaches indicated a zonation of the chimney spire into distinct microhabitats for different bacteria and archaea. The thermal gradient inferred from the mineral composition and porosity of the chimney was consistent with the distribution of bacterial and archaeal phylotypes in the chimney matrix. A novel phylogenetic lineage of euryarchaeota was found that co-occurred with clones related to cultured hyperthermophilic archaea. A few phylotypes related to mesophilic bacteria were found in the hot core of the chimney, indicating that seawater influx during retrieval and cooling of these highly porous structures can entrain microorganisms into chimney layers that are not their native habitat.