气态烃诱导下油气微生物数量及功能基因变化特征

【目的】烃类渗漏是地球化学循环中的自然垂直运移现象。油气微生物勘探技术就是通过检测油气微生物在烃类渗漏条件下形成的异常特征进而预测下伏油气藏。然而,上浮烃类比重小,使得油气微生物丰度小,缺乏对油气藏地表烃类与油气微生物的深入认识。【方法】本研究在人工模拟环境下,采用培养法和定量PCR对油气微生物数量和油气功能基因的变化特征进行研究。【结果】人工模拟的不同渗漏环境,在一定的驯化培养周期下分别考察甲烷氧化菌和丁烷氧化菌数量变化特征,甲烷氧化菌与丁烷氧化菌在不同烃源中呈现不同的发育情况;同时,在气态烃高浓度阳性对照和微渗漏条件下,油气指示基因pmo A与bom X基因丰度呈现增长现象,然而经过吹脱实验基因丰度仍能指示出曾经发育的油气微生物,在油气微生物勘探检测分析时间尺度上精度高于数量水平的检测。【结论】本研究考察了土壤中油气微生物的数量和功能基因变化特征,为烃类渗漏与油气微生物之间的相关性研究奠定了基础,为油气微生物勘探提供直接实验依据。     

油气微生物勘探机理及应用

【目的】微生物油气勘探技术是基于油气藏的轻烃微渗漏原理衍生的地表勘探技术。油气藏中的轻烃部分(C1-C5)以微渗漏的方式通过上覆的沉积层,在近地表土壤中诱导专门利用轻烃的微生物繁殖与生长,油气区的微生物种类与浓度有别于下伏没有油气藏的地区。通过分析微生物的浓度异常特征,对油气富集区及油气藏进行研究和预测。【方法】在人工模拟条件下研究油气微生物数量和群落异常特征,在此基础上,以海相碳酸盐岩气田普光气田为研究对象,进一步开展微生物勘探研究,鉴定油气藏上方气态烃氧化过程的微生物驱动者,提取土壤中的微生物异常信息。【结果】人工模拟条件下发现Lacibacter cauensis、Methylococcaceae、Methylophilaceae与甲烷气体培养正相关(气指示菌),而未培养的硫氧化微生物等则与丁烷培养正相关(油指示菌)。【结论】进一步在普光气田原位研究中进行验证,发现地表油气微生物数量和群落异常与油气藏有较好的关联性;与油气化探指标对比后发现,油气藏上方微生物正异常和轻烃负异常具有较为明显的互补关系。本研究深化了对典型油气藏上方气态烃氧化微生物转化机制的认识,为油气微生物勘探技术提供理论与实践依据。     

黄土高原石油污染土壤微生物群落结构及其代谢特征

针对污染胁迫下土壤微生物群落变化和代谢变异等问题,基于平板稀释法和Biolog微平板分析方法,研究了陕北黄土高原石油污染土壤微生物群落结构、代谢特征及其功能多样性。结果表明,不同类群的土壤微生物对石油污染胁迫的响应不同,污染土壤细菌和真菌数量高出清洁土壤1个数量级,而污染土壤的放线菌数量极显著减少(P0.01);污染土壤和清洁土壤微生物对糖类和多聚物类碳源较易利用,污染土壤微生物总体上代谢碳源的种类和活性均低于清洁土壤。微生物群落主成分分析(PCA)表明,石油污染土壤和清洁土壤的微生物群落存在显著差异(P0.01),起分异作用的碳源主要为糖类,其次是羧酸类和氨基酸类;随着土壤石油含量增加,典型变量值变异(离散)增大,土壤微生物群落结构稳定性降低。微生物群落多样性分析表明,Shannon丰富度指数(H)、McIntosh均一度指数(U)和Simpson优势度指数(1/D)均达到极显著差异(P0.01),污染土壤微生物群落H和U低于清洁土壤,但是一定浓度的石油污染可以刺激土壤微生物群落中优势种群的生长,1/D增高。研究结果为陕北黄土高原石油污染区土壤微生物修复提供理论基础。     

The Dynamic Change of Microbial Communities in Crude Oil-Contaminated Soils from Oil Fields in China

To study the biodegradability of microbial communities in crude oil contamination, crude oil-contaminated soil samples from different areas of China were collected. Using polyphasic approach, this study explored the dynamic change of the microbial communities during natural accumulation in oil field and how the constructed bioremediation systems reshape the composition of microbial communities. The abundance of oil-degrading microbes was highest when oil content was 3–8%. This oil content is potentially optimal for oil degrading bacteria proliferation. During a ～12 months natural accumulation, the quantity of oil-degrading microbes increased from 10⁵ to 10⁸ cells/g of soil. A typical sample of Liaohe (LH, oil-contaminated site near Liaohe River, Liaoning Province, China) was remediated for 50 days to investigate the dynamic change of microbial communities. The average FDA (a fluorescein diacetate approach) activities reached 0.25 abs/hr·g dry soil in the artificially enhanced repair system, 32% higher than the 0.19 abs/hr·g dry soil in natural circumstances. The abundance of oil-degrading microbes increased steadily from 0.001 to 0.068. During remediation treatment, oil content in the soil sample was reduced from 6.0% to 3.7%. GC–MS analysis indicated up to 67% utilization of C₁₀–C₂₀ normal paraffin hydrocarbons, the typical compounds that undergo microbial degradation.     

Microbial communities within field‐collected Culiseta melanura and Coquillettidia perturbans

Although mosquitoes are well‐known vectors of human and animal diseases, pathogens are only minor components of their total endogenous microbial communities. The midguts of many insects, including mosquitoes, contain diverse microbial communities. In this study, we used denaturing gradient gel electrophoresis to identify the diversity of bacteria in field‐collected adult female Culiseta melanura (Diptera: Culicidae) (Coquillett) and Coquillettidia perturbans (Diptera: Culicidae) (Walker). Few significant differences in bacterial fauna between the two mosquito species were found, but the results suggest that host life history may be a determinant of the endogenous bacterial communities in mosquitoes. In the present study, the dominant bacteria are frequently identified as major components of other mosquito species' microbial flora, suggesting the establishment of a stable association between the mosquitoes and the microbes after initial acquisition from the environment.     

A DNA-based Analysis of a Microbial Technique for the Prospecting of Oil and Gas Applied to a Known Oil Field,China

To evaluate the application of a DNA-based analysis of a microbial technique for oil and gas prospecting, the hydrocarbon potential predicted using the methanotrophic pmoA and propanotrophic prmA genes as targets was investigated in soil above a known oil reservoir. In total, 82 soil samples were collected at 50-cm depths above the Xiliu oil reservoir for quantitative real-time polymerase chain reaction (RT-PCR) analysis. The pmoA gene content ranged from 0 to 2.7 × 10⁶ copies/g dw, whereas that of prmA varied from 0 to 1.6 × 10⁶ copies/g dw. Microbial anomaly distribution maps of normalized values for the prmA gene as a main indicator suggested that the area with the highest potential of prospecting was an undeveloped location, and an area with a relatively large prmA background was identified at this oil-producing site. The areas of microbial anomaly exhibited different prmA/pmoA ratios (20, 1–5, 0.0n–0.25 and 0), and this ratio may be used as an indicator for predicting the properties of oil and gas reservoirs and biogenic methane or the influence of oil-producing activities. Our results suggest that a DNA-based analysis of a microbial technique is a powerful tool for oil and gas prospecting. This study provides a new microbial technique for the prospecting of oil and gas.     

芦苇克隆整合对石油污染湿地土壤微生物群落结构和生物量的影响

克隆植物形体相连的无性个体(分株)之间可以进行水分、养分和光合产物的传递和共享,并且这种克隆整合可以显著提高分株对环境胁迫的耐受能力,从而可能进一步影响分株周围的土壤微生物群落结构和生物量。尽管国内外已经开展了大量有关克隆整合对分株耐受胁迫能力影响的研究,但克隆整合对土壤微生物群落结构和生物量影响的研究却十分缺乏。以黄河三角洲芦苇(Phragmites australis)湿地生态系统为研究对象,将直径60 cm的圆形样方进行三个水平的石油添加处理(不添加石油或每年添加5 mm或10 mm厚的石油),同时通过切断或不切断样方内外芦苇根状茎的连接来控制克隆整合的有无。实验连续开展了两年(2014—2015年),每年8月份在样方内进行土壤样品取样,在实验室内采用磷酸脂肪酸(PLFA)法测定土壤微生物总量及主要微生物类群含量,并测定土壤微生物生物量碳和氮含量。取样时间显著影响土壤微生物PLFA总量、微生物碳和氮含量,这3个变量在2015年均显著高于2014年。石油添加在2015年显著增加了土壤微生物PLFA总量,但在2014年却无显著效应;同时,石油添加在2014年降低了土壤微生物碳和氮含量,而在2015年却增加了其含量。然而,无论在2014年还是2015年,芦苇的克隆整合对土壤微生物PLFA含量、微生物碳和氮含量均没有显著影响。土壤微生物PLFA总量与土壤微生物碳和氮含量呈正相关关系。这些结果表明,石油污染可以显著影响湿地土壤微生物动态,但克隆整合却无显著效应。     

Microbial mats in tidal channels at San Carlos,Baja California Sur,Mexico

Microbial communities of stratified phototrophic bacteria in laminated intertidal sediments north of Estuary El Puente, near San Carlos, Baja California Sur, Mexico,‐were studied. This study describes the macroscopic and microscopic characteristics of the mats, including their annual growth. The mats were located in and along meandering mangrove‐lined tidal channels. Their thickness ranged from 0.5 to 25 cm. Square‐meter areas of polygonal mats were detected in several ponds infiltrated by sea water. The principal microbial community of the upper surface of various morphotypes of microbial mats was identified as cyanobacteria belonging to the genera Microcoleus, Lyngbya, Phormidium, and Oscillatoria. Other cyanobacte‐rial genera such as Pseudanabaena, Spirulina, Synechococcus, and Gloeocapsa, as well as many unidentified diatoms, were also present but at lower population densities. The second inward reddish layers of the microbial mats contained similar cyano‐bacterial genera plus anoxygenic phototrophic bacteria belonging to the genera Chloroflexus, Thiocapsa, Chromatium, Prosthecochloris, Rhodopseudomonas, and Chlorobium, as well as several unidentified bacteria. In situ measurements on the growth of the mats, from intermittent tide sites, showed an annual buildup of two layers: green and reddish. These layers corresponded to a vertical growth of 1.4 ± 0.27 mm/year. Permanently submerged mats did not show vertical growth during the same period of time.     

Geochemistry and Microbial Populations in Sediments of the Northern Baffin Bay,Arctic

The Northern Baffin Bay between Greenland and Canada is a remote Arctic area restricted in primary production by seasonal ice cover, with presumably low sedimentation rates, carbon content and microbial activities in its sediments. Our aim was to study the so far unknown subseafloor geochemistry and microbial populations driving seafloor ecosystems. Shelf sediments had the highest organic carbon content, numbers of Bacteria and Archaea, and microcosms inoculated from Shelf sediments showed highest sulfate reduction and methane production rates. Sediments in the central deep area and on the southern slope contained less organic carbon and overall lower microbial numbers. Similar 16S rRNA gene copy numbers of Archaea and Bacteria were found for the majority of the sites investigated. Sulfate in pore water correlated with dsrA copy numbers of sulfate-reducing prokaryotes and differed between sites. No methane was found as free gas in the sediments, and mcrA copy numbers of methanogenic Archaea were low. Methanogenic and sulfate-reducing cultures were enriched on a variety of substrates including hydrocarbons. In summary, the Greenlandic shelf sediments contain vital microbial communities adapted to their specific environmental conditions.     

Silicified Biota in High-Altitude,Geothermally Influenced Ignimbrites at El Tatio Geyser Field,Andean Cordillera (Chile)

Biofilms and filamentous communities provided favorable sites for silica precipitation on deeply weathered ignimbrites that make up the substrate at the hydrothermal field of El Tatio (Andean Cordillera, Chile). The amorphous silica encrustation enabled the preservation of a variety of biotic and abiotic features. An integrated study based on optical/scanning electron microscopy and molecular methods of totally to partially silicified microbial communities and biofilms allowed a comparative evaluation of the microfacies and the microbial diversity in the siliceous sinters produced by the digression of a little braided stream departing from a hot spring pool. This study showed useful convergent identifications of certain groups of microbes, such as filamentous cyanobacteria attributed to the genera Phormidium and Rivularia. Together with these microbes, other presumably initial colonizers, such as the halophilic and thermophilic pennate diatoms Nitzschia and Synedra, were widely present and could have contributed to the formation of biofilms and mucus that, as potential home to early silicification, could have contributed to the preservation of microbiologically derived morphologies.     

基于宏基因组技术分析全球不同温度带土壤微生物多样性

【背景】温度在塑造大尺度的土壤微生物群落方面发挥了重要作用,但目前针对全球不同温度带大尺度土壤微生物多样性方面的研究十分缺乏。【目的】明确不同温度带大尺度土壤微生物组成和功能的差异变化。【方法】从宏观的角度运用宏基因组技术对不同温度带土壤微生物群落的组成和功能进行分析。【结果】细菌的物种多样性随着温度带纬度的升高而增多,真菌的物种多样性在温带最多,在寒带最小且假丝酵母属(Candida)占绝对优势。3个温度带间除物种多样性存在差异外,微生物群落中物种丰度差异也较大,优势属和特殊属各有不同。其中值得注意的是,假单胞菌属(Pseudomonas)和芽孢杆菌属(Bacillus)的丰度在不同温度带间存在显著差异,且随着温度带纬度的升高而增多,而链霉菌属(Streptomyces)、地嗜皮菌属(Geodermatophilus)、红色杆菌属(Rubrobacter)和小单孢菌属(Micromonospora)的丰度随温度带纬度的升高而降低。在功能方面,发现与翻译后修饰、蛋白质周转、伴侣(posttranslational modification, protein turnover, chap...     

Microbial tropicalization driven by a strengthening western ocean boundary current

Western boundary currents (WBCs) redistribute heat and oligotrophic seawater from the tropics to temperate latitudes, with several displaying substantial climate change‐driven intensification over the last century. Strengthening WBCs have been implicated in the poleward range expansion of marine macroflora and fauna, however, the impacts on the structure and function of temperate microbial communities are largely unknown. Here we show that the major subtropical WBC of the South Pacific Ocean, the East Australian Current (EAC), transports microbial assemblages that maintain tropical and oligotrophic (k‐strategist) signatures, to seasonally displace more copiotrophic (r‐strategist) temperate microbial populations within temperate latitudes of the Tasman Sea. We identified specific characteristics of EAC microbial assemblages compared with non‐EAC assemblages, including strain transitions within the SAR11 clade, enrichment of Prochlorococcus, predicted smaller genome sizes and shifts in the importance of several functional genes, including those associated with cyanobacterial photosynthesis, secondary metabolism and fatty acid and lipid transport. At a temperate time‐series site in the Tasman Sea, we observed significant reductions in standing stocks of total carbon and chlorophyll a, and a shift towards smaller phytoplankton and carnivorous copepods, associated with the seasonal impact of the EAC microbial assemblage. In light of the substantial shifts in microbial assemblage structure and function associated with the EAC, we conclude that climate‐driven expansions of WBCs will expand the range of tropical oligotrophic microbes, and potentially profoundly impact the trophic status of temperate waters.     

Review: Microbial synthesis of agrochemical metabolites

The synthesis of agrochemical metabolite reference standards by microbial cultures can serve as a useful alternative to conventional chemical synthesis, particularly when the chemical synthesis is difficult. Microbially generated metabolites of agrochemicals can also be useful for predicting degradative pathways in animals, plants and soils prior to conducting animal, plant and soil metabolism studies which are required by regulatory agencies to support agrochemical registrations. Examples from the literature are used to illustrate the utility of synthesizing metabolites of agrochemicals by common microbes. Received 17 January 1997/ Accepted in revised form 20 March 1997     

Microbial Communities Associated with Tree Bark Foliose Lichens: A Perspective on their Microecology

Tree‐bark, foliose lichens occur widely on a global scale. In some locales, such as forests, they contribute a substantial amount of biomass. However, there are few research reports on microbial communities including eukaryotic microbes associated with foliose lichens. Lichens collected from tree bark at 11 locations (Florida, New York State, Germany, Australia, and the Arctic) were examined to determine the density and C‐biomass of bacteria and some eukaryotic microbes, i.e. heterotrophic nanoflagellates (HNF) and amoeboid protists. A rich microbial diversity was found, including large plasmodial slime molds, in some cases exceeding 100 μm in size. The densities of HNF and amoeboid protists were each positively correlated with densities of bacteria, r = 0.84 and 0.80, respectively (p < 0.01, N = 11 for each analysis) indicating a likely bacterial‐based food web. Microbial densities (number/g lichen dry weight) varied markedly across the geographic sampling sites: bacteria (0.7–13.1 × 10⁸), HNF (0.2–6.8 × 10⁶) and amoeboid protists (0.4–4.6 × 10³). The ranges in C‐biomass (μg/g lichen dry weight) across the 11 sites were: bacteria (8.8–158.5), HNF (0.03–0.85), and amoeboid protists (0.08–540), the latter broad range was due particularly to absence or presence of large slime mold plasmodia.     

Microbial community structure and global trace gases

Global change can affect soil processes by either altering the functioning of existing organisms or by restructuring the community, modifying the fundamental physiologies that drive biogeochemical processes. Thus, not only might process rates change, but the controls over them might also change. Moreover, previously insignificant processes could become important. These possibilities raise the question ‘Will changes in climate and land use restructure microbial communities in a way that will alter trace gas fluxes from an ecosystem?’ Process studies indicate that microbial community structure can influence trace gas dynamics at a large scale. For example, soil respiration and CH₄ production both show ranges of temperature response among ecosystems, indicating differences in the microbial communities responsible. There are three patterns of NH₄⁺ inhibition of CH₄ oxidation at the ecosystem scale: no inhibition, immediate inhibition, and delayed inhibition; these are associated with different CH₄ oxidizer communities. Thus, it is possible that changes in climate, land-use, and disturbance regimes could alter microbial communities in ways that would substantially alter trace gas fluxes; we discuss the data supporting this conclusion. We also discuss approaches to developing research linking microbial community structure and activity to the structure and functioning of the whole ecosystem. Modern techniques allow us to identify active organisms even if they have not been cultivated; in combination with traditional experimental approaches we should be able to identify the linkages between these active populations and the processes they carry out at the ecosystem level. Finally, we describe scenarios of how global change could alter trace gas fluxes by altering microbial communities and how understanding the microbial community dynamics could improve our ability to predict future trace gas fluxes.     

Bacterial Succession on n-Alkanes under the Conditions of Sulfate Reduction

The dynamics of species composition of a hydrocarbon-oxidizing bacteriocenosis of a ground suspension of the Mozhaisk Reservoir has been studied. The bacteriocenosis was undergoing development in a paraffin film (model association composed of sulfate-reducing bacteria and hydrocarbon-oxidizing bacteria). The type of bacterial succession did not depend on the depth, from which ground samples were collected. Two microbial species (Pseudomonas sp. andArthrobacter globiformis) were absolutely dominant. Pseudomonas sp. was dominant at the early and intermediate stages of the succession, whereas A. globiformis was present in the hydrocarbon-oxidizing bacteriocenosis throughout the whole period of the succession. There was a trend toward a gradual increase in the ratio of A. globiformis, and, by the end of the experiment, Pseudomonas sp. was replaced by A. globiformis almost completely. The bacterial species Micrococcus sp. and Rhodococcus erythropolis were minor components of the hydrocarbon-oxidizing bacteriocenosis under the conditions of sulfate reduction. The succession of species of hydrocarbon-oxidizing bacteria in the paraffin film of the model association reflects both the life strategy of the bacterial species under study and the degree of their tolerance to products of sulfate reduction.     

Microbial Diversity in Sediments Collected from the Deepest Cold-Seep Area, the Japan Trench

The Japan Trench land slope at a depth of 6,400 m is the deepest cold-seep environment with Calyptogena communities. Sediment samples from inside and beside the Calyptogena communities were collected, and the microbial diversity in the sediment samples was studied by molecular phylogenetic techniques. From DNA extracted directly from the sediment samples, 16S rDNAs were amplified by the polymerase chain reaction method. The sequences of the amplified 16S rDNAs selected by restriction fragment length polymorphism analysis were determined and compared with sequences in DNA databases. The results showed that 33 different bacterial 16S rDNA sequences from the two samples analyzed fell into similar phylogenetic categories, the α-, γ-, δ-, and ɛ-subdivisions of Proteobacteria, Cytophaga, and gram-positive bacteria; some of the 16S rDNA sequences were common to both samples. δ- and ɛ-Proteobacteria-related sequences were abundant in both sediments. These sequences are mostly related to sulfate-reducing or sulfur-reducing bacteria and epibionts, respectively. Eight different archaeal 16S rDNA sequences were cloned from the sediments. The majority of the archaeal 16S rDNA sequences clustered in Crenarchaeota and showed high similarities to marine group I archaeal rDNA. A Methanococcoides burtonii–related sequence obtained from the sediment clustered in the Euryarchaeota indicating that M. burtonii–related strains in the area of Calyptogena communities may contribute to production of methane in this environment. From these results, we propose a possible model of sulfur circulation within the microbial community and that of Calyptogena clams in the cold-seep environment. Received June 15, 1998; accepted November 10, 1998.     

The Role of Heterotrophic Microbial Communities in Estuarine C Budgets and the Biogeochemical C Cycle with Implications for Global Warming: Research Opportunities and Challenges

Estuaries are among the most productive and economically important marine ecosystems at the land–ocean interface and contribute significantly to exchange of CO₂ with the atmosphere. Estuarine microbial communities are major links in the biogeochemical C cycle and flow of C in food webs from primary producers to higher consumers. Considerable attention has been given to bacteria and autotrophic eukaryotes in estuarine ecosystems, but less research has been devoted to the role of heterotrophic eukaryotic microbes. Current research is reviewed here on the role of heterotrophic eukaryotic microbes in C biogeochemistry and ecology of estuaries, with particular attention to C budgets, trophodynamics, and the metabolic fate of C in microbial communities. Some attention is given to the importance of these processes in climate change and global warming, especially in relation to sources and sinks of atmospheric CO₂, while also documenting the current paucity of research on the role of eukaryotic microbes that contribute to this larger question of C biogeochemistry and the environment. Some recommendations are made for future directions of research and opportunities of applying newer technologies and analytical approaches to a more refined analysis of the role of C in estuarine microbial community processes and the biogeochemical C cycle.     

Methanogenic Microbial Community Composition of Oily Sludge and Its Enrichment Amended with Alkanes Incubated for Over 500 Days

Methanogenic microbial community is responsive to the availability of hydrocarbons and such information is critical for the assessment of hydrocarbon degradation in remediation and also in biologically enhanced recovery of energy from non-producing oil reserves. In this study, methanogenic enrichment cultures from oily sludge amended with n-alkanes (C₁₅-C₂₀) showed a development of active methanogenic alkanes-degrading consortium for over a total of 1000 days of incubation at 37°C. Total genomic DNAs were extracted from three types of samples, the original oily sludge (OS), the sludge after incubation for 500 days under methanogenic condition without any external carbon addition (EC), and the enrichment culture from the EC amended with n-alkanes (ET) incubated for another 500 days. The phylogenetic diversities of microbial communities of the three samples were analyzed by PCR amplification of partial 16S rRNA genes. The catabolic genes encoding benzylsuccinate synthase (bssA) and alkylsuccinate synthase (assA) were also examined by PCR amplification. These results provide important evidence in that microbial populations in an oily sludge shifted from methanogenic aromatic compounds degrading communities to potential methanogenic alkane-degrading communities when the enrichment was supplemented with n-alkanes and incubated under anaerobic conditions.     

Assessment of Microbial Diversity in Saudi Springs by Culture-Dependent and Culture-Independent Methods

Culture-dependent and culture-independent methods were used to evaluate the microbial diversity in two hot springs of the Aljouf region in Saudi Arabia, including Qasr Kaff and Ain Hawas. Physicochemical characteristics of the springs were examined to establish their effect on the biodiversity of thermophilic bacteria and fungi. We employed culture-dependent techniques to study microbial diversity using four different complex media for bacteria and fungi. In addition, the direct count for algal populations from two springs was investigated. We surveyed the microbial diversity in water and sediment samples from both springs by denaturing gradient gel electrophoresis (DGGE) and clone library construction. Bacillariophycaea (18 species) was the most diverse group, followed by Cyanophyceaea. Bacterial isolates closer to the genera Bacillus spp., Geobacillus, Thermoactinomyces, and unidentified actinobacteria were recovered. Fungal isolates were related to Aspergillus, Pezizaceae, Penicillium, Acremonium, Fusarium, Chrysosporium, and Stachybotrys. Using molecular-based techniques, the results were slightly different from those obtained by culture-dependent methods, and more genera were obtained. However, most genera were uncultured microbes, particularly from bacterial communities.