Analysis of the diversity of aerobic,thermophilic endospore-forming bacteria in two Algerian hot springs using cultural and non-cultural methods

Terrestrial hot environments are important resources for isolation of thermophilic microorganisms. Few studies have been made on microbial diversity of Algerian geothermal sites. This paper reports the diversity of thermophilic, aerobic endospore-forming bacteria from water and sediment samples taken from Hammam Ouled Ali and Hammam Debagh, two hot springs with a wide range of temperatures and a very rich mineral composition, located in the region of Guelma, north-east of Algeria using culture-dependent and culture-independent approaches Sequences of the V4 region of the 16S rRNA gene from environmental DNA extracted from sediment samples were analyzed and a set of isolates from water and sediment have been characterized by phenotypic and molecular methods. Phylogenetic surveys using environmental DNA sequences indicated that three families dominated the two hot springs: Planococcaceae, Bacillaceae, and Paenibacillaceae. Phenotypic characterization revealed the morphological, biochemical, and physiological properties of these microorganisms, all of which exhibited a range of common extracellular enzymatic activities. Amplified ribosomal DNA restriction analysis (ARDRA) was used to cluster isolates into different phylotypic groups and phylogenetic analysis of 16S rRNA gene sequences of selected isolates showed that all were closely related to four genera of thermophilic Bacilli: Bacillus, Anoxybacillus, Geobacillus, and Brevibacillus. Our results provide important insights into the microbial ecology of Guelma hot springs. They showed that the phylogenetic diversity of bacterial communities within the two studied hot springs was mostly aerobic, with the presence of taxonomic groups of great biotechnological interest. Bioprospection of thermozymes and other biomolecules within these communities will probably provide a data basis for their industrial exploitation.     

冰川生态系统固碳微生物研究进展

[目的] 海南海口含有丰富的温泉资源,对温泉微生物多样性进行研究,有助于进一步开发和利用海南温泉微生物资源。[方法] 本文采用Illumina HiSeq高通量测序技术对海口3个温泉[海甸岛荣域温泉（S1）、火山口开心农场温泉（S2）和西海岸海长流温泉（S3）] 水样中微生物ITS序列和16S rRNA基因V3-V4区进行测序及生物信息学分析,探究海口市3个不同区域的温泉真菌多样性与细菌多样性。[结果] （1）α多样性分析表明,真菌群落中,S3 > S1 > S2,而在细菌群落中,S2 > S1 > S3。β多样性分析表明,3个温泉真菌群落和细菌群落组成差异皆显著。（2）分类分析表明,温泉真菌群落优势菌门为子囊菌门（Ascomycota）和担子菌门（Basidiomycota）,细菌群落优势菌门为变形菌门（Proteobacteria）、拟杆菌门（Bacteroidetes）、Thermi、硝化螺旋菌门（Nitrospirae）、绿菌门（Chlorobi）、厚壁菌门（Firmicutes）、绿弯菌门（Chloroflexi）、放线菌门（Actinobacteria）。（3）CCA（Canonical correspondence analysis）分析表明,3个温泉的真菌群落主要影响因子是温度,细菌群落主要影响因子是总磷。[结论] 海南省海口市温泉中含有丰富的微生物资源,其微生物群落组成受多种环境因子影响,且影响真菌和细菌的主要环境因子不同。     

Bacterial and archaeal diversities in Yunnan and Tibetan hot springs,China

Thousands of hot springs are located in the north‐eastern part of the Yunnan–Tibet geothermal zone, which is one of the most active geothermal areas in the world. However, a comprehensive and detailed understanding of microbial diversity in these hot springs is still lacking. In this study, bacterial and archaeal diversities were investigated in 16 hot springs (pH 3.2–8.6; temperature 47–96°C) in Yunnan Province and Tibet, China by using a barcoded 16S rRNA gene‐pyrosequencing approach. Aquificae, Proteobacteria, Firmicutes, Deinococcus‐Thermus and Bacteroidetes comprised the large portion of the bacterial communities in acidic hot springs. Non‐acidic hot springs harboured more and variable bacterial phyla than acidic springs. Desulfurococcales and unclassified Crenarchaeota were the dominated groups in archaeal populations from most of the non‐acidic hot springs; whereas, the archaeal community structure in acidic hot springs was simpler and characterized by Sulfolobales and Thermoplasmata. The phylogenetic analyses showed that Aquificae and Crenarchaeota were predominant in the investigated springs and possessed many phylogenetic lineages that have never been detected in other hot springs in the world. Thus findings from this study significantly improve our understanding of microbial diversity in terrestrial hot springs.     

Seasonal hydrologic and geologic forcing drive hot spring geochemistry and microbial biodiversity

Hot springs integrate hydrologic and geologic processes that vary over short- and long-term time scales. However, the influence of temporal hydrologic and geologic change on hot spring biodiversity is unknown. Here, we coordinated near-weekly, cross-seasonal (~140 days) geochemical and microbial community analyses of three widely studied hot springs with local precipitation data in Yellowstone National Park. One spring (‘HFS’) exhibited statistically significant, coupled microbial and geochemical variation across seasons that was associated with recent precipitation patterns. Two other spring communities, ‘CP’ and ‘DS’, exhibited minimal to no variation across seasons. Variability in the seasonal response of springs is attributed to differences in the timing and extent of aquifer recharge with oxidized near-surface water from precipitation. This influx of oxidized water is associated with changes in community composition, and in particular, the abundances of aerobic sulfide-/sulfur-oxidizers that can acidify waters. During sampling, a new spring formed after a period of heavy precipitation and its successional dynamics were also influenced by surface water recharge. Collectively, these results indicate that changes in short-term hydrology associated with precipitation can impact hot spring geochemistry and microbial biodiversity. These results point to potential susceptibility of certain hot springs and their biodiversity to sustained, longer-term hydrologic changes.     

Anaerobic transformation of carbon monoxide by microbial communities of Kamchatka hot springs

Carbon monoxide (CO) is one of the common gaseous compounds found in hot volcanic environments. It is known to serve as the growth substrate for a number of thermophilic prokaryotes, both aerobic and anaerobic. The goal of this work was to study the process of anaerobic transformation of CO by microbial communities inhabiting natural thermal environments: hot springs of Uzon Caldera, Kamchatka. The anaerobic microbial community of Treshchinny Spring (80°C, pH 6.5) was found to exhibit two peaks of affinity for CO (K _S1 = 54 nM and K _S2 = 1 μM). The actual rate of anaerobic CO transformation by the microbial community of this spring, calculated after obtaining the concentration dependence curve and extrapolated to the natural concentration of CO dissolved in the hot spring water (20 nM), was found to be 120 μmol l⁻¹ of sediment day⁻¹. In all the hot springs studied, more than 90% of the carbon of ¹⁴CO upon anaerobic incubation was recovered as ¹⁴CO₂. From 1 to 5% of ¹⁴CO was transformed to volatile fatty acids (VFA). The number of microorganisms capable of anaerobic CO oxidation determined by dilution-to-extinction method reached 10⁶ cells ml⁻¹ of sediment. CO-transforming anaerobic thermophilic microorganisms isolated from the springs under study exhibited hydrogenogenic type of CO oxidation and belonged to the bacterial genera Carboxydocella and Dictyoglomus. These data suggest a significant role of hydrogenogenic carboxydotrophic prokaryotes in anaerobic CO transformation in Uzon Caldera hot springs.     

高通量测序分析云南腾冲热海热泉微生物多样性

【背景】云南腾冲热海热泉中蕴含着丰富的极端微生物资源。【目的】揭示云南腾冲热海热泉中微生物物种多样性及群落结构差异,发掘酸性热泉中铁、硫氧化功能微生物。【方法】采用Illumina HiSeq高通量测序技术对3处热泉15个水体样品中微生物16SrRNA基因V4-V5区进行测序及生物信息学分析。【结果】3处热泉中共获得578061条有效序列,聚类为141个可操作分类单元(Operational taxonomic unit,OTU),包括19个门66个属。鼓鸣泉(GMQ)、蛤蟆嘴(HMZ)、黄瓜箐(HGQ)3处热泉均以泉古菌门(Crenarchaeota)和厚壁菌门(Firmicute)为主。从属水平分析,碱性热泉鼓鸣泉(GMQ)和中性热泉蛤蟆嘴(HMZ)分别注释到37、32个属,优势属均为芽孢杆菌属(Bacillus)和热棒菌属(Pyrobaculum)。酸性热泉黄瓜箐(HGQ)共注释到20个属,优势属为酸杆菌属(Acidibacillus)和酸硫杆状菌属(Acidithiobacillus),此外,具有铁、硫氧化潜力的菌属有喜酸菌属(Acidicaldus)、硫化芽孢杆菌属(Sulfobacillus)、硫化叶菌属(Sulfolobus)及生金球菌属(Metallosphaera)等,进一步通过硫氧化培养基分离获得了这些菌属中的纯菌株。【结论】云南腾冲热海热泉水体中蕴含丰富的微生物资源,热泉间微生物物种组成差异明显;酸性热泉中存在多种具有潜在铁、硫代谢功能的菌种;未分类类群、非培养类群丰度很高,尤其是蕴藏着可观的古菌资源。     

Phylogenetic analysis of the bacterial community in a geothermal spring,Rupi Basin,Bulgaria

Hot environments are between the supporting life extreme niches that appear to have maintained some degree of pristine quality and of special biotechnological interest. Knowledge on biodiversity in terrestrial hot springs is still scanty and has not been compared in the light of the specificity of those extreme ecological niches. Study on diversity of thermophilic bacteria inhabiting a hot spring located in Rupi Basin (RB), South-West Bulgaria, revealed a high phylogenetic richness in it (genotypic diversity is 0.37). A total of 120 clones were examined, and grouped in 28 phylogenetic types by their RFLP profile. 16S rRNA gene analysis allowed the identification of nine divisions from the domain Bacteria and one Candidate division. Ten of the retrieved bacterial sequences representing one third of the sequence types showed less than 97% similarity to the closest neighbor and were referred as new sequences. Four of them were distantly related to validly described bacteria (showed ≤90% similarity) suggesting new taxons on at least genus level. Comparison of biodiversity in the spring from Rupi Basin, Bulgaria with that described from other terrestrial hot springs revealed that Proteobacteria, Hydrogenobacter/Aquifex and Thermus are common bacterial groups for terrestrial hot springs. Simultaneously, specific bacterial taxons were observed in different springs.     

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.     

Archaeal and bacterial communities in geochemically diverse hot springs of Yellowstone National Park, USA

Microbiological and geochemical surveys were conducted at three hot springs (Obsidian Pool, Sylvan Spring, and ‘Bison Pool’) in Yellowstone National Park (Wyoming, USA). Microbial community structure was investigated by polymerase chain reaction (PCR) amplification of 16S rRNA gene sequences from DNA extracted from sediments of each hot spring, followed by molecular cloning. Both bacterial and archaeal DNA was retrieved from all samples. No Euryarchaea were found, but diverse Crenarchaea exist in all three pools, particularly affiliating with deep‐branching, but uncultivated organisms. In addition, cloned DNA affiliating with the Desulphurococcales and Thermoproteales was identified, but the distribution of taxa differs in each hot spring. The bacterial community at all three locations is dominated by members of the Aquificales and Thermodesulfobacteriales, indicating that the ‘knallgas’ reaction (aerobic hydrogen oxidation) may be a central metabolism in these ecosystems. To provide geochemical context for the microbial community structures, energy‐yields for a number of chemolithoautotrophic reactions are provided for >80 sampling sites in Yellowstone, including Obsidian Pool, Sylvan Spring, and ‘Bison Pool’. This energy profile shows that the knallgas reaction is just one of many exergonic reactions in the Yellowstone hot springs, that energy‐yields for certain reactions can vary substantially from one site to the next, and that few of the demonstrated exergonic reactions are known to support microbial metabolism.     

中国温泉微生物物种多样性及其酶活性研究进展

微生物作为生物群体的重要组成成员,其生长受外界物化条件(如温度、盐度、pH等)影响较大。温泉作为极端水生环境之一,属于相对稳定且较为特殊的生态系统,使生长于其中的微生物可能具有适应高温等特殊生境的独特生存生理机制,具体表现为微生物物种及其活性次级代谢产物呈现出一定的多样性与新颖性。本文从菌株物种多样性分析及其酶活性研究方面,综述了近5年来国内温泉微生物相关研究进展,以期为温泉等极端环境微生物资源开发与保护提供参考。     

Biodiversity of the microbial mat of the Garga hot spring

Background

Microbial mats are a good model system for ecological and evolutionary analysis of microbial communities. There are more than 20 alkaline hot springs on the banks of the Barguzin river inflows. Water temperature reaches 75 °C and pH is usually 8.0–9.0. The formation of microbial mats is observed in all hot springs. Microbial communities of hot springs of the Baikal rift zone are poorly studied. Garga is the biggest hot spring in this area.

Results

In this study, we investigated bacterial and archaeal diversity of the Garga hot spring (Baikal rift zone, Russia) using 16S rRNA metagenomic sequencing. We studied two types of microbial communities: (i) small white biofilms on rocks in the points with the highest temperature (75 °C) and (ii) continuous thick phototrophic microbial mats observed at temperatures below 70 °C. Archaea (mainly Crenarchaeota; 19.8% of the total sequences) were detected only in the small biofilms. The high abundance of Archaea in the sample from hot springs of the Baikal rift zone supplemented our knowledge of the distribution of Archaea. Most archaeal sequences had low similarity to known Archaea. In the microbial mats, primary products were formed by cyanobacteria of the genus Leptolyngbya. Heterotrophic microorganisms were mostly represented by Actinobacteria and Proteobacteria in all studied samples of the microbial mats. Planctomycetes, Chloroflexi, and Chlorobi were abundant in the middle layer of the microbial mats, while heterotrophic microorganisms represented mostly by Firmicutes (Clostridia, strict anaerobes) dominated in the bottom part. Besides prokaryotes, we detect some species of Algae with help of detection their chloroplasts 16 s rRNA.

Conclusions

High abundance of Archaea in samples from hot springs of the Baikal rift zone supplemented our knowledge of the distribution of Archaea. Most archaeal sequences had low similarity to known Archaea. Metagenomic analysis of microbial communities of the microbial mat of Garga hot spring showed that the three studied points sampled at 70 °C, 55 °C, and 45 °C had similar species composition. Cyanobacteria of the genus Leptolyngbya dominated in the upper layer of the microbial mat. Chloroflexi and Chlorobi were less abundant and were mostly observed in the middle part of the microbial mat. We detected domains of heterotrophic organisms in high abundance (Proteobacteria, Firmicutes, Verrucomicrobia, Planctomicetes, Bacteroidetes, Actinobacteria, Thermi), according to metabolic properties of known relatives, which can form complete cycles of carbon, sulphur, and nitrogen in the microbial mat. The studied microbial mats evolved in early stages of biosphere formation. They can live autonomously, providing full cycles of substances and preventing live activity products poisoning.

     

Spatial and temporal variability of biomarkers and microbial diversity reveal metabolic and community flexibility in Streamer Biofilm Communities in the Lower Geyser Basin,Yellowstone National Park

Detailed analysis of 16S rRNA and intact polar lipids (IPLs) from streamer biofilm communities (SBCs), collected from geochemically similar hot springs in the Lower Geyser Basin, Yellowstone National Park, shows good agreement and affirm that IPLs can be used as reliable markers for the microbial constituents of SBCs. Uncultured Crenarchaea are prominent in SBS, and their IPLs contain both glycosidic and mixed glyco‐phospho head groups with tetraether cores, having 0–4 rings. Archaeal IPL contributions increase with increasing temperature and comprise up to one‐fourth of the total IPL inventory at >84 °C. At elevated temperatures, bacterial IPLs contain abundant glycosidic glycerol diether lipids. Diether and diacylglycerol (DAG) lipids with aminopentanetetrol and phosphatidylinositol head groups were identified as lipids diagnostic of Aquificales, while DAG glycolipids and glyco‐phospholipids containing N‐acetylgycosamine as head group were assigned to members of the Thermales. With decreasing temperature and concomitant changes in water chemistry, IPLs typical of phototrophic bacteria, such as mono‐, diglycosyl, and sulfoquinovosyl DAG, which are specific for cyanobacteria, increase in abundance, consistent with genomic data from the same samples. Compound‐specific stable carbon isotope analysis of IPL breakdown products reveals a large isotopic diversity among SBCs in different hot springs. At two of the hot springs, ‘Bison Pool’ and Flat Cone, lipids derived from Aquificales are enriched in ¹³C relative to biomass and approach values close to dissolved inorganic carbon (DIC) (approximately 0‰), consistent with fractionation during autotrophic carbon fixation via the reversed tricarboxylic acid pathway. At a third site, Octopus Spring, the same Aquificales‐diagnostic lipids are 10‰ depleted relative to biomass and resemble stable carbon isotope values of dissolved organic carbon (DOC), indicative of heterotrophy. Other bacterial and archaeal lipids show a similar variance, with values resembling the DIC or DOC pool or a mixture thereof. This variance cannot be explained by hot spring chemistry or temperature alone, but instead, we argue that intermittent input of exogenous organic carbon can result in metabolic shifts of the chemotrophic communities from autotrophy to heterotrophy and vice versa.     

Genetic Diversity among Thermophilic Bacteria Isolated from Geothermal Sites by Using Two PCR Typing Methods

Microbial communities thriving at two hot springs, Hammam Pharaon (Pharaoh's Bath) and Oyoun Mossa (Moses springs), in Egypt was studied by cultural and molecular methods. Thirteen morphologically distinct strains of facultative anaerobic thermophilic bacterial isolates have been characterized and identified using phenotypic and genotypic characters including RAPD-PCR, ERIC-PCR typing, plasmid analysis and 16S rRNA sequencing. All isolates produced plasmid DNA with various sizes ranging from 0.7 kb to a larger plasmid 7.2 kb. The bacterial strains could tolerate a temperature range between 45 to 85°C and a pH between 4–11. Also, sulphate-reducing bacteria (SRB) in the thermal springs were investigated with combined biochemical and molecular approaches. A sulphate-reducing bacteria medium containing lactate was used for enrichment and isolation, which yielded Gram negative, rod shaped, anaerobic, non-spore-forming and motile bacteria capable of reducing sulphate to sulphide. These grew at temperatures ranging from 30 to 50°C and could use pyruvate, lactate and ethanol as electron donors. The dissimilatory sulphite reductase (DSR) gene sequences of eleven representative isolates revealed that the strains belonged to the sulphur reducing bacterial species Desulfovibrio vulgaris. 16S rRNA gene partial sequence results indicated the presence of novel or existing species of Bacillus (one species), Anoxybacillus (four species) and Geobacillus (eight species). In this study phenotypic and genotypic diversity were applied for the first time to differentiate thermophilic bacteria of such geothermal sites in Sinai, Egypt.     

Influence of Sulfide and Temperature on Species Composition and Community Structure of Hot Spring Microbial Mats

In solfataric fields in southwestern Iceland, neutral and sulfide-rich hot springs are characterized by thick bacterial mats at 60 to 80°C that are white or yellow from precipitated sulfur (sulfur mats). In low-sulfide hot springs in the same area, grey or pink streamers are formed at 80 to 90°C, and a Chloroflexus mat is formed at 65 to 70°C. We have studied the microbial diversity of one sulfur mat (high-sulfide) hot spring and one Chloroflexus mat (low-sulfide) hot spring by cloning and sequencing of small-subunit rRNA genes obtained by PCR amplification from mat DNA. Using 98% sequence identity as a cutoff value, a total of 14 bacterial operational taxonomic units (OTUs) and 5 archaeal OTUs were detected in the sulfur mat; 18 bacterial OTUs were detected in the Chloroflexus mat. Although representatives of novel divisions were found, the majority of the sequences were >95% related to currently known sequences. The molecular diversity analysis showed that Chloroflexus was the dominant mat organism in the low-sulfide spring (1 mg liter⁻¹) below 70°C, whereas Aquificales were dominant in the high-sulfide spring (12 mg liter⁻¹) at the same temperature. Comparison of the present data to published data indicated that there is a relationship between mat type and composition of Aquificales on the one hand and temperature and sulfide concentration on the other hand.     

Actinobacterial Diversity in Hot Springs in Tengchong (China), Kamchatka (Russia), and Nevada (USA)

Actinobacterial diversity was investigated in three hot springs [Tengchong Frog Mouth (TFM) hot spring (in Tengchong, China), Kamchatka Robb Flag hot spring (in Kamchatka, Russia), and Nevada Boiling Spring (in Nevada, USA)], a Tengchong Frog Mouth hot spring-derived pond and a soil sample near the TFM hot spring. Culture-independent techniques were employed including denaturing gradient gel electrophoresis and actinobacterial 16S rRNA gene phylogenetic analysis. The three hot springs and the hot spring-derived pond had pH of 6.8 to 7.9 and temperature of 50 to 81°C. Actinobacteria were for the first time found to be very diverse in hot springs with temperature up to 81°C, indicating that they have an unexpected capability of adapting to hot spring environments. A total of 346 actinobacterial clones were obtained from the three hot springs, and these clones were identified as 31 RFLP types, falling into the Actinomycetales (only limit to the Frankineae suborder), the Rubrobacterales, uncultured Candidatus Microthrix, unclassified Actinobacteria, and uncultured Candidate Division OP10. Our data have implications for a better understanding of the distribution of Actinobacteria in hot springs.     

Bacterial composition of microbial mats in hot springs in Northern Patagonia: variations with seasons and temperature

Seasonal shifts in bacterial diversity of microbial mats were analyzed in three hot springs (39?C68 °C) of Patagonia, using culture-independent methods. Three major bacterial groups were detected in all springs: Phyla Cyanobacteria and Bacteroidetes, and Order Thermales. Proteobacteria, Acidobacteria and Green Non-Sulfur Bacteria were also detected in small amounts and only in some samples. Thermophilic filamentous heterocyst-containing Mastigocladus were dominant Cyanobacteria in Porcelana Hot Spring and Geyser, and Calothrix in Cahuelmó, followed by the filamentous non-heterocyst Leptolyngbya and Oscillatoria. Bacteroidetes were detected in a wide temperature range and their relative abundance increased with decreasing temperature in almost all samples. Two Meiothermus populations with different temperature optima were found. Overall, fingerprinting analysis with universal bacterial primers showed high similarities within each hot spring despite differences in temperature. On the other hand, Cahuelmó Hot Spring showed a lower resemblance among samples. Porcelana Hot Spring and Porcelana Geyser were rather similar to each other, possibly due to a common geological substrate given their geographic proximity. This was even more evident with specific cyanobacterial primers. The different geological substrate and the seawater influence in Cahuelmó might have caused the differences in the microbial community structure with the other two hot springs.     

Actinobacterial Diversity in Microbial Mats of Five Hot Springs in Central and Central-Eastern Tibet,China

The diversity and community composition of Actinobacteria in microbial mats of five Tibetan hot springs (temperatures 26°C to 81°C) and a sympatric soil were investigated with 16S rRNA gene phylogentic analysis. A total of 278 clones were obtained. The actinobacterial communities in the Tibetan hot springs were diverse, and most of the retrieved clones were affiliated with Actinobacteridae, Acidimicrobidae, and unclassified Actinobacteria. The Actinobacteridae sequences were distributed into seven suborders (e.g., Frankineae, Corynebacterineae, Micromonosporineae, Pseudonocardineae, Propionibacterineae, Micrococcineae, and Actinomycineae) and unclassified Actinobacteridae. The actinobacterial composition varied among different hot springs. Statistical analysis showed that the actinobacterial diversity in the investigated Tibetan hot springs was not significantly correlated with temperature, suggesting that temperature is not a key factor in shaping the actinobacterial diversity in hot springs.     

Influence of sulfide and temperature on species composition and community structure of hot spring microbial mats

In solfataric fields in southwestern Iceland, neutral and sulfide-rich hot springs are characterized by thick bacterial mats at 60 to 80 degrees C that are white or yellow from precipitated sulfur (sulfur mats). In low-sulfide hot springs in the same area, grey or pink streamers are formed at 80 to 90 degrees C, and a Chloroflexus mat is formed at 65 to 70 degrees C. We have studied the microbial diversity of one sulfur mat (high-sulfide) hot spring and one Chloroflexus mat (low-sulfide) hot spring by cloning and sequencing of small-subunit rRNA genes obtained by PCR amplification from mat DNA. Using 98% sequence identity as a cutoff value, a total of 14 bacterial operational taxonomic units (OTUs) and 5 archaeal OTUs were detected in the sulfur mat; 18 bacterial OTUs were detected in the Chloroflexus mat. Although representatives of novel divisions were found, the majority of the sequences were >95% related to currently known sequences. The molecular diversity analysis showed that Chloroflexus was the dominant mat organism in the low-sulfide spring (1 mg liter(-1)) below 70 degrees C, whereas Aquificales were dominant in the high-sulfide spring (12 mg liter(-1)) at the same temperature. Comparison of the present data to published data indicated that there is a relationship between mat type and composition of Aquificales on the one hand and temperature and sulfide concentration on the other hand.     

Bacterial Diversity and Functional Activity of Microbial Communities in Hot Springs of the Baikal Rift Zone

In this study the bacterial diversity of thermophilic microbial mats (40 to 65°C) in three alkaline hot springs of the Baikal Rift Zone (BRZ) was determined through pyrosequencing of 16S rRNA gene libraries. Significant diversity of bacterial species was found in the biomats of the hot springs with total number of detected phylotypes of 607. The highest share of the microbial community was represented by the phyla Chloroflexi (Seya Spring, 76.4%), Deinococcus-Thermus (Alla Spring, 45.1%), Nitrospira (Alla Spring, 36.1%), Cyanobacteria (Tsenkher Spring, 33.1%), and Proteobacteria (Tsenkher Spring, 22.6%), but their ratio varied significantly in different springs. A comparison of the biodiversity and composition of microbial communities between hot springs showed a decrease in biodiversity with increasing temperature. A large number of sequences showed a low degree of similarity with cultivated representatives in public databases. Microbial communities showed intensive rates of production and destruction of organic compounds, as revealed by the quantitative assessment of their functional activity.     

Ribosomal Tag Pyrosequencing of DNA and RNA Reveals “Rare” Taxa with High Protein Synthesis Potential in the Sediment of a Hypersaline Lake in Western Australia

Little is known about the potential activity of microbial communities in hypersaline sediment ecosystems. Ribosomal tag libraries of DNA and RNA extracted from the sediment of Lake Strawbridge (Western Australia) revealed bacterial and archaeal operational taxonomic units (OTUs) with high RNA/DNA ratios providing evidence for the presence of ‘rare’ but potentially “active” taxa. Among the ‘rare’ bacterial taxa Halomonas, Salinivibrio and Idiomarina showed the highest protein synthesis potential. Rare but ‘active’ archaeal OTUs were related to the KTK 4A cluster and the Marine-Benthic-Groups B and D. We present the first molecular analysis of the microbial diversity and protein synthesis potential of rare microbial taxa in a hypersaline sediment ecosystem.