Environmental Factors Affect Acidobacterial Communities below the Subgroup Level in Grassland and Forest Soils

In soil, Acidobacteria constitute on average 20% of all bacteria, are highly diverse, and are physiologically active in situ. However, their individual functions and interactions with higher taxa in soil are still unknown. Here, potential effects of land use, soil properties, plant diversity, and soil nanofauna on acidobacterial community composition were studied by cultivation-independent methods in grassland and forest soils from three different regions in Germany. The analysis of 16S rRNA gene clone libraries representing all studied soils revealed that grassland soils were dominated by subgroup Gp6 and forest soils by subgroup Gp1 Acidobacteria. The analysis of a large number of sites (n = 57) by 16S rRNA gene fingerprinting methods (terminal restriction fragment length polymorphism [T-RFLP] and denaturing gradient gel electrophoresis [DGGE]) showed that Acidobacteria diversities differed between grassland and forest soils but also among the three different regions. Edaphic properties, such as pH, organic carbon, total nitrogen, C/N ratio, phosphorus, nitrate, ammonium, soil moisture, soil temperature, and soil respiration, had an impact on community composition as assessed by fingerprinting. However, interrelations with environmental parameters among subgroup terminal restriction fragments (T-RFs) differed significantly, e.g., different Gp1 T-RFs correlated positively or negatively with nitrogen content. Novel significant correlations of Acidobacteria subpopulations (i.e., individual populations within subgroups) with soil nanofauna and vascular plant diversity were revealed only by analysis of clone sequences. Thus, for detecting novel interrelations of environmental parameters with Acidobacteria, individual populations within subgroups have to be considered.     

Comparison of Bacterial and Fungal Communities Between Natural and Planted Pine Forests in Subtropical China

To improve our understanding of the changes in bacterial and fungal diversity in natural pine and planted forests in subtropical region of China, we examined bacterial and fungal communities from a native and a nearby planted pine forest of the Mt. Lushan by constructing clone libraries of 16S and 18S rRNA genes. For bacterial communities, Proteobacteria and Acidobacteria were dominant bacterial taxa in both two types of forest soils. The Shannon–Wiener diversity index, rarefaction curve analysis, and LibShuff analysis suggest that these two forests contained similar diversity of bacterial communities. Low soil acidity (pH ≈ 4) of our study forests might be one of the most important selection factors determining growth of acidophilic Acidobacteria and Proteobacteria. However, the natural forest harbored greater level of fungal diversity than the planted forest according to the Shannon–Wiener diversity index and rarefaction curve analysis. Basidiomycota and Ascomycota were dominant fungal taxa in the soils of natural and planted forests, respectively. Our results suggest that fungal community was more sensitive than the bacterial community in characterizing the differences in plant cover impacts on the microbial flora in the natural and planted forests. The natural and planted forests may function differently due to the differences in soil fungal diversity and relative abundance.     

Characterization of methanogenic and prokaryotic assemblages based on mcrA and 16S rRNA gene diversity in sediments of the Kazan mud volcano (Mediterranean Sea)

The diversity of the methyl‐coenzyme reductase A (mcrA) and 16S rRNA genes was investigated in gas hydrate containing sediment from the Kazan mud volcano, eastern Mediterranean Sea. mcrA was detected only at 15 and 20 cm below seafloor (cmbsf) from a 40‐cm long push core, while based on chemical profiles of methane, sulfate, and sulfide, possible anaerobic oxidation of methane (AOM) depth was inferred at 12–15 cmbsf. The phylogenetic relationships of the obtained mcrA, archaeal and bacterial 16S rRNA genes, showed that all the found sequences were found in both depths and at similar relative abundances. mcrA diversity was low. All sequences were related to the Methanosarcinales, with the most dominant (77.2%) sequences falling in group mcrA‐e. The 16S rRNA‐based archaeal diversity also revealed low diversity and clear dominance (72.8% of all archaeal phylotypes) of the Methanosarcinales and, in particular, ANME‐2c. Bacteria showed higher diversity but 83.2% of the retrieved phylotypes from both sediment layers belonged to the δ‐Proteobacteria. These phylotypes fell in the SEEP‐SRB1 putative AOM group. In addition, the rest of the less abundant phylotypes were related to yet‐uncultivated representatives of the Actinobacteria, Spirochaetales, and candidate divisions OP11 and WS3 from gas hydrate‐bearing habitats. These phylotype patterns indicate that AOM is occurring in the 15 and 20 cmbsf sediment layers.     

Salinity controls soil microbial community structure and function in coastal estuarine wetlands

Soil salinity acts as a critical environmental filter on microbial communities, but the consequences for microbial diversity and biogeochemical processes are poorly understood. Here, we characterized soil bacterial communities and microbial functional genes in a coastal estuarine wetland ecosystem across a gradient (~5 km) ranging from oligohaline to hypersaline habitats by applying the PCR-amplified 16S rRNA (rRNA) genes sequencing and microarray-based GeoChip 5.0 respectively. Results showed that saline soils in marine intertidal and supratidal zone exhibited higher bacterial richness and Faith's phylogenetic diversity than that in the freshwater-affected habitats. The relative abundance of taxa assigned to Gammaproteobacteria, Bacteroidetes and Firmicutes was higher with increasing salinity, while those affiliated with Acidobacteria, Chloroflexi and Cyanobacteria were more prevalent in wetland soils with low salinity. The phylogenetic inferences demonstrated the deterministic role of salinity filtering on the bacterial community assembly processes. The abundance of most functional genes involved in carbon degradation and nitrogen cycling correlated negatively with salinity, except for the hzo gene, suggesting a critical role of the anammox process in tidal affected zones. Overall, the salinity filtering effect shapes the soil bacterial community composition, and soil salinity act as a critical inhibitor in the soil biogeochemical processes in estuary ecosystems.     

Pyrosequencing-based assessment of bacterial community structure along different management types in German forest and grassland soils

Background

Soil bacteria are important drivers for nearly all biogeochemical cycles in terrestrial ecosystems and participate in most nutrient transformations in soil. In contrast to the importance of soil bacteria for ecosystem functioning, we understand little how different management types affect the soil bacterial community composition.

Methodology/Principal Findings

We used pyrosequencing-based analysis of the V2-V3 16S rRNA gene region to identify changes in bacterial diversity and community structure in nine forest and nine grassland soils from the Schwäbische Alb that covered six different management types. The dataset comprised 598,962 sequences that were affiliated to the domain Bacteria. The number of classified sequences per sample ranged from 23,515 to 39,259. Bacterial diversity was more phylum rich in grassland soils than in forest soils. The dominant taxonomic groups across all samples (>1% of all sequences) were Acidobacteria, Alphaproteobacteria, Actinobacteria, Betaproteobacteria, Deltaproteobacteria, Gammaproteobacteria, and Firmicutes. Significant variations in relative abundances of bacterial phyla and proteobacterial classes, including Actinobacteria, Firmicutes, Verrucomicrobia, Cyanobacteria, Gemmatimonadetes and Alphaproteobacteria, between the land use types forest and grassland were observed. At the genus level, significant differences were also recorded for the dominant genera Phenylobacter, Bacillus, Kribbella, Streptomyces, Agromyces, and Defluviicoccus. In addition, soil bacterial community structure showed significant differences between beech and spruce forest soils. The relative abundances of bacterial groups at different taxonomic levels correlated with soil pH, but little or no relationships to management type and other soil properties were found.

Conclusions/Significance

Soil bacterial community composition and diversity of the six analyzed management types showed significant differences between the land use types grassland and forest. Furthermore, bacterial community structure was largely driven by tree species and soil pH.     

Comparison of Soil Bacterial Communities of Pinus patula of Nilgiris, Western Ghats with Other Biogeographically Distant Pine Forest Clone Libraries

The bacterial community structure of the rhizosphere and non-rhizosphere soil of Pinus patula, found in the Nilgiris region of Western Ghats, was studied by constructing 16S rRNA gene clone libraries. In the rhizosphere and non-rhizosphere soil clone libraries constructed, 13 and 15 bacterial phyla were identified, respectively. The clone libraries showed the predominance of members of culturally underrepresented phyla like Acidobacteria and Verrucomicrobia. The Alphaproteobacteria and Acidobacteria clones were predominant in rhizosphere and non-rhizosphere soil samples, respectively. In rhizosphere, amongst Alphaproteobacteria members, Bradyrhizobium formed the significant proportion, whereas in non-rhizosphere, members of subdivision-6 of phylum Acidobacteria were abundant. The diversity analysis of P. patula soil libraries showed that the phylotypes (16S rRNA gene similarity cutoff, ≥97 %) of Acidobacteria and Bacteroidetes were relatively predominant and diverse followed by Alphaproteobacteria and Verrucomicrobia. The diversity indices estimated higher richness and abundance of bacteria in P. patula soil clone libraries than the pine forest clone libraries retrieved from previous studies. The tools like principal co-ordinate analysis and Jackknife cluster analysis, which were under UniFrac analysis indicated that variations in soil bacterial communities were attributed to their respective geographical locations due to the phylogenetic divergence amongst the clone libraries. Overall, the P. patula rhizosphere and non-rhizosphere clone libraries were found significantly unique in composition, evenly distributed and highly rich in phylotypes, amongst the biogeographically distant clone libraries. It was finally hypothesised that the phylogenetic divergence amongst the bacterial phylotypes and natural selection plays a pivotal role in the variations of bacterial communities across the geographical distance.     

Molecular characterization of bacterial population in the forest soil of Kashmir,India

The bacterial diversity in the forest soil of Kashmir, India was investigated by 16S rDNA-dependent molecular phylogeny. Small subunit rRNA (16S rDNA) from forest soil metagenome were amplified by polymerase chain reaction (PCR) using primers specific to the domain bacteria. 30 unique phylotypes were obtained by PCR based RFLP of 16S rRNA genes using endonucleases Hae 111 and Msp 1, which were most suitable to score the genetic diversity. The use of 16S rRNA analysis allowed identification of several bacterial populations in the soil belonging to the following phyla: Firmicutes (33.3%), Bacteroidetes (13.3%), Proteobacterium (6.6%), Planctomycete (3.3%), and Deferribacteraceae (3.3%) in addition to the others that were not classified, beyond Archaea domain, However, 36.6% of the retrieved bacterial sequences could not be grouped with any phylum/lineage. The large amount of unclassified clone sequence could imply that novel groups of bacteria were present in the forest soil.     

水热增加下黑土细菌群落共生网络特征

黑土是有机质含量高且肥沃的土壤类型之一,气候变化会显著改变黑土中微生物群落的结构,同时影响群落间的潜在相互作用关系。[目的] 揭示水热增加对黑土中的细菌群落结构及潜在互作关系的影响。[方法] 基于土壤移置试验,采用16S rRNA高通量测序解析农田黑土（原位黑土、水热增加1和水热增加2）中的细菌群落结构对水热增加的响应;使用CoNet构建微生物群落共生网络,识别共生网络中的枢纽微生物;利用结构方程模型、相关性分析探究水热条件变化下土壤性质、微生物交互作用、多样性之间的直接、间接关系。[结果] 黑土中的微生物以疣微菌、变形杆菌、酸性杆菌和放线菌为主。水热增加下土壤微生物共生网络的拓扑性质发生显著变化,网络中表征微生物潜在竞争关系的负连线随着水热增加而显著增加。气候因素通过改变微生物潜在相互作用影响了群落水平分类多样性。物种竞争增强可能直接导致了土壤有机碳含量的降低。[结论] 水热增加会显著改变黑土中微生物之间的潜在交互作用,枢纽微生物的响应更加敏感。     

Diversity of prokaryotes associated with soils around coal-fire gas vents in MaNasi county of Xinjiang, China

Bacterial and archaeal diversity in surface soils of three coal-fire vents was investigated by T-RFLP analysis and clone libraries of 16S rRNA genes. Soil analysis showed that underground coal fires significantly influenced soil pH, moisture and NO₃ ^? content but had little effect on other elements, organic matter and available nutrients. Hierarchical cluster analysis showed that bacterial community patterns in the soils were very similar, but abundance varied with geographic distance. A clone library from one soil showed that the bacterial community was mainly composed of Firmicutes, Proteobacteria, Acidobacteria, Bacteroidetes, Planctomycetes, Actinobacteria, and unidentified groups. Of these, Firmicutes was the most abundant, accounting for 71.4 % of the clones, and was mainly represented by the genera Bacillus and Paenibacillus. Archaeal phylotypes were closely related to uncultivated species of the phyla Crenarchaeota (97.9 % of clones) and Thaumarchaeota (2.1 %). About 28 % of archaeal phylotypes were associated with ammonia oxidization, especially phylotypes that were highly related to a novel, ammonia-oxidizing isolate from the phylum Thaumarchaeota. These results suggested that microbial communities in the soils were diverse and might contain a large number of novel cultivable species with the potential to assimilate materials by heterotrophic metabolism at high temperature.     

Bacterial Community Diversity in the Brazilian Atlantic Forest Soils

The aim of this study was to characterize the bacterial community diversity of the Brazilian Atlantic forest soil by means of both cultivation and 16S rRNA clone libraries. A collection of 86 representative isolates, obtained from six samples of Atlantic forest soils from the National Park of Serra dos Órgãos (PARNASO), belonged to the genera Arthrobacter, Bacillus, Burkholderia, Leifsonia, Paenibacillus, Pseudomonas, Ralstonia, Serratia, and Streptomyces according to the 16S rRNA sequences. Representative isolates from the different genera degraded cellulose and lignin. The culture-independent analysis based on 894 partial 16S rRNA gene sequences revealed that the most frequently retrieved groups belonged to the phyla Acidobacteria (29–54%), Proteobacteria (16–38%), and Verrucomicrobia (0.6–14%). The majority of the sequences (82.6%) were unidentified singletons and doubletons, indicating a high diversity of rare unique sequences. Chao1 estimator disclosed a high number of phyla (41–152) and species (263–446). This is the first survey on the Atlantic Forest soils using a combination of cultivation and culture-independent approaches. We conclude that the Brazilian Atlantic Forest soil represents a vast source of novel bacteria.     

An Integrated Study to Analyze Soil Microbial Community Structure and Metabolic Potential in Two Forest Types

Soil microbial metabolic potential and ecosystem function have received little attention owing to difficulties in methodology. In this study, we selected natural mature forest and natural secondary forest and analyzed the soil microbial community and metabolic potential combing the high-throughput sequencing and GeoChip technologies. Phylogenetic analysis based on 16S rRNA sequencing showed that one known archaeal phylum and 15 known bacterial phyla as well as unclassified phylotypes were presented in these forest soils, and Acidobacteria, Protecobacteria, and Actinobacteria were three of most abundant phyla. The detected microbial functional gene groups were related to different biogeochemical processes, including carbon degradation, carbon fixation, methane metabolism, nitrogen cycling, phosphorus utilization, sulfur cycling, etc. The Shannon index for detected functional gene probes was significantly higher (P<0.05) at natural secondary forest site. The regression analysis showed that a strong positive (P<0.05) correlation was existed between the soil microbial functional gene diversity and phylogenetic diversity. Mantel test showed that soil oxidizable organic carbon, soil total nitrogen and cellulose, glucanase, and amylase activities were significantly linked (P<0.05) to the relative abundance of corresponded functional gene groups. Variance partitioning analysis showed that a total of 81.58% of the variation in community structure was explained by soil chemical factors, soil temperature, and plant diversity. Therefore, the positive link of soil microbial structure and composition to functional activity related to ecosystem functioning was existed, and the natural secondary forest soil may occur the high microbial metabolic potential. Although the results can''t directly reflect the actual microbial populations and functional activities, this study provides insight into the potential activity of the microbial community and associated feedback responses of the terrestrial ecosystem to environmental changes.     

辣椒连作对土壤细菌群落的影响

【目的】土壤微生物对农业生态系统的长期可持续性至关重要。为探讨不同连作年限对辣椒土壤细菌群落结构和潜在功能的影响。【方法】采用16S rRNA基因高通量测序PICRUSt功能预测相结合的研究方法,对不同连作年限下(1Y、3Y、5Y和10Y)的辣椒土壤细菌微生物群落结构和功能进行分析。【结果】微生物多样性指数和共生网络复杂度随连作年限的延长而降低,同时,连作年限变化对细菌群落组成有显著影响。不同的土壤细菌种群对连作措施的响应程度不一,长期连作增加了变形菌门和拟杆菌门的相对丰度,但降低了绿弯菌门、酸杆菌门、厚壁菌门和髌骨细菌门的相对丰度。PICRUSt功能预测结果表明,延长连作年限改变了土壤细菌整体的氮、磷代谢能力,导致细菌群预测功能基因发生了变化,能量代谢、氨基酸代谢和碳水化合物代谢等重要代谢功能基因减少,而折叠、分类和降解、复制和修复、膜转运、细胞生长与死亡等功能基因丰度明显增加。冗余分析表明,土壤有机质和有效磷是影响细菌群落迁移和功能变化的关键土壤理化因子。【结论】延长辣椒连作年限后,细菌群落结构改变和多样性下降导致土壤微生物群落功能失调可能是造成辣椒连作障碍的原因之一。     

Examining the global distribution of dominant archaeal populations in soil

Archaea, primarily Crenarchaeota, are common in soil; however, the structure of soil archaeal communities and the factors regulating their diversity and abundance remain poorly understood. Here, we used barcoded pyrosequencing to comprehensively survey archaeal and bacterial communities in 146 soils, representing a multitude of soil and ecosystem types from across the globe. Relative archaeal abundance, the percentage of all 16S rRNA gene sequences recovered that were archaeal, averaged 2% across all soils and ranged from 0% to >10% in individual soils. Soil C:N ratio was the only factor consistently correlated with archaeal relative abundances, being higher in soils with lower C:N ratios. Soil archaea communities were dominated by just two phylotypes from a constrained clade within the Crenarchaeota, which together accounted for >70% of all archaeal sequences obtained in the survey. As one of these phylotypes was closely related to a previously identified putative ammonia oxidizer, we sampled from two long-term nitrogen (N) addition experiments to determine if this taxon responds to experimental manipulations of N availability. Contrary to expectations, the abundance of this dominant taxon, as well as archaea overall, tended to decline with increasing N. This trend was coupled with a concurrent increase in known N-oxidizing bacteria, suggesting competitive interactions between these groups.     

三种蓝莓根际细菌的分离及其对蓝莓苗生长发育的影响

【目的】从3种蓝莓根际土壤中分离细菌,探究蓝莓根际土壤细菌多样性,并筛选具有产酸、促生长、抑菌性能的菌株,为蓝莓专用微生物肥料的研究提供优质菌株资源和理论基础。【方法】选用5种培养基分离3种蓝莓根际土壤细菌,并进行16S rRNA基因测序和系统发育分析。筛选产酸、产吲哚-3-乙酸（indole-3-acetic acid,IAA）和铁载体、固氮、溶磷和抑制灰葡萄孢生长的菌株,挑选最适菌株制备菌剂进行蓝莓苗盆栽实验验证促生能力,并检测菌剂对蓝莓元素吸收和根际土壤肥力的影响。【结果】从3种蓝莓根际土壤分离得到124株细菌,挑选70株代表性菌株进行16S rRNA基因测序,分布于3个门21个属,其中芽孢杆菌属（Bacillus）、假单胞菌属（Pseudomonas）、链霉菌属（Streptomyces）和红球菌属（Rhodococcus）为优势分离菌群。代表性菌株中,21.4%的菌株能产酸,21.4%的菌株产吲哚-3-乙酸,47.1%的菌株具有固氮潜力,65.7%的菌株具有解磷能力,14.3%的菌株能产铁载体。少量菌株同时具有产酸、产IAA、固氮、解磷和抑菌等能力。选取具有产酸和多种促生特征的菌株绿针假单胞菌CSM-70和双鱼假单胞菌CSM-129进行盆栽蓝莓苗处理,发现2株菌均能显著促进蓝莓苗的生长发育并调控根际土壤pH,其中菌株CSM-70处理还显著促进了蓝莓叶片氮、磷元素的吸收,提升了土壤速效钾、碱解氮的含量。【结论】蓝莓根际细菌多样性高且蕴藏着丰富的促生长菌株,绿针假单胞菌CSM-70和双鱼假单胞菌CSM-129能够促进蓝莓苗生长、调控根际土壤pH和肥力,并促进植株养分吸收,具有蓝莓专用微生物菌剂研制与应用的潜力。     

Soil microbiome responses to the short‐term effects of Amazonian deforestation

Slash‐and‐burn clearing of forest typically results in increase in soil nutrient availability. However, the impact of these nutrients on the soil microbiome is not known. Using next generation sequencing of 16S rRNA gene and shotgun metagenomic DNA, we compared the structure and the potential functions of bacterial community in forest soils to deforested soils in the Amazon region and related the differences to soil chemical factors. Deforestation decreased soil organic matter content and factors linked to soil acidity and raised soil pH, base saturation and exchangeable bases. Concomitant to expected changes in soil chemical factors, we observed an increase in the alpha diversity of the bacterial microbiota and relative abundances of putative copiotrophic bacteria such as Actinomycetales and a decrease in the relative abundances of bacterial taxa such as Chlamydiae, Planctomycetes and Verrucomicrobia in the deforested soils. We did not observe an increase in genes related to microbial nutrient metabolism in deforested soils. However, we did observe changes in community functions such as increases in DNA repair, protein processing, modification, degradation and folding functions, and these functions might reflect adaptation to changes in soil characteristics due to forest clear‐cutting and burning. In addition, there were changes in the composition of the bacterial groups associated with metabolism‐related functions. Co‐occurrence microbial network analysis identified distinct phylogenetic patterns for forest and deforested soils and suggested relationships between Planctomycetes and aluminium content, and Actinobacteria and nitrogen sources in Amazon soils. The results support taxonomic and functional adaptations in the soil bacterial community following deforestation. We hypothesize that these microbial adaptations may serve as a buffer to drastic changes in soil fertility after slash‐and‐burning deforestation in the Amazon region.     

Seasonal and spatial diversity of microbial communities in marine sediments of the South China Sea

This study was conducted to characterize the diversity of microbial communities in marine sediments of the South China Sea by means of 16S rRNA gene clone libraries. The results revealed that the sediment samples collected in summer harboured a more diverse microbial community than that collected in winter, Deltaproteobacteria dominated 16S rRNA gene clone libraries from both seasons, followed by Gammaproteobacteria, Acidobacteria, Nitrospirae, Planctomycetes, Firmicutes. Archaea phylotypes were also found. The majority of clone sequences shared greatest similarity to uncultured organisms, mainly from hydrothermal sediments and cold seep sediments. In addition, the sedimentary microbial communities in the coastal sea appears to be much more diverse than that of the open sea. A spatial pattern in the sediment samples was observed that the sediment samples collected from the coastal sea and the open sea clustered separately, a novel microbial community dominated the open sea. The data indicate that changes in environmental conditions are accompanied by significant variations in diversity of microbial communities at the South China Sea.     

Recovery of microbial diversity and activity during bioremediation following chemical oxidation of diesel contaminated soils

To improve the coupling of in situ chemical oxidation and in situ bioremediation, a systematic analysis was performed of the effect of chemical oxidation with Fenton's reagent, modified Fenton's reagent, permanganate, or persulfate, on microbial diversity and activity during 8 weeks of incubation in two diesel-contaminated soils (peat and fill). Chemical oxidant and soil type affected the microbial community diversity and biodegradation activity; however, this was only observed following treatment with Fenton's reagent and modified Fenton's reagent, and in the biotic control without oxidation. Differences in the highest overall removal efficiencies of 69 % for peat (biotic control) and 59 % for fill (Fenton's reagent) were partially explained by changes in contaminant soil properties upon oxidation. Molecular analysis of 16S rRNA and alkane monooxygenase (alkB) gene abundances indicated that oxidation with Fenton's reagent and modified Fenton's reagent negatively affected microbial abundance. However, regeneration occurred, and final relative alkB abundances were 1–2 orders of magnitude higher in chemically treated microcosms than in the biotic control. 16S rRNA gene fragment fingerprinting with DGGE and prominent band sequencing illuminated microbial community composition and diversity differences between treatments and identified a variety of phylotypes within Alpha-, Beta-, and Gammaproteobacteria. Understanding microbial community dynamics during coupled chemical oxidation and bioremediation is integral to improved biphasic field application.     

Soil pH regulates the abundance and diversity of Group 1.1c Crenarchaeota

Archaeal communities in many acidic forest soil systems are dominated by a distinct crenarchaeal lineage Group 1.1c. In addition, they are found consistently in other acidic soils including grassland pasture, moorland and alpine soils. To determine whether soil pH is a major factor in determining their presence and abundance, Group 1.1c community size and composition were investigated across a pH gradient from 4.5 to 7.5 that has been maintained for > 40 years. The abundances of Group 1.1c Crenarchaeota, total Crenarchaeota and total bacteria were assessed by quantitative PCR (qPCR) targeting 16S rRNA genes and the diversity of Group 1.1c crenarchaeal community was investigated by denaturing gradient gel electrophoresis (DGGE) and phylogenetic analysis. The abundance of Group 1.1c Crenarchaeota declined as the pH increased, whereas total Crenarchaeota and Bacteria showed no clear trend. Community diversity of Group 1.1c Crenarchaeota was also influenced with different DGGE bands dominating at different pH. Group 1.1c Crenarchaeota were also quantified in 13 other soils representing a range of habitats, soil types and pH. These results exhibited the same trend as that shown across the pH gradient with Group 1.1c Crenarchaeota representing a greater proportion of total Crenarchaeota in the most acidic soils.     

Archaeal Microbial Diversity of Hypersaline Lake Acıgöl,Denizli, Turkey

Archaeal diversity in Lake Ac?göl, a closed-basin, alkaline, hypersaline lake located at the northern edge of western Tourides in southwest Anatolia, was investigated using culture-independent methods. Microbial mat samples were collected from six different points. Archaeal 16S rRNA gene libraries were generated using domain specific oligonucleotide primers, and 16S rRNA gene sequences of clone libraries were analyzed phylogenetically. Denaturing gradient gel electrophoresis of 16S rRNA genes showed a variance in diversity with spatial differences. Archaeal diversity of Ac?göl is dominated by the members of family Halobacteriaceae which requires both high salt concentration and high pH for growth. Sequence analysis of archaeal 16s rRNA genes indicates the presence of the phylotypes affiliated with the genera Halorubrum, Halosimplex, Halorhabdus, Haloterrigena and Natronococcus in the analyzed samples.