Diversity and abundance of the arsenite oxidase gene aioA in geothermal areas of Tengchong, Yunnan, China

A total of 12 samples were collected from the Tengchong geothermal areas of Yunnan, China, with the goal to assess the arsenite (AsIII) oxidation potential of the extant microbial communities as inferred by the abundance and diversity of the AsIII oxidase large subunit gene aioA relative to geochemical context. Arsenic concentrations were higher (on average 251.68 μg/L) in neutral or alkaline springs than in acidic springs (on average 30.88 μg/L). aioA abundance ranged from 1.63 × 10¹ to 7.08 × 10³ per ng of DNA and positively correlated with sulfide and the ratios of arsenate (AsV):total dissolved arsenic (As_Tot). Based on qPCR estimates of bacterial and archaeal 16S rRNA gene abundance, aioA-harboring organisms comprised as much as ~15 % of the total community. Phylogenetically, the major aioA sequences (270 total) in the acidic hot springs (pH 3.3–4.4) were affiliated with Aquificales and Rhizobiales, while those in neutral or alkaline springs (pH 6.6–9.1) were inferred to be primarily bacteria related to Thermales and Burkholderiales. Interestingly, aioA abundance at one site greatly exceeded bacterial 16S rRNA gene abundance, suggesting these aioA genes were archaeal even though phylogenetically these aioA sequences were most similar to the Aquificales. In summary, this study described novel aioA sequences in geothermal features geographically far removed from those in the heavily studied Yellowstone geothermal complex.     

Sedimentary arsenite-oxidizing and arsenate-reducing bacteria associated with high arsenic groundwater from Shanyin, Northwestern China

Aims:  Shanyin County is one of the most severe endemic arsenism affected areas in China but micro-organisms that potentially release arsenic from sediments to groundwater have not been studied. Our aim was to identify bacteria with the potential to metabolize or transform arsenic in the sediments.
Methods and Results:  Culture and nonculture-based molecular methods were performed to identify arsenite-oxidizing bacteria, arsenate-reducing bacteria and arsenite oxidase genes. Arsenite-oxidizing bacteria were identified only from the land surface to 7 m underground that were affiliated to α- and β-Proteobacteria. Arsenate-reducing bacteria were found in almost all the sediment samples with different depths (0–41 m) and mainly belong to γ-Proteobacteria. Several novel arsenite oxidase genes ( aoxBs ) were identified from the upper layers of the sediments (0–7 m) and were found to be specific for arsenite-oxidizing bacteria.
Conclusions:  The distribution of arsenite-oxidizing bacteria in upper layers and arsenate-reducing bacteria in different depths of the sediments may impact the arsenic release into the nearby tubewell groundwater.
Significance and Impact of the Study:  This study provides valuable sources of micro-organisms (and genes) that may contribute to groundwater arsenic abnormality and may be useful to clean arsenic contaminated groundwater.     

Bacteria and Genes Involved in Arsenic Speciation in Sediment Impacted by Long-Term Gold Mining

The bacterial community and genes involved in geobiocycling of arsenic (As) from sediment impacted by long-term gold mining were characterized through culture-based analysis of As-transforming bacteria and metagenomic studies of the arsC, arrA, and aioA genes. Sediment was collected from the historically gold mining impacted Mina stream, located in one of the world’s largest mining regions known as the “Iron Quadrangle”. A total of 123 As-resistant bacteria were recovered from the enrichment cultures, which were phenotypically and genotypically characterized for As-transformation. A diverse As-resistant bacteria community was found through phylogenetic analyses of the 16S rRNA gene. Bacterial isolates were affiliated with Proteobacteria, Firmicutes, and Actinobacteria and were represented by 20 genera. Most were AsV-reducing (72%), whereas AsIII-oxidizing accounted for 20%. Bacteria harboring the arsC gene predominated (85%), followed by aioA (20%) and arrA (7%). Additionally, we identified two novel As-transforming genera, Thermomonas and Pannonibacter. Metagenomic analysis of arsC, aioA, and arrA sequences confirmed the presence of these genes, with arrA sequences being more closely related to uncultured organisms. Evolutionary analyses revealed high genetic similarity between some arsC and aioA sequences obtained from isolates and clone libraries, suggesting that those isolates may represent environmentally important bacteria acting in As speciation. In addition, our findings show that the diversity of arrA genes is wider than earlier described, once none arrA-OTUs were affiliated with known reference strains. Therefore, the molecular diversity of arrA genes is far from being fully explored deserving further attention.     

典型生境巨菌草根内生固氮菌的群落多样性

【目的】探究不同生境巨菌草内生固氮菌群落组成多样性及其分异规律。【方法】采用高通量测序固氮酶nif H标靶基因方法,研究了我国6个典型地区的巨菌草内生固氮菌群,包括福建闽侯县、新疆墨玉县、内蒙古阿拉善左旗、青海贵德县、甘肃安定区、海南那大镇,结合地理气候因子统计,分析了固氮菌多样性的环境驱动机制。【结果】共获得64122条nif H基因的有效序列,640个OTUs,归属于6个门、10个纲、17个目、24个科、33个属和39个种。不同地区巨菌草中优势内生固氮菌群的种类和丰度存在较大的差异。在门水平上,福州闽侯县、甘肃安定区、新疆墨玉县、内蒙古阿拉善左旗和青海贵德县5个地区的优势菌门均为变形菌门,海南那大镇的优势菌门为变形菌门和蓝藻菌门;属水平上,不同地区巨菌草最优势内生固氮菌类群分别为:福州闽侯县(变形菌门中未定属,80.56%);新疆墨玉县(变形菌门中未定属,33.14%);内蒙古阿拉善左旗(变形菌门中未定属,76.23%);甘肃安定区(α-变形菌纲中的未定属,53.78%);海南那大镇(变形菌门中未定属,38.37%);青海贵德县(变形菌门中未定属,46.12%)。Alpha多样性和Beta多样性分析表明,不同地区巨菌草内生固氮菌群落的多样性存在较大的差异,海南那大镇样本中巨菌草各类内生固氮菌群的多样性及丰富度最高,福建闽侯县样本中巨菌草各类内生固氮菌群的多样性及丰富度最低。典范对应分析(CCA)结果表明,年均降雨量和年均气温是影响巨菌草内生固氮菌群变化的主要因素,其次是土壤有机质、土壤全氮和土壤p H。【结论】不同地区巨菌草内生固氮菌群落的组成及丰度存在着较大的差异,海南那大镇巨菌草内生固氮菌群的种类及相对丰度较高,本研究可为巨菌草内生固氮菌群的资源开发及其固氮微生物肥料的菌种选育和生产应用提供理论支持。     

Detection, diversity and expression of aerobic bacterial arsenite oxidase genes

The arsenic (As) drinking water crisis in south and south-east Asia has stimulated intense study of the microbial processes controlling the redox cycling of As in soil-water systems. Microbial oxidation of arsenite is a critical link in the global As cycle, and phylogenetically diverse arsenite-oxidizing microorganisms have been isolated from various aquatic and soil environments. However, despite progress characterizing the metabolism of As in various pure cultures, no functional gene approaches have been developed to determine the importance and distribution of arsenite-oxidizing genes in soil-water-sediment systems. Here we report for the first time the successful amplification of arsenite oxidase-like genes (aroA/asoA/aoxB) from a variety of soil-sediment and geothermal environments where arsenite is known to be oxidized. Prior to the current work, only 16 aroA/asoA/aoxB-like gene sequences were available in GenBank, most of these being putative assignments from homology searches of whole genomes. Although aroA/asoA/aoxB gene sequences are not highly conserved across disparate phyla, degenerate primers were used successfully to characterize over 160 diverse aroA-like sequences from 10 geographically isolated, arsenic-contaminated sites and from 13 arsenite-oxidizing organisms. The primer sets were also useful for confirming the expression of aroA-like genes in an arsenite-oxidizing organism and in geothermal environments where arsenite is oxidized to arsenate. The phylogenetic and ecological diversity of aroA-like sequences obtained from this study suggests that genes for aerobic arsenite oxidation are widely distributed in the bacterial domain, are widespread in soil-water systems containing As, and play a critical role in the biogeochemical cycling of As.     

Distribution of Microbial Arsenic Reduction,Oxidation and Extrusion Genes along a Wide Range of Environmental Arsenic Concentrations

The presence of the arsenic oxidation, reduction, and extrusion genes arsC, arrA, aioA, and acr3 was explored in a range of natural environments in northern Chile, with arsenic concentrations spanning six orders of magnitude. A combination of primers from the literature and newly designed primers were used to explore the presence of the arsC gene, coding for the reduction of As (V) to As (III) in one of the most common detoxification mechanisms. Enterobacterial related arsC genes appeared only in the environments with the lowest As concentration, while Firmicutes-like genes were present throughout the range of As concentrations. The arrA gene, involved in anaerobic respiration using As (V) as electron acceptor, was found in all the systems studied. The As (III) oxidation gene aioA and the As (III) transport gene acr3 were tracked with two primer sets each and they were also found to be spread through the As concentration gradient. Sediment samples had a higher number of arsenic related genes than water samples. Considering the results of the bacterial community composition available for these samples, the higher microbial phylogenetic diversity of microbes inhabiting the sediments may explain the increased number of genetic resources found to cope with arsenic. Overall, the environmental distribution of arsenic related genes suggests that the occurrence of different ArsC families provides different degrees of protection against arsenic as previously described in laboratory strains, and that the glutaredoxin (Grx)-linked arsenate reductases related to Enterobacteria do not confer enough arsenic resistance to live above certain levels of As concentrations.     

Abundance and Diversity of Sulfate-Reducing Bacteria in High Arsenic Shallow Aquifers

The abundance, diversity, and relative distribution of sulfate-reducing bacteria (SRB) in high arsenic (As) groundwater aquifers of Hangjinhouqi County in the Hetao Basin, Inner Mongolia was investigated using denaturing gradient gel electrophoresis (DGGE) and quantitative polymerase chain reaction (qPCR) analysis of dsrB genes (encoding dissimilatory sulfite reductase beta-subunit). DGGE results revealed that SRB populations were diverse, but were mainly composed of Desulfotomaculum, Desulfobulbus, Desulfosarcina, and Desulfobacca. The abundance of Desulfobulbus was positively correlated with the ratio of Fe(II)/Fe(III). Although qPCR results showed that the dsrB gene abundance in groundwater samples ranged from below detection to 4.9 × 10⁶ copies/L, and the highest percentage of dsrB gene copies to bacterial 16S rRNA gene copies was 2.1%. Geochemical analyses showed that As(III) content and the ratio of Fe(II) to Fe(III) increased with total As, while sulfate concentrations decreased. Interestingly, the dsrB gene abundance was positively correlated with As concentrations. These results indicate that sulfate reduction occurs simultaneously with As and Fe reduction, and might result in increased As release and mobilization when As is not incorporated into iron sulfides. This study improves our understanding of SRB and As cycling in high As groundwater systems.     

Diversity,abundance, and distribution of NO‐forming nitrite reductase–encoding genes in deep‐sea subsurface sediments of the South China Sea

In marine ecosystems, both nitrite‐reducing bacteria and anaerobic ammonium‐oxidizing (anammox) bacteria, containing different types of NO‐forming nitrite reductase–encoding genes, contribute to the nitrogen cycle. The objectives of study were to reveal the diversity, abundance, and distribution of NO‐forming nitrite reductase–encoding genes in deep‐sea subsurface environments. Results showed that higher diversity and abundance of nirS gene than nirK and Scalindua‐nirS genes were evident in the sediments of the South China Sea (SCS), indicating bacteria containing nirS gene dominated the NO‐forming nitrite‐reducing microbial community in this ecosystem. Similar diversity and abundance distribution patterns of both nirS and Scalindua‐nirS genes were detected in this study sites, but different from nirK gene. Further statistical analyses also showed both nirS and Scalindua‐nirS genes respond similarly to environmental factors, but differed from nirK gene. These results suggest that bacteria containing nirS and Scalindua‐nirS genes share similar niche in deep‐sea subsurface sediments of the SCS, but differed from those containing nirK gene, indicating that community structures of nitrite‐reducing bacteria are segregated by the functional modules (NirS vs. NirK) rather than the competing processes (anammox vs. classical denitrification).     

滇藏热泉arxA基因型厌氧砷氧化原核微生物多样性及其影响因素

【目的】探究滇藏地区热泉沉积物微生物及arxA基因的多样性及其影响因素。【方法】采用Illumina MiSeq高通量测序技术和统计学的分析方法,针对3个滇藏地热区的22个样点,进行地球化学分析及微生物多样性分析,并分析其与环境因子之间的相关性。【结果】沉积物微生物群落主要门类及其丰度占比为Chloroflexi(21.27%)、Deinococcus-Thermus(17.25%)、Aquificae(13.39%)、Proteobacteria(9.27%)、Acetothermia(8.3%)、Bacteroidetes(4.96%)与Crenarchaeota(4.57%);具有arxA基因的微生物主要门类及其丰度占比分别为Proteobacteria(64.87%)、Bipolaricaulota (9.55%)、Deinococcus-Thermus (6.42%)与Crenarchaeota (4.05%);不同地热区优势种群有所差异,主要受温度、pH值、砷浓度、总溶解固体(TDS)及海拔等因素的影响,Mantel检验呈显著相关性(P<0.001)。【结论】沉积物中...     

Distribution and Diversity of Aerobic Carbon Monoxide-Oxidizing Bacteria in Geothermal Springs of China,the Philippines,and the United States

Accumulating genomic evidence suggests that a variety of thermophilic bacteria contain cox operons and may be capable of aerobic carbon monoxide (CO) oxidation. However, little is known about the distribution and diversity of the cox-encoding (COXE) bacteria in natural geothermal environments. In this study, we examined coxL gene (encoding the large subunit of carbon monoxide dehydrogenase: CoxL) sequences retrieved from the sediments of 25 geothermal sites located in the Qinghai-Tibetan Plateau (QTP) and Yunnan Province (YP) of China, the Bacon-Manito Geothermal Production Field (BGPF) of the Philippines, and the Great Basin of the United States (USGB). Temperature and pH ranges of the studied hot springs were 22.1 to 90.8°C and 2.7 to 9.4, respectively. Phylogenetic analyses showed that most CoxL sequences were closely related to the classes Actinobacteria, Deinococci, Ktedonobacteria, Thermomicrobia, and Clostridia, and hot springs from different regions hosted different COXE communities. In addition, these hot springs harbored some COXE bacteria that were phylogenetically distinct from those inhabiting nongeothermal ecosystems. This study revealed no significant correlation between temperature or pH and the composition or diversity of COXE communities at the global scale. However, within a given region, temperature was correlated with the COXE bacterial community composition.     

Arsenite oxidation by a facultative chemolithoautotrophic Sinorhizobium sp. KGO-5 isolated from arsenic-contaminated soil

A chemolithoautotrophic arsenite-oxidizing bacterium, designated strain KGO-5, was isolated from arsenic-contaminated industrial soil. Strain KGO-5 was phylogenetically closely related with Sinorhizobium meliloti with 16S rRNA gene similarity of more than 99%, and oxidized 5?mM arsenite under autotrophic condition within 60?h with a doubling time of 3.0?h. Additions of 0.01–0.1% yeast extract enhanced the growth significantly, and the strain still oxidized arsenite efficiently with much lower doubling times of approximately 1.0?h. Arsenite-oxidizing capacities (11.2–54.1?μmol?h^?1?mg dry cells^?1) as well as arsenite oxidase (Aio) activities (1.76–10.0?mU?mg protein^?1) were found in the cells grown with arsenite, but neither could be detected in the cells grown without arsenite. Strain KGO-5 possessed putative aioA gene, which is closely related with AioA of Ensifer adhaerens. These results suggest that strain KGO-5 is a facultative chemolithoautotrophic arsenite oxidizer, and its Aio is induced by arsenic.     

两种不同生境中国沙棘种子内生细菌的多样性

植物内生菌广泛分布于植物的各种组织及器官中,对植物的生长表现出各种作用,而植物种子中的内生菌对植物的作用也越来越受到人们的关注。以榆中县和秦安县两种不同生境的中国沙棘种子为材料,分析中国沙棘种子内生细菌多样性,以期探究生境对种子内生菌多样性的影响,并为进一步研究种子内生菌与沙棘的相互作用提供依据。研究利用纯培养方法和高通量测序方法分别进行中国沙棘种子内生细菌多样性分析。对纯培养分离得到的内生细菌,利用16S rRNA基因序列分析法结合形态学特征进行内生细菌的鉴定;对高通量测序得到的数据进行基于OTUs(Operational Taxonomic units,可操作分类单元)的物种注释分析。通过纯培养方法从榆中县中国沙棘种子中分离得到4株内生细菌,分属于芽孢杆菌属(Bacillus)、葡萄球菌属(Staphylococcus)和假单胞菌属(Pseudomonas);秦安县中国沙棘种子中分离得到5株内生细菌,分属于芽孢杆菌属(Bacillus)、葡萄球菌属(Staphylococcus)和不动杆菌属(Acinetobacter)。采用高通量测序方法检测到榆中县中国沙棘种子内生细菌分属于7个门、68个属,秦安县中国沙棘种子内生细菌分属于5个门、30个属。在门分类水平,榆中县中国沙棘种子内生细菌的主要优势门类是蓝藻门(Cyanobacteria)和变形菌门(Proteobacteria),相对丰度分别为95.62%和2.03%;秦安县中国沙棘种子的主要优势门类是变形菌门(Proteobacteria)和蓝藻门(Cyanobacteria),相对丰度分别为91.68%和8.06%。在属分类水平,榆中县中国沙棘种子内生细菌的优势菌属为蓝藻细菌属(Cyanobacteria),相对丰度为95.09%;秦安县中国沙棘种子内生细菌的优势菌属为寡养单胞菌属(Stenotrophomonas),相对丰度为85.60%。榆中县和秦安县两种不同生境中国沙棘种子内生细菌有着丰富的多样性,且内生细菌的多样性和丰富度存在明显差异,表现为榆中县中国沙棘种子内生细菌的多样性和丰富度均高于秦安县中国沙棘种子内生细菌。     

Metagenomic Approach Reveals Variation of Microbes with Arsenic and Antimony Metabolism Genes from Highly Contaminated Soil

Microbes have great potential for arsenic (As) and antimony (Sb) bioremediation in heavily contaminated soil because they have the ability to biotransform As and Sb to species that have less toxicity or are more easily removed. In this study, we integrated a metagenomic method with physicochemical characterization to elucidate the composition of microbial community and functional genes (related to As and Sb) in a high As (range from 34.11 to 821.23 mg kg⁻¹) and Sb (range from 226.67 to 3923.07 mg kg⁻¹) contaminated mine field. Metagenomic analysis revealed that microbes from 18 phyla were present in the 5 samples of soil contaminated with high As and Sb. Moreover, redundancy analysis (RDA) of the relationship between the 18 phyla and the concentration of As and Sb demonstrated that 5 phyla of microbes, i.e. Actinobacteria, Firmicutes, Nitrospirae, Tenericutes and Gemmatimonadetes were positively correlated with As and Sb concentration. The distribution, diversity and abundance of functional genes (including arsC, arrA, aioA, arsB and ACR3) were much higher for the samples containing higher As and Sb concentrations. Based on correlation analysis, the results showed a positive relationship between arsC-like (R² = 0.871) and aioA-like (R² = 0.675) gene abundance and As concentration, and indicated that intracellular As(V) reduction and As(III) oxidation could be the dominant As detoxification mechanism enabling the microbes to survive in the environment. This study provides a direct and reliable reference on the diversity of microbial community and functional genes in an extremely high concentration As- and Sb-contaminated environment.     

A single Thaumarchaeon drives nitrification in deep oligotrophic Lake Constance

Ammonia released during organic matter mineralization is converted during nitrification to nitrate. We followed spatiotemporal dynamics of the nitrifying microbial community in deep oligotrophic Lake Constance. Depth-dependent decrease of total ammonium (0.01–0.84 μM) indicated the hypolimnion as the major place of nitrification with ¹⁵N-isotope dilution measurements indicating a threefold daily turnover of hypolimnetic total ammonium. This was mirrored by a strong increase of ammonia-oxidizing Thaumarchaeota towards the hypolimnion (13%–21% of bacterioplankton) throughout spring to autumn as revealed by amplicon sequencing and quantitative polymerase chain reaction. Ammonia-oxidizing bacteria were typically two orders of magnitude less abundant and completely ammonia-oxidizing (comammox) bacteria were not detected. Both, 16S rRNA gene and amoA (encoding ammonia monooxygenase subunit B) analyses identified only one major species-level operational taxonomic unit (OTU) of Thaumarchaeota (99% of all ammonia oxidizers in the hypolimnion), which was affiliated to Nitrosopumilus spp. The relative abundance distribution of the single Thaumarchaeon strongly correlated to an equally abundant Chloroflexi clade CL500-11 OTU and a Nitrospira OTU that was one order of magnitude less abundant. The latter dominated among recognized nitrite oxidizers. This extremely low diversity of nitrifiers shows how vulnerable the ecosystem process of nitrification may be in Lake Constance as Central Europe's third largest lake.     

火棘不同组织内生细菌群落多样性

为了解火棘不同组织内生细菌群落多样性,该研究采用高通量测序技术对火棘内生细菌16S rRNA V5～V7可变区进行测序,分析火棘不同组织部位内生细菌群落多样性。结果表明:(1)从火棘根、茎、叶组织中共获得内生细菌OTU 1 818个,其中根部754个,茎部 308 个,叶部756个,三者共有 OTU 152 个。(2)物种分类显示,不同火棘组织内生细菌具有丰富的群落多样性,火棘根部内生细菌种类隶属于23门53纲137目216科373属557种,其中异样根瘤菌属(Allorhizobium-Neorhizobium-Pararhizobium-Rhizobium)和链霉菌属(Streptomyces)为优势属,其相对丰度分别为 10.57%和 8.00%; 茎部内生细菌种类隶属于21门32纲76目126科204属270种,其中马赛菌属(Massilia)和未知分类的丛毛单胞菌科属(unclassified_f_Comamonadaceae)为优势属,其相对丰度分别为31.10%和12.82%; 叶部内生细菌种类隶属于21门52纲130目210科380属581种,其中土芽孢杆菌属(Geobacillus)和假单胞菌属(Pseudomonas)为优势属,其相对丰度分别为12.31%和9.84%。(3)PICRUSt功能预测表明,根部内生细菌物种最丰富,参与各种代谢调控的细菌丰度最高。该研究结果为进一步探讨植物内生细菌功能,挖掘新的有益微生物资源提供了参考。     

Molecular diversity of bacteria in Yunnan yellow cattle (Bos taurs) from Nujiang region, China

The rumen content of four Yunnan Yellow Cattle (Bos taurs) were collected to determine the bacteria diversity by using 16S rRNA gene sequence analysis. A total of 129 sequences were examined and the sequences were referred as 107 OTU (Operational Taxonomy Unit) according to the similarity level of 97% in gene sequence. Similarity analysis revealed that Yunnan Yellow Cattle had 12 sequences (10 OTU) shared 97% or greater similarity with cultured rumen bacteria Butyrivibrio fibrisolvens, Succiniclasticum ruminis, Ruminococcus bromii, Clostridium proteoclasticum, Ruminococcus flavefaciens, Pseudobutyrivibrio ruminis, Jeotgalicoccus psychrophilus, and Prevotella ruminicola, which accounting for 9.3% of the total clones (9.2% of the total OTU). The further 12 sequences (9 OTU) shared 90–97% similarity with cultured bacteria Clostridium aminobutyricum, butyrate-producing bacterium, Schwartzia succinivorans, Prevotella ruminicola, Eubacterium ruminantium, Ruminococcus albus, and Clostridium termitidis, also accounting for 9.3% of the total sequences (8.3% of the total OTU). The remaining 105 sequences (90 OTU) shared less than 90% similarity with cultured bacteria, accounting for 81.4% of the total sequences (82.5% of the total OTU). According to the phylogenetic analysis, all sequences were phylogenetically placed within phyla of low G+C subdivision (accounting for 72.1 and 72.5% of the total clones and OTU, respectively) and CFB subdivision (Cytophaga-Flexibacter-Bacteroides; accounting for 27.9 and 27.5% of the total clones and OTU, respectively). Among the examined clones, rare bacteria Jeotgalicoccus psychrophilus was detected in the rumen of cattle.     

Metagenomic study of red biofilms from Diamante Lake reveals ancient arsenic bioenergetics in haloarchaea

Arsenic metabolism is proposed to be an ancient mechanism in microbial life. Different bacteria and archaea use detoxification processes to grow under high arsenic concentration. Some of them are also able to use arsenic as a bioenergetic substrate in either anaerobic arsenate respiration or chemolithotrophic growth on arsenite. However, among the archaea, bioenergetic arsenic metabolism has only been found in the Crenarchaeota phylum. Here we report the discovery of haloarchaea (Euryarchaeota phylum) biofilms forming under the extreme environmental conditions such as high salinity, pH and arsenic concentration at 4589 m above sea level inside a volcano crater in Diamante Lake, Argentina. Metagenomic analyses revealed a surprisingly high abundance of genes used for arsenite oxidation (aioBA) and respiratory arsenate reduction (arrCBA) suggesting that these haloarchaea use arsenic compounds as bioenergetics substrates. We showed that several haloarchaea species, not only from this study, have all genes required for these bioenergetic processes. The phylogenetic analysis of aioA showed that haloarchaea sequences cluster in a novel and monophyletic group, suggesting that the origin of arsenic metabolism in haloarchaea is ancient. Our results also suggest that arsenite chemolithotrophy likely emerged within the archaeal lineage. Our results give a broad new perspective on the haloarchaea metabolism and shed light on the evolutionary history of arsenic bioenergetics.     

Spatial Distribution and Factors Shaping the Niche Segregation of Ammonia-Oxidizing Microorganisms in the Qiantang River,China

Ammonia oxidation is performed by both ammonia-oxidizing archaea (AOA) and ammonia-oxidizing bacteria (AOB). However, the current knowledge of the distribution, diversity, and relative abundance of these two microbial groups in freshwater sediments is insufficient. We examined the spatial distribution and analyzed the possible factors leading to the niche segregation of AOA and AOB in the sediments of the Qiantang River, using clone library construction and quantitative PCR for both archaeal and bacterial amoA genes. pH and NH₄⁺-N content had a significant effect on AOA abundance and AOA operational taxonomy unit (OTU) numbers. pH and organic carbon content influenced the ratio of AOA/AOB OTU numbers significantly. The influence of these factors showed an obvious spatial trend along the Qiantang River. This result suggested that AOA may contribute more than AOB to the upstream reaches of the Qiantang River, where the pH is lower and the organic carbon and NH₄⁺-N contents are higher, but AOB were the principal driver of nitrification downstream, where the opposite environmental conditions were present.