Carbon Dioxide Fixation by Metallosphaera yellowstonensis and Acidothermophilic Iron-Oxidizing Microbial Communities from Yellowstone National Park

The fixation of inorganic carbon has been documented in all three domains of life and results in the biosynthesis of diverse organic compounds that support heterotrophic organisms. The primary aim of this study was to assess carbon dioxide fixation in high-temperature Fe(III)-oxide mat communities and in pure cultures of a dominant Fe(II)-oxidizing organism (Metallosphaera yellowstonensis strain MK1) originally isolated from these environments. Protein-encoding genes of the complete 3-hydroxypropionate/4-hydroxybutyrate (3-HP/4-HB) carbon dioxide fixation pathway were identified in M. yellowstonensis strain MK1. Highly similar M. yellowstonensis genes for this pathway were identified in metagenomes of replicate Fe(III)-oxide mats, as were genes for the reductive tricarboxylic acid cycle from Hydrogenobaculum spp. (Aquificales). Stable-isotope (¹³CO₂) labeling demonstrated CO₂ fixation by M. yellowstonensis strain MK1 and in ex situ assays containing live Fe(III)-oxide microbial mats. The results showed that strain MK1 fixes CO₂ with a fractionation factor of ∼2.5‰. Analysis of the ¹³C composition of dissolved inorganic C (DIC), dissolved organic C (DOC), landscape C, and microbial mat C showed that mat C is from both DIC and non-DIC sources. An isotopic mixing model showed that biomass C contains a minimum of 42% C of DIC origin, depending on the fraction of landscape C that is present. The significance of DIC as a major carbon source for Fe(III)-oxide mat communities provides a foundation for examining microbial interactions that are dependent on the activity of autotrophic organisms (i.e., Hydrogenobaculum and Metallosphaera spp.) in simplified natural communities.     

Phylogenetic and functional prokaryotic diversity in the Hoito-Gol mesothermal mineral spring (Eastern Sayan Mountains,Buryat Republic)

High-throughput sequencing was used for comparative analysis of microbial communities of the water and mat from the Hoito-Gol mesothermal mineral sulfide spring (Eastern Sayan Mountains, Buryat Republic). Activity of microbial communities was determined. While both spring biotopes were dominated by members of three bacterial phyla—Proteobacteria, Bacteroidetes, and Firmicutes—they differed drastically in the composition of predominant phylotypes (at the genus level). In the water, the organisms widespread in aquatic environments were predominant, mostly aerobic chemoorganotrophs of the genera Acinetobacter, Pedobacter, and Flavobacterium. In the microbial mat, the organisms actively involved in the sulfur cycle predominated, including sulfur-reducing bacteria Sulfurospirillum, sulfate-reducing deltaproteobacteria, sulfuroxidizing chemoautotrophic bacteria, anoxygenic phototrophic bacteria of the phyla Chloroflexi and Chlorobi, as well as purple bacteria belonging to the α-, ß-, and γ-Proteobacteria. Microbial mats of the spring exhibited higher phylogenetic diversity compared to high-temperature mats containing photosynthetic microorganisms.     

Organotrophic bacteria of the Baikal Rift Zone hot springs

Pyrosequencing of the 16S rRNA gene fragments was used to investigate the bacterial community of an Alla hot spring microbial mat. The mat community was mainly represented by the members of five phyla: Deinococcus-Thermus, Nitrospirae, Atribacteria (OP9), Proteobacteria, Chloroflexi, and Firmicutes, with other groups responsible for not more than 2% of the total number. From hot springs of the Baikal Rift Zone (Buryatia, Russia), 13 strains of aerobic alkaliphilic thermophilic organotrophic bacteria were isolated, and their morphology, ecology, physiology, and phylogenetic position were studied. Based on analysis of their 16S rRNA gene sequences, the isolates were identified as members of the family Bacillaceae. Strains Al-9-1, Se-1, Ga-1-1, Ga-9-2, and Se-1-10 were assigned to the genus Anoxybacillus; strains Ur-6, Br-2-2, А2, and Um-09m, to the genus Bacillus; strains Gor-10s and Gа-35, to the genus Paenabacillus. Secreted endopeptidases of the isolates were shown to have relatively narrow substrate specificity. The investigated enzymes were characterized by high pH (6.3–11.4) and temperature stability (23–70°C), which makes it possible to carry out organic matter degradation in the environment under variable ecological conditions.     

Coordinating environmental genomics and geochemistry reveals metabolic transitions in a hot spring ecosystem

We have constructed a conceptual model of biogeochemical cycles and metabolic and microbial community shifts within a hot spring ecosystem via coordinated analysis of the "Bison Pool" (BP) Environmental Genome and a complementary contextual geochemical dataset of ~75 geochemical parameters. 2,321 16S rRNA clones and 470 megabases of environmental sequence data were produced from biofilms at five sites along the outflow of BP, an alkaline hot spring in Sentinel Meadow (Lower Geyser Basin) of Yellowstone National Park. This channel acts as a >22 m gradient of decreasing temperature, increasing dissolved oxygen, and changing availability of biologically important chemical species, such as those containing nitrogen and sulfur. Microbial life at BP transitions from a 92 °C chemotrophic streamer biofilm community in the BP source pool to a 56 °C phototrophic mat community. We improved automated annotation of the BP environmental genomes using BLAST-based Markov clustering. We have also assigned environmental genome sequences to individual microbial community members by complementing traditional homology-based assignment with nucleotide word-usage algorithms, allowing more than 70% of all reads to be assigned to source organisms. This assignment yields high genome coverage in dominant community members, facilitating reconstruction of nearly complete metabolic profiles and in-depth analysis of the relation between geochemical and metabolic changes along the outflow. We show that changes in environmental conditions and energy availability are associated with dramatic shifts in microbial communities and metabolic function. We have also identified an organism constituting a novel phylum in a metabolic "transition" community, located physically between the chemotroph- and phototroph-dominated sites. The complementary analysis of biogeochemical and environmental genomic data from BP has allowed us to build ecosystem-based conceptual models for this hot spring, reconstructing whole metabolic networks in order to illuminate community roles in shaping and responding to geochemical variability.     

Total and active microbial communities and <Emphasis Type="Italic">phoD</Emphasis> as affected by phosphate depletion and pH in soil

Background and Aims

Soil microbial communities contribute to organic phosphorus cycling in a variety of ways, including secretion of the PhoD alkaline phosphatase. We sampled a long-term grassland fertilization trial in Switzerland characterized by a natural pH gradient. We examined the effects of phosphate depletion and pH on total and active microbial community structures and on the structure and composition of the total and active phoD-harboring community.

Methods

Archaeal, bacterial and fungal communities were investigated using T-RFLP and phoD-harboring members of these communities were identified by 454-sequencing.

Results

Phosphate depletion decreased total, resin-extractable and organic phosphorus and changed the structure of all active microbial communities, and of the total archaeal and phoD-harboring communities. Organic carbon, nitrogen and phosphorus increased with pH, and the structures of all total and active microbial communities except the total fungal community differed between the two pH levels. phoD-harboring members were affiliated to Actinomycetales, Bacilliales, Gloeobacterales, Planctomycetales and Rhizobiales.

Conclusions

Our results suggest that pH and associated soil factors are important determinants of microbial and phoD-harboring community structures. These associated factors include organic carbon and total nitrogen, and to a lesser degree phosphorus status, and active communities are more responsive than total communities. Key players in organic P mineralization are affiliated to phyla that are known to be important in organic matter decomposition.

     

Genomics and Biochemistry of Metabolic Pathways for the C<Subscript>1</Subscript> Compounds Utilization in Colorless Sulfur Bacterium <Emphasis Type="Italic">Beggiatoa leptomitoformis</Emphasis> D-402

The metabolic pathways of one-carbon compounds utilized by colorless sulfur bacterium Beggiatoa leptomitoformis D-402 were revealed based on comprehensive analysis of its genomic organization, together with physiological, biochemical and molecular biological approaches. Strain D-402 was capable of aerobic methylotrophic growth with methanol as a sole source of carbon and energy and was not capable of methanotrophic growth because of the absence of genes of methane monooxygenases. It was established that methanol can be oxidized to CO₂ in three consecutive stages. On the first stage methanol was oxidized to formaldehyde by the two PQQ (pyrroloquinolinequinone)-dependent methanol dehydrogenases (MDH): XoxF and Mdh2. Formaldehyde was further oxidized to formate via the tetrahydromethanopterin (H₄MPT) pathway. And on the third stage formate was converted to CO₂ by NAD⁺-dependent formate dehydrogenase Fdh2. Finally, it was established that endogenous CO₂, formed as a result of methanol oxidation, was subsequently assimilated for anabolism through the Calvin–Benson–Bassham cycle. The similar way of one-carbon compounds utilization also exists in representatives of another freshwater Beggiatoa species—B. alba.     

Linking geochemical processes with microbial community analysis: successional dynamics in an arsenic-rich, acid-sulphate-chloride geothermal spring

The source waters of acid‐sulphate‐chloride (ASC) geothermal springs located in Norris Geyser Basin, Yellowstone National Park contain several reduced chemical species, including H₂, H₂S, As(III), and Fe(II), which may serve as electron donors driving chemolithotrophic metabolism. Microorganisms thriving in these environments must also cope with high temperatures, low pH (～3), and high concentrations of sulphide, As(III), and boron. The goal of the current study was to correlate the temporal and spatial distribution of bacterial and archaeal populations with changes in temperature and geochemical energy gradients occurring throughout a newly formed (redirected) outflow channel of an ASC spring. A suite of complimentary analyses including aqueous geochemistry, microscopy, solid phase identification, and 16S rDNA sequence distribution were used to correlate the appearance of specific microbial populations with biogeochemical processes mediating S, Fe, and As cycling and subsequent biomineralization of As(V)‐rich hydrous ferric oxide (HFO) mats. Rapid As(III) oxidation (maximum first order rate constants ranged from 4 to 5 min^?1, t_1/2 = 0.17 ? 0.14 min) was correlated with the appearance of Hydrogenobaculum and Thiomonas–like populations, whereas the biogenesis of As(V)‐rich HFO microbial mats (mole ratios of As:Fe ～0.7) was correlated with the appearance of Metallosphaera, Acidimicrobium, and Thiomonas–like populations. Several 16S sequences detected near the source were closely related to sequences of chemolithotrophic hyperthermophilic populations including Stygiolobus and Hydrogenobaculum organisms that are known H₂ oxidizers. The use of H₂, reduced S(–II,0), Fe(II) and perhaps As(III) by different organisms represented throughout the outflow channel was supported by thermodynamic calculations, confirming highly exergonic redox couples with these electron donors. Results from this work demonstrated that chemical energy gradients play an important role in establishing distinct community structure as a function of distance from geothermal spring discharge.     

Deep sequencing analysis of bacterial community structure of Soldhar hot spring,India

We investigated the bacterial community structure of Soldhar hot spring with extreme high temperature 95°C located in Uttarakhand, India using high throughput sequencing. Bacterial phyla Proteobacteria (88.8%), Deinococcus-Thermus (7.5%), Actinobacteria (2.3%), and Firmicutes (1.07%) were predominated in the sequencing survey, whereas Bacteroidetes, Verrucomicrobia, Aquificae and Acidobacteria were detected in relatively lower abundance in Soldhar hot spring. At the family level, Comamonadaceae (52.5%), Alteromonadaceae (15.9%), and Thermaceae (7.5%) were mostly dominated in the ecosystem followed by Chromatiaceae, Microbacteriaceae, and Cyclobacteriaceae. Besides, members of Rhodobacteraceae, Moraxellaceae, Xanthomonadaceae, Aquificaceae, Enterobacteriaceae, Bacillaceae, Methylophilaceae, etc. were detected as a relatively lower abundance. In the present study we discuss the overall microbial community structure and their relevance to the ecology of the Soldhar hot spring environment.     

Microbial community changes during a toxic cyanobacterial bloom in an alkaline Hungarian lake

The Carpathian Basin is a lowland plain located mainly in Hungary. Due to the nature of the bedrock, alluvial deposits, and a bowl shape, many lakes and ponds of the area are characterized by high alkalinity. In this study, we characterized temporal changes in eukaryal and bacterial community dynamics with high throughput sequencing and relate the changes to environmental conditions in Lake Velence located in Fejér county, Hungary. The sampled Lake Velence microbial populations (algal and bacterial) were analyzed to identify potential correlations with other community members and environmental parameters at six timepoints over 6 weeks in the Spring of 2012. Correlations between community members suggest a positive relationship between certain algal and bacterial populations (e.g. Chlamydomondaceae with Actinobacteria and Acidobacteria), while other correlations allude to changes in these relationships over time. During the study, high nitrogen availability may have favored non-nitrogen fixing cyanobacteria, such as the toxin-producing Microcystis aeruginosa, and the eutrophic effect may have been exacerbated by high phosphorus availability as well as the high calcium and magnesium content of the Carpathian Basin bedrock, potentially fostering exopolymer production and cell aggregation. Cyanobacterial bloom formation could have a negative environmental impact on other community members and potentially affect overall water quality as well as recreational activities. To our knowledge, this is the first prediction for relationships between photoautotrophic eukaryotes and bacteria from an alkaline, Hungarian lake.     

Successional Changes in the Microbial Community of the Alkaline Lake Khilganta during the Dry Season

Microbial processes in a shallow, saline, alkaline Lake Khilganta (Southern Siberia) were studied during the dry season. During the drought, a crust was formed on the lake surface, where low rates of production processes were observed, with predominance of anoxygenic photosynthesis at 2.3 mg C/(dm³ day). The rates of microbial processes increased after short-term rains. During this period, a thin cyanobacterial mat was formed on the bottom, in which filamentous cyanbacteria Geitlerinema spp. predominated and the rate of oxygenic photosynthesis was up to 18 mg C/(dm³ day). Subsequent water evaporation and salinity increase resulted in altered community types and their activity. Red spots emerged on the mat surface, where anoxygenic prototrophic members of the genus Ectothiorhodospira predominated. Anoxygenic photosynthesis became the main production process in microbial mats, with the rate of 60 mg C/(dm³ day). At salinity increase to 200 g/L, the water remained in small depressions on the bottom, where extremophilic green algae Dunaliella sp. predominated, and the rate of oxygenic photosynthesis was 0.877 mg C/(dm³ day). These changes in the type and activity of microbial communities is an example of succession of microbial communities in Southern Siberia saline lakes during drought.     

Occurrence and Carbon Metabolism of Green Nonsulfur-like Bacteria in Californian and Nevada Hot Spring Microbial mats as Revealed by Wax Ester Lipid Analysis

Green nonsulfur-like bacteria (GNSLB) in Yellowstone hot spring microbial mats have been extensively studied and are thought to operate both as photoheterotrophs and photoautotrophs. Here we studied the occurrence and carbon metabolisms of GNSLB by analyzing the distribution and isotopic composition of their characteristic wax ester lipids in four Californian and Nevada hot spring microbial mats at a range of temperatures (37–96°C). The distribution of wax esters varied strongly with temperature. At temperatures between 50–60°C the wax ester composition in each of the four hot spring microbial mats was dominated by C₃₀ to C₃₆ wax esters, consisting of mixtures of C₁₅-C₁₈ n-alkyl and branched fatty acids and alcohols, typical for GNSLB. Stable carbon isotopic analysis showed that these wax esters were only depleted by 5 to 10‰ compared to dissolved inorganic carbon in the overlying water, suggesting that these GNSLB were mainly autotrophic. However, analysis of different depth layers of one microbial mat showed that these GNSLB wax esters were increasingly depleted in ¹³C with depth, suggesting that photoautotrophy mainly occurred in the top layer of the mat. ¹³C-depleted C₃₆-C₄₄ wax esters were found in one hot spring at high temperatures (77–96°C) and are likely derived from allochtonous plant waxes. At several lower temperature sites (35–40°C) the wax esters were predominantly composed of C₂₈, C₃₀ and C₃₂ wax esters consisting of mixtures of C₁₄-C₁₆ fatty acids and n-alkanols and were depleted in ¹³C by 15–20‰ relative to dissolved inorganic carbon, suggesting they may be derived from heterotrophic organisms. Our results indicate that autotrophic GNSLB occur widely in hot springs and that diverse groups of organisms contribute to the pool of wax ester lipids in hot spring environments.     

A novel uncultured bacterium of the family <Emphasis Type="Italic">Gallionellaceae</Emphasis>: Description and genome reconstruction based on metagenomic analysis of microbial community in acid mine drainage

Drainage waters at the metal mining areas often have low pH and high content of dissolved metals due to oxidation of sulfide minerals. Extreme conditions limit microbial diversity in such habitats. A microbial community of cold acid mine drainage (6.5°C, pH 2.65) at the Sherlovaya Gora polymetallic open-cast mine (Transbaikal region, Eastern Siberia, Russia) was studied using metagenomic techniques. Most of microorganisms belonged to a single uncultured lineage representing a new species of the Betaproteobacteria genus Gallionella. Bacteria of the genera Thiobacillus, Acidobacterium, Acidisphaera, and Acidithiobacillus were the minor components of the community. Almost complete (3.4 Mb) composite genome of the new bacterial lineage designated Candidatus Gallionella acididurans ShG14-8 was reconstructed using metagenomic data. Genome analysis revealed that Fe(II) oxidation probably involved the cytochromes localized on the outer cell membrane. The electron transport chain included NADH dehydrogenase, a cytochrome bc1 complex, an alternative complex III, and bd-, cbb3-, and bo3-types cytochrome oxidases. Oxidation of reduced sulfur compounds probably involved the Sox system, sulfide–quinone oxidoreductase, adenyl sulfate reductase, and sulfate adenyltransferase. The genes involved in autotrophic carbon assimilation via the Calvin cycle were present, while no pathway for nitrogen fixation was revealed. High numbers of RND metal transporters and P type ATPases were probably responsible for resistance to heavy metals. The new microorganism was an aerobic chemolithoautotroph that belonged to the group of psychrotolerant iron- and sulfur-oxidizing acidophiles of the family Gallionellaceae, which are widely distributed in acid mine drainage.     

Radioisotopic tracing of carbon monoxide conversion by anaerobic thermophilic prokaryotes

The rate of CO conversion by a pure culture of a thermophilic CO-oxidizing, H₂-producing bacterium Carboxydocella sp. strain 1503 was determined by the radioisotopic method. The overall daily uptake of ¹⁴CO by the bacterium was estimated at 38–56 μmol CO per 1 ml of the culture. A radioisotopic method was developed to separate and quantitatively determine the products of anaerobic CO conversion by microbial communities in hot springs. The new method was first tested on the microbial community from a sample obtained from a hot spring in Kamchatka. The potential rate of CO conversion by the anaerobic microbial community was found to be 40.75 nmol CO/cm³ sediment per day. 85% of the utilized ¹⁴CO was oxidized to carbon dioxide; 14.5% was incorporated into dissolved organic matter, including 0.2% that went into volatile fatty acids; 0.5% was used for cell biomass production; and only just over 0.001% was converted to methane.     

Molecular analysis of microbial diversity in the Zavarzin Spring,Uzon Caldera,Kamchatka

The Zavarzin spring is situated in the caldera of the Uzon volcano, Kamchatka, and is characterized by a temperature of about 60°C, neutral pH, and high concentration of sulfur. The bottom of the spring is covered with a cyanobacterial mat. The structure of the microbial community of the water from the Zavarzin spring was qualitatively and quantitatively characterized by pyrosequencing of the V3 variable region of the 16S rRNA gene, which yielded 37 654 independent sequences. The microbial community includes about 900 bacterial and 90 archaeal genera. Bacteria comprised 95% of the microorganisms and archaea less than 5%. The largest part (32.3%) of the community was constituted by the chemolithoautotrophic bacteria Aquificae from the genera Sulfurihydrogenibium and Thermosulfidibacter. Among autotrophic microorganisms, members of Thermodesulfobacteria (7.3%), the gammaproteobacteria Thiofaba (7.6%), the deltaproteobacteria Desulfurella (2.6%), and the betaproteobacteria Thiomonas (0.6%) were also identified. Heterotrophic bacteria were represented by Calditerrivibrio (12.1%), Thermotogae (6.3%), the betaproteobacteria Tepidimonas (6.0%), Deinococcus-Thermus (4.4%), Caldiserica (1.7%), and Dictyoglomi (1.6%). About 1.9% of microorganisms belonged to the BRC1 phylum, which does not include cultured members, and 0.2% of bacteria formed a new phylogenetic branch of the phylum level, representatives of which have been found only in the Zavarzin spring. Members of all four archaeal phyla were identified: Euryarchaeota (42% of archaeal sequences), Crenarchaeota (50%), Korarchaeota (7.5%), and Nanoarchaeota (0.5%). Thus, in the Zavarzin spring, apart from photosynthesis carried out by the cyanobacterial mat, which covers the bottom, chemolithoautotrophic production of organic matter can occur. In aerobic conditions, it proceeds at the expense of the oxidation of sulfur and its reduced compounds, and in anaerobic conditions, at the expense of the oxidation of hydrogen with sulfur and sulfates as electron acceptors. The organic matter formed by autotrophic bacteria may be utilized by various organotrophic microorganisms, including both fermentative bacteria and organisms that carry out anaerobic respiration with sulfur and nitrate as electron acceptors.     

Phenol Conjugation with Peptides and Final Transformations of Conjugates in English Ryegrass Seedlings

[1-¹⁴C]Phenol transformation in English ryegrass (Lolium perenne L.) sterile seedlings was studied. The compound studied was assimilated by a plant through leaves as vapor. Phenol was bound with ryegrass low-molecular-weight peptides producing phenol-peptide conjugates. Conjugation with endogenous peptides is one of the main pathways of phenol detoxication in ryegrass. Nearly three-fifths of phenol assimilated is conjugated with low-molecular-weight peptides. After removal of the plant from the labeled phenol-containing atmosphere, the content of conjugation products gradually decreased, followed by excretion of labeled carbon dioxide. This fact indicates that the conjugates are destructed and the carbon atoms of their radioactive component are oxidized to carbon dioxide. Almost one-third of assimilated phenol is transformed via the oxidation pathway, but a small part of it is irreversibly bound with biopolymer molecules.     

Perchlorate reduction by hydrogen autotrophic bacteria and microbial community analysis using high-throughput sequencing

Hydrogen autotrophic reduction of perchlorate have advantages of high removal efficiency and harmless to drinking water. But so far the reported information about the microbial community structure was comparatively limited, changes in the biodiversity and the dominant bacteria during acclimation process required detailed study. In this study, perchlorate-reducing hydrogen autotrophic bacteria were acclimated by hydrogen aeration from activated sludge. For the first time, high-throughput sequencing was applied to analyze changes in biodiversity and the dominant bacteria during acclimation process. The Michaelis–Menten model described the perchlorate reduction kinetics well. Model parameters q _max and K _s were 2.521–3.245 (mg ClO₄ ^?/gVSS h) and 5.44–8.23 (mg/l), respectively. Microbial perchlorate reduction occurred across at pH range 5.0–11.0; removal was highest at pH 9.0. The enriched mixed bacteria could use perchlorate, nitrate and sulfate as electron accepter, and the sequence of preference was: NO₃ ^? > ClO₄ ^? > SO₄ ^2?. Compared to the feed culture, biodiversity decreased greatly during acclimation process, the microbial community structure gradually stabilized after 9 acclimation cycles. The Thauera genus related to Rhodocyclales was the dominated perchlorate reducing bacteria (PRB) in the mixed culture.     

Microbial community in a pilot-scale bioreactor promoting anaerobic digestion and sulfur-driven denitrification for domestic sewage treatment

A pilot-scale reactor treating domestic sewage was operated to promote anaerobic digestion and denitrification using endogenous electron donors. While 55 % of organic matter was removed, nitrogen and sulfur showed a different dynamics during the operation. Pyrosequencing analysis clarified this behavior revealing that specific microbial communities inhabited the anaerobic (47.05 % of OTUs) and anoxic (31.39 % of OTUs) chambers. Analysis of 16S rRNA gene partial sequences obtained through pyrosequencing revealed a total of 1727 OTUs clustered at a 3 % distance cutoff. In the anaerobic chamber, microbial community was comprised of fermentative, syntrophic and sulfate-reducing bacteria. The majority of sequences were related to Aminobacterium and Syntrophorhabdus. In the anoxic chamber, the majority of sequences were related to mixotrophic and strictly autotrophic denitrifiers Arcobacter and Sulfuricurvum, respectively, both involved in sulfur-driven denitrification. These results show that pyrosequencing was a powerful tool to investigate the microbial panorama of a complex system, providing new insights to the improvement of the system.     

A thiotrophic microbial community in an acidic brine lake in Northern Chile

The endorheic basins of the Northern Chilean Altiplano contain saline lakes and salt flats. Two of the salt flats, Gorbea and Ignorado, have high acidic brines. The causes of the local acidity have been attributed to the occurrence of volcanic native sulfur, the release of sulfuric acid by oxidation, and the low buffering capacity of the rocks in the area. Understanding the microbial community composition and available energy in this pristine ecosystem is relevant in determining the origin of the acidity and in supporting the rationale of conservation policies. Besides, a comparison between similar systems in Australia highlights key microbial components and specific ones associated with geological settings and environmental conditions. Sediment and water samples from the Salar de Gorbea were collected, physicochemical parameters measured and geochemical and molecular biological analyses performed. A low diversity microbial community was observed in brines and sediments dominated by Actinobacteria, Algae, Firmicutes and Proteobacteria. Most of the constituent genera have been reported to be either sulfur oxidizing microorganisms or ones having the potential for sulfur oxidation given available genomic data and information drawn from the literature on cultured relatives. In addition, a link between sulfur oxidation and carbon fixation was observed. In contrast, to acid mine drainage communities, Gorbea microbial diversity is mainly supported by chemolithoheterotrophic, facultative chemolithoautotrophic and oligotrophic sulfur oxidizing populations indicating that microbial activity should also be considered as a causative agent of local acidity.     

Diversity of anaerobic arsenite-oxidizing bacteria in low-salt environments analyzed with a newly developed PCR-based method

Anaerobic arsenite oxidation is potentially important but the least understood process in the arsenic cycle. The catalytic subunit of the key enzyme for anaerobic arsenite oxidation is encoded by the arxA gene. In this study, a novel primer pair for the arxA gene was designed to detect diverse sequences of this notable gene. Further modification of the designed primer was made by adding extra bases to its 5′- end. This modification made it possible to analyze the PCR products with TA cloning, which provides higher throughput of investigations. With the combination of modified primer pair and TA cloning, diverse arxA gene sequences were effectively obtained from samples of lake water, spring water, and hot spring microbial mat. The sequences detected in the samples characterized by low salinity and nearly neutral pH were phylogenetically distinct from the majority of previously known arxA genes, found in the genome of alkaliphiles and halophiles.