Philosophiae Doctor - PhD / The El Tatio geyser field (ETGF) is the largest known geothermal field in Chile, forming part of a wide spectrum of extremophilic habitats in the country. The ETGF is NaCl rich, with high concentrations of toxic elements such as Li, As and Cs, which are contributed mainly by volcanic activities in the region. Most previous studies in the area have focused on the geology and geochemistry for mining purposes, as well as on the search for geothermal resources for power generation. Very little is currently known about the composition of the microbial communities of the ETGF, which makes the study reported here of particular novelty.A metagenomic approach, involving the amplification of 16S rRNA gene phylogenetic markers from metagenomic DNA was used to investigate seven different sites within the geyser field. The sample sites were characterized by high temperatures (80-85 °C) and a range of pH values (6.3-8). Various molecular methods, including clone library construction and PCR-DGGE analyses were used to target a wide range of microbial populations within the ETGF sites. Multivariate analysis was also applied to assess differences in the microbial diversity from different sites and to correlate microbial diversity with environmental conditions. Culture-dependent screening of novel nanoarchaeal species was also undertaken.These were coupled with PCR and other detection methods such as fluorescent in situ hybridization (FISH) to trace the presence of nanoarchaeal signals from enriched cultures.The results have shown that the ETGF encompasses a limited microbial diversity represented by only 30 dominant phylotypes, and most likely due to the toxic chemical content of the geyser field. The microbial representatives identified were assigned to OTUs from archaeal,nanoarchaeal and bacterial taxonomic groups. The dominant microbial taxa included members of the Proteobacteria, Firmicutes, Aquificae, Actinobacteria, Euryarchaeota(Halobacteriales, Archaeoglobales), Crenarchaeota (Thermoproteales, Desulfurococcales),together with uncultured representatives of the bacteria, archaea and nanoarchaeota. Notably,representatives of mesophilic, thermophilic and hyperthermophilic taxonomic groups were all detected in ETGF samples. This is attributed to various factors such as temperature gradients and dispersal mechanisms (e.g. natural forces such as rain and volcanic activities). Principal component analysis (PCA) showed significant differences (P < 0.05) in the microbial diversity of the ETGF samples, with principal components (based on the sequenced species from both 16S rRNA clone libraries and PCR-DGGE profiles) explaining up to 62.7% of variance. Furthermore, CCA showed that the differences in phylogenetic diversity were most influenced by temperature and salinity. This was also confirmed by the sequencing results,which showed that hyperthermophilic and haloarchaeal taxa were dominant in the ETGF sites. However, conductivity and pH were also found to contribute to variations in the microbial diversity of the experimental samples, with TDS (total dissolved solids) being a less influential factor. Attempts to generate nanoarchaeal-host co-cultures, and to recover sufficient nanoarchaeal genomic DNA for fosmid and/or large insert cloning for comparative genome analysis, were unsuccessful.This study is the first to employ metagenomic approaches to analyse the microbial diversity of sites in the ETGF, and has expanded our knowledge of microbiota present in this geyser field.

Methanogenesis, a metabolic pathway unique to Archaea, is severely inhibited by the reduced form of arsenic (As). Despite this inhibition, methanogenic Archaea are present in some hydrothermal features at the El Tatio Geyser Field (ETGF), a high-arsenic site with 100+ hydrothermal features, including boiling pools, geyers, fumaroles, and springs. The ability of methanogenic Archaea and other microorganisms to withstand elevated arsenic concentrations, and a variety of other extreme environmental conditions at ETGF, may be due to unique adaptations or syntrophic relationships with other microorganisms. ETGF is situated in the Andes Mountains at an altitude of ~4300 meters. UV radiation is elevated in this region and air temperatures fluctuate widely. Most hydrothermal waters discharge at ~85˚C, the local boiling point, and rapidly evaporate due to the arid climate. This concentrates hydrothermal salts and metals, including arsenic (As) and antimony (Sb). Additionally, dissolved inorganic carbon (DIC) concentrations are extremely low in most features and may limit life. Water chemistry analyses done for this study show variability in dissolved constituents between features that are consistent over time. Variations may be due to the source or residence time of waters, and differences in chemistry could be responsible for the presence or absence of methanogenic Archaea at hydrothermal sites. The overlying control on microbial diversity and community composition may be water geochemistry, and potentially specific constituents. The goals of this study were to detect novel microbial taxa at ETGF, including novel methanogens, as well as to document microbial community composition at select hydrothermal features. The distribution and diversity of microorganisms at each feature was analyzed phylogenetically and within an ecological context in order to determine physicochemical and biological controls on community composition. Additionally, a model methanogen was used in laboratory analyses to determine how concentrations and oxidation states affected growth and methane production. This methanogen, Methanothermobacter thermautotrophicus, is found at ETGF, Yellowstone, and other hydrothermal fields, and thrives in high-temperature environments. MPN (most probable number) analyses show that culturable biomass from multiple sites contain metabolically active methanogens. These results support the biogenicity of dissolved methane detected in the field. 16S rRNA surveys of Archaea at four sites show that Archaea are diverse, and archaeal community composition varies across features. Phylogenetic tree construction indicates that Archaea from ETGF group together, suggesting that the isolation and broad environmental constrains on ETGF have some control on phylogenetic diversity. Laboratory analyses of As and Sb concentrations on M. thermautotrophicus suggest that Sb may decrease the inhibition of methanogenesis by As by preventing the formation of As(III) from As(V). Statistical analyses correlating microbial community composition and structure to physicochemical parameters show that archaeal and bacterial communities relate to different variables; with Bacteria correlating to water temperature, and Archaea correlating to dissolved constituents such as hydrogen gas and sulfate. / text