Diversity of Thermophilic Iron-Pyrite-Oxidizing Enrichments from Solfataric Hot Springs in the Chilean Altiplano

Abstract

Relatively little is known about the microbial communities present in natural environments that meet physico-chemical conditions for the development of potential leaching microorganisms such as thermal ecosystems from the Chilean Altiplano. Thermophilic leaching enrichments were obtained and identified from a high altitude solfataric pound in Lirima hot springs in the Chilean Altiplano. This ecosystem is characterized by hot underground freshwaters, enriched in sulfur compounds showing pH from neutral to acidic. Microbial diversity has been scarcely explored here, and preliminary results demonstrate that hydrothermal pounds are represented by thermophilic anaerobic and acidophilic taxa. Thermophilic leaching cultures in shake flasks were obtained using ferrous iron and pyrite as energy source. The presence of Bacteria and Archaea in oxidizing enrichments was determined by PCR amplification of 16S rRNA genes. A preliminary analysis of microbial diversity using massive sequencing revealed that Bacteria were more abundant than Archaea in both enrichments. Specifically for the iron-oxidizing culture, the majority of the sequences clustered within the Proteobacteria phylum (79%). Among Proteobacteria, the proportion of Betaproteobacteria (42.2%) and Gammaproteobacteria (21.27%) was much higher than that of Alphaproteobacteria (15.5%). Within the Betaproteobacteria class, the most frequent genus was Leptothrix-like. Similar results were obtained for the pyrite oxidizing culture. Interestingly, this study shows the presence of microorganisms close to the Leptothrix genus under low pH conditions (1.7-2.8) and their capacity to grow at high temperatures with ferrous iron or pyrite as sole energy source

Diversity of thermophilic archaea and their biotechnological uses

“…Ağız kısımlarında ise ortalama 150 °C dolaylarındadır.  Solfatoralar: Fümerol (latince) çoğunlukla yer kabuğu sıcaklığının çok yüksek olduğu, yakın dönemde etkin yanardağların yer aldığı bölgelerde, karbondioksit, sülfürdioksit, hidrojenklorid ve hidrojen-sülfit gibi gazların, buhar şeklinde salındığı, yer kabuğundaki açıklıklardır [7].  Derin ve sığ hidrotermal sistemler [8] Bununla birlikte termofiller; kompost yığınları ve kömür atık yığınları gibi ortamlarda da bulunabilirler.…”