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首页> 外文期刊>Geomicrobiology journal >Archaeoglobus fulgidus and Thermotoga elfii, Thermophilic Isolates from Deep Geothermal Water of the Paris Basin
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Archaeoglobus fulgidus and Thermotoga elfii, Thermophilic Isolates from Deep Geothermal Water of the Paris Basin

机译:巴黎盆地深层地热水中的嗜热分离物古生菌和嗜热栖热菌

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Thermophilic anaerobic microorganisms with the ability to reduce sulfur compounds (e.g., sulfate and/or thiosulfate) were isolated from water samples collected from about 2000 meters depth at in situ temperatures of 70°C in a geothermal well from the Paris Basin (France). Chemical and isotopic analyses show that microbial sulfate reduction occurred in the samples. Two strains were characterized by both DNA/DNA hybridization and 16S rRNA gene sequence analysis, which indicated that they are most closely related to Thermotoga elfii, a thiosulfate-reducing bacterium, and Archaeoglobus fulgidus, a sulfate- and thiosulfate-reducing archaeon. Besides thiosulfate reduction using H_2 as energy source, both isolates are shown to be able to retrieve energy from H_2/Fe(III), a metabolic capability of importance in a deep biosphere context. It is suggested that T.elfii and A. fulgidus could be used, either as pure culture or as a consortium, in future laboratory studies aiming at better understanding microbial iron (III) and sulfate/thiosulfate reduction, hydrogen production/consumption, as well as the effect of microorganisms on the evolution of CO_2 in deep aquifers. The present work examines numerous culture conditions and demonstrates that in spite of similarities in phylogenetic/genetic characteristics and in growth conditions, there are significant phenotypic differences between the isolated archaeal strain and the type strain of A. fulgidus. These differences, evidenced by a proteomic study, should be taken into account and could be useful parameters to be studied in the deep aquifers by geomicrobiological laboratories.
机译:在巴黎盆地(法国)的地热井中,在70°C的原位温度下,从约2000米深的水样中分离出具有还原硫化合物(例如硫酸盐和/或硫代硫酸盐)能力的嗜热厌氧微生物。化学和同位素分析表明,样品中发生了硫酸盐还原。两种菌株均通过DNA / DNA杂交和16S rRNA基因序列分析进行了表征,这表明它们与减少硫代硫酸盐的细菌Thermotherga elfii和减少硫酸根和硫代硫酸盐的古细菌古细菌fulgidus密切相关。除了使用H_2作为能源进行硫代硫酸盐还原外,两个分离物都能够从H_2 / Fe(III)中获取能量,而H_2 / Fe(III)在深层生物圈中具有重要的代谢能力。建议在未来的实验室研究中,无论是纯培养物还是作为财团,都可以使用T.elfii和A. fulgidus,以更好地了解微生物中的铁(III)和硫酸盐/硫代硫酸盐的还原,产氢/消耗量。微生物对深层含水层中CO_2演变的影响。本工作检查了许多培养条件,并证明,尽管在系统发育/遗传特征和生长条件上相似,但分离出的古细菌菌株和A. fulgidus型菌株之间仍存在明显的表型差异。蛋白质组学研究证明的这些差异应予以考虑,并且可能是地质微生物实验室在深层含水层中研​​究有用的参数。

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