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Oxygen-dependent niche formation of a pyrite-dependent acidophilic consortium built by archaea and bacteria

机译:由古细菌和细菌建立的黄铁矿依赖性嗜酸菌团的氧依赖性生态位形成

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摘要

Biofilms can provide a number of different ecological niches for microorganisms. Here, a multispecies biofilm was studied in which pyrite-oxidizing microbes are the primary producers. Its stability allowed not only detailed fluorescence in situ hybridization (FISH)-based characterization of the microbial population in different areas of the biofilm but also to integrate these results with oxygen and pH microsensor measurements conducted before. The O2 concentration declined rapidly from the outside to the inside of the biofilm. Hence, part of the population lives under microoxic or anoxic conditions. Leptospirillum ferrooxidans strains dominate the microbial population but are only located in the oxic periphery of the snottite structure. Interestingly, archaea were identified only in the anoxic parts of the biofilm. The archaeal community consists mainly of so far uncultured Thermoplasmatales as well as novel ARMAN (Archaeal Richmond Mine Acidophilic Nanoorganism) species. Inductively coupled plasma analysis and X-ray absorption near edge structure spectra provide further insight in the biofilm characteristics but revealed no other major factors than oxygen affecting the distribution of bacteria and archaea. In addition to catalyzed reporter deposition FISH and oxygen microsensor measurements, microautoradiographic FISH was used to identify areas in which active CO2 fixation takes place. Leptospirilla as well as acidithiobacilli were identified as primary producers. Fixation of gaseous CO2 seems to proceed only in the outer rim of the snottite. Archaea inhabiting the snottite core do not seem to contribute to the primary production. This work gives insight in the ecological niches of acidophilic microorganisms and their role in a consortium. The data provided the basis for the enrichment of uncultured archaea.
机译:生物膜可以为微生物提供许多不同的生态位。在这里,研究了一种多物种生物膜,其中黄铁矿氧化微生物是主要生产者。它的稳定性不仅允许对生物膜不同区域中的微生物种群进行详细的基于荧光原位杂交(FISH)的表征,而且还可以将这些结果与之前进行的氧气和pH微传感器测量相结合。 O2浓度从生物膜的外部到内部迅速下降。因此,部分人口生活在低氧或缺氧条件下。钩端螺旋体铁氧体菌株在微生物种群中占主导地位,但仅位于亚硫酸盐结构的有氧边缘。有趣的是,古细菌仅在生物膜的缺氧部分被鉴定。迄今为止,古细菌群落主要由未培养的热质鞘菌和新的ARMAN(Archaeal Richmond Mine Acidophilic Nanoorganism)物种组成。感应耦合等离子体分析和近边缘结构光谱的X射线吸收提供了生物膜特征的进一步见解,但没有发现除氧气以外的其他主要因素会影响细菌和古细菌的分布。除了催化的报告物沉积FISH和氧气微传感器测量外,还使用微放射自显影FISH来识别发生主动CO2固定的区域。钩端螺旋体以及酸性硫杆菌被确定为主要生产者。气态CO2的固定似乎仅在硬石膏的外缘进行。居住在亚硫酸钙岩核中的古细菌似乎对初级生产没有贡献。这项工作提供了对嗜酸微生物的生态位及其在财团中的作用的见解。数据为丰富未培养古细菌提供了基础。

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