首页> 外文期刊>Geobiology >Microbial biogeochemistry of Boiling Springs Lake: a physically dynamic, oligotrophic, low-pH geothermal ecosystem.
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Microbial biogeochemistry of Boiling Springs Lake: a physically dynamic, oligotrophic, low-pH geothermal ecosystem.

机译:沸腾泉湖的微生物生物地球化学:一个物理上动态的,贫营养的,低pH的地热生态系统。

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Boiling Springs Lake (BSL) in Lassen Volcanic National Park, California, is North America's largest hot spring, but little is known about the physical, chemical, and biological features of the system. Using a remotely operated vessel, we characterized the bathymetry and near-surface temperatures at sub-meter resolution. The majority of the 1.2 ha, pH 2.2 lake is 10 m deep and 50-52 C, but temperatures reach 93 C locally. We extracted DNA from water and sediments collected from warm (52 C) and hot (73-83 C) sites separated by 180 m. Gene clone libraries and functional gene microarray (GeoChip 3.0) were used to investigate the BSL community, and uptake of radiolabeled carbon sources was used to assess the relative importance of heterotrophic vs. autotrophic production. Microbial assemblages are similar in both sites despite the strong temperature differential, supporting observations of a dynamic, convectively mixed system. Bacteria in the Actinobacteria and Aquificales phyla are abundant in the water column, and Archaea distantly related to known taxa are abundant in sediments. The functional potential appears similar across a 5-year time span, indicating a stable community with little inter-annual variation, despite the documented seasonal temperature cycle. BSL water-derived DNA contains genes for complete C, N, and S cycles, and low hybridization to probes for N and S oxidation suggests that reductive processes dominate. Many of the detected genes for these processes were from uncultivated bacteria, suggesting novel organisms are responsible for key ecosystem services. Selection imposed by low nutrients, low pH, and high temperature appear to result in low diversity and evenness of genes for key functions involved in C, N, and S cycling. Conversely, organic degradation genes appear to be functionally redundant, and the rapid assimilation of radiolabeled organic carbon into BSL cells suggests the importance of allochthonous C fueling heterotrophic production in the BSL C cycle. 2013 John Wiley & Sons Ltd.
机译:加利福尼亚州拉森火山国家公园的沸腾温泉湖(BSL)是北美最大的温泉,但对该系统的物理,化学和生物学特征知之甚少。我们使用远程操作的船只,以亚米级分辨率表征了测深和近地表温度。 pH值为2.2的1.2公顷湖泊中,大部分位于10 m深和50-52 C,但局部温度达到93C。我们从相距180 m的温暖(52 C)和热(73-83 C)站点收集的水和沉积物中提取DNA。基因克隆文库和功能基因微阵列(GeoChip 3.0)用于研究BSL群落,而放射性标记碳源的摄取用于评估异养与自养生产的相对重要性。尽管温差很大,但两个站点的微生物组成相似,这支持了动态对流混合系统的观察。放线菌中的细菌和门生的Aquificales phyla中的细菌丰富,而与已知分类群关系密切的古细菌在沉积物中也很丰富。尽管记录了季节性温度周期变化,但在5年的时间跨度中,功能潜力似乎相似,这表明社区稳定,年际变化很小。 BSL水衍生的DNA包含完整的C,N和S循环的基因,与N和S氧化探针的低杂交性表明还原过程占主导。这些过程中检测到的许多基因来自未经培养的细菌,这表明新型生物负责关键的生态系统服务。低营养,低pH和高温导致的选择似乎导致涉及C,N和S循环的关键功能基因的多样性和均匀性较低。相反,有机降解基因似乎在功能上是多余的,并且放射性标记的有机碳迅速同化到BSL细胞中,表明异源C在BSL C循环中为异养生产提供了重要的支持。 2013 John Wiley&Sons Ltd.

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