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首页> 外文期刊>Applied Microbiology >Archaeal and Bacterial Communities Respond Differently to Environmental Gradients in Anoxic Sediments of a California Hypersaline Lake, the Salton Sea
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Archaeal and Bacterial Communities Respond Differently to Environmental Gradients in Anoxic Sediments of a California Hypersaline Lake, the Salton Sea

机译:加利福尼亚超盐湖,索尔顿海的缺氧沉积物中,古细菌和细菌群落对环境梯度的反应不同

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Sulfidic, anoxic sediments of the moderately hypersaline Salton Sea contain gradients in salinity and carbon that potentially structure the sedimentary microbial community. We investigated the abundance, community structure, and diversity of Bacteria and Archaea along these gradients to further distinguish the ecologies of these domains outside their established physiological range. Quantitative PCR was used to enumerate 16S rRNA gene abundances of Bacteria , Archaea , and Crenarchaeota . Community structure and diversity were evaluated by terminal restriction fragment length polymorphism (T-RFLP), quantitative analysis of gene (16S rRNA) frequencies of dominant microorganisms, and cloning and sequencing of 16S rRNA. Archaea were numerically dominant at all depths and exhibited a lesser response to environmental gradients than that of Bacteria . The relative abundance of Crenarchaeota was low (0.4 to 22%) at all depths but increased with decreased carbon content and increased salinity. Salinity structured the bacterial community but exerted no significant control on archaeal community structure, which was weakly correlated with total carbon. Partial sequencing of archaeal 16S rRNA genes retrieved from three sediment depths revealed diverse communities of Euryarchaeota and Crenarchaeota , many of which were affiliated with groups previously described from marine sediments. The abundance of these groups across all depths suggests that many putative marine archaeal groups can tolerate elevated salinity (5.0 to 11.8% [wt/vol]) and persist under the anaerobic conditions present in Salton Sea sediments. The differential response of archaeal and bacterial communities to salinity and carbon patterns is consistent with the hypothesis that adaptations to energy stress and availability distinguish the ecologies of these domains.
机译:中等盐度索尔顿海中的硫化物,缺氧沉积物的盐度和碳梯度可能构成沉积微生物群落。我们调查了细菌和古细菌沿这些梯度的丰度,群落结构和多样性,以进一步区分这些域在既定生理范围之外的生态。定量PCR用于计数细菌,古生菌和Crenarchaeota的16S rRNA基因丰度。通过末端限制性片段长度多态性(T-RFLP),优势微生物基因(16S rRNA)频率的定量分析以及16S rRNA的克隆和测序来评估群落结构和多样性。在所有深度上,古细菌在数值上均占优势,并且对环境梯度的响应比细菌弱。 Crenarchaeota的相对丰度在所有深度均较低(0.4至22%),但随着碳含量的降低和盐度的增加而增加。盐度使细菌群落结构化,但对古细菌群落结构没有明显的控制作用,而该细菌与总碳的相关性较弱。从三个沉积物深度取回的古细菌16S rRNA基因的部分测序揭示了Euryarchaeota和Crenarchaeota的不同群落,其中许多与先前从海洋沉积物中描述的群有关。这些群体在所有深度的丰富性表明,许多假定的海洋古细菌群体可以忍受盐度升高(5.0至11.8%[wt / vol]),并在萨尔顿海沉积物中存在的厌氧条件下持续存在。古细菌和细菌群落对盐度和碳模式的不同响应与以下假设一致:对能量压力和可利用性的适应区分了这些域的生态。

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