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Archaeal and bacterial diversity in an arsenic-rich shallow-sea hydrothermal system undergoing phase separation

机译:富含砷的浅海热液系统中的古细菌和细菌多样性经历相分离

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摘要

Phase separation is a ubiquitous process in seafloor hydrothermal vents, creating a large range of salinities. Toxic elements (e.g., arsenic) partition into the vapor phase, and thus can be enriched in both high and low salinity fluids. However, investigations of microbial diversity at sites associated with phase separation are rare. We evaluated prokaryotic diversity in arsenic-rich shallow-sea vents off Milos Island (Greece) by comparative analysis of 16S rRNA clone sequences from two vent sites with similar pH and temperature but marked differences in salinity. Clone sequences were also obtained for aioA-like functional genes (AFGs). Bacteria in the surface sediments (0–1.5 cm) at the high salinity site consisted of mainly Epsilonproteobacteria (Arcobacter sp.), which transitioned to almost exclusively Firmicutes (Bacillus sp.) at ~10 cm depth. However, the low salinity site consisted of Bacteroidetes (Flavobacteria) in the surface and Epsilonproteobacteria (Arcobacter sp.) at ~10 cm depth. Archaea in the high salinity surface sediments were dominated by the orders Archaeoglobales and Thermococcales, transitioning to Thermoproteales and Desulfurococcales (Staphylothermus sp.) in the deeper sediments. In contrast, the low salinity site was dominated by Thermoplasmatales in the surface and Thermoproteales at depth. Similarities in gas and redox chemistry suggest that salinity and/or arsenic concentrations may select for microbial communities that can tolerate these parameters. Many of the archaeal 16S rRNA sequences contained inserts, possibly introns, including members of the Euryarchaeota. Clones containing AFGs affiliated with either Alpha- or Betaproteobacteria, although most were only distantly related to published representatives. Most clones (89%) originated from the deeper layer of the low salinity, highest arsenic site. This is the only sample with overlap in 16S rRNA data, suggesting arsenotrophy as an important metabolism in similar environments.
机译:相分离是海底热液喷口中普遍存在的过程,会产生大量盐度。有毒元素(例如砷)分配到气相中,因此可以在高盐度和低盐度流体中富集。但是,很少研究与相分离有关的部位的微生物多样性。我们通过比较分析两个pH和温度相似但盐度明显不同的通风口的16S rRNA克隆序列,评估了米洛斯岛(希腊)附近富含砷的浅海通风口的原核生物多样性。还获得了aioA样功能基因(AFG)的克隆序列。高盐度位点表面沉积物中的细菌(0-1.5厘米)主要由埃氏菌属细菌(Arcobacter sp。)组成,在约10厘米深度处几乎完全转化为硬毛菌(芽孢杆菌)。然而,低盐度部位由表面上的拟杆菌属(Flavobacteria)和约10 cm深度的Epsilon变形杆菌(Arcobacter sp。)组成。高盐度表层沉积物中的古细菌主要由古细菌和嗜热球菌组成,在较深的沉积物中过渡为嗜热蛋白酶和脱硫球菌(Staphylothermus sp。)。相比之下,低盐度位点主要由表面的 Thermoplasmatales 和深度的 Thermoproteales 决定。气体和氧化还原化学方法的相似性表明,盐度和/或砷浓度可能会选择可耐受这些参数的微生物群落。许多古细菌16S rRNA序列包含插入片段,可能是内含子,包括 Euryarchaeota 的成员。包含AFG的克隆与 Alpha- Betaproteobacteria 相关,尽管大多数克隆与已发表的代表关系较远。大多数克隆(89%)起源于低盐度,最高砷位点的深层。这是唯一在16S rRNA数据中有重叠的样品,这表明在类似环境中,营养不良是重要的新陈代谢。

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