Department of Earth Sciences, University of Southern California Los Angeles, CA, USA.
Front Microbiol. 2013 Jul 9;4:158. doi: 10.3389/fmicb.2013.00158. eCollection 2013.
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.
相分离是海底热液喷口普遍存在的过程,形成了大范围的盐度。有毒元素(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。然而,与相分离相关的微生物多样性研究很少。我们通过对米洛斯岛(希腊)富砷浅海喷口两个具有相似 pH 值和温度但盐度差异明显的喷口的 16S rRNA 克隆序列的比较分析,评估了富砷浅海喷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(0-1.5cm)中的细菌主要为 ε 变形菌(Arcobacter sp.),在10cm 深处几乎全部为厚壁菌(Bacillus sp.)。然而,低盐度位点的表面为黄杆菌(Flavobacteria),在10cm 深处为 ε 变形菌(Arcobacter sp.)。高盐度表面沉积物中的古菌主要由古菌目和热球菌目组成,在更深的沉积物中转变为热脱硫球菌目和脱硫球菌目(Staphylothermus sp.)。相比之下,低盐度位点的表面主要为热原体目,深部为热球菌目。相似的气体和氧化还原化学表明,盐度和/或砷浓度可能选择了能够耐受这些参数的微生物群落。许多古菌 16S rRNA 序列含有插入物,可能是内含子,包括广古菌的成员。含有 AFG 的克隆与 α-或 β-变形菌有关,尽管大多数与已发表的代表只有远缘关系。大多数克隆(89%)来自低盐度、最高砷含量的深部。这是唯一具有 16S rRNA 数据重叠的样本,表明砷营养作用是类似环境中重要的代谢途径。