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Depth-resolved abundance and diversity of arsenite-oxidizing bacteria in the groundwater of Beimen, a blackfoot disease endemic area of southwestern Taiwan

机译:台湾西南部黑脚病流行地区北门市地下水中深度分解的砷氧化细菌的丰富度和多样性

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摘要

The role of arsenite oxidizers in natural attenuation of arsenic pollution necessitates studies on their abundance and diversity in arsenic-contaminated aquifers. In this study, most probable number-polymerase chain reaction (MPN-PCR) and denaturing gradient gel electrophoresis (DGGE) was applied to monitor depth-wise abundance and diversity of aerobic arsenite oxidizers in arsenic-enriched groundwater of Beimen, southwestern Taiwan. The results revealed that the abundance of arsenite oxidizers ranged from 0.04 to 0.22, and the lowest ratio was observed in the most arsenic-enriched and comparatively more reduced groundwater (depth 200 m) of Beimen 1. The highest ratio was observed in the less arsenic-enriched and less reduced groundwater (depth 60 m) of Beimen 2B. DGGE profiles showed a shift in diversity of arsenite oxidizers, consisting of members of the Betaproteobacteria (61%), Alphaproteobacteria (28%) and Gammaproteobacteria (11%), depending on mainly arsenic concentration and redox level in groundwater. Groundwater with the lowest arsenic and highest dissolved oxygen at Beimen 2B harbored 78% of the arsenite oxidizers communities, while groundwater with the highest arsenic and lowest dissolved oxygen at Beimen 1 and Beimen-Jinhu harbored 17 and 22% of arsenite oxidizers communities, respectively. Pseudomonas sp. was found only in groundwater containing high arsenic at Beimen 1 and Beimen-Jinhu, while arsenite oxidizers belonging to Alpha- and Betaproteobacteria were dominated in groundwater containing low arsenic.
机译:砷氧化剂在自然减少砷污染中的作用,需要研究砷污染含水层中的含量和多样性。在这项研究中,最可能的数量聚合酶链反应(MPN-PCR)和变性梯度凝胶电泳(DGGE)用于监测台湾西南部北门富砷地下水中需氧亚砷氧化剂的深度深度丰度和多样性。结果表明,砷氧化剂的丰度范围为0.04至0.22,在砷含量最高且相对减少的北门1号地下水(深度200 m)中,比率最低,而砷含量较低的比率最高。 -富集而减少的北门2B地下水(深度60 m)。 DGGE曲线显示了砷氧化剂的多样性变化,其主要由地下水中的砷浓度和氧化还原水平决定,其中包括β变形细菌(61%),α变形细菌(28%)和γ变形细菌(11%)。北门2B砷含量最低,溶解氧最高的地下水占砷氧化物氧化剂群落的78%,而北门1号和北门金湖地区砷含量最高,溶解氧含量最低的地下水分别具有砷氧化物氧化剂的17%和22%。假单胞菌仅在北门1和北门-金湖的高砷地下水中发现了这种元素,而在低砷的地下水中则占主导地位的是阿尔法和贝塔蛋白菌的亚砷酸盐氧化剂。

著录项

  • 来源
    《Water Research》 |2013年第19期|6983-6991|共9页
  • 作者单位

    Department of Earth Sciences, National Cheng Kung University, Tainan 70101, Taiwan;

    Department of Earth Sciences, National Cheng Kung University, Tainan 70101, Taiwan;

    Department of Earth Sciences, National Cheng Kung University, Tainan 70101, Taiwan;

    Department of Microbiology and Biotechnology Centre, The Maharaja Sayajirao University of Baroda, Vadodara 390002, Gujarat, India;

    Department of Earth Sciences, National Cheng Kung University, Tainan 70101, Taiwan;

    Department of Microbiology and Immunology, Medical College, National Cheng Kung University, Tainan, Taiwan;

    National Centre for Engineering in Agriculture, University of Southern Queensland, Toowoomba, Australia;

  • 收录信息 美国《科学引文索引》(SCI);美国《工程索引》(EI);
  • 原文格式 PDF
  • 正文语种 eng
  • 中图分类
  • 关键词

    Groundwater arsenic; Arsenite oxidizing bacteria; PCR-DGGE; MPN-PCR;

    机译:地下水砷;砷氧化细菌;PCR-DGGE;聚合酶链反应;

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