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Arsenic biogeochemistry in hot springs in Tengchong geothermal area, China

机译:中国腾冲地热区温泉的砷生物园艺

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Arsenic (As) biogeochemistry in acid and alkaline hot springs of Tengchong geothermal area was investigated using Illumina MiSeq sequencing, functional gene clone library and geochemistry analyses. Results showed As(III) could be oxidized to As(V) in the source water of acid hot spring by some putative microbial populations, such as Aquiflcae and Pseudomonas, and then co-deposited with iron at its outflow channel. In sulfide-rich alkaline hot spring, As(III) was firstly derived from thioarsenic transformation probably mediated by Thermocrinis and then oxidized downstream by Thermus and Hydrogenobacter. These results improve our understanding of microbially-mediated As transformation in hot springs.
机译:使用Illumina MiSeq测序,功能基因克隆文库和地球化学分析研究了腾冲地热区域酸和碱热弹簧的砷(AS)生物地球化学。结果显示为(iii)可以通过一些推定的微生物种群(例如Aquiflcae和Pseudomonas)氧化为酸热弹簧源水中的(v),然后在其流出通道上用铁共沉积。在富含硫化物的碱性温泉中,AS(III)首先衍生自Thermocrinis可能介导的硫代醌转化,然后通过热量和氢杆菌氧化下游。这些结果改善了我们对微生物介导的理解作为温泉中的转化。

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