Wang Yanhong, Li Ping, Jiang Zhou, Liu Han, Wei Dazhun, Wang Helin, Wang Yanxin
State Key Laboratory of Biogeology and Environmental Geology, China University of Geosciences, Wuhan, China.
School of Environmental Studies, China University of Geosciences, Wuhan, China.
Ecotoxicology. 2018 Oct;27(8):1047-1057. doi: 10.1007/s10646-018-1958-9. Epub 2018 Jun 28.
Arsenic methylation is regarded as an effective way of arsenic detoxification. Current knowledge about arsenic biomethylation in high arsenic groundwater remains limited. In the present study, 16 high arsenic groundwater samples from deep wells of the Hetao Plain were investigated using clone library and quantitative polymerase chain reaction (qPCR) analyses of arsM genes as well as geochemical analysis. The concentrations of methylated arsenic (including monomethylarsonic acid (MMA) and dimethylarsinic acid (DMA)) varied from 2.40 to 16.85 μg/L. Both bacterial and archaeal arsenic methylating populations were detected in the high arsenic aquifer. They were dominated by Proteobacteria, Firmicutes, Gemmatimonadetes, Nitrospirae, Methanomicrobia and a large unidentified group. The abundances of predominant populations were correlated positively to either total organic carbon or total arsenic and arsenite concentrations. The arsM gene abundances in high arsenic groundwater ranged from below detection to 5.71 × 10 copies/L and accounted for 0-3.32‰ of total bacterial and archaeal 16S rRNA genes. The arsM gene copies in high arsenic groundwater showed closely positive correlations with methylated arsenic concentrations. The overall results implied that arsenic methylating microorganisms were abundant and diverse in high arsenic groundwater. This was the first study of arsenic methylating microbial communities in high arsenic groundwater aquifers and might provide useful information for arsenic bioremediation in groundwater systems.
砷甲基化被视为一种有效的砷解毒方式。目前关于高砷地下水中砷生物甲基化的认识仍然有限。在本研究中,利用克隆文库、arsM基因的定量聚合酶链反应(qPCR)分析以及地球化学分析,对河套平原深井中的16个高砷地下水样本进行了调查。甲基化砷(包括一甲基砷酸(MMA)和二甲基砷酸(DMA))的浓度在2.40至16.85μg/L之间变化。在高砷含水层中检测到了细菌和古菌的砷甲基化菌群。它们主要由变形菌门、厚壁菌门、芽单胞菌门、硝化螺旋菌门、甲烷微菌目以及一个大量未鉴定的类群组成。优势菌群的丰度与总有机碳或总砷及亚砷酸盐浓度呈正相关。高砷地下水中arsM基因的丰度范围从低于检测限到5.71×10拷贝/L,占细菌和古菌16S rRNA基因总数中的0 - 3.32‰。高砷地下水中arsM基因拷贝数与甲基化砷浓度呈密切正相关。总体结果表明,高砷地下水中砷甲基化微生物丰富多样。这是首次对高砷地下水含水层中砷甲基化微生物群落进行的研究,可能为地下水系统中的砷生物修复提供有用信息。