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在受到实验性硫酸盐负荷的淡水沉积物中,微生物群落的多样性使汞甲基化。

Diverse Communities of Microorganisms Methylate Mercury in Freshwater Sediments Subjected to Experimental Sulfate Loading.

机构信息

BioTechnology Institute, University of Minnesota, Saint Paul 55108, Minnesota, United States.

Department of Earth and Environmental Sciences, University of Minnesota, Minneapolis 55455, Minnesota, United States.

出版信息

Environ Sci Technol. 2020 Nov 17;54(22):14265-14274. doi: 10.1021/acs.est.0c02513. Epub 2020 Nov 2.

DOI:10.1021/acs.est.0c02513
PMID:33138371
Abstract

Methylmercury (MeHg) is a bioaccumulative neurotoxin produced by certain sulfate-reducing bacteria and other anaerobic microorganisms. Because microorganisms differ in their capacity to methylate mercury, the abundance and distribution of methylating populations may determine MeHg production in the environment. We compared rates of MeHg production and the distribution of genes in epilimnetic sediments from a freshwater lake that were experimentally amended with sulfate levels from 7 to 300 mg L. The most abundant sequences were associated with clades of , sulfate-reducing , , and unknown environmental sequences. The communities from higher sulfate amendments were less diverse and had relatively more , whereas the communities from lower amendments were more diverse with a larger proportion of sequences affiliated with other clades. Potential methylation rate constants varied 52-fold across the experiment. Both potential methylation rate constants and % MeHg were the highest in sediments from the lowest sulfate amendments, which had the most diverse communities and relatively fewer genes from clades associated with sulfate reduction. Although pore water sulfide concentration covaried with diversity across our experimental sulfate gradient, major changes in the community of organisms occurred prior to a significant buildup of sulfide in pore waters. Our results indicate that methylating communities dominated by diverse anaerobic microorganisms that do not reduce sulfate can produce MeHg as effectively as communities dominated by sulfate-reducing populations.

摘要

甲基汞(MeHg)是由某些硫酸盐还原菌和其他厌氧微生物产生的生物累积性神经毒素。由于微生物将汞甲基化的能力不同,甲基化种群的丰度和分布可能决定环境中 MeHg 的产生。我们比较了来自淡水湖上覆水沉积物中 MeHg 产生速率和基因分布,这些沉积物通过实验添加了 7 至 300mg/L 的硫酸盐。最丰富的序列与硫酸盐还原菌、拟杆菌门、疣微菌门和未知环境序列的分支有关。高硫酸盐添加组的微生物群落多样性较低,相对更多的是 ,而低硫酸盐添加组的微生物群落多样性较高,与其他分支相关的 序列比例较大。潜在的甲基化速率常数在整个实验中变化了 52 倍。潜在的甲基化速率常数和 %MeHg 在硫酸盐添加最低的沉积物中最高,这些沉积物中的微生物群落多样性最高,与硫酸盐还原相关的分支的 基因相对较少。尽管孔隙水中的硫化物浓度与我们实验硫酸盐梯度上的 多样性相关,但在孔隙水中硫化物大量积累之前,微生物群落中的主要变化就已经发生。我们的结果表明,以不还原硫酸盐的多样化厌氧微生物为主导的甲基化群落可以像以硫酸盐还原种群为主导的群落一样有效地产生 MeHg。

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