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盐度对河口沉积物中硫酸盐还原菌汞甲基化活性的影响。

Effect of salinity on mercury-methylating activity of sulfate-reducing bacteria in estuarine sediments.

机构信息

Department of Biochemistry and Microbiology, Cook College, Rutgers University, New Brunswick, New Jersey 08903.

出版信息

Appl Environ Microbiol. 1987 Feb;53(2):261-5. doi: 10.1128/aem.53.2.261-265.1987.

Abstract

The biomethylation of mercury was measured in anoxic estuarine sediments that ranged in salinity from 0.03 to 2.4% with or without added molybdate, an inhibitor of sulfate reducers. Mercury methylation was inhibited by molybdate by more than 95%, regardless of sediment salinity. In the absence of inhibitor, high-salinity sediments methylated mercury at only 40% of the level observed in low-salinity sediments. In response to molybdate inhibition of sulfate reducers, methanogenesis increased up to 258% in high-salinity sediments but only up to 25% in low-salinity sediments. In contrast to an earlier low-salinity isolate, a Desulfovibrio desulfuricans strain from high-salinity sediment required 0.5 M sodium for optimal growth and mercury methylation activity. The formation of negatively charged mercuric chloride complexes at high salinity did not noticeably interfere with the methylation process. Results of these studies demonstrate that sulfate reducers are responsible for mercury methylation in anoxic estuarine sediments, regardless of the prevailing salinity.

摘要

在盐度范围为 0.03 至 2.4%的缺氧河口沉积物中测量了汞的生物甲基化,其中有无添加钼酸盐,钼酸盐是硫酸盐还原菌的抑制剂。无论沉积物的盐度如何,钼酸盐对汞甲基化的抑制作用都超过 95%。在没有抑制剂的情况下,高盐度沉积物中汞的甲基化程度仅为低盐度沉积物中观察到的 40%。作为对硫酸盐还原菌被钼酸盐抑制的响应,高盐度沉积物中的产甲烷作用增加了高达 258%,而低盐度沉积物中仅增加了 25%。与早期低盐度分离株不同,来自高盐度沉积物的脱硫弧菌(Desulfovibrio desulfuricans)菌株需要 0.5 M 钠离子才能实现最佳生长和汞甲基化活性。高盐度下带负电荷的氯化汞络合物的形成并没有明显干扰甲基化过程。这些研究的结果表明,硫酸盐还原菌是缺氧河口沉积物中汞甲基化的原因,而与流行的盐度无关。

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