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受酸沉降影响的水生系统中的汞甲基化。

Mercury methylation in aquatic systems affected by acid deposition.

作者信息

Gilmour C C, Henry E A

机构信息

Academy of Natural Sciences, Benedict Estuarine Research Laboratory, Benedict, MD 20612, USA.

出版信息

Environ Pollut. 1991;71(2-4):131-69. doi: 10.1016/0269-7491(91)90031-q.

Abstract

Recently, it has been noted that fish in acidified lakes may contain elevated levels of mercury. While there is correlation among lakes between depressed pH and high mercury concentrations in fish, the cause of this problem is unknown. A number of hypotheses have been advanced in explanation, including increased mercury deposition, changes in mercury mobility due to acidification, pH dependent changes in mercury uptake by biota, and alterations in population size and/or structure which result in increased bioaccumulation in fish. Because fish accumulate mercury mainly in an organic form, methylmercury, changes in the biogeochemical cycling of this compound might account for elevated bioaccumulation. Mercury methylation is predominantly a microbial process which occurs in situ in lakes. This review focuses on microbiological and biogeochemical changes that may lead to increased levels of methylmercury in fresh waters impacted by acid-deposition. In particular, we focus on the hypothesis that sulfate-reducing bacteria are important mediators of metal methylation in aquatic systems and, moreover, that sulfate-deposition may stimulate methylmercury production by enhancing the activity of sulfate-reducing bacteria in sediments.

摘要

最近,人们注意到酸化湖泊中的鱼类可能含有较高水平的汞。虽然湖泊的pH值降低与鱼类体内高汞浓度之间存在相关性,但这个问题的成因尚不清楚。已经提出了一些假说来解释,包括汞沉积增加、酸化导致汞迁移性的变化、生物群对汞的吸收因pH值而变化,以及种群数量和/或结构的改变导致鱼类生物累积增加。由于鱼类主要以有机形式(甲基汞)积累汞,这种化合物生物地球化学循环的变化可能是生物累积增加的原因。汞甲基化主要是一个微生物过程,发生在湖泊中。本综述重点关注可能导致受酸沉降影响的淡水中甲基汞水平升高的微生物和生物地球化学变化。特别是,我们关注这样一种假说,即硫酸盐还原菌是水生系统中金属甲基化的重要介质,此外,硫酸盐沉降可能通过增强沉积物中硫酸盐还原菌的活性来刺激甲基汞的产生。

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