Biology Department, University of Ottawa, 30 Marie Curie, Ottawa, ON, Canada.
Sci Total Environ. 2011 Feb 1;409(5):968-78. doi: 10.1016/j.scitotenv.2010.11.016. Epub 2010 Dec 21.
The activity of various anaerobic microbes, including sulfate reducers (SRB), iron reducers (FeRP) and methanogens (MPA) has been linked to mercury methylation in aquatic systems, although the relative importance of each microbial group in the overall process is poorly understood in natural sediments. The present study focused on the biogeochemical factors (i.e. the relative importance of various groups of anaerobic microbes (FeRP, SRB, and MPA) that affect net monomethylmercury (MMHg) formation in contaminated sediments of the St. Lawrence River (SRL) near Cornwall (Zone 1), Ontario, Canada. Methylation and demethylation potentials were measured separately by using isotope-enriched mercury species ((200)Hg(2+) and MM(199)Hg(+)) in sediment microcosms treated with specific microbial inhibitors. Sediments were sampled and incubated in the dark at room temperature in an anaerobic chamber for 96h. The potential methylation rate constants (K(m)) and demethylation rates (K(d)) were found to differ significantly between microcosms. The MPA-inhibited microcosm had the highest potential methylation rate constant (0.016d(-1)), whereas the two SRB-inhibited microcosms had comparable potential methylation rate constants (0.003d(-1) and 0.002d(-1), respectively). The inhibition of methanogens stimulated net methylation by inhibiting demethylationand by stimulating methylation along with SRB activity. The inhibition of both methanogens and SRB was found to enhance the iron reduction rates but did not completely stop MMHg production. The strong positive correlation between K(m) and Sulfate Reduction Rates (SRR) and between K(d) and Methane Production Rates (MPR) supports the involvement of SRB in Hg methylation and MPA in MMHg demethylation in the sediments. In contrast, the strong negative correlation between K(d) and Iron Reduction Rates (FeRR) shows that the increase in FeRR corresponds to a decrease in demethylation, indicating that iron reduction may influence net methylation in the SLR sediments by decreasing demethylation rather than favouring methylation.
各种厌氧微生物的活性,包括硫酸盐还原菌(SRB)、铁还原菌(FeRP)和产甲烷菌(MPA),与水生系统中的汞甲基化有关,尽管在自然沉积物中,每种微生物群在整个过程中的相对重要性还了解甚少。本研究重点研究了生物地球化学因素(即各种厌氧微生物群(FeRP、SRB 和 MPA)的相对重要性),这些因素影响了加拿大安大略省康沃尔(Zone 1)附近圣劳伦斯河(SRL)受污染沉积物中的净单甲基汞(MMHg)的形成。通过使用同位素富集的汞物种((200)Hg(2+)和 MM(199)Hg(+))在经过特定微生物抑制剂处理的沉积物微宇宙中分别测量甲基化和脱甲基化潜力。沉积物在黑暗中于室温在厌氧室中孵育 96 小时。发现微宇宙之间的潜在甲基化速率常数(K(m))和脱甲基化速率(K(d))有显著差异。MPA 抑制剂微宇宙具有最高的潜在甲基化速率常数(0.016d(-1)),而两个 SRB 抑制剂微宇宙具有可比的潜在甲基化速率常数(分别为 0.003d(-1)和 0.002d(-1))。甲烷菌的抑制通过抑制脱甲基化和刺激与 SRB 活性一起的甲基化来刺激净甲基化。发现抑制甲烷菌和 SRB 均可提高铁还原率,但不能完全阻止 MMHg 的产生。K(m)与硫酸盐还原速率(SRR)之间以及 K(d)与甲烷产生速率(MPR)之间的强正相关支持了 SRB 参与汞甲基化和 MPA 参与沉积物中 MMHg 的脱甲基化。相比之下,K(d)与铁还原速率(FeRR)之间的强负相关表明,FeRR 的增加对应于脱甲基化的减少,这表明铁还原可能通过减少脱甲基化而不是促进甲基化来影响 SLR 沉积物中的净甲基化。