Levels of methylmercury and controlling factors in surface sediments of the Carson River system, Nevada

Spatial and temporal distribution of methylmercury (MeHg) was determined in surficial sediments collected from a river-reservoir system impacted by Hg-contaminated mine wastes. Despite the fact that total mercury concentrations (HgT) in surface sediments of the Carson River system were in the microg.g(-1) range, levels of MeHg varied from about 2 to 28 ngHg.g(-1) dry weight, representing less than 3% of Hg(T). Concentrations of MeHg were well correlated with both the biotic (r=0.95) and abiotic activity (r=0.85) of the sediment, determined as the ability of each compartment to specifically reduce an alternative electron acceptor. However, the positive relationship between the two measured activities suggests that the abiotic activity may be due to reductant substances produced by micro-organisms. When sediments collected from the Carson River were used in laboratory assays for the determination of potential rates of MeHg production, the addition of inorganic Hg (added as HgCl2) resulted in increased rates of methylation when the spike concentration was lower or equal to 15.3 microg.g(-1) dry weight. This trend was reversed for spike concentration of inorganic Hg above 15.3 microg.g(-1). The reduction of methylation rate was associated with an inhibition of microbial activity. These observations suggest that seasonal inputs into the river of significant amounts of inorganic Hg eroded from mill tailings during winter and spring flooding events could have an inhibiting effect on Hg-methylating micro-organisms. This observation could explain the low MeHg]/HgT] ratios previously documented in waters of the Carson River system.