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In groundwater, chemical reactions of Hg(II) with mineral surfaces play an important role in determining the concentration of mercury that is mobile and bioavailable. In this study, we investigated Hg(II) reduction by the ferrous carbonate mineral, siderite (FeCO 3 ), to better understand reductive transformation of mercury in anoxic carbonate-bearing waters. Kinetic experiments and X-ray adsorption spectroscopy (XAS) were conducted to examine the rate and mechanism of Hg(II) reaction with siderite. Hg(II) was reacted with synthesized siderite mineral at various concentrations and the subsequently formed Hg(0) was measured to assess the extent of mercury reduction by siderite. Our experimental data showed that Hg(II) reduction by siderite resulted in the loss of Hg when reacted with siderite mineral suspensions concurrent to formation of gaseous Hg(0). Hg(II) reduction occurred within minutes and reaction rates increased with increasing siderite surface area. XAS analysis confirmed that Hg(II) was reduced to Hg(0) and revealed that reduced mercury was sorbed to siderite surfaces suggesting that electron transfer reactions occur at siderite/water interface. The results of our study suggest that Hg(II) reduction by siderite is a kinetically favorable pathway for the mercury mobilization in ferruginous carbonate-bearing waters.

Surface water and biota from Great Salt Lake (GSL) contain some of the highest documented concentrations of total mercury (THg) and methylmercury (MeHg) in the United States. In order to identify potential biological sources of MeHg and controls on its production in this ecosystem, THg and MeHg concentrations, rates of Hg(II)-methylation and MeHg degradation, and abundances and compositions of archaeal and bacterial 16 rRNA gene transcripts were determined in sediment along a salinity gradient in GSL. Rates of Hg(II)-methylation were inversely correlated with salinity and were at or below the limits of detection in sediment sampled from areas with hypersaline surface water. The highest rates of Hg(II)-methylation were measured in sediment with low porewater salinity, suggesting that benthic microbial communities inhabiting less saline environments are supplying the majority of MeHg in the GSL ecosystem. The abundance of 16S rRNA gene transcripts affiliated with the sulfate reducer Desulfobacterium sp. was positively correlated with MeHg concentrations and Hg(II)-methylation rates in sediment, indicating a potential role for this taxon in Hg(II)-methylation in low salinity areas of GSL. Reactive inorganic Hg(II) (a proxy used for Hg(II) available for methylation) and MeHg concentrations were inversely correlated with salinity. Thus, constraints imposed by salinity on Hg(II)-methylating populations and the availability of Hg(II) for methylation are inferred to result in higher MeHg production potentials in lower salinity environments. Benthic microbial MeHg degradation was also most active in lower salinity environments. Collectively, these results suggest an important role for sediment anoxia and microbial sulfate reducers in the production of MeHg in low salinity GSL sub-habitats and may indicate a role for salinity in constraining Hg(II)-methylation and MeHg degradation activities by influencing the availability of Hg(II) for methylation.

Estuarine sediments support the production of monomethylmercury (MeHg) which accumulates in aquatic organisms. While natural variation in mercury stable isotope ratios can potentially be used to track sources and transformations of mercury in the environment, the isotopic signature of MeHg in sediments has not been measured directly. The isotopic composition of MeHg has been studied in laboratory experiments and fish using tandem gas chromatography-multicollector inductively coupled plasma mass spectrometry (MC–ICP-MS) systems; however, the precision and sensitivity of this method may be too low for the analysis of many environmental samples including sediments in which MeHg constitutes 1% or less of the total mercury. In this study, we developed an offline separation method for the precise measurement of the Hg isotopic composition of MeHg in estuarine sediments. Separation of MeHg from inorganic species was accomplished by distillation and chemical ethylation-GC, and was followed by gold amalgam trapping to collect and preconcentrate pyrolyzed MeHg, which was then released into an oxidizing solution. MeHg standards processed in this way were collected with an average yield of 97.5%. External precision for all replicate isotope analyses of MeHg process standards was ± 0.14‰ (2 SD, n = 8) for δ202Hg and no detectable fractionation of Hg stable isotopes occurred during the separation. δ202Hg values for MeHg separated from estuarine sediments using our approach varied from − 0.41 to + 0.41‰ and were generally higher, and spatially and temporally more variable, than those for total Hg (− 0.21 to − 0.48‰).

Redox cycling between elemental [Hg(0)] and divalent [Hg(II)] mercury is a key control on the fate and transport of Hg in groundwater systems. In this study, we tested the ability of anaerobic bacteria to oxidize dissolved Hg(0) to Hg(II). Controlled laboratory experiments were carried out with the obligate anaerobic bacterium Geothrix fermentans H5, and the facultative anaerobic bacteria Shewanella oneidensis MR-1 and Cupriavidus metallidurans AE104. Under anoxic conditions, all three bacterial strains reacted with dissolved gaseous Hg(0) to form non-purgeable Hg. In mass balance experiments, the formation of non-purgeable Hg corresponded to the loss of volatile Hg. To determine if the non-purgeable Hg was oxidized, we performed ethylation experiments on Hg(0)-reacted cell suspensions and X-ray absorption near edge structure (XANES) spectroscopy on Hg(0)-reacted cells. Derivatization of non-purgeable Hg to diethylmercury and the Hg L III -edge position of the XANES spectra demonstrated that the reacted bacterial samples contained Hg(II). XANES analysis also revealed that cell-associated Hg(II) was covalently bound to bacterial functional groups, most likely to thiol moieties. Finally, experiments with metabolically active and heat-inactivated cells indicated that both live and dead cells oxidized Hg(0) to Hg(II). Hg(0) oxidation rates for metabolically active cultures increase in the order S. oneidensis MR-1 (1.6 × 10 − 4 fg/cell/min), C. metallidurans AE104 (2.5 × 10 − 4 fg/cell/min), and G. fermentans H5 (23.1 × 10 − 4 fg/cell/min). The results of this study suggest that reactivity towards Hg(0) is widespread among diverse anaerobic bacteria, and passive microbial oxidation of Hg(0) may play an important role in the redox transformation of mercury contaminants in subsurface environments.

The transformation of inorganic mercury (Hg) to methylmercury (MeHg) plays a key role in determining the amount of Hg that is bioaccumulated in aquatic food chains. An accurate knowledge of Hg methylation mechanisms is required to predict the conditions that promote MeHg production in aquatic environments. In this study, we conducted experiments to examine the oxidation and methylation of dissolved elemental mercury [Hg(0)] by the anaerobic bacterium Desulfovibrio desulfuricans ND132. Anoxic cultures of D. desulfuricans ND132 were exposed to Hg(0) in the dark, and samples were collected and analyzed for the loss of Hg(0), formation of non-purgeable Hg, and formation of MeHg over time. We found that D. desulfuricans ND132 rapidly transformed dissolved gaseous mercury into non-purgeable Hg, with bacterial cultures producing approximately 40 μg/L of non-purgeable Hg within 30 min, and as much as 800 μg/L of non-purgeable Hg after 36 h. Derivatization of the non-purgeable Hg in the cell suspensions to diethylmercury and analysis of Hg(0)-reacted D. desulfuricans ND132 cells using X-ray absorption near edge structure (XANES) spectroscopy demonstrated that cell-associated Hg was dominantly in the oxidized Hg(II) form. Spectral comparisons and linear combination fitting of the XANES spectra indicated that the oxidized Hg(II) was covalently bonded to cellular thiol functional groups. MeHg analyses revealed that D. desulfuricans ND132 produced up to 118 μg/L of methylmercury after 36 h of incubation. We found that a significant fraction of the methylated Hg was exported out of the cell and released into the culture medium. The results of this work demonstrate a previously unrecognized pathway in the mercury cycle, whereby anaerobic bacteria produce MeHg when provided with dissolved Hg(0) as their sole Hg source.

Mercury (Hg) is a trace metal with potentially serious public health consequences, especially when its neurotoxic form, monomethylmercury (MMHg), accumulates in aquatic and terrestrial food chains. Given the variation in Hg stable isotope abundances (up to 6‰ in δ 202/198 Hg and 11‰ in Δ 201/198 Hg) in natural environmental samples and evidence for Hg isotopic fractionation during microbial (e.g., reduction of Hg(II), degradation and formation of MMHg) and abiotic processes (e.g., photo-degradation of MMHg and volatilization, evaporation and diffusion of Hg(0)), Hg isotope biogeochemistry is currently being developed as a tool to study sources, sinks, and transformations of Hg in the environment. The use of Hg stable isotopes to identify sources of MMHg in aquatic and terrestrial food chains depends on the knowledge of reasonably precise fractionation factors for individual Hg transformations that influence speciation and accumulation of Hg. Microbial transformations are critical to the formation of MMHg and Hg(0) and to the degradation of MMHg. This article a) highlights the importance of experimental determination of microbial fractionation factors for the development of Hg stable isotope systematics because of the limitations of theoretical calculations; b) provides a summary of the current understanding of microbial stable isotope fractionation of Hg, especially during kinetically controlled processes; and c) demonstrates the various factors likely to affect cell-level fractionation during microbial transformations through use of an iterative finite-step model. We also identify future directions, conditions and controls that could help rigorously advance the development of mass-dependent Hg isotope systematics at the enzymatic, cellular and ecosystem level.

Metals are toxic to both plants and fungi, and elevated soil metal concentrations have been documented to change the structure of ectomycorrhizal communities. Mercury (Hg) is a highly toxic metal and inhibits the growth of ectomycorrhizal fungi (ECMF) in axenic culture. However, the effects of Hg on the growth of tree seedlings and the development of their ECMF communities have not been explored. In the current study, Pinus rigida seedlings were planted in soil amended with 0–366 μg g −1 Hg and incubated for 5 months. Survival and growth of P. rigida seedlings was determined, and their ECMF communities were characterized by morphotype analysis. Seedling survival declined with increasing Hg additions, although no reduction in growth was detected among surviving seedlings. The addition of 88 μg g −1 Hg to soil more than halved the total ectomycorrhizal colonization of root tips and reduced both richness and diversity of root tip morphotypes, while lower Hg additions did not significantly affect ECMF community composition relative to the no Hg control. This suggests that changes in the community of ECMF may occur in contaminated soils before any aboveground effects on surviving seedlings are noticeable, potentially altering the contribution of ECMF to the fitness of established host plants.

Heavy metals have been shown to negatively affect the growth of ectomycorrhizal fungi (ECMF). In addition, ECMF have been shown to accumulate heavy metals and to protect host trees from metal toxicity. However, specific literature on the interactions between ECMF and mercury (Hg) is scant. This paper describes the responses of ECMF to Hg in axenic culture conditions. Six ECMF from an area with no known history of direct Hg contamination were tested to determine their sensitivity to Hg. ECMF were incubated on solid medium amended with Hg (0–50 μM) as HgCl 2 and the effect of Hg on radial growth was determined. The effect of preexposure cultivation on Hg sensitivity, the effect of Hg on biomass production, and the ability to accumulate Hg were determined for four of the ECMF. At micromolar concentrations, Hg significantly inhibited the radial growth rate of ECMF. This inhibitory effect was lessened in some ECMF when an established colony was exposed to Hg. Mercury lowered biomass production by some ECMF, and ECMF accumulate Hg from a solid growth substrate in direct relation to the amount of Hg added to the media. Possible implications for ECMF communities in Hg-impacted areas are discussed.

Controlling bioaccumulation of toxic monomethylmercury (MMHg) in aquatic food chains requires differentiation between biotic and abiotic pathways that lead to its production and degradation. Recent mercury (Hg) stable isotope measurements of natural samples suggest that Hg isotope ratios can be a powerful proxy for tracing dominant Hg transforming pathways in aquatic ecosystems. Specifically, it has been shown that photo-degradation of MMHg causes both mass dependent (MDF) and mass independent fractionation (MIF) of Hg isotopes. Because the extent of MDF and MIF observed in natural samples (e.g., fish, soil and sediments) can potentially be used to determine the relative importance of pathways leading to MMHg accumulation, it is important to determine the potential role of microbial pathways in contributing to the fractionation, especially MIF, observed in these samples. This study reports the extent of fractionation of Hg stable isotopes during degradation of MMHg to volatile elemental Hg and methane via the microbial Hg resistance (mer) pathway in Escherichia coli carrying a mercury resistance (mer) genetic system on a multi-copy plasmid. During experimental microbial degradation of MMHg, MMHg remaining in reactors became progressively heavier (increasing δ202Hg) with time and underwent mass dependent Rayleigh fractionation with a fractionation factor α202/198 = 1.0004 ± 0.0002 (2SD). However, MIF was not observed in any of the microbial MMHg degradation experiments indicating that the isotopic signature left by mer mediated MMHg degradation is significantly different from fractionation observed during DOC mediated photo-degradation of MMHg. Additionally, a clear suppression of Hg isotope fractionation, both during reduction of Hg(II) and degradation of MMHg, was observed when the cell densities increased, possibly due to a reduction in substrate bioavailability. We propose a multi-step framework for understanding the extent of fractionation seen in our MMHg degradation experiments and, based on estimates of the rates of the various steps involved in this mer mediated pathway, suggest which steps in the process could contribute towards the observed extent of fractionation. This framework suggests that at lower cell densities catalysis by MerB was the rate limiting step while at higher cell densities transport into the cell, which does not cause fractionation, became the rate limiting step. In addition to presenting evidence for absence of MIF during mer mediated Hg transformations, based on the nature of Hg compounds and microbe–Hg interactions, we suggest that the nuclear spin dependent MIF (i.e., the magnetic isotope effect) is also unlikely to occur during other non mer mediated ‘dark’ microbial Hg transformations (e.g., formation of MMHg and oxidative degradation of MMHg). Because of the important implications of the absence of MIF during biological processes on Hg isotope systematics, we discuss theoretical considerations and experimental strategies that could be used to confirm this suggestion.

Recent demonstrations of the removal and immobilization of inorganic contaminants by microbial transformations, sorption and mineralization show the potential of both natural and engineered microbes as bioremedial tools. Demonstrations of microbe-mediated mineral formation in biofilms implicate this mode of microbial life in geological evolution and remediation of inorganic contaminants.

The Idrija Mine is the second largest Hg mine in the world which operated for 500 years. Mercury (Hg)-laden tailings still line the banks, and the system is a threat to the Idrija River and water bodies downstream including the Soca/Isonzo River and the Gulf of Trieste in the northern Adriatic Sea. A multidisciplinary study was conducted in June 1998 on water samples collected throughout the Idrija and Soca River systems and waters and sediments in the Gulf. Total Hg in the Idrija River increased >20-fold downstream of the mine from 60 ng liter(-1) with methyl mercury (MeHg) accounting for approximately 0.5%. Concentrations increased again downstream and into the estuary with MeHg accounting for nearly 1.5% of the total. While bacteria upstream of the mine did not contain mercury detoxification genes (mer), such genes were detected in bacteria collected downstream. Benthic macroinvertebrate diversity decreased downstream of the mine. Gulf waters near the river mouth contained up to 65 ng liter(-1) total Hg with approximately 0.05 ng liter(-1) MeHg. Gulf sediments near the river mouth contained 40 microgram g(-1) total Hg with MeHg concentrations of about 3 ng g(-1). Hg in sediment pore waters varied between 1 and 8 ng liter(-1), with MeHg accounting for up to 85%. Hg methylation and MeHg demethylation were active in Gulf sediments with highest activities near the surface. MeHg was degraded by an oxidative pathway with >97% C released from MeHg as CO(2). Hg methylation depth profiles resembled profiles of dissolved MeHg. Hg-laden waters still strongly impact the riverine, estuarine, and marine systems. Macroinvertebrates and bacteria in the Idrija River responded to Hg stress, and high Hg levels persist into the Gulf. Increases in total Hg and MeHg in the estuary demonstrate the remobilization of Hg, presumably as HgS dissolution and recycling. Gulf sediments actively produce MeHg, which enters bottom waters and presumably the marine food chain.

A previously described bioassay using a mer-lux gene fusion for detection of bioavailable mercury was applied for the estimation of the bioavailable fraction of mercury in soil. The bioavailable fraction is defined here as being part of the water leachable fraction. Due to masking of light emission of soil particles leachates had to be cleaned prior to assays. Filtration of leachates through nitro-cellulose filters using pressure resulted in an underestimation of bioavailable mercury. Gravity filtration and centrifugation showed elevated (as compared with untreated leachate) and very similar responses. The utility of the mer-lux biosensor assay was tested by relating measurements of bioavailable and total mercury to the response of the soil microbial community to mercury exposure. Two different soil types (an agricultural and a beech forest soil) were spiked with 2.5 μg Hg(II) g−1 in microcosms and the frequency of mercury resistant heterotrophs and changes in community diversity, defined as the number of different 16S rDNA bands observed in DGGE gels, were monitored. In the agricultural soil the initial concentration of bioavailable mercury was estimated to be 40 ng g−1. This concentration did not change during the first 3 d and coincided with increased degrees of resistance and a decrease in diversity. The concentration of bioavailable mercury decreased subsequently rapidly and remained just above the detection level (0.2 ng g−1) for the remainder of the experiment. As a possible consequence of the decreased selection pressure of mercury, the resistance and diversity gradually returned to pre-exposure amounts. In the beech forest soil the concentration of bioavailable mercury was found to be about 20 ng g−1 throughout the experiment. This concentration did not at any time result in changes in resistance or diversity. This study showed that the bioassay using the mer-lux biosensor is a useful and sensitive tool for estimation of bioavailable mercury in soil.

A new method for the isolation of intracellular and extacellular DNA from a range of sediment types has been developed. This method is based upon the direct lysis of cells in the sediment, extraction of released DNA from the sediments and its subsequent purification by CsCL-EtBr gradient centrifugation and/or hydroxyapatite chromatography. Yields of 26 μg intracellular DNA and 1 μg extracellular DNA have been obtained per gram of sediment.