Mercury (Hg)-impaired aquatic ecosystems often receive multiple inputs of different Hg species with varying potentials for transformation and bioaccumulation. Over time these distinct input pools of Hg homogenize in their relative distributions and bioaccumulation potentials as a result of biogeochemical processes and other aging processes within the ecosystem. This study sought to evaluate the relative timescale for homogenization of multiple Hg inputs to wetlands information that is relevant for ecosystem management strategies that consider Hg source apportionment. We performed experiments in simulated freshwater wetland mesocosms that were dosed with four isotopically labeled mercury forms: two dissolved (Hg2+ and Hg-humic acid) and two particulate (nano-HgS and Hg adsorbed to FeS). Over the course of one year we monitored the four Hg isotope endmembers for their relative distribution between surface water sediment and fish in the mesocosms partitioning between soluble and particulate forms and conversion to methylated mercury (MeHg). We also evaluated the reactivity and mobility of Hg through sequential selective extractions (SSE) of sediment and uptake flux of aqueous Hg in diffusive gradient in thin-film (DGT) passive samplers. We observed that the four isotope spikes were relatively similar in surface water concentration (ca. 3000 ng/L) immediately after spike addition. At 1 to 3 months after dosing Hg concentrations were 1 to 50 ng/L and were greater for the initially dissolved isotope endmembers than the initially particulate endmembers. In contrast the Hg isotope endmembers in surface sediments were similar in relative concentration within 2 months after spike addition. However the uptake fluxes of the Hg in DGT samplers deployed in both the water column and surface sediment were generally greater for initially dissolved Hg endmembers and lower for the initially particulate endmembers. At one year post-dosing the DGT-uptake fluxes were converging toward similar values between the Hg isotope endmembers. However the relative distribution of isotope endmembers were still significantly different in both the water column and sediment (p<0.01 according to one-way ANOVA analysis). In contrast SSE resulted in a homogenous distribution with >90% of each endmember extracted in the KOH fraction suggesting that Hg species were associated with sediment organic matter. For MeHg concentrations in surface sediment and fish the relative contributions from each endmember were significantly different at all sampling time points. Altogether these results provide insights to the timescales of distribution for different Hg species that enter a wetland ecosystem. While these inputs attain homogeneity in concentration in primary storage compartments (i.e. sediments) within weeks after addition these input pools remain differentiated for more than one year in terms of reactivity for passive samplers MeHg concentration and bioaccumulation.
