Reed Harris

Whole-ecosystem study shows rapid fish-mercury response to changes in mercury deposition

Methylmercury contamination of fisheries from centuries of industrial atmospheric emissions negatively impacts humans and wildlife worldwide. The response of fish methylmercury concentrations to changes in mercury deposition has been difficult to establish because sediments/soils contain large pools of historical contamination, and many factors in addition to deposition affect fish mercury. To test directly the response of fish contamination to changing mercury deposition, we conducted a whole-ecosystem experiment, increasing the mercury load to a lake and its watershed by the addition of enriched stable mercury isotopes. The isotopes allowed us to distinguish between experimentally applied mercury and mercury already present in the ecosystem and to examine bioaccumulation of mercury deposited to different parts of the watershed. Fish methylmercury concentrations responded rapidly to changes in mercury deposition over the first 3 years of study. Essentially all of the increase in fish methylmercury concentrations came from mercury deposited directly to the lake surface. In contrast, <1% of the mercury isotope deposited to the watershed was exported to the lake. Steady state was not reached within 3 years. Lake mercury isotope concentrations were still rising in lake biota, and watershed mercury isotope exports to the lake were increasing slowly. Therefore, we predict that mercury emissions reductions will yield rapid (years) reductions in fish methylmercury concentrations and will yield concomitant reductions in risk. However, a full response will be delayed by the gradual export of mercury stored in watersheds. The rate of response will vary among lakes depending on the relative surface areas of water and watershed.

Recovery of Mercury-Contaminated Fisheries

Abstract In this paper, we synthesize available information on the links between changes in ecosystem loading of inorganic mercury (Hg) and levels of methylmercury (MeHg) in fish. Although it is widely hypothesized that increased Hg load to aquatic ecosystems leads to increases in MeHg in fish, there is limited quantitative data to test this hypothesis. Here we examine the available evidence from a range of sources: studies of ecosystems contaminated by industrial discharges, observations of fish MeHg responses to changes in atmospheric load, studies over space and environmental gradients, and experimental manipulations. A summary of the current understanding of the main processes involved in the transport and transformation from Hg load to MeHg in fish is provided. The role of Hg loading is discussed in context with other factors affecting Hg cycling and bioaccumulation in relation to timing and magnitude of response in fish MeHg. The main conclusion drawn is that changes in Hg loading (increase or decrease) will yield a response in fish MeHg but that the timing and magnitude of the response will vary depending of ecosystem-specific variables and the form of the Hg loaded.

Temperature, growth and dietary effects on fish mercury dynamics in two Ontario lakes

A bioenergetics-based model was used to investigate the effects of temperature, growth and dietary exposure on methylmercury dynamics in walleye (Stizostedion vitreum) and yellow perch (Perca flavescens) from two lakes sampled in northwestern Ontario. Orange Lake was smaller, warmer, had slower fish growth and higher mercury concentrations in yearling yellow perch and walleye (three fold difference in 40 cm walleye) than Trout Lake. The model was applied to test the hypothesis that higher water temperatures in Orange Lake increased metabolic needs, food consumption and mercury uptake in fish. The effects of different growths rates in the lakes were also considered. Temperature/metabolic effects and growth effects on internal methylmercury dynamics in walleye and perch were predicted to occur but be of secondary importance. Different dietary exposure to methylmercury was likely the dominant source of variation in fish mercury concentrations between the two lakes.

Ecosystem Responses to Mercury Contamination: Indicators of Change

INTRODUCTION Mercury Emissions and Deposition Mercury Concentration Trends in Fish Book Objectives Sampling Strategy AIRSHEDS AND WATERSHEDS Introduction Airsheds Watersheds MONITORING AND EVALUATING TRENDS IN SEDIMENT AND WATER INDICATORS Introduction Sediment and Water Indicators Candidate Indicators Monitoring Strategy Ancillary Data Anticipating Response Times MONITORING AND EVALUATING TRENDS IN METHYLMERCURY ACCUMULATION IN AQUATIC BIOTA Introduction Objectives Aquatic Biological Indicators Monitoring and Trend Analysis Ancillary Data Interpretation of Biological Monitoring Data WILDLIFE INDICATORS Objectives Host Factors Types of Bioindicators Candidate Bioindicator Species Tissue and Other Samples Physiological, Cellular and Molecular Biomarkers Elements of a Biomonitoring Framework Conclusions AN INTEGRATED FRAMEWORK FOR ECOLOGICAL MERCURY ASSESSMENTS Recurring Themes Complexities/Confounding Factors Recommendations Acknowledgements

Mercury transport and fate in the Gulf of Trieste (Northern Adriatic)—a two-dimensional modelling approach

Abstract The Gulf of Trieste is subject to mercury pollution from the Soca River which drains polluted sediments from the region of a former mercury mine in Idrija, Slovenia. This has resulted in elevated mercury levels in some marine organisms. Due to a concern for human health, a study has been undertaken to predict mercury contamination trends through the use of a field program and a mathematical model. An annual mercury mass balance of the Gulf is presented first in the paper. This confirms the assumption of the importance of the particulate mercury loads and sedimentation in the mercury cycle. A two-dimensional (2D) advection-dispersion model for non-conservative pollutants which simulates mercury cycling in the Gulf, is then described. This model incorporates the results of a 2D steady-state, primarily wind-driven hydrodynamic model and a 2D sediment transport model. A coupling of the submodels and verification of the integral mercury cycling model are also presented.

The role of terrestrial vegetation in atmospheric Hg deposition: Pools and fluxes of spike and ambient Hg from the METAALICUS experiment

[1] As part of the Mercury Experiment to Assess Atmospheric Loading in Canada and the U.S. (METAALICUS), different stable Hg(II) isotope spikes were applied to the upland and wetland areas of a boreal catchment between 2001 and 2006 to examine retention of newly deposited Hg(II). In the present study, a Geographical Information Systems (GIS)-based approach was used to quantify canopy and ground vegetation pools of experimentally applied upland and wetland spike Hg within the METAALICUS watershed over the terrestrial loading phase of the experiment. A chemical kinetic model was also used to describe the changes in spike Hg concentrations of canopy and ground vegetation over time. An examination of the fate of spike Hg initially present on canopy vegetation using a mass balance approach indicated that the largest percentage flux from the canopy over one year post-spray was emission to the atmosphere (upland: 45%; wetland: 71%), followed by litterfall (upland: 14%; wetland: 10%) and throughfall fluxes (upland: 12%; wetland: 9%) and longer term retention of spike in the forest canopy (11% for both upland and wetland). Average half-lives (t1/2) of spike on deciduous (110 � 30 days) and coniferous (180 � 40 days) canopy and ground vegetation (890 � 620 days) indicated that retention of new atmospheric Hg(II) on terrestrial (especially ground) vegetation delays downward transport of new atmospheric Hg(II) into the soil profile and runoff into lakes.

Evasion of added isotopic mercury from a northern temperate lake

Isotopically enriched Hg (90% 202Hg) was added to a small lake in Ontario, Canada, at a rate equivalent to approximately threefold the annual direct atmospheric deposition rate that is typical of the northeastern United States. The Hg spike was thoroughly mixed into the epilimnion in nine separate events at two-week intervals throughout the summer growing season for three consecutive years. We measured concentrations of spike and ambient dissolved gaseous Hg (DGM) concentrations in surface water and the rate of volatilization of Hg from the lake on four separate, week-long sampling periods using floating dynamic flux chambers. The relationship between empirically measured rates of spike-Hg evasion were evaluated as functions of DGM concentration, wind velocity, and solar illumination. No individual environmental variable proved to be a strong predictor of the evasion flux. The DGM-normalized flux (expressed as the mass transfer coefficient, k) varied with wind velocity in a manner consistent with existing models of evasion of volatile solutes from natural waters but was higher than model estimates at low wind velocity. The empirical data were used to construct a description of evasion flux as a function of total dissolved Hg, wind, and solar illumination. That model was then applied to data for three summers for the experiment to generate estimates of Hg re-emission from the lake surface to the atmosphere. Based on ratios of spike Hg to ambient Hg in DGM and dissolved total Hg pools, ratios of DGM to total Hg in spike and ambient Hg pools, and flux estimates of spike and ambient Hg, we concluded that the added Hg spike was chemically indistinguishable from the ambient Hg in its behavior. Approximately 45% of Hg added to the lake over the summer was lost via volatilization.

Mercury cycling in the Florida Everglades: a mechanistic field study

Public concern for wildlife and h uman health resulting from mercury (Hg) toxicity has increased substantially since the mid-1980s. In the Florida Everglades, Hg concentrations in excess o f l. 5 mg g(wet weight) in predator fish have been observed and advisories have been issued for human consumption of all fish. Furthermore, elevated H g levels have been identified as a principal factor in the death of at least one Florida panther which had a liver mercury concemration of 110 mg gOoRDAN 1990), and is strongly implicated in rhe dearhs of rwo other panthers (ROELKE et al. 1991). Restorarion plans for eh e Everglades are nearing completion, and efforts to restore more natural conditions will be forthcoming. State o f Florida and federal agencies need to know if changes resulting from rhese restoration activities will exacerbate or mitigate rhe mercury problem in the Everglades. Mercury research projects in rhe Everglades have been focused on quamifYing and idemifYing sources of Hg and evaluating spatial and temporal distributions in water, sediment, and biota. The Florida Atmospheric Mercury Study (GuENTZEL et al. 1995) has shown that armospheric inputs are the dominant input mechanism for Hg to the Everglades. More recemly, the South Florida Atmospheric Mercury Study has attributed elevated Hg concentrations in several Everglades rain event samples to local sources (DvoNCH et al. 1995). Within rhe Everglades, rhe U.S.E.P.A.s Regional Environmental Assessment and Monitoring (REMAP) study has revealed ecosystem-wide trends in mercury and methylmercury in water, sediments and forage fish (Gambusia) (STOBER er al. 1995).