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projects > integrated biogeochemical studies in the everglades: nutrients and sulfur > abstract
Sulfur, a Key Water Quality Issue in the EvergladesW H Orem1, H E Lerch2, A L Bates3, M Corum4, M Beck5, S Kleckner6 Abstract from the 2002 Spring AGU Meeting.
Sulfur is an important water quality issue in the Everglades because of its role in microbial sulfate reduction and the
methylation of mercury. Methylmercury (MeHg), a neurotoxin that is bioaccumulated, has been found in high concentrations in
freshwater fish from the Everglades, and poses a potential threat to fish-eating wildlife and to human health through fish
consumption. Sulfur appears to play a key role in regulating both the magnitude and distribution of MeHg in the Everglades.
Freshwater wetlands typically have low sulfur concentrations, but marshes in portions of the northern Everglades have average
surface water sulfate concentrations of 60 mg/l, compared to 1 mg/l or less at background sites. Marsh areas with excess
sulfate are concentrated near sites of canal discharge and along canal levees. The canal water that is discharged into the
marshes appears to be the major source of excess sulfate entering the Everglades. This canal water drains the Everglades
Agricultural Area (EAA) and has sulfate concentrations averaging over 70 mg/l and periodically approaching 200 mg/l. We used
sulfate concentration data and the sulfur (d34S) isotopic composition of sulfate in marsh surface water, canal water,
rainwater, and groundwater to trace the source of the excess sulfate entering the Everglades. Results show that canal water
from the EAA is the major source of excess sulfate entering the Everglades. Furthermore, canal water with the highest sulfate
concentrations had d34S values of +16 per mil, similar to the d34S signature of agricultural sulfur used as a soil
amendment in the EAA. Rainwater has too little sulfate to account for the high sulfate concentrations observed in the canals
and in large portions of the Everglades. Groundwater beneath the present day Everglades generally has either too low a
sulfate concentration or a d34S signature that is inconsistent with that of surface water in the Everglades.
The excess sulfate entering the Everglades from canal discharge stimulates sulfate reduction and sulfide buildup in the
sediments. This lowers redox potentials in sulfur-contaminated areas to values more reducing than natural, which may affect
macrophyte growth in the Everglades by limiting oxygen penetration to roots. Excess sulfur has two differential effects with
respect to MeHg production: stimulation through increased sulfate reduction, and inhibition through buildup of excess sulfide
in sediment porewater. The balance between these two effects influences the magnitude and distribution of MeHg production in
the Everglades. Results from this study and research of others suggest that the MeHg problem in the Everglades results
largely from two factors: (1) increased fallout of mercury on the ecoxyxtem, and (2) sulfur contamination of the ecosystem
from agricultural runoff.
1borem@usgs.gov
U.S. Geological Survey, 956 National Center, Reston, VA 20194 United States
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| U.S. Department of the Interior, U.S. Geological Survey, Center for Coastal Geology This page is: http://sofia.usgs.gov /projects/int_geochem_nutrients/abstract-agu02.html Comments and suggestions? Contact: Heather Henkel - Webmaster Last updated: 11 October, 2002 @ 09:30 PM (KP) |