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projects > integrated biogeochemical studies in the everglades: nutrients and sulfur > abstract


Sulfur, a Key Water Quality Issue in the Everglades

W 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
2tlerch@usgs.gov U.S. Geological Survey, 956 National Center, Reston, VA 20194 United States
3abates@usgs.gov U.S. Geological Survey, 956 National Center, Reston, VA 20194 United States
4mcorum@usgs.gov U.S. Geological Survey, 956 National Center, Reston, VA 20194 United States
5mbeck@usgs.gov U.S. Geological Survey, 956 National Center, Reston, VA 20194 United States
6kleckner@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
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Last updated: 11 October, 2002 @ 09:30 PM (KP)