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Spatial and Seasonal Variability of Dissolved Methylmercury in Two Stream Basins in the Eastern United States
Author(s) -
Paul M. Bradley,
Douglas A. Burns,
Karen Riva Murray,
Mark E. Brigham,
Daniel T. Button,
Lia C. Chasar,
Mark Marvin-DiPasquale,
Mark A. Lowery,
Celeste A. Journey
Publication year - 2011
Publication title -
environmental science and technology
Language(s) - English
Resource type - Journals
SCImago Journal Rank - 2.851
H-Index - 397
eISSN - 1520-5851
pISSN - 0013-936X
DOI - 10.1021/es103923j
Subject(s) - methylmercury , wetland , floodplain , environmental science , hydrology (agriculture) , streams , drainage basin , channel (broadcasting) , ecology , geology , geography , bioaccumulation , biology , computer network , geotechnical engineering , cartography , engineering , computer science , electrical engineering
We assessed methylmercury (MeHg) concentrations across multiple ecological scales in the Edisto (South Carolina) and Upper Hudson (New York) River basins. Out-of-channel wetland/floodplain environments were primary sources of filtered MeHg (F-MeHg) to the stream habitat in both systems. Shallow, open-water areas in both basins exhibited low F-MeHg concentrations and decreasing F-MeHg mass flux. Downstream increases in out-of-channel wetlands/floodplains and the absence of impoundments result in high MeHg throughout the Edisto. Despite substantial wetlands coverage and elevated F-MeHg concentrations at the headwater margins, numerous impoundments on primary stream channels favor spatial variability and lower F-MeHg concentrations in the Upper Hudson. The results indicated that, even in geographically, climatically, and ecologically diverse streams, production in wetland/floodplain areas, hydrologic transport to the stream aquatic environment, and conservative/nonconservative attenuation processes in open water areas are fundamental controls on dissolved MeHg concentrations and, by extension, MeHg availability for potential biotic uptake.

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