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Geochemical Data for Mercury and Other Constituents in Redox-Manipulated Sediment Cores from Clear Lake, Lake County, California

Dates

Publication Date
Time Period
2019-11-16

Citation

Marvin-DiPasquale, M.C., Alpers, C.N., Agee, J.L., Kieu, L.H., Kakouros, E., Sadro, S., Framsted, N.T., and Baesman, S.M., 2021, Geochemical Data for Mercury and Other Constituents in Redox-Manipulated Sediment Cores from Clear Lake, Lake County, California. U.S. Geological Survey data release., https://doi.org/10.5066/P9REF3QV.

Summary

Clear Lake, located within the Coast Range west of California’s Central Valley, is the largest natural freshwater lake contained fully within the state and geologically is considered to be the oldest lake in North America. Clear Lake is popular for recreation and provides critical habitat to a wide variety of fish and bird species. Water quality in Clear Lake is degraded by both by mercury contamination and harmful algal blooms (HABs). The mercury contamination is largely associated with the Sulfur Bank Mercury Mine (SBMM), located on the eastern shore of the Oaks Arm in the northeastern portion of the Lake. The mine was operated intermittently from the 1870s until 1957 and is now a U.S. Environmental Protection Agency (USEPA) Superfund [...]

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Attached Files

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SITES_CL.SED-2019.kmz 770 Bytes application/vnd.google-earth.kmz
UCD_CL_Coring_Incubations.jpg thumbnail 204.73 KB image/jpeg
SITES_CL.SED-2019.jpg thumbnail 261.68 KB image/jpeg
T1_Data_Dictionary_CL_SED_2019.csv 24.95 KB text/csv
T2_Data_CL_SED_2019.csv 14.71 KB text/csv
T3_QA_CL_SED_2019.csv 1.47 KB text/csv

Purpose

This product is part of a larger body of on-going USGS research focused on mercury cycling in Clear Lake, California, in which the USGS is assisting the USEPA in developing a Hg monitoring program and remediation strategy for SBMM and portions of Clear Lake. The primary purpose for developing this data set was to leverage ongoing field efforts and laboratory experiments simultaneously being conducted by UCD colleagues, which focused on the flux of nutrients from the surface sediment to the overlying water column under experimentally controlled oxic and anoxic treatment conditions. Methylmercury formation in sediment is primarily an anaerobic microbial process, and the bottom waters within the lake regularly experience strong temporal variations in redox status (as measured by dissolved oxygen in vertical profiles), the experimentally manipulated UCD cores provided an opportunity to examine how oxic versus anoxic conditions affect the speciation of mercury (including methylmercury and reactive divalent inorganic mercury) and the related redox speciation of iron and sulfur, which also are involved in the biogeochemical cycling of mercury.

Additional Information

Identifiers

Type Scheme Key
DOI https://www.sciencebase.gov/vocab/category/item/identifier doi:10.5066/P9REF3QV

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