Trace elemental characteristics of Native Pacific Oysters (Ostrea lurida) fromThompson's Cove (CA-SFR-186H) in San Francisco, California, indicate that Gold Rush-era anthropogenic contamination is present, but not due to hydraulic mining activities in the Sierra Nevada Mountains between 1852 and 1884. Using portable X-ray fluorescence, net photon counts extracted fromtwenty crushed and homogenized O. lurida shells, including two prehistoric, five 1840-1853, seven 1851-1852, and six 1860-1870 shell samples suggest periods of localized contamination. Shell samples 4b (ca. 1851-1852), 16, 17, 7a (ca. 1860-1870), 9, and 11 display high abundances of lead, samples 7a (ca. 1860-1870), 8, 9, 10, 11, and 12 high abundances of zinc and sample 17 (ca. 1860-1870) a high abundance of arsenic, while both prehistoric and all remaining historic shells have little evidence of any heavy metal presence. Localized contamination, possibly from trash and material discarded directly into the San Francisco Bay, is likely driving some heavy metal contamination in Gold Rush-era O. lurida. However, mercury, the expected signal of hydraulic mining, is not abundant in these samples despite widespread documentation of contamination in the historic literature and in recent environmental studies from northern California. (C) 2015 Elsevier Ltd. All rights reserved.
