Environ. Sci. Technol. 1999, 33, 4194-4198
Mercury Profiles in Sediments of the Arctic Ocean Basins CHARLES GOBEIL* Maurice Lamontagne Institute, Department of Fisheries and Oceans, P.O. Box 1000, Mont-Joli, Quebec, G5H 3Z4 Canada ROBIE W. MACDONALD Institute of Ocean Sciences, Department of Fisheries and Oceans, P.O. Box 6000, Sidney, British Columbia, V8L 4B2 Canada JOHN N. SMITH Bedford Institute of Oceanography, Department of Fisheries and Oceans, P.O. Box 1006, Darthmouth, Nova Scotia, B2Y 4A2 Canada
Total Hg distributions have been measured for seven sediment cores collected from the major basins of the Arctic Ocean during the Arctic Ocean Section in 1994. Hg determinations were perfomed on the top 10 cm of the sectioned cores using gold amalgamation atomic fluorescence spectroscopy. In five cores, Hg concentrations decrease downward from 34 to 116 ng g-1 at the sediment surface to 10-65 ng g-1 at 5 cm depth and then remain almost constant with increasing depth. In the other two cores, the Hg decrease with depth is interrupted by a maximum (96107 ng g-1) at 7-8 cm. The obvious inferencespervasive Hg contamination from anthropogenic sources even at the North Polesis discounted after a careful evaluation of sediment geochemistry. The evidence suggests that these Hg profiles have been produced by Hg redistribution during diagenesis. In all seven cores, strong similarities are observed between the Hg and the reactive Fe profiles, implying that a portion of the total Hg deposited is recycled along with Fe during redox changes. Intense redox processing in these cores is demonstrated by sharp decreases in organic content with depth and by vertical profiles showing surface enrichments for Mn and Fe. The crucial factors governing surface Hg enrichments in Arctic basin sediments are the low sedimentation rates (
