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flow to the atmosphere, or about 2,400 tons per year (Kim and Fitzgerald <br />1986). Mercury finds its way into sediments, particularly oceanic sediments, <br />where the retention time can be lengthy (Table 2), and where it may continue <br />to contaminate aquatic organisms (Lindsay and Dimmick 1983). Estimates of the <br />quantities of Hg entering the atmosphere from degassing of the surface of the <br />planet vary widely, but a commonly quoted figure is 30,000 tons annually <br />(Clarkson et al. 1984). In aquatic ecosystems, removal of the source of <br />anthropogenic Hg results in a slow decrease in the Hg content of sediments and <br />biota (NAS 1978). The rate of loss depends, in part, on the initial degree of <br />contamination, the chemical form of Hg, physical and chemical conditions of <br />the system, and the hydraulic turnover time (NAS 1978). <br />6