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| | Bates et al. -- Sulfur Emissions to the Atmosphere from Natural Sources |
 | | Although the sulfide ion is clearly present in surface seawater in concentrations ranging from 0.1 to 1.1 nmol/L (Cutter and Krahforst, 1988), it is likely complexed with trace metals (Elliott, 1988; Dyrssen, 1989; Elliott et al., 1989; Elliott and Rowland, 1990), and hence, not in a volatile form. |
 | | The other potentially important volatile species are methanethiol (CH and dimethyldisulfide (CH Methanethiol is produced in anoxic marine sediments (Kiene and Visscher, 1987; Sorensen, 1988), in decomposing algal mats (Zinder et al., 1977), and in coastal waters (Leck and Rodhe, 1990), but as yet has not been quantified in open ocean surface seawater. |
 | | Our experience has shown that methanethiol and dimethyldisulfide can be produced as an artifact of sampling/analysis if plankton cells undergo anaerobic decomposition (Bates, unpublished data). |
| www.pmel.noaa.gov /pubs/outstand/bate1229/estimate.shtml (4998 words) |
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