Abstract Dissolved trace-metal (Cd, Cu, Fe, Ni and Pb) interactions with C18 Sep-Pak extractable organic matter have been investigated in the Rhone mouth and in the Gulf of Lions in July 1989. Pb and Cd do not show any complexation while Ni and Fe are slightly complexed in surface waters near the Rhone mouth. Up to 40% of total dissolved Cu is complexed by the extractable organic matter in coastal waters and, in open sea waters a subsurface maximum of 64% of complexed Cu was observed, apparently linked to the maximum of primary production. Our results combined with other data on the same area suggest that in the euphotic zone of the western Mediterranean Sea, organic matter directly connected to primary production and associated degradation processes is contributing to this complexation as well as to the enrichment of colloidal fraction and the increase of the discrepancy between concentrations of dissolved organic carbon according to the method of Sugimura and Suzuki (1988) and by traditional techniques.
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