Open ocean studies have shown that dissolved manganese, cobalt and lead exhibit vertical profiles that reflect external sources and short residence times due to scavenging on to particle surfaces. In contrast, dissolved cadmium, copper, nickel and zinc mirror, to different degrees, the profiles of the nutrients. The work reported here for three cruises (November–December 1985, May and July–August 1986) in a shallow shelf sea shows that seasonal variations are shown by metals of the scavenged group, whereas the metals whose cycling in the open ocean parallels those of the nutients, do not show these correlations and, in fact, show no measurable seasonal variability. Concentrations of manganese increased progressively from winter to summer [2.3 ± 0.7(mean± 1σ)to 5.0 ± 3.0 nmol l −1]. A surface enrichment in the upper mixed layer of the western Channel during summer was also observed. Concentrations of cobalt increased from winter to spring (from ≤0.02–0.50 to 0.08–0.71 nmol l −1), paralleling those of manganese, but then decreased into summer (to ≤0.08–0.56 nmol l −1). The regional distribution of lead changed during the spring, possibly reflecting removal by diatoms and decreased river inputs, although overall mean concentrations remained similar throughout the year (0.22 nmol l −1). Concentrations of cadmium (0.20 nmol l −1), copper (3.2 nmol l −1), nickel (3.8 nmol l −1) and zinc (7.6 nmol l −1), and their regional distributions, remained relatively uniform over the period of the observations.
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