Rh. James et al., ASPECTS OF THE GEOCHEMISTRY OF DISSOLVED AND PARTICULATE CD, CU, NI, CO, AND PB IN THE DOVER STRAIT, Oceanologica acta, 16(5-6), 1993, pp. 553-564
Water column samples have been collected at six stations across the Do
ver Strait within the framework of the FluxManche programme every mont
h for fifteen months and analyzed for particulate and dissolved trace
metals. Important seasonal variations in trace metal distributions hav
e been identified. Dissolved Cu and Ni exhibit similar behaviour in th
e Strait; while seasonal variation in their distribution may be determ
ined by changes in freshwater input, additional processes including bi
ological uptake and regeneration and benthic input probably perturb wa
ter column inventories. Consistently with the suggestion of other auth
ors, Co and Mn in both the dissolved and particulate phase exhibit som
e degree of covariance; substantial increases in the concentration of
dissolved Mn in the summer (9.0-69.0 nM as opposed to 3.3-9.6 nM in th
e winter) across the entire Channel are to some extent supported by in
creases in dissolved Co concentrations. Summer maxima are accompanied
by a reduction in the acetic acid leachable particulate Mn, possibly i
mplying release from this phase in the summer or increased uptake duri
ng the winter. Data for particulate cadmium are consistent with the me
tal being largely associated with biogenic material; biological activi
ty is inferred to generate a spring depletion in dissolved Cd concentr
ations. In contrast to deep ocean environments, there is no obvious co
rrespondence between dissolved Cd and the classical nutrient elements
in this environment. Dissolved Pb concentrations appear to be strongly
influenced by seasonal variation in freshwater input and shorter time
scale variation in atmospheric input. There is some evidence that bio
logical activity perturbs the water column inventory. This is supporte
d by observations from the particulate phase where atmospheric or fluv
ially derived particles appear largely to determine the total particul
ate Pb concentration in winter but other phases become important in it
s regulation in summer.