Control of Cd Concentrations in a Coastal Diatom by Interactions among Free Ionic Cd, Zn, and Mn in Seawater

Cadmium and phosphate concentrations in seawater are closely correlated, suggesting that Cd distributions, like those of PO 4, are controlled by algal uptake and regeneration. But the factors controlling Cd levels in phytoplankton are poorly known. Experiments in metal ion buffer systems with a coastal diatom Thalassiosira pseudonana revealed that cellular Cd:C ratios within the Cd ion concentration ([Cd 2+ ]) range (10 - 13 to 10 - 10 M) in seawater were generally proportional to [Cd 2+ ] and inversely related to concentrations of Zn and Mn ions ([Zn 2+ ] and [Mn 2+ ]) and specific growth rate. The effects of Mn and Zn reflect cellular uptake of Cd by two inducible transport systems: the Mn system whose capacity ( V max ) is enhanced at low [Mn 2+ ] and a separate system induced at low cellular zinc. At the low [Zn 2+ ] of surface oceanic waters (≤10 - 11.0 M), Cd uptake is controlled by this latter system and, therefore, is inversely related to ionic zinc levels. However, at the higher [Zn 2+ ] range of coastal waters, Cd uptake by this system is strongly suppressed and Cd instead is taken up by the Mn system; as a result it is inversely related to [Mn 2+ ] and largely independent of variations in [Zn 2+ ]. Because of the suppression of Cd uptake by high [Zn 2+ ] and [Mn 2+ ] in coastal waters, algal Cd concentrations may be lower in these waters than in the ocean despite the presence of higher coastal [Cd 2+ ].