We report the results of a field study, in productive waters off California, of the factors that control the particulate cadmium (Cd):phosphorus (P) composition of natural assemblages of marine phytoplankton, the dominant vector of both elements to the deep ocean. Controlled shipboard incubation experiments (∼2-4 d) demonstrated that while manipulation of pCO2 and dissolved zinc (Zn) and manganese (Mn) concentrations had little effect on the species composition or C:nitrogen (N):P ratios of natural, diatom-dominated phytoplankton assemblages, their Cd:P ratio was negatively correlated to each of these variables. The particulate Cd:P ratios of phytoplankton were two to five times higher for cells grown at low pCO2 than for cells acclimated to growth at pCO2 at or above atmospheric equilibrium values. Addition of Zn to incubations at five- to 20-fold above background concentrations decreased Cd uptake and phytoplankton Cd:P ratios across pCO2 and Mn treatments and suppressed short term Cd uptake rates by a factor of approximately two to four, compared to controls. A broad pattern of Mn suppression of Cd uptake was also evident in our incubations. We propose that natural variability in surface water pCO2 and dissolved Zn and Mn, related to water mass history and biological drawdown, likely govern the degree of Cd uptake and, therefore, the evolution of the dissolved Cd:PO4 ratio in recently upwelled, high-productivity surface waters.
All Science Journal Classification (ASJC) codes
- Aquatic Science