Sn. Luoma et al., METAL UPTAKE BY PHYTOPLANKTON DURING A BLOOM IN SOUTH SAN-FRANCISCO BAY - IMPLICATIONS FOR METAL CYCLING IN ESTUARIES, Limnology and oceanography, 43(5), 1998, pp. 1007-1016
The 1994 spring phytoplankton bloom in South San Francisco Bay caused
substantial reductions in concentrations of dissolved Cd, Ni, and Zn,
but not Cu. We estimate that the equivalent of similar to 60% of the t
otal annual input of Cd, Ni, and Zn from local waste-water treatment p
lants is cycled through the phytoplankton in South Bay. The results su
ggest that processes that affect phytoplankton bloom frequency or inte
nsity in estuaries (e.g. nutrient enrichment) may also affect metal tr
apping. The bloom was characterized by hydrographic surveys conducted
at weekly intervals for 9 weeks. Metal samples were collected from the
water column on three occasions, timed to bracket the period when the
bloom was predicted. Factors that might confound observations of biol
ogical influences, such as freshwater inputs, were relatively constant
during the study. Before the bloom, concentrations of dissolved Cd we
re 0.81 +/- 0.02 nmol kg(-1), Zn concentrations were 19.8 +/- 1.5 nmol
kg(-1), Ni were 42 +/- 1.4 nmol kg(-1), and Cu were 37 +/- 1.4 nmol k
g(-1). These values are elevated relative to riverine and coastal end-
members, reflecting inputs from wastewater and(or) sediments. At the h
eight of the bloom, dissolved Zn, Cd, and Ni were reduced to 19, 50, a
nd 75% of their prebloom concentrations, respectively. Dissolved Cu co
ncentrations increased 20%. The mass of Cd taken up by phytoplankton w
as similar to the mass of Cd removed from solution if particle settlin
g was considered, and Cd concentrations estimated in phytoplankton wer
e higher than concentrations in suspended particulate material (SPM).
Particulate concentrations of Zn and Ni during the bloom appeared to b
e dominated by the influence of changes in resuspension of Zn- and Ni-
rich sediments.