Je. Cloern et al., NOTES ON A MESODINIUM-RUBRUM RED TIDE IN SAN-FRANCISCO BAY (CALIFORNIA, USA), Journal of plankton research, 16(9), 1994, pp. 1269-1276
Discrete red patches of water were observed in South San Francisco Bay
(USA) on 30 April 1993, and examination of live samples showed that t
his red tide was caused by surface accumulations of the pigmented cili
ate Mesodinium rubrum. Vertical profiles showed strong salinity and te
mperature stratification in the upper 5 m, peak chlorophyll fluorescen
ce in the upper meter, and differences in the small-scale density stru
cture and fluorescence distribution among red patches. Events precedin
g this Mesodinium red tide included: (i) heavy precipitation and run-o
ff, allowing for strong salinity stratification; (ii) a spring diatom
bloom where the chlorophyll a concentration reached 50 mg m(-3); (ii)
depletions of dissolved inorganic N and Si in the photic zone; and (iv
) several days of rapid warming and stabilization of the upper surface
layer. These conditions may be general prerequisites for M rubrum blo
oms in temperate estuaries.