T. Kiorboe et al., INTENSIVE AGGREGATE FORMATION WITH LOW VERTICAL FLUX DURING AN UPWELLING-INDUCED DIATOM BLOOM, Limnology and oceanography, 43(1), 1998, pp. 104-116
The surfaces of most pelagic diatoms are sticky at times and may there
fore form rapidly settling aggregates by physical coagulation. Stickin
ess and aggregate formation may be particularly adaptive in upwelling
systems by allowing the retention of diatom populations in the vicinit
y of the upwelling center. We therefore hypothesized that upwelling di
atom blooms are terminated by aggregate formation and rapid sedimentat
ion. We monitored the development of a maturing diatom (mainly Chaetoc
eros spp.) bloom in the Benguela upwelling current during 7 d in Febru
ary. Chlorophyll concentrations remained consistently high during the
observation period (similar to 500 mg Chi m(-2)) and phytoplankton gre
w at an average specific rate of 0.25 d(-1). The diatoms were extraord
inarily sticky, with stickiness coefficients of up to 0.40, which is t
he highest ever recorded for field populations. Combined with estimate
s of turbulent shear in the ocean such stickiness coefficients predict
very high specific coagulation rates (0.3 d(-1)). In situ video obser
vation demonstrated the occurrence of abundant diatom aggregates with
surface water concentrations between 1,000 and 3,000 ppm. Despite the
very high concentration of aggregates, vertical fluxes of phytoplankto
n were very low, with fractional losses <0.005 d(-1), and the aggregat
es thus seemed to be near neutrally buoyant. Losses due to copepod gra
zing were also low (similar to 0.025 d(-1)). Most of the aggregates we
re colonized by the heterotrophic dinoflagellate Noctiluca scintillans
that feed upon diatoms in the aggregates. The system appeared to be i
n near steady state; specific diatom growth rate, coagulation rate, an
d loss rate due to N, scintillans feeding were all of the same magnitu
de (0.25-0.3 d(-1)) and the latter two varied in concert. Our observat
ions provide only partial support for the population retention hypothe
sis because aggregate buoyancy and N, scintillans grazing efficiently
reduced the vertical flux of aggregates in this system.