A. Waite et al., NEW MEASUREMENTS OF PHYTOPLANKTON AGGREGATION IN A FLOCCULATOR USING VIDEOGRAPHY AND IMAGE-ANALYSIS, Marine ecology. Progress series, 155, 1997, pp. 77-88
Diatom aggregation can increase the sedimentation rate of the intense
pulses of carbon formed during diatom blooms. Laboratory studies of ag
gregation dynamics have been troubled by the unavoidable disruption of
aggregates in laboratory flocculators due to subsampling and electron
ic particle counting. Aggregate disruption prevents accurate measureme
nt of aggregation rate and makes observation of particle structure imp
ossible. This led us to develop a new non-disruptive method to quantif
y diatom aggregation using high-resolution video and image analysis. T
he system easily resolved cells of Chaetoceros neogracile 6 to 8 mu m
in diameter, and facilitated observations of aggregate morphology. C.
neogracile made either ball-like or net-like aggregates depending on c
ulture density and physiological state. Only the net like aggregates r
eached a substantial size (>1 mm). A Si-limited batch culture experime
nt indicated that stickiness of C. neogracile increased significantly
with increasing severity of nutrient limitation. This increase was not
detectable by the subsampling and electronic particle counting method
. It is likely that spine formation, cell-surface bound sugars, and tr
ansparent exopolymer particles all played a role in determining aggreg
ate structure and changes in stickiness. The stickiness calculation mo
del assumes cultures are initially suspensions of single cells which f
orm doublets as they aggregate. This assumption was tested by comparin
g mean particle size in a culture with the percentage of tells in aggr
egates as determined using nearest neighbor distances, allowing us to
assess the mean number of cells per aggregate. C. neogracile commonly
formed aggregates containing anywhere between 2 and 10 cells showing t
hat model assumptions can be violated under normal experimental condit
ions. A larger field of view was necessary to estimate the larger part
icle sizes typical of coastal diatom blooms.