C. Huang et Y. Qi, THE ABUNDANCE CYCLE AND INFLUENCE FACTORS ON RED TIDE PHENOMENA OF NOCTILUCA-SCINTILLANS (DINOPHYCEAE) IN DAPENG BAY, THE SOUTH-CHINA SEA, Journal of plankton research, 19(3), 1997, pp. 303-318
?he seasonal occurrence of Noctiluca scintillans and the causative mec
hanisms of red tide phenomena were investigated in the northwestern pa
rt of Dapeng Bay, the South China Sea, from March 1990 to June 1992. I
t occurred in the plankton usually from January through May/June with
peak abundance from March to early May. At least eight red tides of th
is organism, when the surface water was covered with the pink patches
and slicks, were observed during the investigation period, and all of
them took place between March and early May. Noctiluca occurred at tem
peratures from 15.8 to 28.6 degrees C, and the population density was
the highest at temperatures between 19 and 25 degrees C. It disappeare
d from the plankton in summer and fall when the temperature warmed to
lethal level of similar to 30 degrees C and then the population probab
ly was transported to outside of the bay. During the peak period of ab
undance between March and May, the log transformed average density of
Noctiluca at each station showed a significantly positive relationship
with average water temperature, indicating that within its optimum te
mperature a higher temperature promotes the growth of Noctiluca popula
tion. Sharp declines of the population were associated with abrupt dec
reases in salinity due to heavy rain. Hence, rich food supply is basic
ally necessary for Noctiluca to reproduce massively, but the suitable
temperature, stable muggy weather without heavy rain are considered to
be the important factors for the Noctiluca blooms. The surface conver
gence, due to the geographical and tidal features, may also constitute
a direct driving force leading to its frequent occurrences in the stu
dy area. The Noctiluca density showed a negative relationship with chl
orophyll a concentration, indicating that this species gives a predati
on pressure on the phytoplankton.