SIZE DISTRIBUTION OF CHLOROPHYLL-A BIOMASS AND PRIMARY PRODUCTION IN A TEMPERATE ESTUARY (SOUTHAMPTON WATER) - THE CONTRIBUTION OF PHOTOSYNTHETIC PICOPLANKTON
A. Iriarte et Da. Purdie, SIZE DISTRIBUTION OF CHLOROPHYLL-A BIOMASS AND PRIMARY PRODUCTION IN A TEMPERATE ESTUARY (SOUTHAMPTON WATER) - THE CONTRIBUTION OF PHOTOSYNTHETIC PICOPLANKTON, Marine ecology. Progress series, 115(3), 1994, pp. 283-297
Size-fractionated chlorophyll a (chi a) biomass and primary production
rate (> 3 mu m 1-3 mu m and < 1 mu m) and picophytoplankton abundance
(both prokaryotic and eukaryotic) were investigated in Southampton Wa
ter (south coast of England), with routine sampling at 2 stations, rep
resentative of conditions in the mid and outer estuary. In the mid est
uary the cycle of chi a biomass in the > 3 mu m size fraction was char
acterized by a small spring peak and a more intense summer peak. In th
e outer estuary a chl a maximum in the > 3 mu m size fraction occurred
in spring; phytoplankton in this size fraction may have been nutrient
limited in summer at this station. Phycoerythrin-containing picocyano
bacteria, eukaryotic picophytoplankton cell numbers, and chi a biomass
and primary production rate by the < 1 mu m size fraction all showed
a positive correlation with temperature and peaked during summer at bo
th stations. The 1-3 and < 1 mu m size fractions contributed around 14
and 6 %, respectively, to the estimated annual rate of depth-integrat
ed plankton community primary production. These results suggest that t
he impact of the photosynthetic picoplankton diminishes in an increasi
ng eutrophication gradient, from offshore (> 50 %) to coastal (ca 20 %
) and estuarine waters (< 10 %). This pattern in relation to a eutroph
ication gradient was also apparent on a seasonal basis, the < 1 mu m f
raction having its maximum significance at times of lowest overall chi
a concentration. It is thus suggested that factors limiting growth an
d accumulation of larger phytoplankton are the primary cause of an inc
rease in the relative significance of picophytoplankton.