TEMPORAL AND SPATIAL VARIABILITY OF PHYTOPLANKTON AND CHLOROPHYLL-A -LESSONS FROM THE SOUTH COAST OF NORWAY AND THE SKAGERRAK

Regular monitoring of phytoplankton has been carried out on the Norweg ian Skagerrak coast three times a week since 1989, and samples from th e upper 3 m of the water column have been analysed for chlorophyll a ( Chl a) concentrations and dominant species. Selected potentially toxic or harmful species of phytoplankton have also been quantified. Chl a appears to fluctuate considerably on a short time scale (2-3 days), an d simple analyses suggest that Chl a should be measured at least twice a week to obtain reliable annual estimates. By contrast. at the insho re. monitoring station Chl a is significantly correlated with transect measurements across most of the Skagerrak. indicating a high spatial homogeneity. Hence, measurements at the inshore stations are likely to reflect concentrations over a large area and meteorological condition s are suggested to be the most likely driving force controlling the va riability. The traditional view of a marked spring and autumn bloom in temperate stratified waters does not seem to be a predominant feature of the production cycle in the Skagerrak. In fact. Chl a concentratio ns >4 mu g l(-1) rarely last for more than a week. In addition to shor t-term variability, there is also high inter-annual variability in the production cycle. This picture is reinforced by large variations in s pecies composition of the phytoplankton community; the abundance of al l species analysed varies substantially from one year to the next. (C) 1998 International Council for the Exploration of the Sea.