OCEANOGRAPHIC CONDITIONS IN THE SANDSFJORD SYSTEM, WESTERN NORWAY, AFTER A BLOOM OF THE TOXIC PRYMNESIOPHYTE PRYMNESIUM-PARVUM CARTER IN AUGUST 1990

As in 1989 the algal bloom was toxic and mortal to Atlantic salmon and rainbow trout in fish-farms. The brachish layer, with salinities between 5 and 25 parts per thousand, was characterized by a high N : P ratio reflecting the low phosphate content in the freshwater supplied to the fjord system. An overflow discharge of freshwater close to the power plant at Hylen created a vigorous 'upwelling' and dominated the hydrographical conditions in Hylsfjorden and Sandfjorden during the bloom. As a result a compensation current in Hylsfjorden was created resulting in a prolonged residual time in the upper 1-2 m, where most of the P. parvum was observed. The entrainment of seawater into the brackish-layer at Hylen was about four times greater than that under normal wind conditions in the fjord system. The calculated nitrate consumption in the fjord system was about 2 800 kg day-1 and compared well with the measured in situ production of about 900 mgC m-2 day-1. The supply of phosphate from fresh and seawater into the brackish layer, could only support about 20% of the theoretical normal phosphate requirements for phytoplankton growth. As in 1989 there was a close relationship between the start of the freshwater discharge, the associated upwelling at Hylen and the time of onset of a pelagical phase of the P. parvum bloom. It is suggested that the low salinity conditions, the prolonged residence time in the surface layer and the artificial 'upwelling' in Hylsfjorden set the stage for the bloom. The high N : P ratio and the associated phosphate limitation, probably played a major role in causing P. parvum to become toxic.