PATTERNS OF SPATIAL AND TEMPORAL VARIATION IN PHYTOPLANKTON CHLOROPHYLL-A IN THE RIVER TRENT AND ITS TRIBUTARIES

The variation in phytoplankton chlorophyll a was measured regularly on the River Trent, UK, and its tributaries between April 1995 and July 1997. During the spring maximum the concentration of chlorophyll a inc reased with distance down the river, consistent with net in situ growt h. The apparent rate of net increase in spring ranged from 0.004 to 0. 044 km(-1), which is calculated from water velocity estimates to be eq uivalent to a specific growth rate of between 0.04 and 0.57 day(-1). D uring late summer, however, the concentration of chlorophyll a decline d down river, the apparent rate of decline being between 0.001 and 0.0 32 km(-1), equivalent to a specific growth rate of between -0.01 and - 0.78 day(-1). At the lower tidal limit, the seasonal chlorophyll a con centration ranged between an annual minimum of 1.4-1.7 mu g l(-1) in D ecember and January and an annual maximum of 121-162 mu g l(-1) in May or June. The chlorophyll a maximum was short lived and the concentrat ion decreased to 6-18 mu g l(-1) in August-October. The chlorophyll a concentration in four major tributaries, the Tame, Dove, Derwent and D evon, was low in comparison with the main river. In another tributary, the Soar, chlorophyll a concentrations were relatively high and reach ed an annual maximum of 74 mu g l(-1) in 1995 and 70 mu g l(-1) in 199 7. Significant differences in chlorophyll a concentration across the m ain river were detected on one of the three occasions studied. The pos sible influence of physical, chemical and biological factors in contro lling the concentration of phytoplankton chlorophyll a is discussed. ( C) 1998 Elsevier Science B.V.