In this work we have studied the possibility of determining the rate of phytoplankton
photosynthesis in situ using a submersible pump-and-probe fluorometer
in water areas differing in their trophic level, as well as in climatic and hydrophysical
characteristics. A biophysical model was used to describe the relationship between photosynthesis, underwater irradiance, and the intensity of phytoplankton fluorescence
excited by an artificial light source. Fluorescence intensity was used as
a measure of light absorption by phytoplankton and for assessing the efficiency of
photochemical energy conversion at photosynthetic reaction centers. Parameters
of the model that could not be measured experimentally were determined by
calibrating fluorescence and irradiance data against the primary production
measured in the Baltic Sea with the radioactive carbon method. It was shown
that the standard deviation of these parameters in situ did not exceed 20%,
and the use of their mean values to estimate the phytoplankton photosynthetic
rate showed a good correlation between the calculated and measured data on
primary production in the Baltic (r = 0.89), Norwegian (r = 0.77) and South
China (r = 0.76) Seas.
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