Abstract
Based on the comparative analysis of the characteristics of the early summer maxima of the normalized radiance from the satellite ocean color data, the seasonal trend of the concentration of the chlorophyll “a,” and the species composition of the phytoplankton from determinations in water samples from the Black Sea, it is concluded that the summer chlorophyll maximum is due to the coccolithophorid bloom occurring from late May to mid June in the Black Sea basin.
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