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South of 59°N the phytoplankton index has increased, diatoms have declined and <i>Ceratium</i> spp have remained at a constant level of abundance . a possible explanation of the increase in the phytoplankton index at a time when the diatoms were declining south of 59°N is the development of unidentified phytoplankton organisms such as microflagellates. As many of the variables influencing phytoplankton standing crop are governed in turn by the prevailing weather, the phytoplankton changes may well be a consequence of the general deterioration, since 1940, of North Atlantic weather. 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