Phytoplankton dynamics in a subarctic fjord during the under-ice – open water transition.

The spring blooms of phytoplankton play a key role in the functioning of marine ecosystems in the polar regions. A spring bloom in the Subarctic White Sea was observed in order to determine the effect of ice cover on the distribution, composition, and temporal changes of phytoplankton communities. The obtained results clearly show that in the White Sea, as in other freezing Arctic seas, ice melting and ice removal both play an essential role in the onset and development of spring phytoplankton blooms. This facilitates the release of ice algae and ice-pelagic algae into the water, as well as the rapid development of true planktonic taxa within the euphotic zone. One major peak of algal biomass is associated with ice removal while the other is recorded in the early summer. Comparison of our results with earlier data from 1960s to 1990s indicated strong year-to-year variation in terms of ice removal, the onset of the spring bloom, and the abundance and composition of the dominant phytoplankton taxa. • In the White Sea ice removal determines the onset and development of spring bloom. • 130 taxa of phytoplankton were determined during spring bloom in the White Sea. • Three major groups of algal communities were revealed during spring bloom. • High year-to-year variation in ice removal and spring bloom features was recorded. [ABSTRACT FROM AUTHOR]