Influences of sea ice on eastern Bering Sea phytoplankton

The influence of sea ice on the species composition and cell density of phytoplankton was investigated in the eastern Bering Sea in spring 2008. Diatoms,particularly pennate diatoms,dominated the phytoplankton community. The dominant species were G rammonema islandica(Grunow in Van Heurck) Hasle,Fragilariopsis cylindrus(Grunow) Krieger,F. oceanica(Cleve) Hasle,Navicula vanhoeffenii Gran,Thalassiosira antarctica Comber,T. gravida Cleve,T. nordenskieldii Cleve,and T. rotula Meunier. Phytoplankton cell densities varied from 0.08×104 to 428.8×104 cells/L,with an average of 30.3×104 cells/L. Using cluster analysis,phytoplankton were grouped into three assemblages defined by ice-forming conditions: open water,ice edge,and sea ice assemblages. In spring,when the sea ice melts,the phytoplankton dispersed from the sea ice to the ice edge and even into open waters. Thus,these phytoplankton in the sea ice may serve as a "seed bank" for phytoplankton population succession in the subarctic ecosystem. Moreover,historical studies combined with these results suggest that the sizes of diatom species have become smaller,shifting from microplankton to nannoplankton-dominated communities.

The influence of sea ice on the species composition and cell density of phytoplankton was investigated in the eastern Bering Sea in spring 2008. Diatoms, particularly pennate diatoms, dominated the phytoplankton community. The dominant species were Grammonema islandica （Grunow in Van Heurck） Hasle, Fragilariopsis cylindrus （Grunow） Krieger, F. oceanica （Cleve） Hasle, Navicula vanhoeffenii Gran, Thalassiosira antarctica Comber, T. gravida Cleve, T. nordenskioeldii Cleve, and T. rotula Meunier. Phytoplankton cell densities varied from 0.08× 10^4 to 428.8× 10^4 cells/L, with an average of 30.3× 10^4 cells/L. Using cluster analysis, phytoplankton were grouped into three assemblages defined by ice-forming conditions： open wate.r, ice edge, and sea ice assemblages. In spring, when the sea ice melts, the phytoplankton dispersed from the sea ice to the ice edge and even into open waters. Thus, these phytoplankton in the sea ice may serve as a “seed bank” for phytoplankton population succession in the subarctic ecosystem. Moreover, historical studies combined with these results suggest that the sizes of diatom species have become smaller, shifting from microplankton to nannoplankton-dominated communities.