Abstract

In the eastern Canadian Arctic, algae greater than 1·0 μm in diameter dominated both phytoplankton biomass and primary production. In these waters, correlations between cell volume, cellular chlorophyll a (chl a) or chl a: cell volume and cellular primary production (pg C h-1 cell-1) were not significant at the individual species level. Correlations were significant only when all data were pooled or treated as taxonomic groups of diatoms and dinoflagellates. In individual species a weak dependence was observed between the cellular chl a or chl a: phaeophytin and the carbon assimilation ratios (pg C h- pg-1 chl a). Assimilation ratios for individual species fall into a narrow range (0·06–1·31), similar to that observed on bulk natural Arctic phytoplankton or on senescent cultures. On a cell basis, however, the production ratios varied widely (8–9220 pg C h-1 cell-1), with marked intraspecific variations, suggesting that the cells are accumulating chl a in excess of their division. Thus, chl a in the Arctic waters seems to have limited utility as a unit of biomass for normalizing photosynthesis. The observed wide differences in the interspecific and intraspecific photosynthetic rates (pg C h-1 cell-1) are of the same magnitude as those from bulk algal cultures.

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