Size-fractionated phytoplankton biomass and species composition in the Indian sector of the Southern Ocean during austral summer

During the late austral summer of 1994, Antarctic waters were characterized by low phytoplankton biomass. Along the 62 degrees E meridian transect, be tween 49 degrees S and 67 degrees S, chlorophyll (Chl.) a concentration in the upper 150 m was on average 0.2 mg m(-3). However, in the Seasonal Ice Z one (SIZ) chlorophyll a concentrations were higher, with a characteristic d eep chlorophyll maximum. The highest value (0.6 mg Chi. a m(-3)) was measur ed at the Antarctic Divergence, 64 degrees S, corresponding to the depth of the temperature minimum (similar to 100 m). This deep biomass maximum decr eased from South to North, disappeared in the Permanently Open Ocean Zone ( POOZ) and reappeared with less vigour in the vicinity of the Polar Front Zo ne (PFZ). In the SIZ, the upper mixed layer was shallow, biomass was higher and the > 10 mu m fraction was predominant. In this zone the > 10 mu m, 2- 10 mu m and < 2 mu m size fractions represented on the average 46%, 25.1% a nd 28.9% of the total integrated Chi. a stock in the upper 100 m, respectiv ely. The phytoplankton assemblage was diverse, mainly composed of large dia toms and dinoflagellate cells which contributed 42.7% and 33.1% of the auto trophic carbon biomass, respectively. Moving northwards, in parallel with t he decrease in biomass, the biomass of autotrophic pico- and nanoflagellate s (mainly Cryptophytes) increased steadily. In the POOZ, the picoplanktonic size fraction contributed 47.4% of the total integrated Chi. a stock. A ph ytoplankton community structure with low biomass and picoplankton-dominated assemblage in the POOZ contrasted with the relatively rich, diverse and di atom-dominated assemblage in the SIZ. These differences reflect the spatial and temporal variations prevailing in the Southern Ocean pelagic ecosystem .