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JOURNAL OF PLANKTON RESEARCH | VOLUME 16 | NUMBER 8 | PAGES 945-959 | 1994
© Oxford University Press


research-article

Autotrophic picoplankton in southern Lake Baikal: abundance, growth and grazing mortality during summer

Toshi Nagata, Kenji Takai, Kyoko Kawanobe1, Dong-Sup Kim2, Ryoji Nakazato2, Nina Guselnikova3, Nina Bondarenko3, Oliga Mologawaya3, Tatyana Kostrnova3, Valentine Drucker3, Yasuhiro Satoh4 and Yasunori Watanabe2

1National Institute for Environmental Studies Tsukuba, Ibaraki 305 2Department of Biology, Faculty of Science, Tokyo Metropolitan University Minami-Osawa, Hachioji, Tokyo 192-03, Japan 3Limnological Institute, Siberian Branch of Academy of Sciences Russia, Ulan-Botorskaya, Irkutsk, Russia 664033 4Department of Chemistry, Faculty of Science, Yamagata University Yamagata 990, Japan Institute for Hydrospheric-Atmospheric Sciences, Nagoya University Chikusa, Nagoya 464-01

Received on October 13, 1993; accepted on March 13, 1994 Autotrophic picoplankton were highly abundant during the thermal stratification period in late July in the pelagic area (water depth 500–1300 m) of southern Lake Baikal; maximum numbers were 2 x 106 cells ml–1 in the euphotic zone ({small tilde}15 m). Unicellular cyanobacteria generally dominated the picoplankton community, although unidentified picoplankton that fluoresced red under blue excitation were also abundant (maximum numbers 4 x 105 cells ml–1) and contributed up to {small tilde}40% of the total autotrophic picoplankton on occasions. Carbon and nitrogen biomasses of autotrophic picoplankton estimated by conversion from biovolumes were 14–84 µg C l–1 and 3.6–21 µg N l–1. These were comparable to or exceeded the biomass of heterotrophic bacteria. Autotropic picoplankton and bacteria accounted for as much as 33% of paniculate organic carbon and 81% of nitrogen in the euphotic zone. Measurements of the photosynthetic uptake of [l4C]bicarbonate and the growth of picoplankton in diluted or size-fractionated waters revealed that 80% of total primary production was due to picoplankton, and that much of this production was consumed by grazers in the <20 µ.m cell-size category. These results suggest that picoplankton-protozoan trophic coupling is important in the pelagic food web and biogeochemical cycling of Lake Baikal during summer.


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