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Nutrient limitation of the primary production of phytoplankton in Lake Baikal
Authors:Yasuhiro Satoh  Toshiya Katano  Takeshi Satoh  Osamu Mitamura  Kaori Anbutsu  Shin-ichi Nakano  Hiroyuki Ueno  Masaki Kihira  Valentin Drucker  Yuji Tanaka  Tetsuro Mimura  Yasunori Watanabe  Masahito Sugiyama
Institution:(1) Faculty of Science, Yamagata University, Yamagata 990-8560, Japan;(2) CMES, Ehime University, Matsuyama, Japan;(3) School of Environmental Science, University of Shiga Prefecture, Hikone, Japan;(4) Limnological Institute, Siberian Branch, Russian Academy of Science, Irkutsk, Russia;(5) Department of Ocean Sciences, Tokyo University of Fisheries, Tokyo, Japan;(6) Faculty of Science, Nara Women’s University, Nara, Japan;(7) Department of Biology, Tokyo Metropolitan University, Tokyo, Japan;(8) Graduate School of Human Environmental Studies, Kyoto University, Kyoto, Japan
Abstract:Nutrient limitation of the primary production of phytoplankton at some stations in southern and central Lake Baikal was studied by nutrient enrichment experiments in August 2002. Chlorophyll (Chl.) a concentrations ranged from 0.7 to 5.8μgl−1. Inorganic nutrient concentrations were low: soluble reactive phosphorus ranged from 0.05 to 0.20μmoll−1, ammonia from 0.21 to 0.41μmoll−1, and nitrite plus nitrate from 0.33 to 0.37μmoll−1. In the five enrichment experiments, phosphate spikes and phosphate plus nitrate spikes always stimulated primary production. Nitrate spikes also stimulated primary production in four of the experiments. Significant differences were detected between the controls and phosphate spikes and between the controls and phosphate plus nitrate spikes. Thus, the first limiting nutrient is thought to be phosphorus, but once phosphorus is supplied to the surface water, the limiting nutrient will quickly shift from phosphorus to nitrogen.
Keywords:Enrichment experiments  Nitrate  Phosphate  Summer
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