Diel vertical migration and nutrient transport of the dinoagellate Peridinium bipes f. occultatum in a thermally stratied reservoir T. Inoue and Y. Iseri ABSTRACT Field observations were conducted with respect to the vertical migration of the dinoagellate Peridinium bipes and its inuence on vertical nutrient transport in a stratied reservoir. P. bipes migrated vertically with circadian rhythms; that is, P. bipes migrated downward and accumulated in the top layer of the hypolimnion from evening to night and then migrated upward and accumulated in the epilimnion in the early morning. In the top layer of the hypolimnion, a rapid decrease in nutrient concentration was observed in the evening, presumably due to uptake by P. bipes. Active migration from the epilimnion to the top of the hypolimnion was also suggested by estimation of the descent velocity of P. bipes, which was advantageous for the uptake of nutrients. Moreover, based on the equilibrium of forces during migration, the energy cost of vertical migration could be inferred to be negligible. The results suggest that active vertical migration of P. bipes played an important role in nutrient transport between the hypolimnion and the epilimnion in a stratied reservoir. T. Inoue (corresponding author) Coastal and Estuarine Environment Research Field, Port and Airport Research Institute, 3-1-1 Nagase, Yokosuka 239-0826, Japan E-mail: inoue-t@ipc.pari.go.jp Y. Iseri West Japan Engineering Consultants, Inc., 1-1-1 Watanabe-dori, Chuo-ku, Fukuoka 810-0004, Japan Key words | dinoagellate, nutrient transport, stratied reservoir, vertical migration INTRODUCTION The water blooms of specic phytoplanktons and freshwater red tides cause serious problems in enclosed waters, and nutrient concentration is considered as one of the most important parameters for the problem. As phosphorus is supplied due to the benthic release or microbial degra- dation, phosphorus depletion will be the most important limiting factor for primary production when the vertical den- sity stratication is secure in a water column. Dinoagellates overcome such nutrient depletion by vertical migration to access a layer in which the nutrient concentration is high enough for primary production (Lunven et al. ; Town- send et al. ; Ralston et al. ). Their motility allows them to accumulate not only in a nutrient-rich layer (nutri- cline), but also in a preferred layer where the light conditions are optimal for reproduction ( Ji & Franks ). The vertical migration of dinoagellates has fre- quently been investigated, and their circadian rhythm is considered to be related to the photoresponse, endogenous rhythm, and internal nutritional state (Forward & Daven- port ; Ji & Franks ; Ralston et al. ). However, there are few studies on nutrient transport via the vertical migration of freshwater phytoplankton (Yamada et al. ). This led us to investigate nutrient uptake and trans- port due to the vertical migration of Peridinium bipes, which is often dominant in oligotrophic or mesotrophic lakes and reservoirs, based on eld observations at a small, stratied reservoir with no obvious current. MATERIALS AND METHODS Field observations Field observations were conducted at Imuta Reservoir, a man-made reservoir located in Fukuoka prefecture, Japan (15,000 m 2 in area, 5.0 m in maximum depth, 33 W 38.9 0 N, 130 W 30.1 0 E). The reservoir, surrounded by paved roads and a golf course, is in a predominately residential area. Because there are no inowing or outowing rivers, the water quality is mainly controlled by weather conditions, and horizontal water-quality proles are homogeneous. On average, conductivity, pH, and oxidationreduction poten- tial during the summer season are 150 μS cm 1 , 9.2, and 140 mV in the surface layer and 200 μS cm À1 , 6.6, and 1212 © IWA Publishing 2012 Water Science & Technology | 66.6 | 2012 doi: 10.2166/wst.2012.302