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Seasonal changes in zooplankton abundance,biomass, size structure and dominant copepods in the Oyashio region analysed by an optical plankton counter
Institution:1. Sorbonne Universités, UPMC Univ Paris 06, UMR 7093, LOV, Observatoire océanologique, F-06230 Villefranche/mer, France;2. CNRS, UMR 7093, LOV, Observatoire océanologique, F-06230 Villefranche/mer, France;3. Hellenic Centre for Marine Research, Institute of Oceanography, PO Box 2214, 71003 Heraklion, Crete, Greece;4. University of Crete, Department of Biology, University Campus, 70013 Heraklion, Crete, Greece;5. Oceanography Division, OGS (Instituto Nazionale di Oceanografia e di Geofisica Sperimentale), v. A. Piccard 54, I-34151 Trieste, Italy;1. Division of Marine Bioresource and Environmental Science, Graduate School of Fisheries Sciences, Hokkaido University, 3-1-1 Minato-cho, Hakodate, Hokkaido 041-8611, Japan;2. Moune Institute for Forest-Sato-Sea Studies, 212 Karakuwa-cho Higashi-moune, Kesennuma, Miyagi 988-0582, Japan;3. Hokkaido Research Organization, Fisheries Research Department, Hakodate Fisheries Research Institute, 20 Benten-cho, Hakodate, Hokkaido 040-0051, Japan;4. Hokkaido Research Organization, Fisheries Research Institute, 238 Hamanaka-cho, Yoichi, Hokkaido 046-8555, Japan;1. Graduate School of Fisheries Sciences, Hokkaido University, 3-1-1 Minato-cho, Hakodate, Hokkaido 041-8611, Japan;2. Tokyo Institute of Technology, School of Environment and Society, 2-12-1-M1-4 Ookayama, Meguro, Tokyo 152-8552, Japan;3. National Research Institute of Fisheries Science, 2-12-4 Fukuura, Kanazawa, Kanagawa 236-8648, Japan;4. Australian Antarctic Division,203 Channel Highway, Kingston, Tasmania, 7050, Australia;1. Research Center for Ocean Energy and Strategies, National Taiwan Ocean University, Keelung 202, Taiwan;2. Taiwan Ocean Research Institute, National Applied Research Laboratories, Kaoshiung 701, Taiwan;3. Department of Marine Environmental Informatics, National Taiwan Ocean University, Keelung 202, Taiwan;4. Department of Harbor and River Engineering, National Taiwan Ocean University, Keelung 202, Taiwan;1. Graduate School of Environment and Information Sciences, Yokohama National University, 79-1 Tokiwadai, Hodogaya, Yokohama, Kanagawa 240-8501, Japan;2. National Research Institute of Fisheries Science, Fisheries Research Agency (FRA), 2-12-4 Fukuura, Kanazawa, Yokohama, Kanagawa 236-8648, Japan;3. Tohoku National Fisheries Research Institute, Fisheries Research Agency (FRA), 3-27-5 Shinhama, Shiogama, Miyagi 985-0001, Japan;4. Hokkaido National Fisheries Research Institute, Fisheries Research Agency (FRA), Kushiro Laboratory, 116 Katsurakoi, Kushiro, Hokkaido 085-0802, Japan;1. Québec-Océan, Département de biologie, Université Laval, Québec, QC G1V 0A6, Canada;2. Norwegian Polar Institute, N-9296 Tromsø, Norway;3. Akvaplan-niva, Fram Centre for Climate and the Environment, N-9296 Tromsø, Norway;4. Institute of Arctic and Marine Biology, Faculty of Biosciences, Fisheries and Economics, University of Tromsø, N-9037 Tromsø, Norway;5. Alfred Wegener Institute for Polar and Marine Research, Am Handelshafen 12, D-27570 Bremerhaven, Germany
Abstract:To identify seasonal patterns of change in zooplankton communities, an optical plankton counter (OPC) and microscopic analysis were utilised to characterise zooplankton samples collected from 0 to 150 m and 0 to 500 m in the Oyashio region every one to three months from 2002 to 2007. Based on the OPC measurements, the abundance and biomass of zooplankton peaked in June (0–150 m) or August (150–500 m), depending on the depth stratum. The peak periods of the copepod species that were dominant in terms of abundance and biomass indicated species-specific patterns. Three Neocalanus species (Neocalanus cristatus, Neocalanus flemingeri and Neocalanus plumchrus) exhibited abundance peaks that occurred before their biomass peaks, whereas Eucalanus bungii and Metridia pacifica experienced biomass peaks before their abundance peaks. The abundance peaks corresponded to the recruitment periods of early copepodid stages, whereas the biomass peaks corresponded to the periods when the dominant populations reached the late copepodid stages (C5 or C6). Because the reproduction of Neocalanus spp. occurred in the deep layer (>500 m), their biomass peaks were observed when the major populations reached stage C5 after the abundance peaks of the early copepodid stages. The reproduction of E. bungii and M. pacifica occurred near the surface layer. These species first formed biomass peaks of C6 and later developed abundance peaks of newly recruited early copepodid stages. From the comparison between OPC measurements and microscopic analyses, seasonal changes in zooplankton biomass at depths of 0–150 m were governed primarily by E. bungii and M. pacifica, whereas those at depths of 150–500 m were primarily caused by the three Neocalanus species.
Keywords:ESD  Life cycle  OPC
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