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Juvenile nursery colonization patterns for the European flounder (Platichthys flesus): A latitudinal approach
Institution:1. Centre for Functional Ecology (CFE), Department of Life Sciences, University of Coimbra, Apartado 3046, 3001-401 Coimbra, Portugal;2. Royal Netherlands Institute for Sea Research (NIOZ), PO Box 59, 1790 AB Den Burg Texel, The Netherlands;3. Centro de Oceanografia, Faculdade de Ciências da Universidade de Lisboa, Campo Grande, 1749-016 Lisboa, Portugal;1. Department of Marine Sciences, University of Gothenburg, S-40530 Gothenburg, Sweden;2. Department of Marine Sciences, Kristineberg Marine Biological Laboratory, University of Gothenburg, S-45178 Fiskebäckskil, Sweden;3. Groningen Institute for Evolutionary Life Sciences, University of Groningen, Postbus 11103, 9700 CC Groningen, The Netherlands;1. School of Marine Science and Policy, University of Delaware, Lewes, DE 19958, USA;2. Institute of Marine Research, PB 1870 Nordnes, 5817 Bergen, Norway;3. Department of Biology, University of Bergen, PB 7803, 5020 Bergen, Norway;1. EPHYSLAB, Environmental PHYsics LABoratory, Facultad de Ciencias, Universidad de Vigo, 32004 Ourense, Spain;2. CESAM, Physics Department, University of Aveiro, Aveiro 3810-193, Portugal
Abstract:In this work, we analysed the latitudinal trends in the nursery habitat colonization processes of the European flounder (Platichthys flesus). This was accomplished by estimating the duration of the pelagic and metamorphic stages, as well as the duration of the spawning period, in several nursery areas across its geographical distribution range in the European Atlantic Coast: Mondego estuary (Portugal), Vilaine estuary (France), Slack estuary (France), Wadden Sea (Netherlands) and the Sørfjord (Norway). All juvenile flounders were captured with beam trawls in June/July 2010, and otolith microstructure was used to determine the duration of each stage by means of daily growth increments. The pelagic and metamorphic stages were longer at the middle of the distribution range, and lasted in total up to two months after hatching. The spawning period occurred between mid-January and early-July over the species' distribution range, with a time lapse of nearly two months between the Mondego estuary and the Sørfjord, as a consequence of warmer water temperature earlier in the season in southern areas. In general, total length of the captured fish showed a latitudinal cline between the northernmost and southernmost sampling sites, with higher values at the middle of the distribution range. The results also suggested the existence of a countergradient growth compensation mechanism in the northernmost populations. Apart from temperature, which sets the general metabolic pace of organisms, differences between sites were also related with local features, such as the extension of the continental platform and adaptations to transport and retention mechanisms.
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