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Jane A. Godiksen Martin-A. Svenning J. Brian Dempson Maare Marttila Andrea Storm-Suke Michael Power 《Hydrobiologia》2010,650(1):67-77
A species-specific fractionation equation for Arctic charr (Salvelinus alpinus (L.)) was developed experimentally for use in ecological studies of temperature-driven phenologies for the species. Juvenile Arctic charr were reared in controlled conditions at different temperatures (2–14°C), with three replicates of each temperature. Otoliths from the fish and water samples from the chambers were analysed for oxygen isotope composition and used to estimate temperature-dependent fractionation equations relating the isotopic ratio to rearing temperature. A linear and a second order polynomial relationship were estimated and validated using comparable Arctic charr data from another study. Temperatures predicted using the polynomial equation were not significantly different from recorded experimental temperatures, whereas with the linear equation there were significant differences between the predicted and measured temperatures. The polynomial equation also showed the least bias as measured by mean predictive error. Statistical comparisons of the polynomial fractionation equation to a similarly estimated equation for brook charr (Salvelinus fontinalis (Mitchill)) indicated significant differences. Results imply the need for species-specific fractionation equations, even for closely related fish. Results further suggest the polynomial form of the fractionation equation will facilitate more accurate characterisation of water temperatures suitable for use in ecological studies of temperature-driven phenologies of Arctic charr. 相似文献
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Marttila Maare Louhi Pauliina Huusko Ari Vehanen Teppo Mäki-Petäys Aki Erkinaro Jaakko Syrjänen Jukka Tapani Muotka Timo 《Reviews in Fish Biology and Fisheries》2019,29(3):513-527
Reviews in Fish Biology and Fisheries - River restoration offers the potential to enhance biological integrity, often measured as fish population changes. We used a meta-analytical approach to... 相似文献
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Maare Marttila Pauliina Louhi Ari Huusko Aki Mki‐Petys Timo Yrjn Timo Muotka 《Ecohydrology》2016,9(2):280-289
Studies on the effectiveness of in‐stream restoration have generally reported increased habitat heterogeneity, but biological responses have been more variable. One hypothesis states that the restored habitat structure does not persist through time, resulting in fading biological responses. We studied the durability of in‐stream restoration in northern and central Finland by assessing short‐term (0–1 years) and long‐term (≥10 years) changes in habitat structure after restoration. In 2010, we repeated the field surveys first conducted in the 1990s in 27 stream reaches. We also made similar habitat measurements in ten near‐pristine sites. Restoration caused significant changes in the stream habitat that either remained unaltered or were reinforced through time, with several of the restored sites resembling closely the near‐pristine reference sites 10–20 years post‐restoration. Cover of aquatic mosses initially decreased sharply but recovered close to near‐pristine level within about 15 years. However, substrate variability still remained somewhat lower in the restored than in near‐pristine streams. Individual restoration structures had changed little over time. The most evident failures were the disappearance and entrenchment of gravel beds. Restoration of our study sites had shifted the sites to a trajectory towards more natural habitat conditions, and our results do not support the hypothesis that gradual destruction of the restored habitat might partly explain weak biological responses. From the perspective of channel evolution, the restorations were still fairly recent, and only long‐term monitoring will tell if the sites will continue on the trajectory to hydromorphological and ecological recovery. Copyright © 2015 John Wiley & Sons, Ltd. 相似文献
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