13 research outputs found

    Effects of geothermal effluents on macrobenthic communities in a pristine sub-arctic lake

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    We studied the effects of warm effluents from the Nesjavellir geothermal power plant on benthic invertebrate communities along a depth gradient of 4 m in lake Þingvallavatn, Iceland. Four study sites were selected: 2 heataffected sites and 2 cold reference sites. Thermal pollution was detected down to 0.4 m at both heat-affected sites, which were 7-12 °C higher than at the same depth at the reference sites. Sustained temperatures ≥27 °C, which is 10-17 °C above ambient water temperatures, seems to be detrimental to the gastropod Radix peregra and several of the littoral chironomid species. Such effects were, however, confined to a small area inside a sheltered rift pool at one of the heat-affected sites. Moderate warming up to ~10 °C above ambient lake temperature in summer, seems to benefit R. peregra, potentially through both a higher survival rate and a shorter life cycle. At the heat-affected sites, sustained high temperatures transformed a relatively diverse chironomid community to a species-poor community, dominated by Paratanytarsus sp. and Cricotopus sylvestris. In contrast, the chironomid Eukiefferiella minor was much more prominent at one of the reference sites. To separate thermal from biological effects, more studies are needed on speciesspecific attributes, including time-series data on growth, survival, and reproduction of the main littoral zoobenthic species. Although our research examined short-term responses of aquatic invertebrates to local thermal stress, our results may also be relevant to long-term responses of freshwater ecosystems at high latitudes to climate change and warming

    Physicochemical properties and fish occurrence in 35 Icelandic lakes housing Arctic charr (Salvelinus alpinus)

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    The common occurrence of parallel phenotypic patterns suggests that a strong relationship exists between ecological dynamics and micro-evolution. Comparative studies from a large number of populations under varying sets of ecological drivers could contribute to a better understanding of this relationship. We used data on morphology of arctic charr (Salvelinus alpinus) and ecological factors from 35 Icelandic lakes to test the hypothesis that morphological patterns among monomorphic charr populations from different lakes are related to interlake variation in ecological characteristics. There is extensive phenotypic diversity among populations of Icelandic charr, and populations are easily distinguished based on overall body morphology. The results obtained in the present study showed that the morphological diversity of charr was related to large-scale diversity in lake ecology. Variation in charr morphology was related to water origin (e.g. spring fed versus run-off), bedrock age, and fish community structure. The present study shows how various ecological factors can shape the biological diversity that we observe

    Intraspecific diversity in Arctic charr, Salvelinus alpinus, in Iceland: II. Which environmental factors influence resource polymorphism in lakes?

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    ABSTRACT Background: The mechanisms causing resource polymorphism are not well understood, but likely include frequency-dependent selection. However, other selection mechanisms could also explain the development of resource polymorphism. Comparative analyses of polymorphic and monomorphic systems are uncommon, making it difficult to distinguish the effects of geography, frequency-dependent selection, niche expansion, and species interactions. Detailing ecological conditions associated with the development of resource polymorphism is necessary to discern demographic and environmental processes that may cause it. Goal: Test for environmental correlations with (a) the presence of resource polymorphism and (b) the degree of differentiation in polymorphic systems, to evaluate the hypotheses that the development of resource polymorphism results from (1) frequency dependence, (2) expansion to include a zooplanktivorous niche, or (3) lower survivorship due to predation on intermediate trait values. Trends in prey consumption, as they related to the presence of polymorphism and limnetic lake characteristics, were also analysed. Organism: Arctic charr (Salvelinus alpinus) populations from lakes sampled in 1994-2004 across Iceland. Methods: Random forest and multiple regression models assessing the presence and degree of resource polymorphism using environmental variables reflecting physical, chemical, and biological conditions. Prey consumption was fitted to the presence of polymorphism and brown trout abundance in negative binomial generalized linear models. The proportion of individuals consuming zooplankton within monomorphic versus polymorphic populations was also measured to test the idea that more widespread zooplankton consumption reflects niche expansion. Results: In Iceland, polymorphic populations tended to occur in cooler lakes with few brown trout (Salmo trutta), a trophic competitor, and in lakes where Arctic charr consumed more zooplankton. Lakes with greater limnetic habitat, fewer nutrients, and greater potential to consume zooplankton appeared to promote resource polymorphism, thereby supporting the presence of niche expansion. The overall results supported the frequency dependence hypothesis, as well as the niche expansion hypothesis in most cases. However, morphs tha

    Short-and long term niche segregation and individual specialization of brown trout (Salmo trutta) in species poor Faroese lakes

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    Trophic niche divergence is considered to be a major process by which species coexistence is facilitated. When studying niche segregation in lake ecosystems, we tend to view the niche on a one-dimensional pelagic-littoral axis. In reality, however, the niche use may be more complex and individual fidelity to a niche may be variable both between and within populations. In order to study this complexity, relative simple systems with few species are needed. In this paper, we study how competitor presence affects the resource use of brown trout (Salmo trutta) in 11 species-poor Faroese lakes by comparing relative abundance, stable isotope ratios and diet in multiple habitats. In the presence of three-spined sticklebacks (Gasterosteus aculeatus), a higher proportion of the trout population was found in the pelagic habitat, and trout in general relied on a more pelagic diet base as compared to trout living in allopatry or in sympatry with Arctic charr (Salvelinus alpinus). Diet analyses revealed, however, that niche-segregation may be more complex than described on a one-dimensional pelagic-littoral axis. Trout from both littoral and offshore benthic habitats had in the presence of sticklebacks a less benthic diet as compared to trout living in allopatry or in sympatry with charr. Furthermore, we found individual habitat specialization between littoral/benthic and pelagic trout in deep lakes. Hence, our findings indicate that for trout populations interspecific competition can drive shifts in both habitat and niche use, but at the same time they illustrate the complexity of the ecological niche in freshwater ecosystems

    Impacts of climate warming on the long-term dynamics of key fish species in 24 European lakes

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    Fish play a key role in the trophic dynamics of lakes. With climate warming, complex changes in fish assemblage structure may be expected owing to direct effects of temperature and indirect effects operating through eutrophication, water level changes, stratification and salinisation. We reviewed published and new long-term (10–100 years) fish data series from 24 European lakes (area: 0.04–5,648 km2; mean depth: 1–177 m; a north–south gradient from Sweden to Spain). Along with an annual temperature increase of about 0.15–0.3°C per decade profound changes have occurred in either fish assemblage composition, body size and/or age structure during recent decades and a shift towards higher dominance of eurythermal species. These shifts have occurred despite a reduction in nutrient loading in many of the lakes that should have benefited the larger-sized individuals and the fish species typically inhabiting cold-water, low-nutrient lakes. The cold-stenothermic Arctic charr has been particularly affected and its abundance has decreased in the majority of the lakes where its presence was recorded. The harvest of cool-stenothermal brown trout has decreased substantially in two southern lakes. Vendace, whitefish and smelt show a different response depending on lake depth and latitude. Perch has apparently been stimulated in the north, with stronger year classes in warm years, but its abundance has declined in the southern Lake Maggiore, Italy. Where introduced, roach seems to take advantage of the higher temperature after years of low population densities. Eurythermal species such as common bream, pike–perch and/or shad are apparently on the increase in several of the lakes. The response of fish to the warming has been surprisingly strong and fast in recent decades, making them ideal sentinels for detecting and documenting climate-induced modifications of freshwater ecosystems

    Long-term ice phenology records spanning up to 578 years for 78 lakes around the Northern Hemisphere

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    In recent decades, lakes have experienced unprecedented ice loss with widespread ramifications for winter ecological processes. The rapid loss of ice, resurgence of winter biology, and proliferation of remote sensing technologies, presents a unique opportunity to integrate disciplines to further understand the broad spatial and temporal patterns in ice loss and its consequences. Here, we summarize ice phenology records for 78 lakes in 12 countries across North America, Europe, and Asia to permit the inclusion and harmonization of in situ ice phenology observations in future interdisciplinary studies. These ice records represent some of the longest climate observations directly collected by people. We highlight the importance of applying the same definition of ice-on and ice-off within a lake across the time-series, regardless of how the ice is observed, to broaden our understanding of ice loss across vast spatial and temporal scales
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