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  • 1
    Electronic Resource
    Electronic Resource
    Oxford, UK : Blackwell Publishing Ltd
    Freshwater biology 24 (1990), S. 0 
    ISSN: 1365-2427
    Source: Blackwell Publishing Journal Backfiles 1879-2005
    Topics: Biology
    Notes: SUMMARY. 〈list xml:id="l1" style="custom"〉1 The composition and abundance of diatom assemblages were studied together with physiographical and physicochemical variables in twenty-eight springs in the Central Pyrenees during the period 1987–88.2 Characteristic groupings of diatom taxa are revealed by Principal Components Analysis. One group, made up of assemblages of the taxa Navicula cincta, Caloncis spp. and Niizschia elliptica, is characteristic of springs with waters of high ionic strength. Certain diatom taxa are characteristic of hard water springs, either in quiet waters (Denticula tenuis, Achnanthes minutissima, Eunotia spp.) or fast flowing ones (Fragilaria spp., Diatoma hiemale). Other taxa are representative of relatively quiet, softwater springs: Anomoeoneis bracfiysira, Tabellaria flocculosa, Aulacoseira distans and Fragilaria vaucheriae.3 Five different spring types were identified, with respect to diatom assemblages, using discriminant analysis. The first consisted of high mountain springs with cold, fast waters and low ionic strength. The second group, distributed throughout the Pyrenees, had similar environmental characteristics to the first group but with intermediate water velocity and slightly higher mineral content. The third contained springs in calcareous regions of the Pyrenees, mainly slow-flowing and with hard waters. The fourth was composed of softwater springs, whilst the fifth consisted of two springs which were subject to stressful conditions (limitation of light, abundance of nitrates or high salinity).4 Ionic strength and current velocity appeared to be the dominant environmental factors affecting diatom distribution in Pyrenean springs. These factors also seem to determine diatom communities in some other geographical areas. In some springs, however, peculiar environmental factors (dim light, salinity, and high temperature) affect the structure of diatom assemblages.
    Type of Medium: Electronic Resource
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  • 2
    ISSN: 1420-9055
    Keywords: Key words: Lake La Cruz, trophic changes, meromixis, diatoms, cladocera, ostracoda and pollen stratigraphy.
    Source: Springer Online Journal Archives 1860-2000
    Topics: Biology
    Notes: Abstract: A sediment core from a Mediterranean karstic lake was studied through its pollen, diatom, chydorid, ostracod, charcoal and authigenic mineral composition. Information about environmental history recorded in the sediment sequence since the Middle Ages is presented. The main fluctuations of water volume and trophic status of the lake occurred during periods of great change in land management and during climatic cold phases. The synergetic effect of these two factors led to a high water level phase and triggered a rising of the trophic level which produced meromixis. The onset of meromictic conditions at about 1700 AD coincides with the Maunder minimum in the Little Ice Age as well as with a period of increasing human population, woodland clearance and agricultural expansion to the detriment of the nomadic livestock breeding or transhumance ("Mesta").
    Type of Medium: Electronic Resource
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  • 3
    ISSN: 1573-5117
    Keywords: Ostracod shells ; calcium content ; water temperature ; auto-ecology ; palaeoecology
    Source: Springer Online Journal Archives 1860-2000
    Topics: Biology
    Notes: Abstract Cultures of the freshwater ostracod Herpetocyprisbrevicaudata were kept under laboratory conditions in ordertostudy effects of water temperature on development time andcalcification process. Four culture temperatures were used:12.4,14.6, 19.8 and 23.3 °C.H. brevicaudata cultured at 19.8 and 23.3 °Cshowedhigher survival rate and faster development than thosecultured at12.4 and 14.6 °C. Water temperature also has a clearinfluence on the degree of calcification of the ostracodshells.For H. brevicaudata, the 15–19 °C temperaturerangeconstitutes a threshold below which Ca content of valvessignificantly decreases. Time required to calcify is alsolongerbelow this threshold. The increase of the calcification timedue tolower water temperatures seems to induce low survivalrates.
    Type of Medium: Electronic Resource
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