Abstract
Microstratification of phytoplankton in the large shallow Lake Balaton (Hungary) was studied during a 24 h period. Dissolved O2 showed biological stratification; flagellates exhibited a definite circadian rhythm. In the middle of the investigation a heavy storm broke out which was followed by the disappearance of differences between different layers of water. Storm-induced destratification is described by cluster-analysis. Abundances of dominant species changed differently in connection with the storm. Numbers of Nitzschia sp. increased due to stirring up from the sediment surface. Numbers of single-celled or colony-forming species (Cyclotella comta, Crucigenia quadrata, Coelosphaerium kuetzingianum) practically did not change. Numbers of all the three dominant filamentous species (Aphanizomenon flos-aquae f. klebahnii, Lyngbya limnetica, Planctonema lauterbornii) significantly decreased, which might be attributed to an unknown loss process and was followed by a competitive displacement by algae of small cell size.
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© 1990 Kluwer Academic Publishers, Dordrecht
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Padisák, J., G.-Tóth, L., Rajczy, M. (1990). Stir-up effect of wind on a more-or-less stratified shallow lake phytoplankton community, Lake Balaton, Hungary. In: Biró, P., Talling, J.F. (eds) Trophic Relationships in Inland Waters. Developments in Hydrobiology, vol 53. Springer, Dordrecht. https://doi.org/10.1007/978-94-009-0467-5_27
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DOI: https://doi.org/10.1007/978-94-009-0467-5_27
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