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dc.contributor.authorRychtecký, Pavel
dc.date.accessioned2021-12-06T14:06:56Z
dc.date.available2021-12-06T14:06:56Z
dc.date.issued2014
dc.date.submitted2013-12-20
dc.identifier.urihttps://dspace.jcu.cz/handle/123456789/24585
dc.format15
dc.format15
dc.language.isoeng
dc.publisherJihočeská univerzitacze
dc.rightsBez omezení
dc.subjectPhytoplanktoneng
dc.subjectReservoireng
dc.subjectSpatial heterogeneityeng
dc.subjectSeasonal successioneng
dc.subjectFunctional classificationeng
dc.subjectFlood eventeng
dc.titleSpatial heterogeneity and seasonal succession of phytoplankton along the longitudinal gradient in a eutrophic reservoircze
dc.title.alternativeSpatial heterogeneity and seasonal succession of phytoplankton along the longitudinal gradient in a eutrophic reservoireng
dc.typerigorózní prácecze
dc.identifier.stag36407
dc.description.abstract-translatedSpatial distribution and seasonal succesion of phytoplankton along the longitudinal axis of a eutrophic Římov reservoir (Czech Republic) was investigated from April to October 2007, at 1?2 week intervals. Phytoplankton spatial heterogeneity was the most apparent during the summer reflecting a pronounced gradient of environmental parameters from the river inflow to the dam. The riverine zone differed markedly from downstream parts of the reservoir, being dominated by functional groups D and J (large cryptophytes and colonial diatoms). While a dense cyanobacterial bloom (groups H1 and M) occurred in the transition zone, considerably lower biomass of desmids (Group N) was found at lacustrine zone at the same time. A sudden flood event considerably altered nutrient and light availability, and later even resulted in cyanobacterial dominance in the whole reservoir.eng
dc.date.accepted2014-02-12
dc.description.departmentPřírodovědecká fakultacze
dc.thesis.degree-disciplineEkologiecze
dc.thesis.degree-grantorJihočeská univerzita. Přírodovědecká fakultacze
dc.thesis.degree-nameRNDr.
dc.thesis.degree-programEkologiecze
dc.description.gradeDokončená práce s úspěšnou obhajoboucze


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