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2014
DOI: 10.1007/s10661-014-3690-0
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Ecological validity of river-floodplain system assessment by planktonic crustacean survey (Branchiata: Branchiopoda)

Abstract: Studies of the Slovakian Danube have indicated profound changes in the structures of several invertebrate assemblages in the section of the river bypassed by the Gabčíkovo hydroelectric project in 1992 and in adjacent floodplain water bodies. The present study investigates the relationship between hydrological connectivity and species diversity in the old main channel and adjacent left-bank water bodies, using resident cladocerans as indicators of the ecological integrity of the river-floodplain system. The wo… Show more

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Cited by 10 publications
(3 citation statements)
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“…Cladocera is important on the water quality and ecology of the lakes when appeared in the middle level of trophic degree [24]. Also, Cladocera has been defined as a good indicator of hydrological dynamism of the water floor and the heterogeneity of the habitat [25]. Rotifera, Cladocera, and Copepoda are the basic groups of zooplankton in freshwaters.…”
Section: Introductionmentioning
confidence: 99%
“…Cladocera is important on the water quality and ecology of the lakes when appeared in the middle level of trophic degree [24]. Also, Cladocera has been defined as a good indicator of hydrological dynamism of the water floor and the heterogeneity of the habitat [25]. Rotifera, Cladocera, and Copepoda are the basic groups of zooplankton in freshwaters.…”
Section: Introductionmentioning
confidence: 99%
“…owing to several problems (economical, social, ecological or political), Slovakia begun to build water scheme without the support of Hungary (Jansky et al, 2004). The main disadvantages of this decision were major ecological consequences in surrounding areas (Lehotský et al, 2013;illyová, Matečný, 2014;oťaheľová et al, 2007;Jansky et al, 2004). average annual discharge in the by-passed Danube river channel (measured in section 1 848, 4 rkm) was decreased after waterworks initiation in 1993 from 1 900 to 350 m 3 s −1 , resp.…”
Section: Gabčíkovo-nagymaros Waterwork and Sedimentationmentioning
confidence: 99%
“…average annual discharge in the by-passed Danube river channel (measured in section 1 848, 4 rkm) was decreased after waterworks initiation in 1993 from 1 900 to 350 m 3 s −1 , resp. to 220 m 3 s −1 in 1994 (in the winter) and maximum current velocities declined from 2.0−3.5 to 1 m s −1 (vranovský, 1997;illyová, Matečný, 2014). Landforms accumulation on groynes started to form a scrollbar that has developed into floodplain pockets.…”
Section: Gabčíkovo-nagymaros Waterwork and Sedimentationmentioning
confidence: 99%