About: Long-term changes in cladoceran assemblages in the Danube floodplain area (Slovak- Hungarian stretch)     Goto   Sponge   NotDistinct   Permalink

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  • In this paper, the distribution of Cladocera species in the different sampling sites: the main channel/old river bed, parapotamal type side arms and plesiopotamal side arms, is described. The structure of cladoceran assemblages in the by-passed Danube section and in the adjacent floodplain water bodies has changed since the Gabcikovo hydropower plant was put into operation. Great changes have been observed in the previous parapotamal side arm situated between river km 1840 and 1820, artificially fed with water from the head-race canal. The dominance of tychoplanktonic (benthic and phytophilous) species has increased, while the typical euplanktonic species have disappeared. Three characteristic groups of cladoceran assemblages were recorded when a different type of habitat was taken into consideration. Euplanktonic cladocerans prevailed on all sampling sites before damming. In periods after damming, littoral species, and later also a euplanktonic forms, dominated on the main channel sampling sites.
  • In this paper, the distribution of Cladocera species in the different sampling sites: the main channel/old river bed, parapotamal type side arms and plesiopotamal side arms, is described. The structure of cladoceran assemblages in the by-passed Danube section and in the adjacent floodplain water bodies has changed since the Gabcikovo hydropower plant was put into operation. Great changes have been observed in the previous parapotamal side arm situated between river km 1840 and 1820, artificially fed with water from the head-race canal. The dominance of tychoplanktonic (benthic and phytophilous) species has increased, while the typical euplanktonic species have disappeared. Three characteristic groups of cladoceran assemblages were recorded when a different type of habitat was taken into consideration. Euplanktonic cladocerans prevailed on all sampling sites before damming. In periods after damming, littoral species, and later also a euplanktonic forms, dominated on the main channel sampling sites. (en)
Title
  • Long-term changes in cladoceran assemblages in the Danube floodplain area (Slovak- Hungarian stretch)
  • Long-term changes in cladoceran assemblages in the Danube floodplain area (Slovak- Hungarian stretch) (en)
skos:prefLabel
  • Long-term changes in cladoceran assemblages in the Danube floodplain area (Slovak- Hungarian stretch)
  • Long-term changes in cladoceran assemblages in the Danube floodplain area (Slovak- Hungarian stretch) (en)
skos:notation
  • RIV/00216224:14310/05:00021390!RIV10-MSM-14310___
http://linked.open...avai/riv/aktivita
http://linked.open...avai/riv/aktivity
  • Z(MSM0021622412)
http://linked.open...iv/cisloPeriodika
  • 4
http://linked.open...vai/riv/dodaniDat
http://linked.open...aciTvurceVysledku
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  • 528403
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  • RIV/00216224:14310/05:00021390
http://linked.open...riv/jazykVysledku
http://linked.open.../riv/klicovaSlova
  • Crustacea; Cladoceran assemblages; inundation; habitat requirements; Gabčíkovo (en)
http://linked.open.../riv/klicoveSlovo
http://linked.open...odStatuVydavatele
  • DE - Spolková republika Německo
http://linked.open...ontrolniKodProRIV
  • [AFC4C2B86AD7]
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  • Limnologica
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http://linked.open...cetTvurcuVysledku
http://linked.open...UplatneniVysledku
http://linked.open...v/svazekPeriodika
  • 35
http://linked.open...iv/tvurceVysledku
  • Haruštiaková, Danka
  • Illyová, Marta
http://linked.open...ain/vavai/riv/wos
  • 000234083900004
http://linked.open...n/vavai/riv/zamer
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  • 0075-9511
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  • 14310
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