Dulic, Zorka; Markovic, Zoran; Zivic, Miroslav; Ciric, Milos; Stankovic, Marko; Subakov-Simic, Gordana; Zivic, Ivana (2013): List of phytoplankton, zooplankton and zoobenthos species abundances [dataset]. PANGAEA, https://doi.org/10.1594/PANGAEA.807448,

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Supplement to: Dulic, Z et al. (2013): The response of phytoplankton, zooplankton and zoobenthos communities to changes in the quality of inflow water of small aquaculture ponds. Limnologica, 50(2), 131-141, https://doi.org/10.1051/limn/2014005

We studied the effects of changed quality of inflow water of aquaculture ponds on three aquatic communities, phytoplankton, zooplankton and zoobenthos, during two seasons of rearing common carp (Cyprinus carpio). The new water source coming from a deep tube well was markedly different in water chemistry from the surface water sources previously used to maintain the investigated fish ponds. Ponds supplied by the tube well water were characterized by lower oxygen and water hardness, and higher total ammonia and conductivity reaching subsaline conditions. Multivariate analysis (co-inertia) revealed that all investigated groups, except Mollusca (zoobenthos), decreased in species richness, abundance and biomass due to changed water chemistry, but differed in the level of susceptibility to stressors. Assemblages of Rotifera and Cladocera were the most affected showing a sharp decline in density and number of species since 29 out of 44 species disappeared from the ponds. The abundance of Copepoda (Cyclopoida) was relatively high although significantly lower in new environmental conditions (P<0.05), with adults being more tolerant to changed inflow water than larvae. Phytoplankton, except Bacillariophyta, had a highest potential to replace previous species with newcomers more adapted to changed inflow water, providing 36 immigrant species while 49 became extinct. Although mainly influenced by fish predation, Chironomidae (zoobenthos) were undoubtedly affected by changed water chemistry, decreasing from 11 to only 3 species. These results suggest that this pattern was a result of the shift from freshwater to subsaline conditions.

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