Spatial Distribution of Plankton in Response to Ecological Dynamics in Tropical Shallow Lakes: Insight from Lake Malombe, Malawi

This study assessed plankton density and biomass in an attempt to better understand their spatial and seasonal variation in Lake Malombe. Samples were collected for analysis during the hot dry season (HDS) and cool dry windy season (CDWS). The zooplankton identified were T. cunningtoni (TC), M. aEq. Aequatorialis (MAA), T. neglectus (TN), Bosmina longirostris (BL), Diaphanosoma spp (DS), Nauplii, and Rotifer. These zooplankton groups belong to copepods, Cyclopidae, Cladocera, Ctenopod, and Rotifers. The phytoplankton biomass exhibited a strong seasonal variation with the highest value observed in HDS and lowest in CDWS. Zooplankton such as T. cunningtoni, M. aEq. Aequatorialis, T. neglectus, Bosmina longirostris, Diaphanosoma spp, Nauplii, and Rotifer were dominant during the HDS. The WT, pH, and DO, Chlo-a positively correlated with all zooplankton groups. The Na+ and K+ positively correlated with TC, MAA, DS, Nauplii, and Rotifers. The Cl− positively correlated with DS, Rotifers while, CO32− positively correlated with TC. HCO3− correlated with DS and Rotifers positively while TDS correlated with BL, Nauplii, and Rotifers negatively. Nitrite affected all zooplankton groups negatively while SRP had a positive effect on all zooplankton density. The study revealed that physical-chemical variables, some major ions, and Chlo-a are the most important factors influencing the spatial and seasonal variation of zooplankton density in the lake. These findings demonstrate the interaction between physical-chemical variables, phytoplankton, and zooplankton and highlight the significance of ecological understanding of the complex dynamics of food web system in tropical shallow lakes - under the changing climate.

Reconstruction of flood events in an oxbow lake (Marótzugi-Holt-Tisza, NE Hungary) by using subfossil cladocerans remains and sediments

<p>Oxbow lakes are important components of the floodplain systems of lowland rivers. During flood events, oxbows are connected with the main river channel, and behave as lotic systems, while during inter-flood periods, these lakes can be considered as lentic ecosystems. Rivers are generally poor in planktonic organisms and their sediments contain scarce biological remains in comparison to lentic water ecosystems. However, due to their alternating running and standing water regime, sedimentary biological remains of oxbow lakes can be used as proxies for tracking changes of past hydrological regimes. In this study we investigated how cladoceran communities respond to flood events, and whether flood events can be recognized by community analysis of cladoceran remains. A sediment core from Marótzugi-Holt-Tisza oxbow lake was analyzed for identification of past flood events based on changes in the subfossil Cladocera community. Floods were defined based on the proportion of fine sand (50 µm grain size) in the oxbow sediments. If the fine sand portion was &lt;3%, the water regime of the oxbow was considered as lentic, otherwise it was lotic. Both organic and pigment contents were significantly higher in the core sections deposited during lentic stages. Thirty-four Cladocera species were determined in this core, all common to littoral habitats of eutrophic shallow lakes in Hungary. One planktonic (<em>Bosmina longirostris</em>) and four chydorid species (<em>Alona rectangula</em>, <em>Acroperus harpae</em>, <em>Alonella nana</em> and <em>Chydorus sphaericus</em>) were dominant throughout the core and contributed &gt;90% of total remains. Discriminant analysis on cladoceran data confirmed that lotic and lentic hydrological stages were characterized by different Cladocera species associations. <em>Bosmina longirostris, Chydorus sphaericus, Alona rectangula, Acroperus harpae, Leydigia leydigi, A. quadrangularis </em>and<em> A. nana</em> were mainly responsible for the differences between lotic and lentic species assemblages. Our results revealed that Cladocera remains can be used to track changes in the hydrological regime of oxbow lakes. </p><p> </p>