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Morphological changes of Microcystis aeruginosa colonies in culture
4668PDF: 1231HTML: 2052 -
Temporal changes in nutrients in a deep oligomictic lake: the role of external loads versus climate change
1866PDF: 403Supplementary: 76HTML: 61 -
Higher late summer methane emission from central than northern European lakes
4391PDF: 1117Supplementary: 473HTML: 1325 -
Morphology-based classification of functional groups for potamoplankton
3648PDF: 1053Supplementary: 332HTML: 909 -
Metabarcoding to monitor the crustacean zooplankton of a lake improves when using a reference DNA library from local samples
2366PDF: 581HTML: 116Supplementary: 72Supplementary Data: 107 -
Degree of high phenotypic plasticity in wild populations of Daphnia in early spring
1334PDF: 410Supplementary: 171HTML: 40 -
Changes in and driving factors of the lake area of Huri Chagannao’er Lake in Inner Mongolia
1930PDF: 296Supplementary: 153HTML: 75 -
Daphnia magna fitness during low food supply under different water temperature and brownification scenarios
4518PDF: 1125Supplementary: 348HTML: 1602 -
Deep-mixing and deep-cooling events in Lake Garda: Simulation and mechanisms
1951PDF: 776Supplementary: 129HTML: 90 -
Predicting aquatic macrophyte occurrence in soft-water oligotrophic lakes (Pyrenees mountain range)
4205PDF: 912Supplementary: 257HTML: 516 -
Daphnia diversity in water bodies of the Po River Basin
4084PDF: 829Supplementary: 374HTML: 829 -
Exploiting high frequency monitoring and satellite imagery for assessing chlorophyll-a dynamics in a shallow eutrophic lake
1973PDF: 303Supplementary 1: 58Supplementary 2: 58Supplementary 3: 61HTML: 73 -
Faunistic survey of the zooplankton community in an oligotrophic sinkhole, Cenote Azul (Quintana Roo, Mexico), using different sampling methods, and documented with DNA barcodes Zooplankton baseline in a karstic system
2069PDF: 682Id Tree of all specimens: 295HTML: 88 -
Thermal regime of a highly regulated Italian river (Ticino River) and implications for aquatic communities
3468PDF: 1063Supplementary: 243HTML: 1415