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Morphological changes of Microcystis aeruginosa colonies in culture
4676PDF: 1234HTML: 2052 -
Temporal changes in nutrients in a deep oligomictic lake: the role of external loads versus climate change
1882PDF: 405Supplementary: 77HTML: 61 -
Higher late summer methane emission from central than northern European lakes
4399PDF: 1120Supplementary: 474HTML: 1325 -
Morphology-based classification of functional groups for potamoplankton
3656PDF: 1055Supplementary: 334HTML: 910 -
Metabarcoding to monitor the crustacean zooplankton of a lake improves when using a reference DNA library from local samples
2380PDF: 584HTML: 116Supplementary: 73Supplementary Data: 107 -
Degree of high phenotypic plasticity in wild populations of Daphnia in early spring
1336PDF: 413Supplementary: 173HTML: 41 -
Changes in and driving factors of the lake area of Huri Chagannao’er Lake in Inner Mongolia
1946PDF: 297Supplementary: 155HTML: 75 -
Daphnia magna fitness during low food supply under different water temperature and brownification scenarios
4529PDF: 1128Supplementary: 350HTML: 1602 -
Deep-mixing and deep-cooling events in Lake Garda: Simulation and mechanisms
1959PDF: 777Supplementary: 134HTML: 91 -
Predicting aquatic macrophyte occurrence in soft-water oligotrophic lakes (Pyrenees mountain range)
4214PDF: 915Supplementary: 258HTML: 516 -
Daphnia diversity in water bodies of the Po River Basin
4096PDF: 830Supplementary: 376HTML: 829 -
Exploiting high frequency monitoring and satellite imagery for assessing chlorophyll-a dynamics in a shallow eutrophic lake
1981PDF: 304Supplementary 1: 61Supplementary 2: 60Supplementary 3: 63HTML: 76 -
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
2079PDF: 683Id Tree of all specimens: 296HTML: 88 -
Thermal regime of a highly regulated Italian river (Ticino River) and implications for aquatic communities
3469PDF: 1064Supplementary: 244HTML: 1415