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Is there a common threshold to subfossil chironomid assemblages at 16 m water depth? Evidence from the Tibetan Plateau 16 m water depth – a chironomid depth threshold?
1293PDF: 443Supplementary: 114HTML: 8 -
Morphological changes of Microcystis aeruginosa colonies in culture
4670PDF: 1231HTML: 2052 -
Hydrological characteristics of extreme floods in the Klaserie River, a headwater stream in southern Africa
2000PDF: 428Supplementary: 52HTML: 49 -
Anuran larvae diet from agroecosystem’s ponds: environmental quality and implications for their populations
2643PDF: 947Supplementary: 343HTML: 1508 -
Influence of re-flooding on phytoplankton assemblages in a temperate wetland following prolonged drought
3532PDF: 1280Supplementary: 431HTML: 1894 -
Sources of organic matter affect depth-related microbial community composition in sediments of Lake Erhai, Southwest China
3320PDF: 1022Supplementary: 358HTML: 1945 -
Ostracod valves as efficient UV protection
2716PDF: 864HTML: 589 -
Response of sedimentary processes to cyanobacteria loading
3681PDF: 1259HTML: 1156 -
Environmental drivers influencing stonefly assemblages along a longitudinal gradient in karst lotic habitats Stonefly ecological traits
1620PDF: 562HTML: 31 -
Relationship between bream (Abramis brama) activity and water turbidity in a shallow lake under different season conditions
1514PDF: 500Supplementary: 96HTML: 21