Abstract

Elucidating the causes of cyanobacterial bloom in continental inland waters is an urgent problem in freshwater biology. The following factors are now generally believed to induce cyanobacterial bloom [1]: a stable vertical stratification of the water column, a high water temperature and high illuminance above water, an enhanced phosphorus load, a total nitrogen to total phosphorus concentration ratio below 30 : 1, high concentrations of organic matter and microelements, and a low pressure from consumers (zooplankton). However, the presence of one or several of these factors does not guarantee the bloom (or its absence) in a given water basin.

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