Microcystins (MC) can be detected in water bodies worldwide. MC-producing cyanobacteria including Microcystis, Planktothrix and Anabaena are apparently cosmopolitan and the eutrophication of many water bodies enables their (massive) proliferation. Studies from different countries have found MCs in 80-100% of samples containing Microcystis, Planktohrix and/or Anabena. Thus, the presence of microcystins should be assumed during occurrence of these cyanobacteria, unless proven otherwise.
With Microcystis the concentration of microcystins in the open water are mostly below 100 µg/l. However, Microcystis usually forms surface scums or accumulations at shorelines during calm weather conditions, which can lead to microcystin concentrations that are several orders of magnitude higher compared to those in the open water. Concentrations between 1000 – 40000 µg/l have been reported from blooms and shoreline accumulations with a high variation over time and space due to changing wind directions and speed and the morphology of the water body (Fig.1).
Planktothrix rubescens displays another pattern of concentration variation within a water body: during summer stratification of a water body this species grows in the metalimnion with microcystin concentrations usually between < 1-10 µg/l in this layer. During the autumn turnover the cells (and MC) are entrained into the whole water column and also surface scums with extremely high microcystin concentrations have been reported ( >> 10000 µg/l).
Also in dense populations of Planktohrix agardhii MC concentrations can amount 100 µg/l or even more, but as this species usually occurs in shallow and thus frequently mixed lakes surface scums or accumulations at shorelines do not occur.
MCs are largely cell-bound and enter the water phase only during dying-off of the cells. In healthy populations, the dissolved microcystins usually account for less than about 10% of the total microcystin concentration. Higher concentrations of dissolved microcystins are observed after the break-down of blooms, but are often (though not always) quickly diluted within the water column and degraded by bacteria within several days.
Relationship of microcystin to biovolume
A quick estimation of the risk due to microcystins when a cyanobacterial bloom occurs can be done roughly with toxin concentrations per biomass units derived from field samples.
For microcystins, a number of data sets are available which use either the biovolume (BV) or chlorophyll- a (Chl-a) concentration as biomass reference unit. Culture strains mostly produce 0.5-5 µg microcystin per mm³ BV. In the field, concentrations are often below 1 µg microcystin per mm³ BV or 0,3 per µg Chl-a (Fig.1) probably due to the mixture of microcystin-producing and non-producing genotypes. In some cases, however, higher (up to 6 –fold) concentrations per biomass unit are reported.
Uncertainty arises when using chlorophyll-a as a reference unit due to the variability of cellular Chl-a content due to environmental conditions as well as to the variable contribution of the cyanobacteria to the whole phytoplankton. Though biovolume is the more accurate reference unit, the determination of biovolume is less widely practised and requires more experience than chlorophyll-a analysis. For a first “worst case” estimation of the toxin concentration per Chl-a (0.3 µg MC/µg Chl.a) or biovolume (1 µg MC/mm³ BV) are therefore both acceptable.
Fig. 1: Concentrations of microcystins along the shorelines of the river Havel (Berlin, Germany) during a mass development of Microcystis sp. (MC: columns, MC/Chl-a relation: black dots).