Despite their pivotal role as primary producers, there is little information as to the diversity and physiology of cyanobacteria in the meltwater ecosystems of polar regions. Thirty cyanobacterial mats from Adelaide Island, Antarctica were investigated using 16S rRNA gene pyrosequencing and automated ribosomal intergenic spacer analysis, and screened for cyanobacterial toxins using molecular and chemical approaches. A total of 274 operational taxonomic units (OTUs) were detected. The richness ranged between 8 and 33 cyanobacterial OTUs per sample, reflecting a high mat diversity. Leptolyngbya and Phormidium (c. 55% and 37% of the OTUs per mat) were dominant. Cyanobacterial community composition was similar between mats, particularly those obtained from closely adjacent locations. The cyanotoxin microcystin was detected in 26 of 27 mats (10–300 ng g-1 organic mass), while cylindrospermopsin, detected for the first time in Antarctica, was present in 21 of 30 mats (2–156 ng g-1 organic mass). The latter was confirmed via liquid chromatography-mass spectrometry and by the presence of the cyrAB and cyrJ genes. This study demonstrates the usefulness of pyrosequencing for characterizing diverse cyanobacterial communities, and confirms that cyanobacteria from extreme environments produce a similar range of cyanotoxins as their temperate counterparts.

The river Nile is the main source of drinking water in Egypt. Nutrient loading coupled with year-round warm weather favor the growth of cyanobacteria, several of which can produce cyanotoxins, especially the potent liver toxins called microcystins. Most microcystin resides inside or closely attached to cyanobacteria cells, and are released into the water column as cells lyse from senescence or chemical treatment. The present study evaluated microcystin levels, as measured by immunoassay (ELISA), in both raw and finished drinking water of the river Nile, during the warm season (May-October), near the drinking water intake for Sohag City, Egypt. The results showed that microcystin content within the cells correlated better with type of microcystin-producing cyanobacteria (Gomphosphaeria, Microcystis, Oscillatoria) rather than chlorophyll a. Microcystin concentration in cell-free water correlated significantly with that measured within the cells, with maximum values being recorded in September (0.4-0.78 µg l-1). Microcystin levels in the finished drinking water were low (56.1- 87.1 ng l-1) and were detected only in May and June. The study indicates that microcystin is present in the raw and finished drinking water at Sohag City but that levels did not exceed the World Health Organization (WHO) drinking water guideline level of 1µg l-1 during May-October 1999.

The production of potent toxins by bloom-, scum- and mat-forming cyanobacteria, in fresh-, brackish and marine waters, appears to be a global phenomenon. Cyanobacterial toxins can also be produced by cyanobacteria from terrestrial sources. The range and number of known cyanobacterial toxins are increasing apace as associated poisoning incidents are investigated, and increasingly powerful analytical methods are applied to complement toxicity-based studies on both natural samples and laboratory isolates of cyanobacteria. Water quality management to reduce toxic cyanobacterial mass developments, and schemes to mitigate the potential effects of cyanobacterial toxins, require an understanding of the occurrence and properties of the toxins and of the exposure routes via which the toxins present risks to health. Here, we review advances in the recognition of cyanobacterial toxins and their toxicity, and of the exposure routes with reference to human health, namely via skin contact, inhalation, haemodialysis and ingestion (the oral route).

During the last two decades, more than 100 cattle deaths have been reported from 11 alpine sites in south-eastern Switzerland. Pathological findings and the histological examination of their organs strongly indicated acute hepatotoxicosis. Clinical symptoms suggestive of neurotoxicity were also observed in some cases. To elucidate the etiology of these poisonings, different water bodies in one of the affected alpine pastures were investigated for cyanobacterial toxins. The waters were highly oligotrophic, cold and turbid, and the ice-free period was limited to 3–4 months. The algal community in these waters consisted mostly of benthic cyanobacteria forming dense mats on the surface of sediments and on submerged rocks. Oscillatoria limosa and Phormidium konstantinosum (=Oscillatoria tenuis) dominated these populations, but occasionally other species of Oscillatoria, Phormidium, Tychonema and Pseudanabaena also occurred in the mats. Samples from the cyanobacterial mats yielded positive results in a protein phosphatase inhibition assay, reacted with antibodies against microcystins in an enzyme-linked immunosorbent assay and were hepatotoxic in a mouse bioassay. The same cyanobacterial material also included neurological effects in mice. High-performance liquid chromatography was used to identify a microcystin, in these cyanobacterial samples as well as in the corresponding lake water. To our knowledge, this is the first documented example of hepatotoxicity associated with benthic cyanobacteria, and the first report of toxic cyanobacteria from the remote, oligotrophic alpine environment.