| Literature DB >> 30275378 |
Mikhail Grachev1, Ilya Zubkov2, Irina Tikhonova3, Maria Ivacheva4, Anton Kuzmin5,6, Elena Sukhanova7, Ekaterina Sorokovikova8, Galina Fedorova9, Aleksandr Galkin10, Maria Suslova11, Olga Netsvetayeva12, Elena Eletskaya13, Tatyana Pogadaeva14, Vladimir Smirnov15, Andrey Ivanov16, Vladimir Shagun17, Viktor Minaev18, Olga Belykh19.
Abstract
An area of discolored water 50 m wide and 30 m long was found in September 2017 close to the dam of the Irkutsk hydroelectric power station. Water from this spot was sampled for investigation in the present study. Microscopic analysis revealed that the suspended matter in the sample was composed of clumps of filaments, vegetative cells, akinetes and heterocysts that formed short filaments and solitary cells. This matter was found to consist of partially degraded cells of the cyanobacterium Dolichospermum lemmermannii. Nucleotide sequencing of DNA isolated from the biomass revealed the presence of the sxtA gene which is involved in the synthesis of saxitoxin. Water from the polluted area contained 600 ± 100 μg L-1 saxitoxin as measured by HPLC-MS with pre-column modification of the toxin with 2,4-dinitrophenylhydrazine. Immunoassay analysis (ELISA) showed a concentration of saxitoxins in the water of 2900 ± 900 μg L-1. Hydrochemical and microbiological analyses suggested the contaminated area appeared as a result of a D. lemmermannii bloom, followed by its decay and release of saxitoxin and nutrients. The present paper describes the results of a case study. Better understanding of the phenomenon will depend on the possibility to perform implementation of a large-scale monitoring program.Entities:
Keywords: Dolichospermum lemmermannii; ELISA; HPLC-MS; Irkutsk reservoir; Lake Baikal; cyanobacteria; hydrochemical analysis; saxitoxin
Mesh:
Substances:
Year: 2018 PMID: 30275378 PMCID: PMC6215233 DOI: 10.3390/toxins10100402
Source DB: PubMed Journal: Toxins (Basel) ISSN: 2072-6651 Impact factor: 4.546
Figure 1Irkutsk Reservoir and its location relative to Lake Baikal.
Figure 2General view of Dolichospermum lemmermannii in the sample of water from the Irkutsk Reservoir: (a,с) light microscopy, (b,d) epifluorescence microscopy: (b) DAPI dye, (d) autofluorescence of phicobilins in akinetes. Notations: А—akinetes, Н—heterocysts, V—vegetative cells. Scale: (а)—50 μm, (b–d)—20 μm.
Figure 3Extracted ion current chromatogram (m/z = 462.15 ± 0.10) of the water sample taken from the polluted area near the dam of the Irkutsk hydroelectric power station. Isotopic distribution of saxitoxin-2,4-dinitrophenylhydrazone is shown in the insert.
Figure 4Mechanism of the reaction resulting in the Z-isomer of saxitoxin-2,4-dinitrophenyl hydrazone as suggested by quantum chemical calculations.
Results of hydrochemical analysis of water from the polluted area compared with the surface water of Lake Baikal.
| Indicator | Polluted Area Near the Dam of the Irkutsk Reservoir, 1 September 2017 | Surface Water of Southern Lake Baikal, Mean Values for the Last 5 Years |
|---|---|---|
| NH4+, mg L−1 | 10.8 | 0.0–0.01 |
| NO2−, mg L−1 | 0.29 | 0.0–0.003 |
| NO3−, mg L−1 | 9.72 | 0.1–0.26 |
| PO43−, mg L−1 | 6.8 | 0.003–0.01 |
| Total P (filtered sample), mg L−1 | 2.5 | 0.001–0.01 |
| Total P (unfiltered sample), mg L−1 | 11.0 | No data |
| Permanganate index, mgО2 L−1 | 824 | 2.0 |
| COD 1, mgО2 L−1 | 10,050 | 4.0 |
| pH | 6.13 | 8.08 |
| Ec 2, μSm cm−1 | 646.70 | 109.9 |
| Mineralisation | 554.84 | - |
| НСО3−, mg L−1 | 274.4 | 64.60 |
| SO42−, mg L−1 | 7.76 | 5.2 |
| Cl−, mg L−1 | 1.6 | 0.45 |
| Na+, mg L−1 | 12.0 | 3.36 |
| K+, mg L−1 | 57.6 | 0.96 |
| Ca2+, mg L−1 | 28.0 | 15.9 |
| Mg2+, mg L−1 | 8.0 | 3.1 |
1 Chemical oxygen demand; 2 Electro conductivity.