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Responses of diatom composition and teratological forms to environmental pollution in a post‑mining lake (SW Poland)

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    SYSNO ASEP0578856
    Document TypeJ - Journal Article
    R&D Document TypeJournal Article
    Subsidiary JČlánek ve WOS
    TitleResponses of diatom composition and teratological forms to environmental pollution in a post‑mining lake (SW Poland)
    Author(s) Sienkiewicz, E. (PL)
    Gąsiorowski, M. (PL)
    Sekudewicz, I. (PL)
    Kowalewska, U. (PL)
    Matoušková, Šárka (GLU-S) RID, SAI
    Source TitleEnvironmental Science and Pollution Research. - : Springer - ISSN 0944-1344
    Roč. 30, č. 51 (2023), s. 110623-110638
    Number of pages16 s.
    Languageeng - English
    CountryDE - Germany
    KeywordsDiatom teratologies ; Heavy metals ; Acidic water ; Lignite ; Mining lake ; Environmental reconstruction
    OECD categoryEnvironmental sciences (social aspects to be 5.7)
    Method of publishingOpen access
    Institutional supportGLU-S - RVO:67985831
    UT WOS001096214900010
    DOI10.1007/s11356-023-30113-7
    AnnotationVarious types of environmental stressors, such as heavy metals, lignite residues, or extremely low water pH, cause the formation of teratological forms of diatoms during the reproductive cycle. The damage mainly includes an abnormal diatom valve outline, changes in the striation pattern, anomalies in the raphe line/sternum, reduction in the cell size, metabolism alterations, or combined deformities. Diatom remains with such morphological deformities occur in the sediments of post-mining lake ŁK-46 (SW Poland). This lake was formed by excavation after the end of lignite exploitation in the mid-1960s. The percentage of teratological valves in the studied lake ranged from 12 to 33% of the relative abundance. The majority of abnormal diatoms have been observed in species of Eunotia. The reconstruction of the diatom-inferred pH (DI-pH), together with the concentration of heavy metals in the sediments and contemporary measurements of the water pH, indicates that the lake was contaminated to varying degrees and was acidic from the beginning of lake creation until today. The lake is located in an area of acid mine drainage (AMD), and in its vicinity, there are overburden heaps containing lignite residues, which are eroded and supplied to the lake, constantly acidifying the water. In the youngest sediments, the concentration of heavy metals increased, while the percentage of abnormal diatoms decreased. Determining which factor, i.e., extremely low water pH and the presence of lignite or heavy metals, was responsible for the formation or reduction of teratogenic forms of diatoms is very difficult.
    WorkplaceInstitute of Geology
    ContactJana Popelková, popelkova@gli.cas.cz, Sabina Janíčková, Tel.: 233 087 272
    Year of Publishing2024
    Electronic addresshttps://link.springer.com/article/10.1007/s11356-023-30113-7#Fun
Number of the records: 1  

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