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Uranium, thorium and rare earth elements in macrofungi: what are the genuine concentrations?

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    SYSNO ASEP0364069
    Document TypeJ - Journal Article
    R&D Document TypeJournal Article
    Subsidiary JČlánek ve WOS
    TitleUranium, thorium and rare earth elements in macrofungi: what are the genuine concentrations?
    Author(s) Borovička, Jan (GLU-S) RID, SAI, ORCID
    Kubrová, J. (CZ)
    Rohovec, Jan (GLU-S) RID, SAI
    Řanda, Zdeněk (UJF-V) RID
    Dunn, C. E. (CA)
    Source TitleBiometals. - : Springer - ISSN 0966-0844
    Roč. 24, č. 5 (2011), s. 837-845
    Number of pages9 s.
    Publication formWWW - WWW
    Languageeng - English
    CountryGB - United Kingdom
    KeywordsICP-MS ; ENAA ; REE ; fungi ; bioaccumulation ; metals
    Subject RIVDD - Geochemistry
    R&D ProjectsIAA600480801 GA AV ČR - Academy of Sciences of the Czech Republic (AV ČR)
    CEZAV0Z30130516 - GLU-S (2005-2011)
    AV0Z10480505 - UJF-V (2005-2011)
    UT WOS000294463300005
    EID SCOPUS80052405310
    DOI10.1007/s10534-011-9435-4
    AnnotationConcentrations of uranium, thorium and rare earth elements (REE) in 36 species of ectomycorrhizal (26 samples) and saprobic (25 samples) macrofungi from unpolluted sites with differing bedrock geochemistry were analyzed by inductively coupled plasma mass spectrometry (ICP-MS). Analytical results are supported by use of certified reference materials (BCR-670, BCR-667, NIST-1575a) and the reliability of the determination of uranium was verified by epithermal neutron activation analysis (ENAA). It appears that data recently published on these elements are erroneous, in part because of use of an inappropriate analytical method; and in part because of apparent contamination by soil particles resulting in elevated levels of thorium and REE. Macrofungi from unpolluted areas, in general, did not accumulate high levels of the investigated metals. Concentrations of uranium and thorium were generally below 30 and 125 ppb (dry weight), respectively. Concentrations of REE in macrofungi did not exceed 360 ppb (dry weight) and their distribution more or less followed the trend observed in post-Archean shales and loess.
    WorkplaceInstitute of Geology
    ContactJana Popelková, popelkova@gli.cas.cz, Sabina Janíčková, Tel.: 233 087 272
    Year of Publishing2012
Number of the records: 1  

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