Disentangling the factors of contrasting silver and copper accumulation in sporocarps of the ectomycorrhizal fungus Amanita strobiliformis from two sites
Language English Country Netherlands Media print-electronic
Document type Journal Article
PubMed
31400682
DOI
10.1016/j.scitotenv.2019.133679
PII: S0048-9697(19)33605-8
Knihovny.cz E-resources
- Keywords
- (206)Pb/(207)Pb ratio, BCR sequential extraction, Hyperaccumulation, Lead isotopes, Soil mycelium quantification, qPCR,
- MeSH
- Amanita physiology MeSH
- Soil Pollutants metabolism MeSH
- Copper metabolism MeSH
- Environmental Monitoring * MeSH
- Mycorrhizae MeSH
- Silver metabolism MeSH
- Publication type
- Journal Article MeSH
- Names of Substances
- Soil Pollutants MeSH
- Copper MeSH
- Silver MeSH
Amanita strobiliformis (European Pine Cone Lepidella) is an ectomycorrhizal fungus of the Amanitaceae family known to hyperaccumulate Ag in the sporocarps. Two populations (ecotypes) of A. strobiliformis collected from two urban forest plantations in Prague, Czech Republic, were investigated. The concentrations of Ag, Cu, Cd, and Zn were determined in the mushrooms. The metal mobility and fractionation in the soils was investigated by single extractions and sequential extraction. The soil distribution of A. strobiliformis mycelium was assessed by quantitative polymerase chain reaction (qPCR). The metal uptake from the soil into the mushroom sporocarps was traced by Pb isotopic fingerprinting. The findings suggested that A. strobiliformis (i) accumulates primarily Ag from the topsoil layer (circa 12cm deep) and (ii) accumulates Ag associated with the "reducible soil fraction". The concentrations of all metals, particularly Ag and Cu, were significantly higher in the A. strobiliformis sporocarps from one of the investigated sites (Klíčov). The elevated concentrations of Ag in the sporocarps from Klíčov can possibly be attributed to the higher Ag content in the topsoil layer found at this site. However, the simultaneously elevated concentrations of Cu in A. strobiliformis from Klíčov cannot be explained by the differences in the geochemical background and should be attributed to biological factors.
Institute of Geology Czech Academy of Sciences Rozvojová 269 16500 Prague 6 Czech Republic
Institute of Microbiology Czech Academy of Sciences Vídeňská 1083 14220 Prague 4 Czech Republic
Nuclear Physics Institute Czech Academy of Sciences Hlavní 130 25068 Husinec Řež Czech Republic
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