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Changes in Mg-Cu-Zn isotopic features in a system red cracking bolete - soil over an extended period

Identifikátory výsledku

  • Kód výsledku v IS VaVaI

    <a href="https://www.isvavai.cz/riv?ss=detail&h=RIV%2F00025798%3A_____%2F25%3A10169611" target="_blank" >RIV/00025798:_____/25:10169611 - isvavai.cz</a>

  • Výsledek na webu

    <a href="https://doi.org/10.1016/j.apgeochem.2025.106315" target="_blank" >https://doi.org/10.1016/j.apgeochem.2025.106315</a>

  • DOI - Digital Object Identifier

    <a href="http://dx.doi.org/10.1016/j.apgeochem.2025.106315" target="_blank" >10.1016/j.apgeochem.2025.106315</a>

Alternativní jazyky

  • Jazyk výsledku

    angličtina

  • Název v původním jazyce

    Changes in Mg-Cu-Zn isotopic features in a system red cracking bolete - soil over an extended period

  • Popis výsledku v původním jazyce

    We studied Mg-Cu-Zn isotope systematics of the Xerocomellus chrysenteron mushroom samples collected during two consecutive growing seasons from three sites underlain by granite, amphibolite, and serpentinite bedrock. None of the elements analyzed in mushrooms (Mg, Cu, Zn) displayed site-dependency in concentrations. The studied soils were depleted in 26Mg isotope (delta 26Mg =-0.78 to-0.30%o) and displayed a very wide range of delta 65Cu values (-0.85 to +0.67%o). Values of delta 66Zn were mostly negative for soils from the granite-based site (-0.33 to +0.07%o), positive for soils from the amphibolite-based site (+0.03 to +0.12%o), and only slightly deviated from zero for soils from the serpentinite-based site (-0.09 to +0.09%o). Observed difference in isotope compositions between the mushroom-bearing and mushroom-free soils was most likely due to the presence of mushroom&apos;s mycelium in the mushroom-bearing soils. Isotopes of Mg, Cu, and Zn fractionated to different extent during both uptake and within-mushroom translocation. Mushrooms displayed higher uptake of isotopically light Mg (Delta 26MgFB-soil =-0.71 to-0.12%o), isotopically heavy Zn (Delta 66ZnFB-soil = 0.61-0.91%o), and isotopically variable Cu (Delta 65CuFB-soil =-1.22 to +1.03%o). The ranges of the within-mushroom isotope fractionation were significant: Delta 26Mg displayed a total range of values of 1.09%o; Delta 65Cu, of 0.65%o; and Delta 66Zn, of 0.38%o. No uniform scheme of the within-mushroom isotope fractionation was observed for any studied element.

  • Název v anglickém jazyce

    Changes in Mg-Cu-Zn isotopic features in a system red cracking bolete - soil over an extended period

  • Popis výsledku anglicky

    We studied Mg-Cu-Zn isotope systematics of the Xerocomellus chrysenteron mushroom samples collected during two consecutive growing seasons from three sites underlain by granite, amphibolite, and serpentinite bedrock. None of the elements analyzed in mushrooms (Mg, Cu, Zn) displayed site-dependency in concentrations. The studied soils were depleted in 26Mg isotope (delta 26Mg =-0.78 to-0.30%o) and displayed a very wide range of delta 65Cu values (-0.85 to +0.67%o). Values of delta 66Zn were mostly negative for soils from the granite-based site (-0.33 to +0.07%o), positive for soils from the amphibolite-based site (+0.03 to +0.12%o), and only slightly deviated from zero for soils from the serpentinite-based site (-0.09 to +0.09%o). Observed difference in isotope compositions between the mushroom-bearing and mushroom-free soils was most likely due to the presence of mushroom&apos;s mycelium in the mushroom-bearing soils. Isotopes of Mg, Cu, and Zn fractionated to different extent during both uptake and within-mushroom translocation. Mushrooms displayed higher uptake of isotopically light Mg (Delta 26MgFB-soil =-0.71 to-0.12%o), isotopically heavy Zn (Delta 66ZnFB-soil = 0.61-0.91%o), and isotopically variable Cu (Delta 65CuFB-soil =-1.22 to +1.03%o). The ranges of the within-mushroom isotope fractionation were significant: Delta 26Mg displayed a total range of values of 1.09%o; Delta 65Cu, of 0.65%o; and Delta 66Zn, of 0.38%o. No uniform scheme of the within-mushroom isotope fractionation was observed for any studied element.

Klasifikace

  • Druh

    J<sub>imp</sub> - Článek v periodiku v databázi Web of Science

  • CEP obor

  • OECD FORD obor

    10511 - Environmental sciences (social aspects to be 5.7)

Návaznosti výsledku

  • Projekt

  • Návaznosti

    I - Institucionalni podpora na dlouhodoby koncepcni rozvoj vyzkumne organizace

Ostatní

  • Rok uplatnění

    2025

  • Kód důvěrnosti údajů

    S - Úplné a pravdivé údaje o projektu nepodléhají ochraně podle zvláštních právních předpisů

Údaje specifické pro druh výsledku

  • Název periodika

    Applied Geochemistry

  • ISSN

    0883-2927

  • e-ISSN

    1872-9134

  • Svazek periodika

    182

  • Číslo periodika v rámci svazku

    106315

  • Stát vydavatele periodika

    GB - Spojené království Velké Británie a Severního Irska

  • Počet stran výsledku

    17

  • Strana od-do

    nestránkováno

  • Kód UT WoS článku

    001432505300001

  • EID výsledku v databázi Scopus

    2-s2.0-85218233414