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'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'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