The role of soils in environmental sorption and degradation processes of selected Fusarium mycotoxins

Abstract Mycotoxins, toxic secondary metabolites produced by fungi, enter soils via various pathways. The contamination of soils with mycotoxins has been extensively documented, but their persistence remain uncertain. In a microcosm study, we investigated the adsorption–desorption behaviour and micr...

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Main Authors: Sven Korz, Katherine Muñoz
Format: Article
Language:English
Published: Springer 2025-06-01
Series:Discover Soil
Online Access:https://doi.org/10.1007/s44378-025-00070-3
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author Sven Korz
Katherine Muñoz
author_facet Sven Korz
Katherine Muñoz
author_sort Sven Korz
collection DOAJ
description Abstract Mycotoxins, toxic secondary metabolites produced by fungi, enter soils via various pathways. The contamination of soils with mycotoxins has been extensively documented, but their persistence remain uncertain. In a microcosm study, we investigated the adsorption–desorption behaviour and microbial transformation of four mycotoxins (LogK ow < −0.5) Deoxynivalenol (DON), Nivalenol (NIV), 15-Acetyl-Deoxynivalenol (15A-DON), and Zearalenone (ZEN, LogK ow = 3.83) in three agricultural soil types. We did not focus on the degradation potential of single species, but rather on the potential of soil microbiome as a whole. Mycotoxin adsorption varied depending on mycotoxin physicochemical properties and soil characteristics, with ZEN exhibiting the highest sorption affinity (> 88%), in contrast to DON and NIV (< 35% adsorption). Sorption of 15A-DON was significantly affected by the soil type (ranging from 21 to 97%), following the clay fraction, soil pH and to a lesser extent the organic matter content. The degradation of mycotoxins in all soils was found to be exclusively of microbial nature, with varying half-lives ranging from < 1 h for 15A-DON and up to 19 days for ZEN. The degradation was aligned with the soil microbial biomass (Cmic) and activity (respiration). The microbial O-deacetylation of 15A-DON to DON was confirmed in all investigated soils. Chemical modifications in the structure of mycotoxins resulted in more complex interactions with soil fractions affecting adsorption to soil i.e. 15A-DON and clay content. Independent of the mycotoxin, degradation was in line with the microbial activity of the soil ). These results highlight the pivotal role of soil characteristics in dictating mycotoxin mobility and stability, which is of paramount importance for environmental monitoring strategies and for ensuring agricultural safety and environmental contamination mitigation. Graphical Abstract
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spelling doaj-art-040ab672918d4d408f34a89778e27e3f2025-08-20T03:45:40ZengSpringerDiscover Soil3005-12232025-06-012111510.1007/s44378-025-00070-3The role of soils in environmental sorption and degradation processes of selected Fusarium mycotoxinsSven Korz0Katherine Muñoz1Department of Natural and Environmental Sciences, Institute for Environmental Sciences (iES Landau), RPTU Kaiserslautern-LandauDepartment of Natural and Environmental Sciences, Institute for Environmental Sciences (iES Landau), RPTU Kaiserslautern-LandauAbstract Mycotoxins, toxic secondary metabolites produced by fungi, enter soils via various pathways. The contamination of soils with mycotoxins has been extensively documented, but their persistence remain uncertain. In a microcosm study, we investigated the adsorption–desorption behaviour and microbial transformation of four mycotoxins (LogK ow < −0.5) Deoxynivalenol (DON), Nivalenol (NIV), 15-Acetyl-Deoxynivalenol (15A-DON), and Zearalenone (ZEN, LogK ow = 3.83) in three agricultural soil types. We did not focus on the degradation potential of single species, but rather on the potential of soil microbiome as a whole. Mycotoxin adsorption varied depending on mycotoxin physicochemical properties and soil characteristics, with ZEN exhibiting the highest sorption affinity (> 88%), in contrast to DON and NIV (< 35% adsorption). Sorption of 15A-DON was significantly affected by the soil type (ranging from 21 to 97%), following the clay fraction, soil pH and to a lesser extent the organic matter content. The degradation of mycotoxins in all soils was found to be exclusively of microbial nature, with varying half-lives ranging from < 1 h for 15A-DON and up to 19 days for ZEN. The degradation was aligned with the soil microbial biomass (Cmic) and activity (respiration). The microbial O-deacetylation of 15A-DON to DON was confirmed in all investigated soils. Chemical modifications in the structure of mycotoxins resulted in more complex interactions with soil fractions affecting adsorption to soil i.e. 15A-DON and clay content. Independent of the mycotoxin, degradation was in line with the microbial activity of the soil ). These results highlight the pivotal role of soil characteristics in dictating mycotoxin mobility and stability, which is of paramount importance for environmental monitoring strategies and for ensuring agricultural safety and environmental contamination mitigation. Graphical Abstracthttps://doi.org/10.1007/s44378-025-00070-3
spellingShingle Sven Korz
Katherine Muñoz
The role of soils in environmental sorption and degradation processes of selected Fusarium mycotoxins
Discover Soil
title The role of soils in environmental sorption and degradation processes of selected Fusarium mycotoxins
title_full The role of soils in environmental sorption and degradation processes of selected Fusarium mycotoxins
title_fullStr The role of soils in environmental sorption and degradation processes of selected Fusarium mycotoxins
title_full_unstemmed The role of soils in environmental sorption and degradation processes of selected Fusarium mycotoxins
title_short The role of soils in environmental sorption and degradation processes of selected Fusarium mycotoxins
title_sort role of soils in environmental sorption and degradation processes of selected fusarium mycotoxins
url https://doi.org/10.1007/s44378-025-00070-3
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