Rapid allocation of freshly added organic nitrogen to particulate organic matter in ectomycorrhiza- but not arbuscular mycorrhiza-dominated forests

Mycorrhizal fungi mediate the partitioning and transformation of organic matter in forest soils worldwide. Ectomycorrhizal (ECM) and arbuscular mycorrhizal (AM) fungi differently influence the formation of soil organic matter (SOM) pools, such as decomposable particulate (POM) and persistent mineral-associated organic matter (MaOM). While plant-derived effects were studied extensively, the role of other organic resources in SOM formation across different mycorrhizal systems remains understudied. To address this, we investigated the incorporation of carbon and nitrogen derived from more bioavailable (bacterial and fungal biomass) and less bioavailable (litter, artificial MaOM; a-MaOM) source organic matter into soil POM and MaOM pools in ECM- and AM-dominated soils, using a dual stable isotope ( 13 C and 15 N) labelling approach in a temperate experimental forest (MyDiv experiment). We detected 15 N, but not 13 C label in mycelium and POM across treatments (except a-MaOM) and mycorrhizal types, while no label was detected in soil MaOM. ECM mycelium showed higher 15 N uptake from litter, while AM mycelium accumulated more 15 N after the addition of fungal biomass. POM in ECM systems had a higher 15 N label compared to AM systems in all bacteria, fungi and litter treatments, indicating the role of ECM fungi as important drivers of fresh organic nitrogen allocation in temperate forest soils. The absence of any label in MaOM indicates its slow turnover in Chernozem soil across forests dominated by a single mycorrhizal type. Overall, our study highlights the fast incorporation of freshly added organic nitrogen into the mycelium of mycorrhizal fungi and POM, emphasizing its fast turnover in forest soils. • The formation of SOM fractions in ECM and AM-dominated systems remains not completely understood • Multi-resource dual-labelling ( 13 C and 15 N) was performed in a temperate experimental forest • 15 N label was detected in fungal mycelium and soil POM, but not in MaOM • 13 C label was poorly detected across treatments and mycorrhizal types • POM in ECM systems received more freshly added N compared to AM systems

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Journal
Soil Biology and Biochemistry
Published
2025-10-03
DOI
https://doi.org/10.1016/j.soilbio.2025.109999
Primary Topic
Forest Ecology and Biodiversity Studies
Type
article
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article

Rapid allocation of freshly added organic nitrogen to particulate organic matter in ectomycorrhiza- but not arbuscular mycorrhiza-dominated forests

Martti Vasar, Anton Potapov, Epp Maria Lillipuu, Gerrit Angst et al.
Soil Biology and Biochemistry
Forest Ecology and Biodiversity Studies
article

Rapid allocation of freshly added organic nitrogen to particulate organic matter in ectomycorrhiza- but not arbuscular mycorrhiza-dominated forests

Martti Vasar, Anton Potapov, Epp Maria Lillipuu, Gerrit Angst, Nico Eisenhauer, Maarja Öpik, Stephanie D. Jurburg, Andrey G. Zuev, Olga Ferlian, Anna I. Zueva, Ajuan Zhang, Antonis Chatzinotas, Amelie Hauer
article en

Abstract

Mycorrhizal fungi mediate the partitioning and transformation of organic matter in forest soils worldwide. Ectomycorrhizal (ECM) and arbuscular mycorrhizal (AM) fungi differently influence the formation of soil organic matter (SOM) pools, such as decomposable particulate (POM) and persistent mineral-associated organic matter (MaOM). While plant-derived effects were studied extensively, the role of other organic resources in SOM formation across different mycorrhizal systems remains understudied. To address this, we investigated the incorporation of carbon and nitrogen derived from more bioavailable (bacterial and fungal biomass) and less bioavailable (litter, artificial MaOM; a-MaOM) source organic matter into soil POM and MaOM pools in ECM- and AM-dominated soils, using a dual stable isotope ( 13 C and 15 N) labelling approach in a temperate experimental forest (MyDiv experiment). We detected 15 N, but not 13 C label in mycelium and POM across treatments (except a-MaOM) and mycorrhizal types, while no label was detected in soil MaOM. ECM mycelium showed higher 15 N uptake from litter, while AM mycelium accumulated more 15 N after the addition of fungal biomass. POM in ECM systems had a higher 15 N label compared to AM systems in all bacteria, fungi and litter treatments, indicating the role of ECM fungi as important drivers of fresh organic nitrogen allocation in temperate forest soils. The absence of any label in MaOM indicates its slow turnover in Chernozem soil across forests dominated by a single mycorrhizal type. Overall, our study highlights the fast incorporation of freshly added organic nitrogen into the mycelium of mycorrhizal fungi and POM, emphasizing its fast turnover in forest soils. • The formation of SOM fractions in ECM and AM-dominated systems remains not completely understood • Multi-resource dual-labelling ( 13 C and 15 N) was performed in a temperate experimental forest • 15 N label was detected in fungal mycelium and soil POM, but not in MaOM • 13 C label was poorly detected across treatments and mycorrhizal types • POM in ECM systems received more freshly added N compared to AM systems

Soil Biology and BiochemistryVol. 212
Helmholtz Centre for Environmental Research (DE), Leipzig University of Applied Sciences (DE), Czech Academy of Sciences (CZ), Charles University (CZ), German Centre for Integrative Biodiversity Research (DE), Institute of Botany of the Slovak Academy of Sciences (SK), Institute of Soil Biology (CZ), Senckenberg Museum für Naturkunde Görlitz (DE), International University Institute (IHI) Zittau (DE), Severtsov Institute of Ecology and Evolution (RU), Chengdu Institute of Biology (CN), Czech Academy of Sciences, Biology Centre (CZ), Institute of Botany (AM), University of Tartu (EE), Leipzig University (DE)
Openalex Percentile: Top 75%
Forest Ecology and Biodiversity Studies
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