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Tree species and soil depth affect microbial necromass contribution to soil organic matter in temperate forest soils, surpassing the impact of microbial and faunal community composition

The result's identifiers

  • Result code in IS VaVaI

    <a href="https://www.isvavai.cz/riv?ss=detail&h=RIV%2F60077344%3A_____%2F25%3A00638846" target="_blank" >RIV/60077344:_____/25:00638846 - isvavai.cz</a>

  • Alternative codes found

    RIV/61389005:_____/25:00638846 RIV/00216208:11310/25:10507436

  • Result on the web

    <a href="https://besjournals.onlinelibrary.wiley.com/doi/pdfdirect/10.1111/1365-2435.70111" target="_blank" >https://besjournals.onlinelibrary.wiley.com/doi/pdfdirect/10.1111/1365-2435.70111</a>

  • DOI - Digital Object Identifier

    <a href="http://dx.doi.org/10.1111/1365-2435.70111" target="_blank" >10.1111/1365-2435.70111</a>

Alternative languages

  • Result language

    angličtina

  • Original language name

    Tree species and soil depth affect microbial necromass contribution to soil organic matter in temperate forest soils, surpassing the impact of microbial and faunal community composition

  • Original language description

    Forest management and climate change inevitably lead to shifts in the composition of temperate forest stands from coniferous to deciduous species, potentially affecting the crucial role of forest soil organic carbon (SOC) stocks in mitigating climate change. Here, we provide the first comprehensive field study focusing on mineral topsoils (0-10 cm) and subsoils (50-60 cm) in temperate deciduous (beech), coniferous (spruce) and mixed forests. Moreover, we investigate the contribution of microbial-derived C to free particulate organic matter (fPOM), occluded POM (oPOM) and mineral-associated OM (MAOM) fractions as affected by differences in the composition of the microbial and micro- and mesofaunal communities. Our results show a relatively high microbial necromass contribution not only to MAOM (61%) and oPOM (36%), but also to fPOM (36%). The contribution of microbial-derived C in MAOM was higher in deciduous (72%) than in coniferous (48%) forest stands and the contribution of microbial-derived C was higher in the topsoil (51%) than in the subsoil (37%). Our data also showed that fungi dominated microbial necromass contribution to POM. In contrast, bacteria dominated microbial necromass contribution to MAOM, and the importance of certain microbial (bacterial) groups in governing microbial-derived soil organic matter (SOM) varies with the forest stand, soil horizon and the SOM fraction. Finally, neither micro- nor mesofaunal community composition as affected by forest stand or soil horizon was associated with microbial necromass contribution to SOM. Our study highlights the need to include the microbial necromass contribution to all SOM fractions in temperate forest soils within SOC models and predictions. Our study also indicates that expected shifts in forest stand composition will lead to higher and more effective SOM stabilization, with the topsoil strongly influenced by a more active soil biota community.

  • Czech name

  • Czech description

Classification

  • Type

    J<sub>imp</sub> - Article in a specialist periodical, which is included in the Web of Science database

  • CEP classification

  • OECD FORD branch

    40104 - Soil science

Result continuities

  • Project

    Result was created during the realization of more than one project. More information in the Projects tab.

  • Continuities

    I - Institucionalni podpora na dlouhodoby koncepcni rozvoj vyzkumne organizace

Others

  • Publication year

    2025

  • Confidentiality

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

Data specific for result type

  • Name of the periodical

    Functional Ecology

  • ISSN

    0269-8463

  • e-ISSN

    1365-2435

  • Volume of the periodical

    39

  • Issue of the periodical within the volume

    9

  • Country of publishing house

    US - UNITED STATES

  • Number of pages

    15

  • Pages from-to

    2219-2233

  • UT code for WoS article

    001534622600001

  • EID of the result in the Scopus database

    2-s2.0-105011826593