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Shift in tree species from coniferous to broadleaf reduces soil organic matter stabilization in the short term

Identifikátory výsledku

  • Kód výsledku v IS VaVaI

    <a href="https://www.isvavai.cz/riv?ss=detail&h=RIV%2F60077344%3A_____%2F25%3A00641817" target="_blank" >RIV/60077344:_____/25:00641817 - isvavai.cz</a>

  • Výsledek na webu

    <a href="https://www.sciencedirect.com/science/article/pii/S0929139325007061?via%3Dihub" target="_blank" >https://www.sciencedirect.com/science/article/pii/S0929139325007061?via%3Dihub</a>

  • DOI - Digital Object Identifier

    <a href="http://dx.doi.org/10.1016/j.apsoil.2025.106568" target="_blank" >10.1016/j.apsoil.2025.106568</a>

Alternativní jazyky

  • Jazyk výsledku

    angličtina

  • Název v původním jazyce

    Shift in tree species from coniferous to broadleaf reduces soil organic matter stabilization in the short term

  • Popis výsledku v původním jazyce

    Climate change may eventually result in tree species shifts in temperate forests. However, little is known on further consequences to litter decomposition and stabilization in the soil. This study thus investigates the effects of the shift in tree species from coniferous to broadleaf on litter decomposition and soil organic matter (OM) stabilization in Central European temperate forest soils. Using a 12-month laboratory microcosm experiment, surface mineral soils from coniferous (spruce), mixed and broadleaf (beech) forests were incubated with and without beech leaf litter. Microbial activity as an indicator of litter decomposition was monitored during the whole incubation period and carbon (C) content in the soil OM fractions as an indicator of OM stabilization was analysed at the end. The results demonstrate that decomposition rates were 65 % lower in the coniferous soil than in the broadleaf soil, suggesting that the microbial community in the coniferous soil is less adapted to the high-quality beech litter. Regarding OM stabilization, beech litter addition increased free particulate OM in the coniferous soil by 140 %, but stabilization via mineral association was 60 % more efficient in the broadleaf soil, where beech litter was more readily incorporated. Overall, the findings indicate that the shift from coniferous to broadleaf forests may initially result in reduced soil OM stabilization in coniferous soils, most probably due to microbial adaptation constraints. These insights highlight the complex interactions between litter quality, microbial communities and soil C dynamics. Further research should focus on longer-term effects of the tree species shift.

  • Název v anglickém jazyce

    Shift in tree species from coniferous to broadleaf reduces soil organic matter stabilization in the short term

  • Popis výsledku anglicky

    Climate change may eventually result in tree species shifts in temperate forests. However, little is known on further consequences to litter decomposition and stabilization in the soil. This study thus investigates the effects of the shift in tree species from coniferous to broadleaf on litter decomposition and soil organic matter (OM) stabilization in Central European temperate forest soils. Using a 12-month laboratory microcosm experiment, surface mineral soils from coniferous (spruce), mixed and broadleaf (beech) forests were incubated with and without beech leaf litter. Microbial activity as an indicator of litter decomposition was monitored during the whole incubation period and carbon (C) content in the soil OM fractions as an indicator of OM stabilization was analysed at the end. The results demonstrate that decomposition rates were 65 % lower in the coniferous soil than in the broadleaf soil, suggesting that the microbial community in the coniferous soil is less adapted to the high-quality beech litter. Regarding OM stabilization, beech litter addition increased free particulate OM in the coniferous soil by 140 %, but stabilization via mineral association was 60 % more efficient in the broadleaf soil, where beech litter was more readily incorporated. Overall, the findings indicate that the shift from coniferous to broadleaf forests may initially result in reduced soil OM stabilization in coniferous soils, most probably due to microbial adaptation constraints. These insights highlight the complex interactions between litter quality, microbial communities and soil C dynamics. Further research should focus on longer-term effects of the tree species shift.

Klasifikace

  • Druh

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

  • CEP obor

  • OECD FORD obor

    40104 - Soil science

Návaznosti výsledku

  • Projekt

    <a href="/cs/project/GA22-02550S" target="_blank" >GA22-02550S: SOMForClim: Frakce půdní organické hmoty a ukládání uhlíku ovlivněné typem lesa a klimatickou změnou</a><br>

  • 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 Soil Ecology

  • ISSN

    0929-1393

  • e-ISSN

    1873-0272

  • Svazek periodika

    216

  • Číslo periodika v rámci svazku

    December

  • Stát vydavatele periodika

    NL - Nizozemsko

  • Počet stran výsledku

    6

  • Strana od-do

    106568

  • Kód UT WoS článku

    001607068400002

  • EID výsledku v databázi Scopus

    2-s2.0-105020902291