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Microbial communities in soil macro-aggregates with less connected networks respire less across successional and geographic gradients

Identifikátory výsledku

  • Kód výsledku v IS VaVaI

    <a href="https://www.isvavai.cz/riv?ss=detail&h=RIV%2F60077344%3A_____%2F22%3A00557142" target="_blank" >RIV/60077344:_____/22:00557142 - isvavai.cz</a>

  • Nalezeny alternativní kódy

    RIV/00216208:11310/22:10445576

  • Výsledek na webu

    <a href="https://www.sciencedirect.com/science/article/pii/S116455632100114X?via%3Dihub" target="_blank" >https://www.sciencedirect.com/science/article/pii/S116455632100114X?via%3Dihub</a>

  • DOI - Digital Object Identifier

    <a href="http://dx.doi.org/10.1016/j.ejsobi.2021.103378" target="_blank" >10.1016/j.ejsobi.2021.103378</a>

Alternativní jazyky

  • Jazyk výsledku

    angličtina

  • Název v původním jazyce

    Microbial communities in soil macro-aggregates with less connected networks respire less across successional and geographic gradients

  • Popis výsledku v původním jazyce

    The formation of soil aggregates is related to the stability of soil organic carbon, which distinguishes the living conditions of microbial communities in different micro-niches. Here, we investigated fungal and bacterial community structure, networks, biomass and respiration in individual micro-niches between and within soil aggregates using seven different chronosequences (both primary and secondary successions from pioneer stages to well-developed ecosystems) on a European-scale gradient from a maritime climate in Belgium to a more continental climate in Hungary. We showed that geographical location was the most important factor (74% for bacterial community, 53% for fungal community) affecting microbial community composition, while soil aggregates (5% for bacterial community and 12% for fungal community) were the second most important factor followed by age of succession and vegetation. Moreover, aggregates (52%) were the most important factor influencing the biomass of major microbial groups, followed by location (37%) and age of succession (6%). Interestingly, macro-aggregates had less interconnected microbial networks and low microbial respiration rates compared to other aggregate sizes. We therefore hypothesize that the embedding of organic particles in the mineral matrix of macro-aggregates is a crucial point in microbial community organization, as evidenced by microbial community connectivity and microbial respiration. Our results demonstrate the importance of soil aggregates for microbial community organization and soil carbon stabilization.

  • Název v anglickém jazyce

    Microbial communities in soil macro-aggregates with less connected networks respire less across successional and geographic gradients

  • Popis výsledku anglicky

    The formation of soil aggregates is related to the stability of soil organic carbon, which distinguishes the living conditions of microbial communities in different micro-niches. Here, we investigated fungal and bacterial community structure, networks, biomass and respiration in individual micro-niches between and within soil aggregates using seven different chronosequences (both primary and secondary successions from pioneer stages to well-developed ecosystems) on a European-scale gradient from a maritime climate in Belgium to a more continental climate in Hungary. We showed that geographical location was the most important factor (74% for bacterial community, 53% for fungal community) affecting microbial community composition, while soil aggregates (5% for bacterial community and 12% for fungal community) were the second most important factor followed by age of succession and vegetation. Moreover, aggregates (52%) were the most important factor influencing the biomass of major microbial groups, followed by location (37%) and age of succession (6%). Interestingly, macro-aggregates had less interconnected microbial networks and low microbial respiration rates compared to other aggregate sizes. We therefore hypothesize that the embedding of organic particles in the mineral matrix of macro-aggregates is a crucial point in microbial community organization, as evidenced by microbial community connectivity and microbial respiration. Our results demonstrate the importance of soil aggregates for microbial community organization and soil carbon stabilization.

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/GA18-24138S" target="_blank" >GA18-24138S: Tvorba půdních agregátů během sukcese a její úloha v akumulaci uhlíku a zadržování vody v půdě</a><br>

  • Návaznosti

    I - Institucionalni podpora na dlouhodoby koncepcni rozvoj vyzkumne organizace

Ostatní

  • Rok uplatnění

    2022

  • Kód důvěrnosti údajů

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

Údaje specifické pro druh výsledku

  • Název periodika

    European Journal of Soil Biology

  • ISSN

    1164-5563

  • e-ISSN

    1778-3615

  • Svazek periodika

    108

  • Číslo periodika v rámci svazku

    January-February

  • Stát vydavatele periodika

    FR - Francouzská republika

  • Počet stran výsledku

    10

  • Strana od-do

    103378

  • Kód UT WoS článku

    000784268000005

  • EID výsledku v databázi Scopus

    2-s2.0-85121234541