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Contrasting stability of fungal and bacterial communities during long-term decomposition of fungal necromass in Arctic tundra

The result's identifiers

  • Result code in IS VaVaI

    <a href="https://www.isvavai.cz/riv?ss=detail&h=RIV%2F60077344%3A_____%2F25%3A00638882" target="_blank" >RIV/60077344:_____/25:00638882 - isvavai.cz</a>

  • Alternative codes found

    RIV/61388971:_____/25:00638882 RIV/00216208:11310/25:10509458

  • Result on the web

    <a href="https://environmentalmicrobiome.biomedcentral.com/articles/10.1186/s40793-025-00730-5" target="_blank" >https://environmentalmicrobiome.biomedcentral.com/articles/10.1186/s40793-025-00730-5</a>

  • DOI - Digital Object Identifier

    <a href="http://dx.doi.org/10.1186/s40793-025-00730-5" target="_blank" >10.1186/s40793-025-00730-5</a>

Alternative languages

  • Result language

    angličtina

  • Original language name

    Contrasting stability of fungal and bacterial communities during long-term decomposition of fungal necromass in Arctic tundra

  • Original language description

    Decomposition is a crucial process in terrestrial ecosystems, driving nutrient cycling and carbon storage dynamics. Considering the amount of fungal necromass produced in soils annually, its decomposition represents an important nutrient recycling process. Understanding the decomposition dynamics and associated microbial communities of fungal necromass is essential for elucidating ecosystem functioning, especially in environmentally sensitive regions such as the Arctic tundra, which remain under-explored. In a three-year field experiment conducted in the Svalbard archipelago, we investigated the decomposition of two types of fungal necromass with differing biochemical properties. We studied the decomposition rate, changes in chemical composition, and the succession of fungal and bacterial communities associated with the decaying fungal necromass. We discovered that up to 20% of fungal necromass remained even after three years of decomposition, indicating that the decomposition process was incomplete. Our results indicate the crucial role of Pseudogymnoascus in decomposing low-quality, highly melanized necromass with a high C:N ratio in Arctic soils, underscoring its importance in carbon cycling in the Arctic tundra. Notably, we observed dynamic changes in bacterial communities, with increasing richness over time and a shift from copiotrophic to oligotrophic species specializing in decomposing recalcitrant material. Our study indicates the strong potential that fungal necromass can play in carbon sequestration of arctic soils and reveals the distinct dynamics between rather stable fungal and rapidly changing bacterial communities associated with the decomposing fungal necromass in the Arctic tundra. These findings enhance our understanding of microbial succession during decomposition in extreme environments and highlight the potentially differing roles of fungi and bacteria in these processes.

  • 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

    10606 - Microbiology

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

    Environmental Microbiome

  • ISSN

    2524-6372

  • e-ISSN

    2524-6372

  • Volume of the periodical

    20

  • Issue of the periodical within the volume

    1

  • Country of publishing house

    GB - UNITED KINGDOM

  • Number of pages

    14

  • Pages from-to

    75

  • UT code for WoS article

    001512307600001

  • EID of the result in the Scopus database

    2-s2.0-105008739384