Long-term soil warming decreases soil microbial necromass carbon by adversely affecting its production and decomposition
© 2024 John Wiley & Sons Ltd.
Veröffentlicht in: | Global change biology. - 1999. - 30(2024), 6 vom: 21. Juni, Seite e17379 |
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1. Verfasser: | |
Weitere Verfasser: | , , , , , , |
Format: | Online-Aufsatz |
Sprache: | English |
Veröffentlicht: |
2024
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Zugriff auf das übergeordnete Werk: | Global change biology |
Schlagworte: | Journal Article enzymes activity long‐term soil warming microbial biomass carbon microbial carbon use efficiency microbial necromass carbon soil phosphorus temperate forest Soil Carbon mehr... |
Zusammenfassung: | © 2024 John Wiley & Sons Ltd. Microbial necromass carbon (MNC) accounts for a large fraction of soil organic carbon (SOC) in terrestrial ecosystems. Yet our understanding of the fate of this large carbon pool under long-term warming is uncertain. Here, we show that 14 years of soil warming (+4°C) in a temperate forest resulted in a reduction in MNC by 11% (0-10 cm) and 33% (10-20 cm). Warming caused a decrease in the content of MNC due to a decline in microbial biomass carbon and reduced microbial carbon use efficiency. This reduction was primarily caused by warming-induced limitations in available soil phosphorus, which, in turn, constrained the production of microbial biomass. Conversely, warming increased the activity of soil extracellular enzymes, specifically N-acetylglucosaminidase and leucine aminopeptidase, which accelerated the decomposition of MNC. These findings collectively demonstrate that decoupling of MNC formation and decomposition underlie the observed MNC loss under climate warming, which could affect SOC content in temperate forest ecosystems more widespread |
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Beschreibung: | Date Completed 20.07.2024 Date Revised 20.07.2024 published: Print Citation Status MEDLINE |
ISSN: | 1365-2486 |
DOI: | 10.1111/gcb.17379 |