Changes in soil oxidase activity induced by microbial life history strategies mediate the soil heterotrophic respiration response to drought and nitrogen enrichment

微生物种群生物学 异养 作文(语言) 氮气 呼吸 化学 环境化学 生物 细菌 农学 植物 语言学 遗传学 哲学 有机化学
作者
Weirong Zhuang,Yong Li,Xiaoming Kang,Liang Yan,Xiaodong Zhang,Zhongqing Yan,Kerou Zhang,Ao Yang,Yuechuan Niu,Xiaoshun Yu,Huan Wang,M. An,Rongxiao Che
出处
期刊:Frontiers in Microbiology [Frontiers Media]
卷期号:15 被引量:10
标识
DOI:10.3389/fmicb.2024.1375300
摘要

Drought and nitrogen deposition are two major climate challenges, which can change the soil microbial community composition and ecological strategy and affect soil heterotrophic respiration (Rh). However, the combined effects of microbial community composition, microbial life strategies, and extracellular enzymes on the dynamics of Rh under drought and nitrogen deposition conditions remain unclear. Here, we experimented with an alpine swamp meadow to simulate drought (50% reduction in precipitation) and multilevel addition of nitrogen to determine the interactive effects of microbial community composition, microbial life strategy, and extracellular enzymes on Rh. The results showed that drought significantly reduced the seasonal mean Rh by 40.07%, and increased the Rh to soil respiration ratio by 22.04%. Drought significantly altered microbial community composition. The ratio of K- to r-selected bacteria (B K:r ) and fungi (F K:r ) increased by 20 and 91.43%, respectively. Drought increased hydrolase activities but decreased oxidase activities. However, adding N had no significant effect on microbial community composition, B K:r , F K:r , extracellular enzymes, or Rh. A structural equation model showed that the effects of drought and adding nitrogen via microbial community composition, microbial life strategy, and extracellular enzymes explained 84% of the variation in Rh. Oxidase activities decreased with B K:r , but increased with F K:r . Our findings show that drought decreased Rh primarily by inhibiting oxidase activities, which is induced by bacterial shifts from the r-strategy to the K-strategy. Our results highlight that the indirect regulation of drought on the carbon cycle through the dynamic of bacterial and fungal life history strategy should be considered for a better understanding of how terrestrial ecosystems respond to future climate change.
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