生物多样性

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高山松火烧迹地不同恢复阶段土壤微生物多样性和群落特征

温昊1,2, 林波3, 陈婧1,2, 尚鹤1, 陈展1,2*   

  1. 1.中国林业科学研究院森林生态环境与自然保护研究所/森林生态系统保护修复国家林业和草原局重点实验室 北京 100091;2.湖北秭归三峡库区森林生态系统定位观测研究站 秭归 443699;3.四川省林业和草原调查规划院 成都 610081
  • 收稿日期:2026-03-10 修回日期:2026-05-28 接受日期:2026-07-08
  • 通讯作者: 陈展

Soil microbial diversity and community characteristics in post-fire recovery stages of Pinus densata forests

Wen Hao1,2, Lin Bo3, Chen Jing1,2, Shang He1, Chen Zhan1,2*   

  1. 1 Key Laboratory of National Forestry and Grassland Administration on Forest Ecosystem Conservation and Restoration, Ecology and Nature Conservation Institute, Chinese Academy of Forestry, Beijing 100091, China 

    2 Hubei Zigui Three Gorges Reservoir Forest Ecosystem Observation and Research Station, Zigui 443600, China 

    3 Sichuan Forestry and Grassland Survey and Planning Institute, Sichuan 610081, China

  • Received:2026-03-10 Revised:2026-05-28 Accepted:2026-07-08
  • Contact: Zhan Chen

摘要: 为揭示高山松(Pinus densata)林火烧迹地土壤微生物群落的恢复特征,本研究以高山松林火烧迹地为研究对象,利用Illumina MiSeq高通量测序技术,探究火干扰后5年与14年土壤微生物群落的恢复状态。结果表明:(1)恢复14年后,部分土壤养分指标恢复并超过未受火干扰样地,其中0-5 cm有机质、全氮、全磷、硝态氮、pH升高较为显著(P < 0.05);5-10 cm有机质、全磷和硝态氮升高较为显著(P < 0.05)。(2)0-5 cm Fire5和Fire14的细菌群落的Shannon指数显著高于未受火干扰样地(CK)(P < 0.05),而5-10cm的细菌和两个土层真菌在不同恢复阶段间均无显著差异(P > 0.05)。(3)两土层细菌群落以放线菌门、变形菌门、酸杆菌门为主;真菌群落以子囊菌门和担子菌门为主。恢复14年后细菌绝对丰度高于CK,而真菌绝对丰度仍低于CK。(4)共生型和腐生型真菌在不同土层表现出差异化恢复趋势,多营养类型真菌相对丰度表现为先增加后降低。(5)火干扰后的恢复时间显著影响两个土层细菌和真菌的群落结构(P < 0.05)。pH、有机质及氮磷养分等因子与微生物群落分异密切相关。本研究表明,火后恢复时间是驱动高山松林浅层土壤微生物群落重建的重要因素,可为高山松林火后土壤生态恢复评估提供科学依据。

关键词: 火干扰, 绝对丰度, 土壤恢复, 高山松, 恢复阶段

Abstract

Aims: This study aimed to evaluate the effects of fire disturbance on soil microbial communities in Pinus densata forests and to characterize their recovery trajectories across different post-fire recovery stages. 

Methods: Soil microbial communities in unburned plots and fire-affected plots at 5 and 14 years post-fire in Pinus densata forests were investigated using Illumina MiSeq high-throughput sequencing combined with bioinformatic analyses. 

Results: (1) By fourteen years post-fire, several soil nutrient indices had recovered to, and in some cases exceeded, the levels of the unburned plots. In the 0–5 cm layer, soil organic matter, total nitrogen, total phosphorus, nitrate nitrogen, and pH increased significantly (P < 0.05), while in the 5–10 cm layer, significant increases were observed only in soil organic matter, total phosphorus, and nitrate nitrogen (P < 0.05). (2) In the 0-5 cm soil layer, the Shannon index of bacterial communities in Fire5 and Fire14 was significantly higher than that in the unburned plots (P < 0.05), whereas no significant differences were observed among the different post-fire recovery stages for bacteria in the 5-10 cm layer or for fungi in either soil layer (P > 0.05). (3) In both 0-5 cm and 5-10 cm soil layers, bacterial communities were dominated by Actinobacteriota, Proteobacteria, and Acidobacteriota, While fungal were primarily composed of Ascomycota and Basidiomycota. By 14 years post-fire bacterial absolute abundance exceeded that in unburned plots, whereas fungal absolute remained lower. (4) Symbiotrophic and saprotrophic fungi exhibited differentiated recovery trends across soil layers, whereas the relative abundance of multitrophic fungi showed an initial increase followed by a decrease. (5) Post-fire recovery time significantly affected the community structures of both soil bacteria and fungi in the 0-5 cm and 5-10 cm layers (P < 0.05), with pH, organic matter, and nitrogen and phosphorus availability closely associated with microbial community differentiation. 

Conclusion: Long-term recovery following fire disturbance led to significant changes in soil organic matter, total nitrogen, total phosphorus, pH, and nitrate nitrogen, which indirectly influenced the Shannon index of bacterial communities in the 0–5 cm layer and the overall microbial community structure in both soil layers. Multitrophic fungi, capable of utilizing multiple carbon sources simultaneously, gained a competitive advantage for resources after fire disturbance, resulting in a relative increase in abundance in the short term. As recovery time increases, the ecosystem gradually stabilizes, allowing monotrophic fungi to reoccupy their ecological niches. Because environmental factors were highly synchronized between the two soil layers, microbial community structure did not differ significantly along the vertical (depth) gradient within any given recovery stage.

Key words: fire disturbance, absolute abundance, soil recovery, pinus densata, recovery stage