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亚热带植被恢复对球囊霉素相关土壤蛋白的影响

廖以淞, 张锐, 郭志红, 项文化, 胡保安, 邓湘雯, 欧阳帅   

  1. 中南林业科技大学, 410004
    湖南会同杉木林生态系统国家野外科学观测研究站, 438107
    重庆市林业科学研究院, 4300036
  • 收稿日期:2026-04-10 修回日期:2026-06-15
  • 基金资助:
    国家自然科学基金(32371849); 国家自然科学基金(32071561)

Effects of Subtropical Vegetation Restoration on Glomalin-Related Soil Protein

OUYANG Shuai   

  1. , Central South University of Forestry and Technology 410004,
    , Hunan Huitong Chinese Fir Forest Ecosystem National Field Scientific Observation and Research Station Huitong 438107,
    , Cohngqing Academy of Forestry Chongqing 4300036,
  • Received:2026-04-10 Revised:2026-06-15
  • Supported by:
    the National Natural Science Foundation of China(32371849); the National Natural Science Foundation of China(32071561)

摘要: 为明晰亚热带植被恢复过程中球囊霉素相关土壤蛋白(GRSP)的动态变化特征,探讨土壤理化性质和微生物特性对GRSP的影响,以期为提升亚热带生态系统土壤生态功能提供科学依据。本研究选取我国亚热带地区5个植被恢复阶段(草本、灌木、前期、中期和后期森林)为研究对象,采集土壤样品,系统测定土壤理化性质、GRSP(包括总提取球囊霉素相关土壤蛋白T-GRSP和易提取球囊霉素相关土壤蛋白EE-GRSP)、土壤微生物生物量和微生物群落组成等指标,并结合随机森林模型与偏最小二乘路径模型分析T-GRSP和EE-GRSP的主要影响因子。结果显示,植被恢复显著促进GRSP的积累。T-GRSP和EE-GRSP含量由草本阶段(1.73±0.19和0.64±0.03 g·kg-1)逐步增加至后期森林阶段(7.86±0.46和2.07±0.06 g·kg-1)。然而GRSP对土壤有机碳(SOC)的贡献随植被恢复呈下降趋势,T-GRSP/SOC由13.24±2.39%降低至5.28±0.20%,EE-GRSP/SOC由4.98±0.92%降低至1.40±0.06%,且草本阶段显著高于其他阶段。SOC、pH、全氮、全磷、微生物生物量碳、革兰氏阳性细菌和真菌/细菌是驱动GRSP积累的关键因素。

关键词: 亚热带, 植被恢复, 球囊霉素, 微生物特性, 土壤有机碳

Abstract: Abstract Aims To elucidate the dynamic changes of glomalin-related soil protein (GRSP) during subtropical vegetation restoration and to explore the effects of soil physicochemical properties and microbial characteristics on GRSP, this study aimed to provide a scientific basis for improving soil ecological functions in subtropical ecosystems. Methods Five vegetation restoration stages (herb, shrub, early forest, middle forest, and late forest) in the subtropical region of China were selected. Soil samples were collected to systematically determine soil physicochemical properties, GRSP (including total GRSP, T-GRSP, and easily extractable GRSP, EE-GRSP), soil microbial biomass, and microbial community composition. Random forest and partial least squares path modeling were employed to identify the main factors influencing T-GRSP and EE-GRSP. Important findings Vegetation restoration significantly promoted the accumulation of GRSP. The contents of T-GRSP and EE-GRSP increased from 1.73±0.19 and 0.64±0.03 g·kg-1 at the herb stage to 7.86±0.46 and 2.07±0.06 g·kg-1 at the late forest stage, respectively. However, the contribution of GRSP to soil organic carbon (SOC) decreased along the restoration gradient. The ratio of T-GRSP/SOC declined from 13.24±2.39% to 5.28±0.20%, and EE-GRSP/SOC decreased from 4.98±0.92% to 1.40±0.06%, with significantly higher values observed at the herb stage compared to other stages. SOC, pH, total nitrogen, total phosphorus, microbial biomass carbon, gram-positive bacteria, and the fungi-to-bacteria ratio were identified as key drivers of GRSP accumulation.

Key words: subtropical, vegetation restoration, glomalin, microbial characteristics, soil organic carbon