2025年04月08日 星期二

广西师范大学学报（自然科学版） ›› 2025, Vol. 43 ›› Issue (1): 9-19.doi: 10.16088/j.issn.1001-6600.2024051902

• “生态保护与资源可持续利用”专辑 • 上一篇    下一篇

桂北喀斯特植被恢复对球囊霉素相关土壤蛋白的影响

唐利1,2, 李梦霞1,2, 黄慧欣1,2, 潘心茹1,2, 姜雪芳1,2, 杨淑君1,2, 潘于1,2, 覃云斌1,2,3*   

  1. 1.珍稀濒危动植物生态与环境保护教育部重点实验室(广西师范大学), 广西 桂林 541006;
    2.广西漓江流域景观资源保育与可持续利用重点实验室(广西师范大学), 广西 桂林 541006;
    3.广西师范大学 可持续发展创新研究院, 广西 桂林 541006
  • 收稿日期:2024-05-19 修回日期:2024-07-16 出版日期:2025-01-05 发布日期:2025-02-07
  • 通讯作者: 覃云斌(1990—),男,广西桂林人,广西师范大学讲师,博士。E-mail:shuibaoqinyunbin@163.com
  • 基金资助:
    国家自然科学基金青年科学基金(32201416); 广西师范大学大学生创新创业训练计划(S202210602089)

Effects of Karst Vegetation Restoration on GRSP in Northern Guangxi

TANG Li1,2, LI Mengxia1,2, HUANG Huixin1,2, PAN Xinru1,2, JIANG Xuefang1,2, YANG Shujun1,2, PAN Yu1,2, QIN Yunbin1,2,3*   

  1. 1. Key Laboratory of Ecology of Rare and Endangered Species and Environmental Protection (Guangxi Normal University), Ministry of Education, Guilin Guangxi 541006, China;
    2. Guangxi Key Laboratory of Landscape Resources Conservation and Sustainable Utilization in Lijiang River Basin (Guangxi Normal University), Guilin Guangxi 541006, China;
    3. Institute for Sustainable Development and Innovation, Guangxi Normal University, Guilin Guangxi 541006, China
  • Received:2024-05-19 Revised:2024-07-16 Online:2025-01-05 Published:2025-02-07

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摘要： 球囊霉素相关土壤蛋白(glomalin related soil protein, GRSP)是土壤有机质的重要组分,有加强土壤团聚体水稳定性、促进土壤碳储存等作用。为研究广西北部喀斯特植被恢复过程中GRSP的含量变化及其影响因子,本研究选取桂北喀斯特地区3个不同植被恢复阶段(灌木林阶段、灌乔过渡阶段和乔木林阶段)的根际土、非根际土和农田(对照)土壤作为研究对象,测定总土壤球囊霉素相关土壤蛋白(total glomalin-related soil protein,T-GESP)和易提取球囊霉素相关土壤蛋白(easily extractable glomalin-related soil protein,EE-GRSP)含量,并分析影响GRSP含量变化的关键环境因子。结果表明:各植被恢复阶段根际土中的T-GRSP和EE-GRSP含量均显著高于农田阶段(P<0.05),且T-GRSP含量在乔木林阶段最高。T-GRSP/SOC(土壤有机碳)的比值为4.45%～18.05%,EE-GRSP/SOC 的比值为0.23%～1.35%,农田的T-GRSP/SOC和EE-GRSP/SOC比值均显著高于各植被恢复阶段(P<0.001)。灌乔过渡阶段和乔木林阶段根际土的T-GRSP含量显著高于非根际土(P<0.05)。土壤有机碳和硝态氮含量是引起T-GRSP含量正向变化的关键因素,而土壤全氮、有机碳和微生物生物量氮含量是影响EE-GRSP正向变化的关键因素。因此,桂北喀斯特植被恢复能有效促进GRSP的积累,进而促进SOC的积累与稳定。

关键词: 喀斯特地区, 植被恢复, 丛枝菌根真菌, 球囊霉素, 土壤蛋白, 根际土壤

Abstract: The glomalin-related soil protein (GRSP)is a crucial constituent of soil organic matter, contributing to the enhancement of soil aggregate water stability and the promotion of soil carbon storage. This study focused on investigating the variations in GRSP content and its influencing factors during karst vegetation restoration in northern Guangxi. Rhizosphere soil, non-rhizosphere soil, and farmland (control) soil from three different stages of vegetation restoration (shrub stage, transition stage with irrigation, and forest stage) were selected as research subjects. The analysis included total glomalin-related soil protein (T-GRSP), as well as easily extractable glomalin-related soil protein (EE-GRSP), along with an examination of key environmental factors affecting changes in GRSP content. The findings revealed significantly higher T-GRSP and EE-GRSP contents in rhizosphere soils at each vegetation restoration stage compared with those in farmland (P<0.05). Additionally, the T-GRSP content was highest during the forest stage. The ratios of T-GRSP/SOC ranged from 4.45% to 18.05%, while the ratios of EE-GRSP/SOC ranged from 0.23% to 1.35%. Furthermore, these ratios were significantly higher in farmland than at each vegetation restoration stage (P<0.001). Notably, T-GRSP content was significantly higher in rhizosphere soils than non-rhizosphere soils during both transition and forest stages (P<0.05). Soil organic carbon and nitrate nitrogen content emerged as key factors driving positive changes in T-GRSP content; meanwhile, the contents of total nitrogen, organic carbon, and microbial nitrogen were identified as key influencers for positive changes observed in EE-GRSP. In conclusion, karst vegetation restoration in northern Guangxi effectively promotes GRSP accumulation and subsequently enhances SOC accumulation and stability.

Key words: karst area, vegetation restoration, arbuscular mycorrhizal fungi, glomalin, soil protein, rhizosphere soil

中图分类号:  S153.621;X171.4

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