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应用生态学报 ›› 2025, Vol. 36 ›› Issue (3): 911-917.doi: 10.13287/j.1001-9332.202503.017

• 研究论文 • 上一篇    下一篇

不同退化程度高寒草地土壤微生物残体和球囊霉素积累及其对有机碳的贡献

张浩林1, 李娅芸2, 胡洋3, 李会军4, 周玥3, 安韶山1,4, 朱兆龙1,4*   

  1. 1西北农林科技大学水土保持科学与工程学院, 陕西杨凌 712100;
    2黄河水资源保护科学研究院, 郑州 450004;
    3西北农林科技大学资源与环境学院, 陕西杨凌 712100;
    4西北农林科技大学水土保持与荒漠化整治全国重点实验室, 陕西杨凌 712100
  • 收稿日期:2024-08-20 接受日期:2025-01-17 出版日期:2025-03-18 发布日期:2025-05-15
  • 通讯作者: * E-mail: zhu_zl@nwafu.edu.cn
  • 作者简介:张浩林, 男, 2000年生, 硕士研究生。主要从事土壤微生物固碳研究。E-mail: zhanghaolin@nwafu.edu.cn
  • 基金资助:
    第二次青藏高原综合科学考察研究项目(2019QZKK0603)和中国科学院西部之光基金项目(xbzg-zdsys-202009)

Accumulation of microbial necromass and glomalin and their contribution to organic carbon in alpine grasslands with different degradation degrees

ZHANG Haolin1, LI Yayun2, HU Yang3, LI Huijun4, ZHOU Yue3, AN Shaoshan1,4, ZHU Zhaolong1,4*   

  1. 1College of Soil and Water Conservation Science and Engineering, Northwest A&F University, Yangling 712100, Shaanxi, China;
    2Institute of Yellow River Water Resources Protection, Zhengzhou 450004, China;
    3College of Natural Resources and Environment, Northwest A&F University, Yang-ling 712100, Shaanxi, China;
    4State Key Laboratory of Soil and Water Conservation and Desertification Control, Northwest A&F University, Yangling 712100, Shaanxi, China
  • Received:2024-08-20 Accepted:2025-01-17 Online:2025-03-18 Published:2025-05-15

摘要: 青藏高原是全球变化研究的“敏感区”,其草地退化严重影响土壤微生物和有机碳(SOC)积累。土壤微生物残体(MNC)和球囊霉素相关土壤蛋白(GRSP)作为稳定的微生物代谢产物在SOC的形成和稳定中发挥着关键作用。本研究选取青藏高原不同退化程度(未退化、轻度退化、中度退化和重度退化)的高寒草地为研究对象,测定土壤中的MNC和GRSP,分析它们对SOC的贡献及其影响因素。结果表明: 1)随着高寒草地退化程度的加剧,土壤中MNC(6.04~14.27 mg·g-1)和GRSP的含量(2.55~7.64 mg·g-1)显著减少,但对SOC的贡献变化不显著。2)MNC对SOC的贡献(7.5%~68.3%)高于GRSP(3.3%~26.5%),前者平均为后者的2.8倍;高寒草地退化导致在SOC降低的过程中,MNC减少的速率是GRSP的1.7倍。3)土壤理化性质和微生物生物量是影响MNC和GRSP积累的重要因素。综上,微生物代谢产物(如MNC和GRSP)对SOC的维持具有重要意义,能够在高寒草地退化过程中缓解SOC含量的下降,在应对和减缓高寒草地退化方面扮演着关键角色。

关键词: 高寒草地, 草地退化, 土壤有机碳, 球囊霉素相关土壤蛋白, 微生物残体碳

Abstract: The Qinghai-Xizang Plateau is sensitive to global change. Grassland degradation in this region severely affects soil microorganisms and soil organic carbon (SOC). As stable microbial metabolites, soil microbial necromass C (MNC) and glomalin-related soil proteins (GRSP) play a key role in the formation and stabilization of SOC. We investigated the content of MNC and GRSP in alpine grasslands with different degradation degrees (non-degradation, light degradation, moderate degradation, and heavy degradation) on the Qinghai-Xizang Plateau. We further analyzed their contributions to SOC and influencing factors. The results showed that: 1) The contents of MNC (6.04-14.27 mg·g-1) and GRSP (2.55-7.64 mg·g-1) significantly decreased with increasing degradation degrees. T heir contributions to SOC remained stable. 2) The contribution of MNC to SOC (7.5%-68.3%) was 2.8 times as high as that of GRSP (3.3%-26.5%). With the decreases of SOC owing to degradation, the MNC was accordingly reduced at 1.7 times as GRSP. 3) Soil physicochemical properties and microbial biomass were key factors affecting the accumulation of MNC and GRSP. In summary, microbial metabolites (e.g., MNC and GRSP) were key for SOC maintenance, and consequently played a crucial role in alleviating the impacts of alpine grassland degradation.

Key words: alpine grassland, grassland degradation, soil organic carbon, glomalin-related soil protein, microbial necromass carbon