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热带低地雨林土壤酶活性及其化学计量对模拟干旱和磷添加的响应

吕泽文, 栾军伟, 李丝雨, 谭欣, 梁天, 王一, 刘翠菊, 刘世荣   

  1. 国际竹藤中心竹藤资源与环境研究所 国家林业和草原局/北京市共建竹藤科学与技术重点实验室, 北京 100102 中国
    国际竹藤中心三亚研究基地, 572022
    中国林业科学研究院森林生态环境与自然保护研究所, 国家林业和草原局森林生态环境重点实验室, 100091
  • 收稿日期:2025-12-18 修回日期:2026-05-26
  • 基金资助:
    国家自然基金委区域创新发展联合基金项目(U23A2002); 中央科研事业单位基本科研业务费专项资金项目(1632021023); 中央科研事业单位基本科研业务费专项资金项目(1630032024002); “十四五”国家重点研发计划项目(2024YFD2201402); 中央科研事业单位基本科研业务费专项资金项目(1630032025005)

Soil enzyme activities in response to manipulative drought and phosphorus addition in a tropical lowland rain forest

Lv Zewen, Luan, Li, Tan, Liang, Wang   

  1. , 100102, China
    , 572022,
    , 100091,
  • Received:2025-12-18 Revised:2026-05-26
  • Supported by:
    Joint Fund for Regional Innovation and Development of the National Natural Science Foundation of China(U23A2002); Special Fund Project for Basic Scientific Research Business Expenses of Central Scientific Research Institutions(1632021023); Special Fund Project for Basic Scientific Research Business Expenses of Central Scientific Research Institutions(1630032024002); National Key R&D Program of China in the 14th Five-Year Plan(2024YFD2201402); Special Fund Project for Basic Scientific Research Business Expenses of Central Scientific Research Institutions(1630032025005)

摘要: 干旱是影响森林生态系统的关键胁迫因子,对植物与土壤微生物造成直接生理限制。热带雨林作为全球生态系统的重要组成部分,其普遍受磷限制的同时正面临日益加剧的干旱胁迫。菌根是土壤碳和养分持续供给的重要途径,而土壤酶活性是表征微生物活性及养分循环的关键生物指标,但其如何响应干旱尚不清楚。本研究在海南三亚甘什岭自然保护区热带低地雨林中,建立了穿透雨减少与磷添加双因素交互实验平台,实验处理3年后,结合不同孔径中宇宙(1.45 mm、0.053 mm、0.001 mm)原位培养调控参与土壤过程生物组分,探讨土壤C、N、P循环相关酶活性对干旱与磷添加的响应及其与土壤理化性质的关系。结果表明:模拟干旱是抑制土壤酶活性的主导因素,尤其对碳循环相关的水解酶和氧化酶产生显著负面影响。磷添加直接缓解了微生物的磷限制,导致其投资策略转变。磷添加缓解了干旱对部分水解酶的抑制,但对氧化酶则表现出协同抑制。菌根途径对土壤酶活性的影响为间接调控,根与菌丝的物理排除并未显著改变酶活性格局。研究揭示了热带森林土壤微生物群落在干旱胁迫条件下通过调节群落结构与体内储存,维持胞外酶投资相对稳定的强内稳态能力,并进一步阐明了土壤酶活性在干旱与磷添加下的复杂响应机制,为预测热带森林地下生态过程及其对全球变化的反馈提供了重要科学依据。

关键词: 干旱, 磷添加, 土壤酶, 热带雨林, 酶化学计量, 气候变化

Abstract: Aims Drought is a key stress factor affecting forest ecosystem, which causes direct physiological constraints on plants and soil microorganisms. As an important part of the global ecosystem, tropical rain forests are normally phosphorus limited and facing increasing drought stress. Mycorrhiza is an important way of continuous supply of soil carbon and nutrients, and soil enzyme activity is the key biological index to characterize the underground nutrient cycle, but how it responds to drought and phosphorus addition is still unclear. Methods In a tropical lowland rainforest of Ganzhaling Nature Reserve in Sanya, Hainan island, a two factorial manipulative experiment of throughfall reduction and phosphorus addition was established since May 2019. Combined with the in-situ incubation of mesocosms with different mesh sizes (1.45 mm, 0.053 mm, 0.001 mm), soil C, N, P cycle related enzyme activities and their relationship with soil physical and chemical properties were analyzed. Important findings Simulated drought inhibited soil enzyme activities, especially has significant negative impacts on hydrolase and oxidase related to carbon cycle. Phosphorus addition alleviated the phosphorus limitation of microorganisms, leading to changes of their investment strategy. Phosphorus addition alleviated the inhibition of drought on some hydrolases, but showed synergistic inhibition on oxidase. The mycorrhizae indirectly regulated soil enzyme activities, and the physical exclusion of root and hypha did not significantly affect the pattern of enzyme activity. This study reveals that the tropical forest soil microbial community has a strong ability to maintain a relatively stable investment of extracellular enzymes by regulating the community structure and internal storage, and further demonstrated the complex response mechanism of mycorrhizal mediated soil enzyme activity to drought. Our findings provided an important understanding for predicting the underground ecological process of tropical forest and its feedback to global change.

Key words: Drought, Phosphorus addition, Soil enzymes, Tropical rainforest, Enzyme stoichiometry, Global climate change