Journal of Plant Ecology ›› 2025, Vol. 18 ›› Issue (5): 1-45.DOI: 10.1093/jpe/rtaf087
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Yong Bao1, Xiuxian Men1, Chang Liao1, Deping Zhai1, Jinsheng Li3, Yiyue Wang1, Chi Wang1,2, Xiaoli Cheng1,2*
1State Key Laboratory for Vegetation Structure, Functions and Construction and Ministry of Education Key Laboratory for Transboundary Ecosecurity of Southwest China and Key Laboratory of Soil Ecology and Health in Universities of Yunnan Province, School of Ecology and Environmental Sciences, Yunnan University, Kunming 650500, China, 2Yunnan Key Laboratory of Soil Erosion Prevention and Green Development, Institute of International Rivers and Eco-security, Yunnan University, Kunming 650091, China, 3School of Resources and Environment, Anhui Agricultural University, Hefei 230036, China
*Corresponding author. E-mail: xlcheng@ynu.edu.cn
摘要: 土壤溶解性有机质(DOM)在陆地生态系统碳(C)循环中至关重要。然而,森林类型和海拔对山地生态系统土壤DOM动态的调控效应尚未完全明晰。本研究在横断山脉海拔梯度(2600–3500 m)上,系统研究了土壤DOM含量、光谱特征、分子特性及其潜在驱动因子。结果表明,阔叶林土壤(2900和3500 m)的溶解性有机碳(DOC)含量均显著高于针叶林土壤(2600和3200 m),且湿季DOM含量普遍高于干季。腐殖化指数(HIX)与DOC含量变化趋势一致,而芳香性指数(AI)则呈相反趋势,这些模式与凋落物碳源质量密切相关。DOM的分子水平分析表明,木质素类结构化合物和单宁是土壤DOM的主要成分,表明研究区土壤DOM的分子组成具有典型的植物源特征。此外,干季期间,木质素化合物的相对丰度随海拔升高逐渐降低。干季土壤DOM动态主要受土壤性质(尤其是NH₄⁺-N含量)的调控,而湿季则主要受凋落物特性(如叶DOC含量)影响。总体而言,本研究揭示了凋落物特性和土壤性质主导调控了沿海拔梯度的土壤DOM的变化机制,表明在未来气候变化背景下,高山生态系统土壤DOM动态可能因树种差异而对土壤碳固存产生差异性影响。