Journal of Plant Ecology ›› 2026, Vol. 19 ›› Issue (1): 1-.DOI: 10.1093/jpe/rtaf140
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Jiaojiao Wang1,2, Fei Zang1,2,*, Ruochun Wang1,2, Fangyuan Huang1,2, Wenfang Zeng3, Hu Hao3 and Chuanyan Zhao1,2
1State Key Laboratory of Herbage Improvement and Grassland Agro-Ecosystems, Key Laboratory of Grassland Livestock Industry Innovation, Ministry of Agriculture and Rural Affairs, Engineering Research Center of Grassland Industry, Ministry of Education, College of Pastoral Agriculture Science and Technology, Lanzhou University, Lanzhou 730000, China, 2Observation Station of Subalpine Ecology Systems in the Middle Qilian Mountains, Zhangye 734000, China, 3Gansu Qilian Mountain National Nature Reserve Management and Protection Center, Zhangye 734000, China
*Corresponding author. Email: zangfei@lzu.edu.cn
摘要: 气候变暖会影响草地生态系统结构和功能。然而,目前学术界仍不清楚草地植物和土壤中微量元素如何响应气候变暖。本研究基于开顶箱(OTC)增温实验,探究了短期增温对祁连山中部亚高山草地冰草(Agropyron cristatum)和芨芨草(Achnatherum splendens)生物量、微量元素含量和土壤酶活性的影响。结果表明,增温显著提高了冰草地上生物量(117.0%)和地下生物量(64.1%),以及芨芨草地上生物量(112.5%)。增温处理中冰草地下部Cu、Fe、Mo、Co和V浓度、芨芨草地上部Cu和Mo浓度和地下部Ni浓度显著高于对照处理,而芨芨草地下部Zn浓度则呈相反趋势。增温显著降低芨芨草0–10 cm土壤中碱性蛋白酶(30.6%)、10–20 cm土壤中淀粉酶(30.9%)、碱性蛋白酶(23.7%)和脲酶活性(57.2%)。结构方程模型表明,增温直接或间接(通过影响相对湿度,土壤pH值,尤其是微量元素浓度)负向调控土壤酶活性。本研究为深入认识气候变暖背景下亚高山草地微量元素的迁移和转化规律,及其环境效应提供理论基础。