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Yaping Lin1,2,3, Qiufang Zhang1,2,3*, Hao Sun1,2,3, Jiaohong Lu1,2,3, Zehong Yao1,2,3, Quanxin Zeng1,4, Chenxing Lian1,2,3, Huizhi Pi1,2,3, Xiaochun Yuan5, Yuehmin Chen1,2,3*
1Key Laboratory of Humid subtropical Eco-geographical Process of Ministry of Education, School of Geographical Sciences, Fujian Normal University, Fuzhou 350117, China
2Fujian Sanming Forest Ecosystem National Observation and Research Station, Fujian Normal University, Fuzhou 350117, China
3Fujian Provincial Key Laboratory for Subtropical Resources and Environment, Fujian Normal University, Fuzhou 350117, China
4State Key Laboratory of Vegetation Structure, Function and Construction (VegLab), Ministry of Education Key Laboratory of Earth Surface Processes, and College of Urban and Environmental Sciences, Peking University, Beijing 100871, China
5College of Tourism, Wuyi University, Wuyishan 354300, China.
*Corresponding author: Qiufang Zhang and Yuehmin Chen
Email: qiufangzh@fjnu.edu.cn (Qiufang Zhang); ymchen@fjnu.edu.cn (Yuehmin Chen)
摘要: 微生物碳利用效率(CUE)和氮利用效率(NUE)是决定土壤碳(C)和氮(N)归宿的关键参数。然而,不同土层中微生物CUE和NUE对氮沉降的响应尚不明确。本研究以罗浮栲(Castanopsis faberi)林为对象,通过氮添加试验,采集表层(0–10 cm)和亚表层(20–30 cm)土壤样品,探讨不同土层微生物CUE和NUE对氮添加的响应,并测定土壤碳组分、微生物生物量、酶活性及微生物群落组成等指标。结果显示,微生物CUE与NUE呈显著正相关,揭示了碳氮代谢的耦合关系。氮添加降低了表层和亚表层土壤的CUE和NUE,但在亚表层土壤中的负效应较弱。氮添加显著改变了土壤不同碳组分的积累:在表层土壤中,氮添加增加了易降解碳和颗粒态有机碳含量,而在亚表层土壤中,氮添加减少了矿物结合态有机碳和难降解碳含量。微生物CUE和NUE与土壤碳组分含量显著相关。与表层相比,亚表层土壤的CUE、NUE和可溶性有机碳含量较低,但C/N比更高,表明不同土层CUE和NUE的差异同时受碳数量和质量的调控。本研究揭示了氮添加对微生物资源利用效率的一致负效应及其对土层的依赖性,为深入理解森林生态系统碳氮耦合过程提供了新见解。