Dai Licong, Ke Xun, Du Yangong, Zhang Fawei, Li Yikang, Li Qian, Lin Li, Peng Cuoji, Shu Kai, Cao Guangmin, Guo Xiaowei
Key Laboratory of Adaptation and Evolution of Plateau Botany, Northwest Institute of Plateau Biology Chinese Academy of Science Xining China.
University of Chinese Academy of Science Beijing China.
Ecol Evol. 2019 Jul 16;9(15):8865-8875. doi: 10.1002/ece3.5442. eCollection 2019 Aug.
Net primary production (NPP) is a fundamental property of natural ecosystems. Understanding the temporal variations of NPP could provide new insights into the responses of communities to environmental factors. However, few studies based on long-term field biomass measurements have directly addressed this subject in the unique environment of the Qinghai-Tibet plateau (QTP). We examined the interannual variations of NPP during 2008-2015 by monitoring both aboveground net primary productivity (ANPP) and belowground net primary productivity (BNPP), and identified their relationships with environmental factors with the general linear model (GLM) and structural equation model (SEM). In addition, the interannual variation of root turnover and its controls were also investigated. The results show that the ANPP and BNPP increased by rates of 15.01 and 143.09 g/m per year during 2008-2015, respectively. BNPP was mainly affected by growing season air temperature (GST) and growing season precipitation (GSP) rather than mean annual air temperature (MAT) or mean annual precipitation (MAP), while ANPP was only controlled by GST. In addition, available nitrogen (AN) was significantly positively associated with BNPP and ANPP. Root turnover rate averaged 30%/year, increased with soil depth, and was largely controlled by GST. Our results suggest that alpine meadow was an N-limited ecosystem, and the NPP on the QTP might increase further in the future in the context of global warming and nitrogen deposition.
净初级生产力(NPP)是自然生态系统的一个基本属性。了解NPP的时间变化可以为群落对环境因素的响应提供新的见解。然而,在青藏高原(QTP)独特的环境中,基于长期野外生物量测量的研究很少直接涉及这个主题。我们通过监测地上净初级生产力(ANPP)和地下净初级生产力(BNPP),研究了2008 - 2015年期间NPP的年际变化,并使用一般线性模型(GLM)和结构方程模型(SEM)确定了它们与环境因素的关系。此外,还研究了根系周转的年际变化及其控制因素。结果表明,2008 - 2015年期间,ANPP和BNPP分别以每年15.01和143.09 g/m的速率增加。BNPP主要受生长季气温(GST)和生长季降水量(GSP)的影响,而不是年平均气温(MAT)或年平均降水量(MAP),而ANPP仅受GST的控制。此外,有效氮(AN)与BNPP和ANPP显著正相关。根系周转率平均为每年30%,随土壤深度增加,且在很大程度上受GST控制。我们的研究结果表明,高寒草甸是一个受氮限制的生态系统,在全球变暖和氮沉降的背景下,QTP上的NPP未来可能会进一步增加。