Wang Dan, Ling Tianqi, Wang Pengpeng, Jing Panpan, Fan Jiazhi, Wang Hao, Zhang Yaoqi
International Center for Ecology, Meteorology and Environment, Jiangsu Key Laboratory of Agricultural Meteorology, Nanjing University of Information Science and Technology, Nanjing, China.
School of Forestry and Wildlife Sciences, Auburn University, Auburn, AL, United States.
Front Plant Sci. 2018 Sep 11;9:1290. doi: 10.3389/fpls.2018.01290. eCollection 2018.
Understanding how nitrogen (N) and/or phosphorus (P) addition affects plants carbon- and water- related ecophysiological characteristics is essential for predicting the global change impact on the alpine meadow ecosystem structure and function in carbon and water cycling. The Qinghai-Tibetan Plateau (QTP) with the largest alpine meadow in the world is regarded as the third pole in the earth and has been experiencing increased atmospheric N deposition. In this project, we focused on two key species ( and ) of the alpine meadow on the Tibetan Plateau and investigated the variability of photosynthetic and stomatal responses to 8-year N and/or P treatments through field measurements and modeling. We measured photosynthesis- and g-response curves to generate parameter estimates from individual leaves with two widely used stomatal models (the BWB model and MED model) for validation of growth and ecosystem models and to elucidate the physiological basis for observed differences in productivity and WUE. We assessed WUE by means of gas exchange measurements (WUE) and stable carbon isotope composition (ΔC) to get the intrinsic and integrated estimates of WUE of the two species. P and N+P treatments, but not N, improved the photosynthetic capacity (A and V) for both species. Stomatal functions including instaneous measurements of stomatal conductance, intrinsic water-use efficiency and stomatal slope parameters of the two widely used stomatal models were altered by the addition of P or N+P treatment, but the impact varied across years and species. The inconsistent responses across species suggest that an understanding of photosynthetic, stomatal functions and water-use should be evaluated on species separately. WUE estimated by ΔC values had a positive relationship with A and g and a negative relationship with WUE. Our findings should be useful for understanding the underlying mechanisms of the response of alpine plants growth and alpine meadow ecosystem to global change.
了解氮(N)和/或磷(P)添加如何影响植物与碳和水相关的生态生理特征,对于预测全球变化对高山草甸生态系统结构以及碳和水循环功能的影响至关重要。拥有世界上最大高山草甸的青藏高原(QTP)被视为地球的第三极,并且一直在经历大气氮沉降增加的情况。在这个项目中,我们聚焦于青藏高原高山草甸的两个关键物种(和),并通过实地测量和建模研究了8年氮和/或磷处理下光合和气孔响应的变异性。我们测量了光合作用和气孔导度响应曲线,以使用两种广泛使用的气孔模型(BWB模型和MED模型)从单叶生成参数估计值,用于验证生长和生态系统模型,并阐明观察到的生产力和水分利用效率差异的生理基础。我们通过气体交换测量(WUE)和稳定碳同位素组成(ΔC)来评估水分利用效率,以获得这两个物种水分利用效率的内在和综合估计值。磷和氮 + 磷处理,而非氮处理,提高了两个物种的光合能力(A和V)。添加磷或氮 + 磷处理改变了气孔功能,包括两种广泛使用的气孔模型的气孔导度瞬时测量、内在水分利用效率和气孔斜率参数,但影响因年份和物种而异。物种间不一致的响应表明,对光合、气孔功能和水分利用的理解应分别在物种层面进行评估。通过ΔC值估计的水分利用效率与A和气孔导度呈正相关,与水分利用效率呈负相关。我们的研究结果对于理解高山植物生长和高山草甸生态系统对全球变化响应的潜在机制应该是有用的。