Key Laboratory of Vegetation Restoration and Management of Degraded Ecosystems, Guangdong Provincial Key Laboratory of Applied Botany, South China Botanical Garden, and Center for Plant Ecology, Core Botanical Gardens, Chinese Academy of Sciences, Guangzhou, China.
College of Life Sciences, Gannan Normal University, Ganzhou, China.
Glob Chang Biol. 2020 Jun;26(6):3585-3600. doi: 10.1111/gcb.15071. Epub 2020 Apr 8.
A mechanistic understanding of plant photosynthetic response is needed to reliably predict changes in terrestrial carbon (C) gain under conditions of chronically elevated atmospheric nitrogen (N) deposition. Here, using 2,683 observations from 240 journal articles, we conducted a global meta-analysis to reveal effects of N addition on 14 photosynthesis-related traits and affecting moderators. We found that across 320 terrestrial plant species, leaf N was enhanced comparably on mass basis (N , +18.4%) and area basis (N , +14.3%), with no changes in specific leaf area or leaf mass per area. Total leaf area (TLA) was increased significantly, as indicated by the increases in total leaf biomass (+46.5%), leaf area per plant (+29.7%), and leaf area index (LAI, +24.4%). To a lesser extent than for TLA, N addition significantly enhanced leaf photosynthetic rate per area (A , +12.6%), stomatal conductance (g , +7.5%), and transpiration rate (E, +10.5%). The responses of A were positively related with that of g , with no changes in instantaneous water-use efficiency and only slight increases in long-term water-use efficiency (+2.5%) inferred from C composition. The responses of traits depended on biological, experimental, and environmental moderators. As experimental duration and N load increased, the responses of LAI and A diminished while that of E increased significantly. The observed patterns of increases in both TLA and E indicate that N deposition will increase the amount of water used by plants. Taken together, N deposition will enhance gross photosynthetic C gain of the terrestrial plants while increasing their water loss to the atmosphere, but the effects on C gain might diminish over time and that on plant water use would be amplified if N deposition persists.
为了可靠地预测在长期大气氮(N)沉降条件下陆地碳(C)增益的变化,我们需要对植物光合作用的反应机制有一个深入的了解。在这里,我们使用 240 篇期刊文章中的 2683 个观测值,进行了一项全球元分析,以揭示 N 添加对 14 种与光合作用相关的性状的影响及其影响的调节因子。我们发现,在 320 种陆地植物物种中,叶片 N 的质量基础(N, +18.4%)和面积基础(N, +14.3%)都得到了显著增强,而比叶面积或叶面积与质量比没有变化。总叶面积(TLA)显著增加,表现为总叶生物量增加(+46.5%)、植物叶面积增加(+29.7%)和叶面积指数(LAI,+24.4%)。与 TLA 相比,N 添加对叶片光合速率/面积(A, +12.6%)、气孔导度(g, +7.5%)和蒸腾速率(E,+10.5%)的增强程度要小一些。A 的响应与 g 的响应呈正相关,没有观察到瞬时水分利用效率的变化,只有长期水分利用效率略有增加(+2.5%),这是从 C 组成推断出来的。性状的响应取决于生物、实验和环境调节因子。随着实验持续时间和 N 负荷的增加,LAI 和 A 的响应减弱,而 E 的响应显著增加。TLA 和 E 的增加模式表明,N 沉积将增加植物用水量。总的来说,N 沉积将增强陆地植物的总光合 C 增益,同时增加其向大气的水分损失,但随着时间的推移,对 C 增益的影响可能会减弱,如果 N 沉积持续下去,对植物水分利用的影响将会放大。