J Plant Ecol ›› Advance articles     DOI:10.1093/jpe/rtag116

• Research Article •     Next Articles

Drought and nitrogen addition shape leaf litter multi-element characteristics in a temperate grassland

Xue Cui 1,2, Wang Ma 1,*, Shuang-Li Hou 1, Bing-Chuan Zhang 1, Jia-Xin Hu 1,2, Zheng-Wen Wang1,3,*   

  1. 1 Erguna Forest-Steppe Ecotone Research Station, CAS Key Laboratory of Forest Ecology and Silviculture, Institute of Applied Ecology, Chinese Academy of Sciences, Shenyang 110016, China
    2 College of Resources and Environment, University of Chinese Academy of Sciences, Beijing 100049, China
    3 College of Life Science, Shenyang Normal University, Shenyang 110034, China
    * Correspondence: Zheng-Wen Wang & Wang Ma
    Email: wangzw@iae.ac.cn (Zheng-Wen Wang), mawang@iae.ac.cn (Wang Ma).
    Tel: +86-24-83970392 (Zheng-Wen Wang), +86 17302419446 (Wang Ma).
  • Received:2025-09-19 Accepted:2026-05-14 Published:2026-05-26
  • Supported by:
    This research was supported by the National Natural Science Foundation of China (42230515).

干旱与氮添加重塑温带草原叶片凋落物多元素化学特征

Abstract: Litter plays a critical role in biogeochemical cycling, yet how its multi-element traits respond to concurrent global changes, such as extreme drought, nitrogen deposition and snowpack changes and their combinations, remains poorly understood. To address this gap, we established a multifactorial manipulative experiment in a temperate grassland, where drought, nitrogen deposition and snowmelt delay and all their combinations were simulated. We measured the concentrations of a suite of primary macronutrients (C, N, P, K), secondary macronutrients (Ca, Mg) and micronutrients (Mn, Fe, Cu, Zn) of plant litter. Afterwards, we examined the individual and combined effects of N addition, drought, and snowmelt delay on the concentrations of community-level litter elements, and quantified the relative contributions of intraspecific trait variation (ITV) and species turnover. The results showed that the element concentrations of leaf litter were primarily shaped by drought and N addition, with limited response to snowmelt delay. Community-level litter element responses were largely driven by ITV, which increased the concentrations of elements such as N, K, Mn, and Zn, and concurrently decreased the concentration of Mg. In contrast, species turnover was the dominant mechanism responsible for reducing litter Ca concentration under all conditions and for increasing litter C concentration under N addition, and it weakened the community-level response to environmental change by offsetting the ITV-driven increase in Mn. Our results demonstrate that ITV acts as the dominant mechanism, working in concert with species turnover to drive the responses of litter multi- element traits in the temperate grassland to multiple global change factors.

Litter elemental traits determine its decomposition. This study found that drought and nitrogen addition, not snowmelt delay, dominated shifts in plant litter element concentrations, and such shifts at community level were driven rather by intraspecific trait variation than by species turnover.

Key words: global change, macronutrients, micronutrients, intraspecific trait variation, species turnover, temperate grassland

摘要:
凋落物在生物地球化学循环中扮演关键角色,但其多种化学元素特征如何响应极端干旱、氮沉降、积雪变化等多重全球变化及其组合,目前仍缺乏系统认知。为弥补这一知识缺口,本研究在温带草原开展全球变化多因子控制实验,同时模拟干旱、氮沉降和融雪延迟及其全部组合处理,测定了草原植物凋落物大量元素(C、N、P、K)、中量元素(Ca、Mg)及微量元素(Mn、Fe、Cu、Zn)的浓度。探讨了氮添加、干旱、延迟融雪三种处理单独及交互作用对群落水平凋落物元素浓度的影响,并量化了种内性状变异( ITV)与物种周转对凋落物多元素特征变化的相对贡献。结果表明,凋落物元素特征主要受干旱和氮添加的调控,对融雪延迟的响应有限。群落水平凋落物元素浓度的响应以种内性状变异为主导,种内性状变异显著提高了N、K、Mn、Zn等元素的浓度,同时降低了Mg的浓度;与之相反,物种周转是各处理下凋落物Ca浓度降低、以及氮添加单独处理下凋落物C浓度升高的主导驱动机制。此外,物种周转可通过抵消种内性状变异导致的凋落物Mn浓度上升而削弱群落水平凋落物Mn浓度对环境变化的响应程度。本研究证实,种内性状变异作为主导机制,与物种周转共同驱动温带草原凋落物初始多元素特征对全球变化多因子的响应。

关键词: 大量元素, 微量元素, 种内性状变异, 物种周转, 温带草原