J Plant Ecol ›› Advance articles     DOI:10.1093/jpe/rtag252

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Carbon sink strength and its environmental controls in ecosystems along an elevational gradient in dryland mountains

Ying Wang1,2,3, Dan Lu1,2,3, Yi-Fan Jiang2,3,4, Yi-Xuan Qu1,2, Xiao-Jun Ma3, Jin-Gui Zhang3, Chao Guan1,2,3,5*, Chang-Ming Zhao1,2,3,5   

  1. 1. State Key Laboratory of Herbage Improvement and Grassland Agro-ecosystems, College of Ecology, Lanzhou University, Lanzhou 730000, China;
    2. Yuzhong Mountain Ecosystems Observation and Research Station, Lanzhou University, Lanzhou 730000, China;
    3. Gansu Provincial Climate Change Science Data Center, Lanzhou University, Lanzhou 730000, China;
    4. School of Life Sciences, Lanzhou University, Lanzhou 730000, China;
    5. Center for Remote Sensing of Ecological Environments in Cold and Arid Regions, Lanzhou University, Lanzhou 730000, China
    *Corresponding author:
    Chao Guan,E-mail: guanchao@lzu.edu.cn
  • Received:2025-10-23 Revised:2026-08-16 Accepted:2026-09-24 Published:2026-10-28
  • Supported by:
    The authors gratefully acknowledge the staff at the Gansu Xinglong Mountain National Nature Reserve for their invaluable assistance and support. ChatGPT was used solely to improve the language and readability of the manuscript.

Abstract: Ecosystems in dryland mountains occur along pronounced elevational gradients and exhibit high environmental heterogeneity, playing key roles in the global carbon cycle. However, their CO2 flux dynamics and environmental controls remain insufficiently understood. In this study, we established three eddy covariance flux sites along an elevational gradient in a dryland mountain region of Northwest China, representing a Larix principis-rupprechtii plantation, a Rhododendron lapponicum shrubland, and an alpine meadow. Continuous observations from 2020 to 2022 quantified seasonal and cross-ecosystem variations in net ecosystem productivity (NEP), gross primary productivity (GPP), and ecosystem respiration (Re), and examined their responses to environmental and physiological variables. Annual GPP and Re decreased significantly with increasing elevation. The plantation showed the strongest net CO2 uptake, the shrubland maintained variable net CO2 uptake, and the alpine meadow remained close to CO2 neutrality, shifting between weak net CO2 uptake and weak net CO2 release. Monthly anomaly analysis showed that NEP anomalies were most pronounced during the peak growing season and were mainly driven by GPP anomalies, while Re anomalies either amplified or offset GPP effects on NEP. Random forest and structural equation modeling analyses revealed that dominant controls shifted along the elevational gradient, with lower-elevation ecosystems being primarily regulated by vegetation activity, photosynthetic capacity, and atmospheric water demand, whereas higher-elevation ecosystems showed stronger temperature and water limitations. These results highlight that magnitude of net CO2 uptake was jointly influenced by vegetation activity, thermal conditions, and water availability through their contrasting effects on photosynthetic CO2 uptake and ecosystem respiration.

Plant-pollinator and plant-VOC networks showed congruent temporal dynamics. Monthly shifts in pollinator composition were tightly coupled with changes in floral VOC profiles. Associations between specific VOC classes and pollinator groups were highly context-dependent, varying in both strength and direction across months.

Key words: elevational gradient, eddy covariance, net ecosystem productivity, environmental drivers, alpine meadow, forest ecosystems