Chin J Plant Ecol ›› 2025, Vol. 49 ›› Issue (7): 1053-1069.DOI: 10.17521/cjpe.2024.0376  cstr: 32100.14.cjpe.2024.0376

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Effects of elevated atmospheric CO2 concentration and warming on stability of soil organic carbon pool accumulation, molecular composition and structure stability

FAN Ya-Ran1, XIA Shao-Pan1,*(), YU Bing-Bing1, ZHU Zi-Qi1, YANG Wei2, FAN Yu-Chuan3, LIU Xiao-Yu1, ZHANG Xu-Hui1, ZHENG Ju-Feng1   

  1. 1Institute of Resource, Ecosystem and Environment of Agriculture, College of Resources and Environmental Sciences, Nanjing Agricultural University, Nanjing 210095, China
    2College of Grassland Science, Inner Mongolia Agricultural University, Hohhot 010018, China
    3Department of Soil, Water, and Ecosystem Sciences, University of Florida-IFAS, Gainesville, FL 32603, USA
  • Received:2024-10-21 Accepted:2025-02-26 Online:2025-07-20 Published:2025-02-26
  • Contact: XIA Shao-Pan
  • Supported by:
    Natural Science Foundation of Jiangsu Province(BK20221028);National Natural Science Foundation of China(42303078)

Abstract:

In the context of carbon sequestration, emission reduction, and the “Dual Carbon” goals, the impact of climate change characterized by the combined effects of elevated atmospheric carbon dioxide (CO2) concentration and global warming on the dynamics of soil organic carbon (SOC) has emerged as a critical research focus. Understanding the mechanisms through of climate change influences SOC pools remains a significant challenge in academic research. Previous studies on the effect of climate change on terrestrial ecosystem carbon cycling have predominantly examined single factors, such as increased CO2 concentration or warming, with a focus on plant growth, litter substrate quality, soil physicochemical properties, physical/chemical fractions of organic carbon, and microbial community structure. Building on recent advancements in both domestic and international research, this review synthesizes the effects and underlying mechanisms of elevated CO2 concentration and warming on SOC accumulation. By integrating the coupling effects of SOC fractions, molecular composition, structural characteristics, and the differential responses of topsoil and subsoil, we elucidate the intrinsic mechanism governing SOC carbon accumulation and transformation under these climatic conditions. Furthermore, we highlight key areas for future research, including (1) clarifying the coupling relationships among SOC end-member inputs, molecular composition, and structural characteristics, and (2) uncovering the mechanisms by which long-term climate change influences the stability and burial potential of SOC across diverse ecosystems. To fully understand the carbon source/sink functions of soil, it is essential to comprehensively investigate the biogeochemical processes governing SOC sources, transformation, burial, and decomposition in terrestrial ecosystems under climate change. This review aims to provide a robust scientific foundation for future soil carbon management strategies and decision-making in support of carbon neutrality goals.

Key words: climate change, soil organic carbon, molecular composition and structure, stability, subsoil, terrestrial ecosystems, biogeochemical cycle