植物生态学报 ›› 2026, Vol. 50 ›› Issue (预发表): 0-.DOI: 10.17521/cjpe.2025.0416

• •    下一篇

长期氮沉降改变热带森林土壤木质素酚积累的调控路径

马云瀚, 鲁显楷, 贾永霞, 朱晓敏   

  1. 中国科学院华南植物园, 广东 510650 中国
    中国科学院大学, 101408
    中国科学院华南植物园公共实验室中心, 510650
  • 收稿日期:2025-11-24 修回日期:2026-03-06 出版日期:2026-06-20

Long-term nitrogen deposition alters the regulatory pathways of lignin phenol accumulation in tropical forest

Ma Yunhan, Lu Xiankai, Jia Yongxia, Zhu Xiaomin   

  1. , 510650, China
    , 101408,
    , 510650,
  • Received:2025-11-24 Revised:2026-03-06 Online:2026-06-20
  • Supported by:
    Supported by the National Natural Science Foundation of China(32371735); Supported by the National Natural Science Foundation of China(32271687); and the Funding from the Guangdong Province Science and Technology Project(2022B1111230001)

摘要: 森林土壤有机碳(SOC)对全球变化响应的研究一直是生态学科的前沿热点问题。尽管大量研究表明氮沉降能够促进森林SOC积累并提高其稳定性,但其对SOC中特异性植物源组分(如木质素酚)积累过程的影响尚不明确,这限制了我们深入理解森林碳循环过程及其在维持全球碳平衡中的重要作用。基于鼎湖山长期(>20年)氮沉降试验平台(112° 10′ E,23° 10′ N),本研究系统探讨了长期施氮对不同土层木质素酚积累模式的影响及其潜在机制。研究发现:(1)木质素酚含量随着土壤深度而显著下降;施氮使0-10cm土层木质素酚含量提高了23.7%,但对10-30cm土层没有显著影响。(2)在对照处理下,碳降解酶的活性是木质素酚积累的关键影响因素;施氮抑制了碳降解酶活性,削弱了其对木质素酚积累的调控作用。但是木质素酚更多地通过与土壤矿物结合实现物理化学保护,有效地降低了木质素酚的生物可利用性。综上所述,长期氮沉降对热带森林植物源碳的影响具有显著的土层依赖性,其作用仅限于促进表层土壤木质素酚的积累。长期高氮输入改变了热带常绿阔叶林土壤植物源碳积累的调控路径,由依赖微生物降解过程转向以物理化学保护作用为主导。该研究揭示了氮沉降背景下热带森林土壤碳库稳定性维持的新机制,为预测森林土壤碳动态提供了重要理论依据。

关键词: 木质素酚积累, 矿物物理化学保护, 土壤有机碳固存, 氮沉降, 热带森林

Abstract: Aims The response of forest soil organic carbon (SOC) to global change has remained a prominent frontier issue in ecological research. Although numerous studies have demonstrated that nitrogen deposition can promote the accumulation and of forest SOC and enhance its stability, the impact of nitrogen deposition on the accumulation process of specific plant-derived components in SOC, such as lignin phenols, remains unclear. This knowledge gap limits our in-depth understanding of forest carbon cycling processes and their pivotal role in maintaining global carbon balance. Methods Based on the long-term (more than 20 years) nitrogen deposition experimental platform in Dinghu Mountain(112° 10′ E, 23° 10′ N), this study systematically investigated the effects of long term nitrogen addition on the accumulation patterns of lignin phenols across different soil layers and their underlying mechanisms. Important findings The results indicated that: (1) Lignin phenol content significantly decreases with soil depth; Nitrogen addition increased lignin phenol content by 23.7% in the 0-10 cm soil layer but had no significant effect on the 10-30 cm layer. (2) Under the control treatment, the activity of C-degrading enzymes is a key factor influencing lignin phenol accumulation; Nitrogen addition inhibited C-degrading enzyme activityand weakened their regulatory effect on the accumulation of lignin phenols. However, lignin phenols were more effectively protected through physical and chemical binding with soil minerals, thereby significantly reducing their bioavailability. In summary, the impact of long-term nitrogen deposition on plant-derived carbon in tropical forests exhibits significant soil layer dependency, with its effects limited to promoting lignin phenol accumulation in the surface soil layer. long term high nitrogen input has altered the regulatory pathways of plant-derived carbon accumulation in tropical evergreen broadleaf forest soils, shifting from microbial degradation processes to physicochemical protection as the dominant mechanism. This study unveils a novel mechanism for maintaining the stability of tropical forest soil carbon pools under nitrogen deposition, providing crucial theoretical insights for predicting forest soil carbon dynamics.

Key words: lignin phenol accumulation, mineral physical and chemical protectio, soil organic carbon sequestration, nitrogen deposition, tropical forest