J Plant Ecol ›› Advance articles     DOI:10.1093/jpe/rtag136

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Soil carbon sequestration in mangrove restoration: the role of flooding duration and stand type

Kai Shu1,2, Xue Gao1,2, Mengying Liu1,2, Lei Zhao1,2,3*   

  1. 1 Sanya Institute of China Agricultural University, Sanya, Hainan 572025, China;
    2 Beijing Key Laboratory of Biodiversity and Organic Farming, College of Resources and Environmental Sciences, China Agricultural University, Beijing 100193, China;
    3 State Key Laboratory of Nutrient Use and Management, Beijing 100193, China
    *Corresponding author: Lei Zhao (lei.zhao@cau.edu.cn)
  • Received:2026-02-19 Revised:2026-04-22 Accepted:2026-02-19 Published:2026-06-08
  • Supported by:
    This study was supported by the Hainan Provincial Joint Project of Sanya Yazhou Bay Science and Technology City (No. 2021JJLH0005), the National Natural Science Foundation of China (32471558), the National Key Research and Development Program of China (No. 2021YFD1900903 and 2023YFD1902703), and the 2115 Talent Development Program of China Agricultural University (No. 2018096).

红树林修复的土壤碳固存:淹水时长及林分类型的作用

Abstract: Flooding duration and vegetation structure are key regulators of soil organic carbon (SOC) dynamics in mangrove ecosystems, yet their interactive effects and underlying mechanisms remain poorly understood. Here, we investigated how flooding duration and stand type jointly influence SOC content, molecular composition, and microbial community structure in mangrove soils. Our results show that flooding duration and stand type exert significant and interactive effects on SOC dynamics rather than acting independently. Flooding duration primarily constrained organic matter decomposition by regulating soil redox conditions, whereas stand type controlled carbon inputs through differences in litter quantity and quality. Microbial community shifts mediated the responses and were associated with changes in SOC molecular characteristics, indicating coupled controls on carbon stabilization. By integrating SOC quantity, molecular composition, and microbial mediation, this study provides a mechanistic framework for understanding SOC stabilization in flooded forest soils. Our findings highlight that effective mangrove restoration and blue carbon management should consider the combined and interactive influences of hydrological regimes and vegetation structure under changing coastal environments.

Key words: mangrove restoration, soil organic carbon, flooding duration, microbial community, carbon sequestration

摘要:
淹水持续时间和植被结构是调控红树林生态系统土壤有机碳(SOC)动态的关键因素,但二者的交互作用及其潜在机制仍缺乏深入认识。本研究探讨了淹水持续时间与林分类型如何共同影响红树林土壤中的SOC含量、分子组成以及微生物群落结构。结果表明,淹水持续时间与林分类型对SOC动态具有显著且相互作用的影响,而非彼此独立发挥作用。淹水持续时间主要通过调控土壤氧化还原条件来限制有机质分解过程,而林分类型则通过凋落物数量与质量的差异控制碳输入。微生物群落结构的变化介导了这些响应过程并与SOC分子特征的改变密切相关,表明碳稳定化受到协同调控。通过整合SOC含量、分子组成和微生物介导机制,本研究构建了一个理解淹水林地土壤中SOC稳定化的机制框架研究结果强调,在不断变化的沿海环境背景下,开展有效的红树林恢复与“蓝碳”管理时,应综合考虑水文格局与植被结构的联合作用及其交互影响。

关键词: 红树林修复, 土壤有机碳, 淹水时长, 微生物群落, 碳固存