J Plant Ecol ›› Advance articles     DOI:10.1093/jpe/rtag173

• Research Article •     Next Articles

Porewater iron dynamics drive microbial metabolic stratification and carbon transformation in a subtropical sphagnum multifibrosum peatland

Tu Feng1, Qing Zhao2, Ying Shao2, Zechao Li3, Wei Zhang3, Ya Zhang3, Xiaolong Bai4, Bin He4, Wangjun Li4, Shun Zou4, Fei, Li5, Zhongli Chen2*   

  1. 1School of Science, Kaili University, Kaili, 556011, China
    2Key Laboratory of the Three Gorges Reservoir Region’s Eco-Environment, Ministry of Education, Chongqing University, 400045 Chongqing, China
    3 Dapingjing National Wetland Park, Nayong, 553300, Guizhou, China
    4 College of Ecological Engineering, Guizhou University of Engineering Science, Bijie, 551700, China
    5 Chongqing Ecological and Environment Monipitoring Center, 4011147 Chongqing, China
    Tu Feng and Qing Zhao contributed equally to this work.
    * Corresponding author: Dr. Zhongli Chen, College of Environment and Ecology, Chongqing University, 400045 Chongqing, China. E-mail: zhongli.chen@cqu.edu.cn
  • Received:2025-11-18 Accepted:2026-07-09 Published:2026-07-29
  • Supported by:
    This work was supported by the Fundamental Research Funds for the Central Universities (No: 2023CDJKYJH038 and 2024CDJYDYL012) and High- level Innovative Talents Project in Guizhou Province (No. [2016]4).

Abstract: Peatlands are the densest terrestrial carbon stocks, and iron is a key redox-active element that strongly influences microbial metabolism and carbon preservation. However, the role of microbial metabolic stratification and its coupling with geochemical factors, such as iron in governing carbon stability remain poorly understood. Here, we employed a metagenomic approach to investigate the vertical distribution of microbial communities and their functional potential in a subtropical Sphagnum multifibrosum peatland in Southwest China. By integrating genetic data with porewater geochemistry across a depth profile (0-60 cm), we identified a coherent tripartite microbial metabolic pattern. The aerobic surface layer (0–20 cm) was dominated by Pseudomonadota harbouring genes for labile carbon degradation and nitrogen fixation. The microaerophilic middle layer (20–40 cm), enriched with Acidobacteriota, was a hotspot for denitrification (narG, nirK) and sulfate reduction (dsrA). The anaerobic deep layer (40–60 cm) was characterized by Euryarchaeota and genes for methanogenesis (mcrA) and sulfur disproportionation (TST). Porewater Fe2+ concentrations were exceptionally high and strongly correlated with this stratification. Iron-reducing bacteria (Geobacter) linked carbon mineralization to the potential for re-stabilization via iron oxide formation. Plant community composition, specifically the shift from Sphagnum- to vascular plant-dominance, was a primary determinant of carbon quality and the resulting microbial functional network. Our findings provide a genomic blueprint for carbon transformation in peatlands, in which a tightly coupled plant-iron-microbe nexus shapes metabolic stratification and carbon sequestration potential. This integrative framework generates testable predictions about the stability of carbon stocks under disturbances such as vascular plant encroachment.

This study reveals that porewater iron dynamics are a key driver of vertical microbial metabolic stratification and carbon transformation in a subtropical Sphagnum multifibrosum peatland. By integrating metagenomics and geochemistry, we demonstrate that plant-iron-microbe interactions regulate carbon degradation, stabilization, and the potential resilience of peatland carbon stocks under vegetation shifts.

Key words: Sphagnum multifibrosum Peatland, Vegetation and microbial patterns, Metagenomics analysis, Biochemical Process, Ecological functions