Aerenchyma in emergent plants and rhizospheric microbial communities promote methane fluxes in wetlands

通气组织 根际 湿地 石首鱼 微生物种群生物学 环境科学 营养物 美人蕉 微生物 植物 生态学 环境化学 生物 细菌 化学 生物化学 遗传学 淀粉
作者
Shaozhuang Guo,Songhe Zhang,Xin Lv,Hezhou Chen,Jie Chen,Junfeng Gao,Wenming Zhang
出处
期刊:Limnology and Oceanography [Wiley]
卷期号:69 (9): 2109-2122 被引量:12
标识
DOI:10.1002/lno.12653
摘要

Abstract Wetlands are the largest natural source of CH 4 globally, yet our understanding of how environmental parameters and microorganisms affect the production and emission of CH 4 in emergent plant–sediment systems remains limited. In this study, CH 4 fluxes were investigated in a wetland with Canna indica for 42 d, as well as nutrients and microbial community. It was found that the chimney effect formed by aerenchyma in roots, stems, and leaves of C. indica promoted the emission and oxidation of CH 4 in the wetland and reduced the CH 4 concentration in sediments. Canna indica reduced the nutrient release from surface sediments into the overlying water. Pearson correlation analysis showed that temperature, pH, and oxidation–reduction potential were the main influencing factors for CH 4 production and oxidation in the wetland. Canna indica inhibited the diversity of archaeal community but promoted the diversity of bacterial community in the rhizosphere. Stochastic processes had a greater impact on bacterial and archaeal succession trajectories in wetland sediments. Network analysis showed that C. indica promoted interactions among bacteria and archaea that enhanced their ability to resist environmental interference. The well‐developed aerenchyma of C. indica provided an important passage for the transport of CH 4 from sediments to the atmosphere and shaped the microbial community structure in the rhizosphere. Meanwhile, CH 4 emissions were also constrained by several variables, such as temperature and physiological adaptation in the long term. Thus, it is necessary to plant emergent plants in areas with low CH 4 emissions and optimize plant configuration in the context of global warming.
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