Luo Chai, Bai Shuang, Sun Jing, Wang Fushun, Ma Shuwen, Xu Tian, Ma Jing, Chen Xue-Ping
Department of Environmental Science and Engineering, School of Environmental and Chemical Engineering, Shanghai University, 150#, 99 Shangda Road, Shanghai, 200444, China.
Department of Ocean Science, The Hong Kong University of Science and Technology, Hong Kong, China.
Curr Microbiol. 2024 Dec 24;82(1):55. doi: 10.1007/s00284-024-04038-4.
Freshwater ecosystem is a significant natural source of CH emission in the atmosphere. To fully understand the dynamics of methane emissions in reservoirs, it is essential to grasp the temporal and vertical distribution patterns, as well as the factors that influence the methanogenic bacterial communities within the sediments. This study investigates the methane dynamics, carbon isotope fractionation (δCH), and abundance of functional microorganisms along the geochemical gradient in the in situ sedimentary column of Hongfeng Reservoir (China). Notably, the methane concentration in sediment in summer ranged in 15.39-127.22 µmol/L, which is twice as high as wintertime concentrations in the surface layer near the sediment-water interface (0-10 cm depth). Illumina sequencing of the sediments identified 11 genera affiliated with methanogenic archaea, with dominant genus Methanosaeta reaching a relative abundance of 34.95% in summer. The total carbon (TOC) content in sedimentary columns in different seasons is positively correlated with Methanosarcina (P < 0.05). In addition, seasonal discrepancies are observed in the sediment profiles for total nitrogen (TN), sulfate (SO), and ferrous iron (Fe) concentrations. The concentration of total nitrogen (TN) is higher in summer than in winter. In summer, sulfate accumulates in the middle layer of the sedimentary column, while in winter, the maximum concentration of sulfate in the surface layer reaches 0.65 mmol/L. These geochemical gradients drive the biological transformation of nitrogen, sulfur, and iron, may also be linked to the consumption of methane. Thus, it is established that the temporal and spatial dynamics of methanogenic communities in sediments significantly influence the fluctuations in methane release fluxes within reservoirs, highlighting the necessity to account for seasonal biological variations when assessing greenhouse gas emissions from reservoirs.
淡水生态系统是大气中CH排放的重要自然来源。为了全面了解水库中甲烷排放的动态,必须掌握其时间和垂直分布模式,以及影响沉积物中产甲烷细菌群落的因素。本研究调查了中国红枫水库原位沉积柱中沿地球化学梯度的甲烷动态、碳同位素分馏(δCH)和功能微生物丰度。值得注意的是,夏季沉积物中的甲烷浓度在15.39 - 127.22 µmol/L范围内,是沉积物 - 水界面附近表层(0 - 10 cm深度)冬季浓度的两倍。对沉积物进行的Illumina测序鉴定出11个与产甲烷古菌相关的属,其中优势属甲烷八叠球菌在夏季的相对丰度达到34.95%。不同季节沉积柱中的总碳(TOC)含量与甲烷八叠球菌呈正相关(P < 0.05)。此外,在沉积物剖面中观察到总氮(TN)、硫酸盐(SO)和亚铁(Fe)浓度的季节性差异。总氮(TN)浓度夏季高于冬季。夏季,硫酸盐在沉积柱中层积累,而冬季表层硫酸盐的最大浓度达到0.65 mmol/L。这些地球化学梯度驱动了氮、硫和铁的生物转化,也可能与甲烷的消耗有关。因此,可以确定沉积物中产甲烷群落的时空动态显著影响水库内甲烷释放通量的波动,这突出了在评估水库温室气体排放时考虑季节性生物变化的必要性。