Vertically stratified methane, nitrogen and sulphur cycling and coupling mechanisms in mangrove sediment microbiomes

生物地球化学循环 反硝化 产甲烷 环境化学 氮气循环 沉积物 甲烷厌氧氧化 变形菌纲 亚硝酸盐还原酶 生态学 厌氧氨氧化菌 生物地球化学 红树林 生物 硝酸盐 甲烷 氮气 化学 亚硝酸盐 反硝化细菌 细菌 γ蛋白杆菌 古生物学 有机化学 遗传学 16S核糖体RNA
作者
Lu Qian,Xiaoli Yu,Hang Gu,Fei Liu,Yijun Fan,Cheng Wang,Qiang He,Yun Tian,Yisheng Peng,Longfei Shu,Shanquan Wang,Zhijian Huang,Qingyun Yan,Jianguo He,Guangli Liu,Qichao Tu,Zhili He
出处
期刊:Microbiome [BioMed Central]
卷期号:11 (1) 被引量:29
标识
DOI:10.1186/s40168-023-01501-5
摘要

Abstract Background Mangrove ecosystems are considered as hot spots of biogeochemical cycling, yet the diversity, function and coupling mechanism of microbially driven biogeochemical cycling along the sediment depth of mangrove wetlands remain elusive. Here we investigated the vertical profile of methane (CH 4 ), nitrogen (N) and sulphur (S) cycling genes/pathways and their potential coupling mechanisms using metagenome sequencing approaches. Results Our results showed that the metabolic pathways involved in CH 4 , N and S cycling were mainly shaped by pH and acid volatile sulphide (AVS) along a sediment depth, and AVS was a critical electron donor impacting mangrove sediment S oxidation and denitrification. Gene families involved in S oxidation and denitrification significantly ( P < 0.05) decreased along the sediment depth and could be coupled by S-driven denitrifiers, such as Burkholderiaceae and Sulfurifustis in the surface sediment (0–15 cm). Interestingly, all S-driven denitrifier metagenome-assembled genomes (MAGs) appeared to be incomplete denitrifiers with nitrate/nitrite/nitric oxide reductases (Nar/Nir/Nor) but without nitrous oxide reductase (Nos), suggesting such sulphide-utilizing groups might be an important contributor to N 2 O production in the surface mangrove sediment. Gene families involved in methanogenesis and S reduction significantly ( P < 0.05) increased along the sediment depth. Based on both network and MAG analyses, sulphate-reducing bacteria (SRB) might develop syntrophic relationships with anaerobic CH 4 oxidizers (ANMEs) by direct electron transfer or zero-valent sulphur, which would pull forward the co-existence of methanogens and SRB in the middle and deep layer sediments. Conclusions In addition to offering a perspective on the vertical distribution of microbially driven CH 4 , N and S cycling genes/pathways, this study emphasizes the important role of S-driven denitrifiers on N 2 O emissions and various possible coupling mechanisms of ANMEs and SRB along the mangrove sediment depth. The exploration of potential coupling mechanisms provides novel insights into future synthetic microbial community construction and analysis. This study also has important implications for predicting ecosystem functions within the context of environmental and global change.
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