鸟岛湿地土壤产甲烷菌群落对不同降水梯度的响应OA北大核心CSTPCD
Response of soil methanogenic bacterial communities to different precipitation gradients in the Bird Island Wetland
产甲烷菌在湿地CH4 排放过程中发挥着重要作用,降水格局的改变已经并将持续影响湿地生态系统的结构与功能,进而对湿地CH4 排放过程产生影响.本研究以青海湖鸟岛湖滨湿地为研究对象,设置 5 个降水梯度处理,并利用mcrA扩增子测序技术对土壤产甲烷菌进行检测,探究鸟岛土壤产甲烷菌群落特征对不同降水梯度的响应.结果表明,鸟岛土壤产甲烷菌群落的优势菌目为甲烷微菌目(Methanomicrobiales)、甲烷八叠球菌目(Methanosarcinales)和甲烷杆菌目(Methanobacteriales).FAPROTAX功能预测显示土壤中氢营养型产甲烷菌占优势,由此推测H2/CO2 还原为鸟岛土壤CH4 产生的主要途径.LEfSe分析表明,5 个降水梯度共存在 31 个差异菌群,以增雨 50%处理下差异菌群数量最多,从目水平到种水平共有 10 个差异菌群.整体而言,鸟岛土壤产甲烷菌的群落多样性较为稳定,而群落结构对降水变化的响应较为敏感,部分菌群的相对丰度发生了显著变化(P<0.05).研究结果可为预测降水变化对鸟岛湿地土壤碳循环的影响提供一定的参考依据.
Methanogenic bacteria play an important role in the process of wetland CH4 emission.Changes in precipitation patterns have and will continue to affect the structure and function of wetland ecosystems,affecting the process of wetland CH4 emission.In this study,the lakeside wetland of Bird Island in Qinghai Lake was taken as the research object,five precipitation gradients were set up,and the mcrA Amplifier sequencing technique was used to detect soil methanogenic bacteria in order to explore changes in their community characteristics in response to to different precipitation gradients.The results showed that the dominant methanogenic bacteria in the soil of Bird Island were Methanomicrobiales,Methanosarcinales,and Methanobacteriales.The prediction of the FAPROTAX function showed that hydrogen-trophic methanogens were dominant in soil,which inferred that H2/CO2 reduced to the main pathway of CH4 production in Bird Island soil.LEfSe analysis showed that five precipitation gradients coexisted with 31 different microflora,and the number of differential microflora was the most under the treatment of 50%precipitation,with 10 different microflora from the order to species level.Overall,the community diversity of methanogens in Bird Island soil was stable,but the community structure was sensitive to changes in precipitation,and the relative abundance of some microflora changed significantly(P<0.05).The results can provide some reference for predicting the influence of precipitation change on soil carbon cycle in BirdIsland wetland.
王霞;陈克龙;杜岩功;章妮;车子涵;暴涵;王恒生
青海师范大学生命科学学院,青海西宁 810008||青海省自然地理与环境过程重点实验室,青海西宁 810008||青海师范大学青藏高原地表过程与生态保育教育部重点实验室,青海西宁 810008||青海青海湖湿地生态系统国家定位观测研究站,青海西宁 810008青海省自然地理与环境过程重点实验室,青海西宁 810008||青海师范大学青藏高原地表过程与生态保育教育部重点实验室,青海西宁 810008||青海青海湖湿地生态系统国家定位观测研究站,青海西宁 810008||高原科学与可持续发展研究院,青海西宁 810008中国科学院西北高原生物研究所,青海西宁 810000青海省自然地理与环境过程重点实验室,青海西宁 810008||青海师范大学青藏高原地表过程与生态保育教育部重点实验室,青海西宁 810008||青海青海湖湿地生态系统国家定位观测研究站,青海西宁 810008合肥师范学院生命科学学院,安徽合肥 230000
高寒湿地碳循环气候变化产甲烷菌微生物群落mcrA青藏高原
alpine wetlandscarbon cycleclimate changemethanogensmicrobial communitymcrAQinghai-Tibet Plateau
《草业科学》 2024 (002)
284-296 / 13
青海湖入湖河流原位净化及河口湿地生态治理技术集成与示范项目(2022-QY-204);水位上升下青海湖湖滨带生态系统变化及其对碳循环影响研究项目(2023-ZJ-905T)
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