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青藏高原东北部油藏沉积物中产甲烷菌群特征及其影响因素

Methanogenic Community Characteristics and Its Influencing Factors in Reservoir Sediments on the Northeastern Qinghai Plateau.

作者信息

Liu Zebi, Mao Xufeng, Wu Yi, Xia Liang, Yu Hongyan, Tang Wenjia, Qi Yanhong, Zhang Ziping, Xiao Feng, Ji Haichuan

机构信息

Key Laboratory of Qinghai Province Physical Geography and Environmental Process, Qinghai Normal University, Xining 810008, China.

Key Laboratory of Tibetan Plateau Land Surface Processes and Ecological Conservation (Ministry of Education), Qinghai Normal University, Xining 810008, China.

出版信息

Biology (Basel). 2024 Aug 14;13(8):615. doi: 10.3390/biology13080615.

Abstract

Reservoirs are a hotspot for methane emissions, a potent greenhouse gas. However, the microbial basis for methane production in the Qinghai Plateau reservoirs remains unclear. To explore the characteristics of methanogenic communities in reservoir sediments on the northeastern Qinghai Plateau, sediment samples were collected from 18 reservoirs in the Yellow River basin during May 2023 (dry season) and August 2023 (wet season). High-throughput sequencing technology was employed to analyze the community composition, diversity, and co-occurrence network of methanogens. Furthermore, FAPROTAX and Mantel analysis were used to assess the metabolic functions of methanogens and their influencing factors. The results showed that (1) the predominant genera of methanogens were (28.87%) and (21.67%). Hydrogenotrophic methanogenesis was the main pathway in the sediments. (2) Significant spatiotemporal differences were observed in the diversity of methanogenic communities ( < 0.05). The composition and diversity of these communities were found to be significantly influenced by temperature, pH, altitude, organic carbon, and total nitrogen ( < 0.05). (3) , , and play crucial roles in maintaining the stability of methanogenic community networks. The co-occurrence network nodes are predominantly positively correlated (99.82%). These results provide data for further studies on carbon cycling in the Qinghai Plateau reservoirs.

摘要

水库是甲烷排放的热点区域,甲烷是一种强效温室气体。然而,青藏高原水库甲烷产生的微生物基础仍不清楚。为了探究青藏高原东北部水库沉积物中产甲烷群落的特征,于2023年5月(旱季)和2023年8月(雨季)从黄河流域的18个水库采集了沉积物样本。采用高通量测序技术分析产甲烷菌的群落组成、多样性和共现网络。此外,还利用FAPROTAX和Mantel分析来评估产甲烷菌的代谢功能及其影响因素。结果表明:(1)产甲烷菌的优势属为(28.87%)和(21.67%)。氢营养型产甲烷作用是沉积物中的主要途径。(2)产甲烷群落的多样性存在显著的时空差异(<0.05)。发现这些群落的组成和多样性受温度、pH值、海拔、有机碳和总氮的显著影响(<0.05)。(3)、和在维持产甲烷群落网络的稳定性方面发挥着关键作用。共现网络节点主要呈正相关(99.82%)。这些结果为进一步研究青藏高原水库的碳循环提供了数据。

https://cdn.ncbi.nlm.nih.gov/pmc/blobs/bc37/11351834/876119c50760/biology-13-00615-g001.jpg

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