AI Article Synopsis

  • * Sediment samples from 18 reservoirs were analyzed using advanced sequencing techniques, revealing that hydrogenotrophic methanogenesis is the primary methane production pathway, with certain methanogen genera being predominant.
  • * The study found notable seasonal and spatial variations in the diversity of methanogenic communities, influenced by factors like temperature and organic content, highlighting the importance of specific genera in stabilizing these microbial networks.

Article 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.

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http://www.ncbi.nlm.nih.gov/pmc/articles/PMC11351834PMC
http://dx.doi.org/10.3390/biology13080615DOI Listing

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