Microorganisms as bio‐filters to mitigate greenhouse gas emissions from high‐altitude permafrost revealed by nanopore‐based metagenomics

• Published in: iMeta
• Main Authors: Dang, Chenyuan, Wu, Ziqi, Zhang, Miao, Li, Xiang, Sun, Yuqin, Wu, Ren'an, Zheng, Yan, Xia, Yu
• Format: Article in Journal/Newspaper
• Language: English
• Published: Wiley 2022
• Subjects: permafrost
• Online Access: http://dx.doi.org/10.1002/imt2.24; https://onlinelibrary.wiley.com/doi/pdf/10.1002/imt2.24; https://onlinelibrary.wiley.com/doi/full-xml/10.1002/imt2.24

Abstract The distinct climatic and geographical conditions make high‐altitude permafrost on the Tibetan Plateau suffer more severe degradation than polar permafrost. However, the microbial responses associated with greenhouse gas production in thawing permafrost remain obscured. Here we applied nanopore‐based long‐read metagenomics and high‐throughput RNA‐seq to explore microbial functional activities within the freeze‐thaw cycle in the active layers of permafrost at the Qilian Mountain. A bioinformatic framework was established to facilitate phylogenetic and functional annotation of the unassembled nanopore metagenome. By deploying this strategy, 42% more genera could be detected and 58% more genes were annotated to nitrogen and methane cycle. With the aid of such enlarged resolution, we observed vigorous aerobic methane oxidation by Methylomonas , which could serve as a bio‐filter to mitigate CH 4 emissions from permafrost. Such filtering effect could be further consolidated by both on‐site gas phase measurement and incubation experiment that CO 2 was the major form of carbon released from permafrost. Despite the increased transcriptional activities of aceticlastic methanogenesis pathways in the thawed permafrost active layer, CH 4 generated during the thawing process could be effectively consumed by the microbiome. Additionally, the nitrogen metabolism in permafrost tends to be a closed cycle and active N 2 O consumption by the topsoil community was detected in the near‐surface gas phase. Our findings reveal that although the increased thawed state facilitated the heterotrophic nitrogen and methane metabolism, effective microbial methane oxidation in the active layer could serve as a bio‐filter to relieve the overall warming potentials of greenhouse gas emitted from thawed permafrost.