ArticleFrontiers in microbiology2022
Biogeographic distributions of microbial communities associated with anaerobic methane oxidation in the surface sediments of deep-sea cold seeps in the South China Sea.
Article in Frontiers in microbiology, 2022. The graph could read no effect estimate from its abstract, so it casts no vote on the map. Cited by 6 papers.
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Who cites it
6 citing papers in PubMed, 12 citations in OpenAlex.
- Syntrophic interactions driving anaerobic methane oxidation in deep-sea cold seeps revealed by DNA-SIP.iScience · 2026Article
- Methane filtration and metabolic cooperation of microbial communities in cold seep water columns from South China Sea.Communications biology · 2025Article
- Cold seeps are potential hotspots of deep-sea nitrogen loss driven by microorganisms across 21 phyla.Nature communications · 2025Article
- Lignin Unlocks Stealth Carbon Sinks in Cold Seeps via Microbial Enzymatic Gatekeeping.Research (Washington, D.C.) · 2025Article
- Heterogeneity of the horizontal environment drives community assemblages and species coexistence of prokaryotic communities in cold seep sediments.Frontiers in microbiology · 2025Article
- The diversification and potential function of microbiome in sediment-water interface of methane seeps in South China Sea.Frontiers in microbiology · 2024Article
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Authors and funding
4 authors at 1 institution in 1 country.
Funding
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Abstract
Cold seeps are oasis for the microbes in the deep-sea ecosystems, and various cold seeps are located along the northern slope of the South China Sea (SCS). However, by far most microbial ecological studies were limited to specific cold seep in the SCS, and lack of comparison between different regions. Here, the surface sediments (0-4 cm) from the Site F/Haima cold seeps and the Xisha trough in the SCS were used to elucidate the biogeography of microbial communities, with particular interest in the typical functional groups involved in the anaerobic oxidation of methane (AOM) process. Distinct microbial clusters corresponding to the three sampling regions were formed, and significantly higher gene abundance of functional groups were present in the cold seeps than the trough. This biogeographical distribution could be explained by the geochemical characteristics of sediments, such as total nitrogen (TN), total phosphorus (TP), nitrate (NO
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