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cognitis nomina
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Authors Zhou

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Zhou, Lei


Publications
3

CitationNamesAbstract
Methanosuratincola petrocarbonis gen. nov., sp. nov., a methyl-reducing methanogen isolated from Shengli oil field, and proposal of Methanosuratincolaceae fam. nov., Methanosuratincolales ord. nov. and Methanosuratincolia classis nov. in the phylum Thermoproteota Wu et al. (2025). International Journal of Systematic and Evolutionary Microbiology 75 (7) Methanosuratincola petrocarbonis T Methanosuratincola Methanosuratincolaceae Methanosuratincolales Methanosuratincolia Ca. Methanomethylicia
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Discovery of the non‐cosmopolitan lineages in Candidatus Thermoprofundales Liu et al. (2022). Environmental Microbiology 24 (7) Ca. Thermoprofundales
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Anaerobic Degradation of Paraffins by Thermophilic Actinobacteria under Methanogenic Conditions Liu et al. (2020). Environmental Science & Technology 54 (17) “Syntrophaliphaticia”

Methanosuratincola petrocarbonis gen. nov., sp. nov., a methyl-reducing methanogen isolated from Shengli oil field, and proposal of Methanosuratincolaceae fam. nov., Methanosuratincolales ord. nov. and Methanosuratincolia classis nov. in the phylum Thermoproteota
An anaerobic, thermophilic methanogen, designated strain LWZ-6T, was isolated from the Shengli oil field, China. The cells of strain LWZ-6T were non-motile cocci, with a diameter of 0.5–1.0 µm, and formed aggregates. They reduced methanol and monomethylamine into methane, using H2 as an electron donor. Dimethylamine, trimethylamine and methanethiol, H2/CO2, formate, acetate, pyruvate, lactate and glucose were not used as energy sources. Strain LWZ-6T required yeast extract, acetate or CO2 as carbon sources. Strain LWZ-6T grew at 35–65 °C (optimum 55 °C), pH 5.0–8.0 (optimum 6.0–6.5) and 0–60 g l−1 NaCl (optimum 9 g l−1). The genome was 1.54 Mbp with a G+C content of 54.42 mol%. Strain LWZ-6T shared 83.54% 16S rRNA gene sequence identity with Infirmifilum lucidum strain 3507LTT in the class Thermoprotei. Phylogenetic analysis based on the 16S rRNA gene, along with phylogenomic analysis, indicated that strain LWZ-6T belonged to the candidate class ‘Candidatus Methanomethylicia’, which lacks cultivated representatives. Based on these findings, a new species within a new genus, Methanosuratincola petrocarbonis gen. nov., sp. nov., is proposed for LWZ-6T (=CCAM 1872T=JCM 39528T). In addition, we propose the Methanosuratincolia class. nov. for candidate class ‘Ca. Methanomethylicia’ represented by Methanosuratincolaceae fam. nov. and Methanosuratincolales ord. nov. within the phylum Thermoproteota.
Discovery of the non‐cosmopolitan lineages in Candidatus Thermoprofundales
Summary The recently proposed order Candidatus Thermoprofundales, currently containing only one family‐level lineage Marine Benthic Group‐D (MBG‐D), is distributed in global subsurface ecosystems and ecologically important, but its diversity, evolution and metabolism remain largely unknown. Here we described two novel family‐level specialized lineages in Ca . Thermoprofundales, JdFR‐43 and HyVt, which are restricted to specific biotopes (primarily in marine hydrothermal vents and occasionally in oil reservoirs and hot springs) in contrast to the cosmopolitan lineage MBG‐D. The comparative genomics revealed that the specialized lineages have streamlined genomes, higher GC contents, enriched genes associated with nucleotide biosynthesis, ribosome biogenesis and DNA repair and additional thermostable aminopeptidases, enabling them to adapt to high‐temperature habitats such as marine hydrothermal vents, deep subsurface oil reservoirs and hot springs. On the contrary, the unique metabolic traits of the cosmopolitan MBG‐D, motility, glycolysis, butanoate metabolism, secondary metabolites production and additional genes for specific peptides and carbohydrates degradation potentially enhance its response to environmental change. Substrate preference is found for most MAGs across all lineages with the ability to utilize both polysaccharides (chitin and starch) and proteinaceous substances, whereas JdFR‐43 members from oil reservoirs can only utilize proteins. These results expand the diversity of C a . Thermoprofundales significantly and further improve our understandings of the adaptations of C a . Thermoprofundales to various environments.
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