Abstract
Methanogenesis mediated by archaea is the main source of methane, a strong greenhouse gas, and thus is critical for understanding Earth’s climate dynamics. Recently, genes encoding diverse methanogenesis pathways have been discovered in metagenome-assembled genomes affiliated with several archaeal phyla1,2,3,4,5,6,7. However, all experimental studies on methanogens are at present restricted to cultured representatives of the Euryarchaeota. Here we show methanogenic growth by a member of the lineage Korarchaeia within the phylum Thermoproteota (TACK superphylum)5,6,7. Following enrichment cultivation of ‘Candidatus Methanodesulfokora washburnenis’ strain LCB3, we used measurements of metabolic activity and isotope tracer conversion to demonstrate methanol reduction to methane using hydrogen as an electron donor. Analysis of the archaeon’s circular genome and transcriptome revealed unique modifications in the energy conservation pathways linked to methanogenesis, including enzyme complexes involved in hydrogen and sulfur metabolism. The cultivation and characterization of this new group of archaea is critical for a deeper evaluation of the diversity, physiology and biochemistry of methanogens.
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Data availability
The 16S rRNA gene and mcrA gene amplicon data, metagenomic reads and metatranscriptomic reads are deposited at NCBI under BioProject PRJNA913929. Metagenomes and genomes are available on IMG/M (JGI) under IMG Genome IDs 3300005860 (WHS), 3300043541 (LCB058), 3300028675 (LCB003), 8012931703 (‘Ca. M. washburnensis’ strain LCB3), 8015587805 (Archaeoglobaceae archaeon LCB3), 8015589684 (Thermofilum sp. LCB3-A), 8015591669 (Thermofilum sp. LCB3-B), 8015593670 (Fervidicoccaceae archaeon LCB3), 8015596852 (Ignisphaera sp. LCB3) and 8015595177 (Desulfurococcaceae archaeon LCB3). Source data are provided with this paper.
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Acknowledgements
This study was funded through a NASA Exobiology programme award (grant no. 80NSSC19K1633). V.K. was supported in part by a grant from the NSF (grant no. MCB-1817428 to R.H.). A.K. was supported in part by a fellowship by the Montana Space Grant Consortium. A portion of this research was performed under the Facilities Integrating Collaborations for User Science programme (proposal no. 10.46936/fics.proj.2017.49972/6000002) and the Community Science Program (proposal no. 10.46936/10.25585/60008108), and used resources at the Department of the Environment (DOE) Joint Genome Institute (https://ror.org/04xm1d337), which is a DOE Office of Science User Facility operated under contract no. DE-AC02-05CH11231. We thank the US National Park Service for permitting work in YNP under permit number YELL-SCI-8010. We thank L. McKay and M. Lynes (both Montana State University) for discussions that informed field sampling, cultivation, taxonomy and manuscript preparation, S. Scheller (Aalto University) for discussing methanogen biochemistry and P. Schlegel (Montana State University) for assistance in cultivation.
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V.K., A.J.K. and R.H. designed experiments. V.K., A.J.K. and Z.J.J. conducted field work, reconstructed the metabolic potential of strain LCB3 and performed phylogenetic analysis. V.K. and A.J.K. performed cultivation and analysed gene expression data. Z.J.J. and A.J.K. processed metagenomic data and performed phylogenomic analysis. V.K. performed amplicon sequencing, BONCAT and CARD-FISH experiments. A.J.K. extracted DNA for metagenome sequencing, performed FISH, stable isotope tracing, substrate testing and transcriptomics experiments, and developed gas chromatography and mass spectrometry protocols. Z.J.J. performed whole-genome comparisons and determined environmental distributions. R.H. was responsible for funding and supervision of the project. All authors contributed to writing of the paper.
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Extended data figures and tables
Extended Data Fig. 1 Images of hot springs used as source material for cultivation.
A. Washburn Hot Springs. B. Hot spring LCB003. C. Hot spring LCB058. All three hot springs are located in Yellowstone National Park (WY, USA). All work in Yellowstone National Park was performed under research permit YELL-SCI-8010 to R.H.
Extended Data Fig. 2 Comparison of Korarchaeia genomes and MAGs.
A. Pairwise comparisons of average nucleotide (below dotted line) and amino acid (above dotted line) identities (%) of ‘Ca. Methanodesulfokora’ and ‘Ca. Korarchaeum’ genomes and Washburn Hot Spring MAGs. B. ‘Ca. M. washburnensis’ strain LCB3 genome and 16S rRNA gene read abundances in environmental metagenomes LCB003, LCB058, and WHS and in culture LCB3 at day 180 and 352.
Extended Data Fig. 3 Phylogenetic affiliation of ‘Ca. M. washburnensis’ strain LCB3.
A. Maximum likelihood phylogenomic tree of archaea based on 33 single copy marker genes. The tree was constructed with IQtree and the best-fit model LG+F+R10, from the concatenated alignment of conserved arCOGs. The ‘Ca. M. washburnensis’ strain LCB3 genome is highlighted in red. Circles indicate ultrafast bootstrap values >95. B. Maximum likelihood phylogenetic tree of 16S rRNA genes from culture LCB3. The tree was constructed with fasttree including the 16S rRNA gene from the LCB3 genome (red), 16S rRNA genes in MAGs from culture LCB3 and reference sequences. Circles indicate bootstrap support values >95.
Extended Data Fig. 4 Representative fluorescence micrographs of culture LCB3.
A. Cells visualized with DAPI (blue). B. Cells visualized by DOPE-FISH using a ‘Ca. M. washburnensis’ specific 16S rRNA-targeted oligonucleotide probe (KRmw515, red). C. Overlay of A and B. D. Cells visualized with DAPI (blue). E. Cells visualized with DAPI (blue, same field of view as in D) combined with dual CARD-FISH using the ‘Ca. M. washburnensis’ specific 16S rRNA-targeted oligonucleotide probe (KRmw515, red) and a general archaea probe (Arch915, green). Note that because of two mismatches of the Arch915 probe to the 16S rRNA of ‘Ca. M. washburnensis’ there is no overlap of signal from probes KRmw515 and Arch915. Representative micrographs from n = 3 independent samples from culture LCB3. Scale bars 5 µm.
Extended Data Fig. 5 Methane production in culture LCB3 under different experimental conditions.
A. Methane production curves for SIP incubations (shown in Fig. 1b) amended with 12C-methanol (open white circles), 13C-methanol (gray filled circles), or 13C-methanol with BES (black filled circles). Data are presented as mean values +/− standard deviation (n = 3 biological replicates). B. Methane production curves for BONCAT-FISH incubations (shown in Fig. 3c) amended with methanol and hydrogen, spiked with BES at day 15 (filled symbols, dashed line) and spiked with HPG at day 18 (filled symbols). Controls were not spiked (open symbols), representing growth under standard cultivation conditions, or were spiked with BES at day 0 (open symbols, dashed line), inhibiting methane production. Incubations were sampled for cell visualization via BONCAT-FISH after 24 h of incubation with HPG (day 19). Data are presented as mean values +/− standard deviation (n = 3 biological replicates). C. Methane produced with different substrates after 85 days of incubation. Concentrations were 10 mM for methanol (MeOH), monomethylamine (MMA), dimethylamine (DMA), trimethylamine (TMA), ethanol (EtOH), and isopropanol (Prop); 2mM for lactate (Lac); and 50% for hydrogen (H2).
Extended Data Fig. 6 Gene expression of ‘Ca. M. washburnensis’ strain LCB3 during methanogenic growth on hydrogen and methanol.
Extended Data Fig. 7 Phylogenetic classification of [NiFe]-hydrogenases in ‘Ca. M. washburnensis’ strain LCB3.
A. Maximum likelihood phylogenetic tree of group 1 [NiFe]-hydrogenases. The tree was constructed using IQtree2 with the best fit model LG+R10 and 1000 ultrafast bootstraps. Hydrogenase classes were assigned according to the HydDB. The sequence from the LCB3 genome is highlighted in red. Black circles indicate ultrafast bootstrap values >95. B. Maximum likelihood phylogenetic tree of group 4 [NiFe]-hydrogenases. The tree was constructed using IQtree2 with the best fit model LG+R10 and 1000 ultrafast bootstraps. Clades containing sequences from the LCB3 genome are highlighted in red. Black circles indicate ultrafast bootstrap values >95.
Extended Data Fig. 8 Annotation of enzyme complexes in ‘Ca. M. washburnensis’ strain LCB3.
A. Comparison of group 1 [NiFe]-hydrogenase organization and structure between ‘Ca. M. washburnensis’ strain LCB3 and other MCR-encoding archaeal lineages. Models of the enzyme arrangement in the membrane with matching colors between the models indicating conserved function. Transmembrane helix (TMH) probabilities for intermembrane subunits. Groups 1j/1k have b-type cytochrome containing subunits with five helices, while the Korarchaeia group 1g [NiFe]-hydrogenase has an NrfD-like subunit (HcaC) with ten helices and lacks b-type cytochromes. B. Annotation of the ‘Ca. M. washburnensis’ strain LCB3 HdrDE complex. Model representing the arrangement of genes in the membrane. All HdrE subunits analyzed have 5 TMHs. The HdrD subunit in the LCB3 genome has cysteine residues that are conserved in HdrD subunits from other lineages. Transmembrane helices were predicted using the TMHMM 2.0 server.
Extended Data Fig. 9 Phylogenetic tree of geranylfarnesyl diphosphate synthase homologs in archaea and bacteria.
Red clades and text correspond to homologs encoded in ‘Ca. M. washburnensis’ strain LCB3. Red star indicates the clade containing the Methanosarcina mazei homolog involved in methanophenazine biosynthesis. Circles represent ultrafast bootstrap values >95. Short-chain and long-chain designations according to Ou et al.73.
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Krukenberg, V., Kohtz, A.J., Jay, Z.J. et al. Methyl-reducing methanogenesis by a thermophilic culture of Korarchaeia. Nature 632, 1131–1136 (2024). https://doi.org/10.1038/s41586-024-07829-8
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DOI: https://doi.org/10.1038/s41586-024-07829-8