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Lynes MM, Jay ZJ, Kohtz AJ, Hatzenpichler R. Methylotrophic methanogenesis in the Archaeoglobi revealed by cultivation of Ca. Methanoglobus hypatiae from a Yellowstone hot spring. ISME J 2024; 18:wrae026. [PMID: 38452205 PMCID: PMC10945360 DOI: 10.1093/ismejo/wrae026] [Citation(s) in RCA: 0] [Impact Index Per Article: 0] [Reference Citation Analysis] [What about the content of this article? (0)] [Affiliation(s)] [Abstract] [Key Words] [MESH Headings] [Grants] [Track Full Text] [Subscribe] [Scholar Register] [Received: 11/13/2023] [Revised: 01/09/2024] [Accepted: 02/08/2024] [Indexed: 03/09/2024]
Abstract
Over the past decade, environmental metagenomics and polymerase chain reaction-based marker gene surveys have revealed that several lineages beyond just a few well-established groups within the Euryarchaeota superphylum harbor the genetic potential for methanogenesis. One of these groups are the Archaeoglobi, a class of thermophilic Euryarchaeota that have long been considered to live non-methanogenic lifestyles. Here, we enriched Candidatus Methanoglobus hypatiae, a methanogen affiliated with the family Archaeoglobaceae, from a hot spring in Yellowstone National Park. The enrichment is sediment-free, grows at 64-70°C and a pH of 7.8, and produces methane from mono-, di-, and tri-methylamine. Ca. M. hypatiae is represented by a 1.62 Mb metagenome-assembled genome with an estimated completeness of 100% and accounts for up to 67% of cells in the culture according to fluorescence in situ hybridization. Via genome-resolved metatranscriptomics and stable isotope tracing, we demonstrate that Ca. M. hypatiae expresses methylotrophic methanogenesis and energy-conserving pathways for reducing monomethylamine to methane. The detection of Archaeoglobi populations related to Ca. M. hypatiae in 36 geochemically diverse geothermal sites within Yellowstone National Park, as revealed through the examination of previously published gene amplicon datasets, implies a previously underestimated contribution to anaerobic carbon cycling in extreme ecosystems.
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Affiliation(s)
- Mackenzie M Lynes
- Department of Chemistry and Biochemistry, Center for Biofilm Engineering, Thermal Biology Institute, Montana State University, Bozeman, MT 59717, United States
| | - Zackary J Jay
- Department of Chemistry and Biochemistry, Center for Biofilm Engineering, Thermal Biology Institute, Montana State University, Bozeman, MT 59717, United States
| | - Anthony J Kohtz
- Department of Chemistry and Biochemistry, Center for Biofilm Engineering, Thermal Biology Institute, Montana State University, Bozeman, MT 59717, United States
| | - Roland Hatzenpichler
- Department of Chemistry and Biochemistry, Center for Biofilm Engineering, Thermal Biology Institute, Montana State University, Bozeman, MT 59717, United States
- Department of Microbiology and Cell Biology, Montana State University, Bozeman, MT 59717, United States
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Wood C, Bruinink A, Trembath-Reichert E, Wilhelm MB, Vidal C, Balaban E, McKay CP, Swan R, Swan B, Goordial J. Active microbiota persist in dry permafrost and active layer from Elephant Head, Antarctica. ISME Commun 2024; 4:ycad002. [PMID: 38304082 PMCID: PMC10833075 DOI: 10.1093/ismeco/ycad002] [Citation(s) in RCA: 0] [Impact Index Per Article: 0] [Reference Citation Analysis] [What about the content of this article? (0)] [Affiliation(s)] [Abstract] [Key Words] [Grants] [Track Full Text] [Figures] [Subscribe] [Scholar Register] [Received: 09/24/2023] [Revised: 10/03/2023] [Accepted: 11/07/2023] [Indexed: 02/03/2024]
Abstract
Dry permafrost is a challenging environment for microbial life due to cold, dry, and often oligotrophic conditions. In 2016, Elephant Head, Antarctica, was confirmed as the second site on Earth to contain dry permafrost. It is geographically distinct from the McMurdo Dry Valleys where dry permafrost has been studied previously. Here, we present the first study of the microbial activity, diversity, and functional potential of Elephant Head dry permafrost. Microbial activity was measured using radiorespiration assays with radiolabeled acetate as a carbon source at 5, 0, and -5°C. Low, but detectable, rates of microbial activity were measured in some samples at 0 and -5°C. This is distinct from previous studies of McMurdo Dry Valley dry permafrost which concluded that dry permafrost represents a cold-arid limit to life on the planet. The isolation of cold-adapted organisms from these soils, including one capable of subzero growth, further supports that the Elephant Head dry active layer and dry permafrost harbor viable microbial life, which may be active in situ. Metagenomic, 16S rRNA gene, and internal transcribed spacer and amplicon sequencing identified similar microbial communities to other Antarctic and cold environments. The Elephant Head microbial community appears to be adapted for survival in cold, dry, and oligotrophic conditions based on the presence of cold adaptation and stress response genes in the metagenomes. Together, our results show that dry permafrost environments do not exclude active microbial life at subzero temperatures, suggesting that the cold, dry soils of Mars may also not be as inhospitable as previously thought.
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Affiliation(s)
- Claudia Wood
- School of Environmental Sciences, University of Guelph, 50 Stone Rd E, Guelph, Ontario N1G 2W1, Canada
| | - Alyssa Bruinink
- School of Environmental Sciences, University of Guelph, 50 Stone Rd E, Guelph, Ontario N1G 2W1, Canada
| | - Elizabeth Trembath-Reichert
- School of Earth and Space Exploration, Arizona State University, 781 Terrace Mall, Tempe, AZ 85287, United States
| | - Mary Beth Wilhelm
- Space Science & Astrobiology Division, NASA Ames Research Center, Moffett Field, CA 94035, United States
| | - Chanel Vidal
- School of Earth and Space Exploration, Arizona State University, 781 Terrace Mall, Tempe, AZ 85287, United States
| | - Edward Balaban
- Space Science & Astrobiology Division, NASA Ames Research Center, Moffett Field, CA 94035, United States
| | - Christopher P McKay
- Space Science & Astrobiology Division, NASA Ames Research Center, Moffett Field, CA 94035, United States
| | - Robert Swan
- 2041 Foundation, 130 Wescott Ct, Auburn, CA 95603, United States
| | - Barney Swan
- 2041 Foundation, 130 Wescott Ct, Auburn, CA 95603, United States
| | - Jackie Goordial
- School of Environmental Sciences, University of Guelph, 50 Stone Rd E, Guelph, Ontario N1G 2W1, Canada
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Zhang F, Romaniello SJ, Algeo TJ, Lau KV, Clapham ME, Richoz S, Herrmann AD, Smith H, Horacek M, Anbar AD. Multiple episodes of extensive marine anoxia linked to global warming and continental weathering following the latest Permian mass extinction. Sci Adv 2018; 4:e1602921. [PMID: 29651454 PMCID: PMC5895439 DOI: 10.1126/sciadv.1602921] [Citation(s) in RCA: 7] [Impact Index Per Article: 1.2] [Reference Citation Analysis] [What about the content of this article? (0)] [Affiliation(s)] [Abstract] [Grants] [Track Full Text] [Subscribe] [Scholar Register] [Received: 11/22/2016] [Accepted: 02/26/2018] [Indexed: 05/07/2023]
Abstract
Explaining the ~5-million-year delay in marine biotic recovery following the latest Permian mass extinction, the largest biotic crisis of the Phanerozoic, is a fundamental challenge for both geological and biological sciences. Ocean redox perturbations may have played a critical role in this delayed recovery. However, the lack of quantitative constraints on the details of Early Triassic oceanic anoxia (for example, time, duration, and extent) leaves the links between oceanic conditions and the delayed biotic recovery ambiguous. We report high-resolution U-isotope (δ238U) data from carbonates of the uppermost Permian to lowermost Middle Triassic Zal section (Iran) to characterize the timing and global extent of ocean redox variation during the Early Triassic. Our δ238U record reveals multiple negative shifts during the Early Triassic. Isotope mass-balance modeling suggests that the global area of anoxic seafloor expanded substantially in the Early Triassic, peaking during the latest Permian to mid-Griesbachian, the late Griesbachian to mid-Dienerian, the Smithian-Spathian transition, and the Early/Middle Triassic transition. Comparisons of the U-, C-, and Sr-isotope records with a modeled seawater PO43- concentration curve for the Early Triassic suggest that elevated marine productivity and enhanced oceanic stratification were likely the immediate causes of expanded oceanic anoxia. The patterns of redox variation documented by the U-isotope record show a good first-order correspondence to peaks in ammonoid extinctions during the Early Triassic. Our results indicate that multiple oscillations in oceanic anoxia modulated the recovery of marine ecosystems following the latest Permian mass extinction.
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Affiliation(s)
- Feifei Zhang
- School of Earth and Space Exploration, Arizona State University, Tempe, AZ 85287–6004, USA
- Corresponding author.
| | - Stephen J. Romaniello
- School of Earth and Space Exploration, Arizona State University, Tempe, AZ 85287–6004, USA
| | - Thomas J. Algeo
- Department of Geology, University of Cincinnati, Cincinnati, OH 45221–0013, USA
- State Key Laboratories of Biogeology and Environmental Geology and Geological Processes and Mineral Resources, China University of Geosciences, Wuhan 430074, China
| | - Kimberly V. Lau
- Deparment of Earth Sciences, University of California, Riverside, Riverside, CA 92521, USA
| | - Matthew E. Clapham
- Department of Earth and Planetary Sciences, University of California, Santa Cruz, Santa Cruz, CA 95064, USA
| | - Sylvain Richoz
- Institute of Earth Sciences, NAWI Graz, University of Graz, Heinrichstraße 26, 8010 Graz, Austria
- Department of Geology, Lund University, Sölvegatan 12, 22362 Lund, Sweden
| | - Achim D. Herrmann
- Department of Geology and Geophysics, Louisiana State University, Baton Rouge, LA 70803, USA
| | - Harrison Smith
- School of Earth and Space Exploration, Arizona State University, Tempe, AZ 85287–6004, USA
| | - Micha Horacek
- Institute of Earth Sciences, NAWI Graz, University of Graz, Heinrichstraße 26, 8010 Graz, Austria
- Lehr- und Forschungszentrum Francisco-Josephinum, 3250 Wieselburg, Austria
- Department of Lithospheric Research, Vienna University, Althanstr. 14, 1090 Vienna, Austria
| | - Ariel D. Anbar
- School of Earth and Space Exploration, Arizona State University, Tempe, AZ 85287–6004, USA
- School of Molecular Sciences, Arizona State University, Tempe, AZ, 85287, USA
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