Microbial methane production from calcium carbonate at moderately alkaline pH

Abstract Carbonate minerals are considered a metastable carbon reservoir under alkaline conditions. Here we demonstrate calcium carbonate as a sole inorganic carbon source at moderately alkaline pH for a methanogenic microbial community enriched from alkaline, saline wetland soil. In reactors amende...

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Main Authors: Nicole A. Fiore, Anthony J. Kohtz, Daniel N. Miller, Sanjay Antony-Babu, Donald Pan, Caitlin Lahey, Xi Huang, Yongfeng Lu, Nicole R. Buan, Karrie A. Weber
Format: Article
Language:English
Published: Nature Portfolio 2025-02-01
Series:Communications Earth & Environment
Online Access:https://doi.org/10.1038/s43247-025-02057-y
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author Nicole A. Fiore
Anthony J. Kohtz
Daniel N. Miller
Sanjay Antony-Babu
Donald Pan
Caitlin Lahey
Xi Huang
Yongfeng Lu
Nicole R. Buan
Karrie A. Weber
author_facet Nicole A. Fiore
Anthony J. Kohtz
Daniel N. Miller
Sanjay Antony-Babu
Donald Pan
Caitlin Lahey
Xi Huang
Yongfeng Lu
Nicole R. Buan
Karrie A. Weber
author_sort Nicole A. Fiore
collection DOAJ
description Abstract Carbonate minerals are considered a metastable carbon reservoir under alkaline conditions. Here we demonstrate calcium carbonate as a sole inorganic carbon source at moderately alkaline pH for a methanogenic microbial community enriched from alkaline, saline wetland soil. In reactors amended with calcium carbonate as the sole source of inorganic carbon, concentrations of methane and aqueous calcium increased concurrent with headspace hydrogen depletion. Cells were observed in association with the carbonate mineral matrix via coherent anti-Stokes Raman scattering and two-photon excitation fluorescence microscopy. Genome-resolved metagenomics of the enrichment community confirmed the presence of a methanogen (Methanobacterium sp.) with the metabolic potential for hydrogenotrophic methanogenesis in addition to five bacterial community members. These results demonstrate that carbonate minerals can serve as an inorganic carbon source for hydrogenotrophic methanogenesis, leading to mineral dissolution under stable alkaline conditions. As such, hydrogenotrophic methanogens may impact carbon biogeochemistry and carbonate mineral stability in environmental systems.
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spelling doaj-art-d143f0f576df46c1bfd70191c4eea8022025-02-09T12:56:05ZengNature PortfolioCommunications Earth & Environment2662-44352025-02-016111310.1038/s43247-025-02057-yMicrobial methane production from calcium carbonate at moderately alkaline pHNicole A. Fiore0Anthony J. Kohtz1Daniel N. Miller2Sanjay Antony-Babu3Donald Pan4Caitlin Lahey5Xi Huang6Yongfeng Lu7Nicole R. Buan8Karrie A. Weber9School of Biological Sciences, University of Nebraska–LincolnSchool of Biological Sciences, University of Nebraska–LincolnAgroecosystem Management Research Unit, Agricultural Research Service, United States Department of AgricultureSchool of Biological Sciences, University of Nebraska–LincolnSchool of Biological Sciences, University of Nebraska–LincolnSchool of Biological Sciences, University of Nebraska–LincolnDepartment of Electrical and Computer Engineering, University of Nebraska–LincolnDepartment of Electrical and Computer Engineering, University of Nebraska–LincolnDepartment of Biochemistry, University of Nebraska–LincolnSchool of Biological Sciences, University of Nebraska–LincolnAbstract Carbonate minerals are considered a metastable carbon reservoir under alkaline conditions. Here we demonstrate calcium carbonate as a sole inorganic carbon source at moderately alkaline pH for a methanogenic microbial community enriched from alkaline, saline wetland soil. In reactors amended with calcium carbonate as the sole source of inorganic carbon, concentrations of methane and aqueous calcium increased concurrent with headspace hydrogen depletion. Cells were observed in association with the carbonate mineral matrix via coherent anti-Stokes Raman scattering and two-photon excitation fluorescence microscopy. Genome-resolved metagenomics of the enrichment community confirmed the presence of a methanogen (Methanobacterium sp.) with the metabolic potential for hydrogenotrophic methanogenesis in addition to five bacterial community members. These results demonstrate that carbonate minerals can serve as an inorganic carbon source for hydrogenotrophic methanogenesis, leading to mineral dissolution under stable alkaline conditions. As such, hydrogenotrophic methanogens may impact carbon biogeochemistry and carbonate mineral stability in environmental systems.https://doi.org/10.1038/s43247-025-02057-y
spellingShingle Nicole A. Fiore
Anthony J. Kohtz
Daniel N. Miller
Sanjay Antony-Babu
Donald Pan
Caitlin Lahey
Xi Huang
Yongfeng Lu
Nicole R. Buan
Karrie A. Weber
Microbial methane production from calcium carbonate at moderately alkaline pH
Communications Earth & Environment
title Microbial methane production from calcium carbonate at moderately alkaline pH
title_full Microbial methane production from calcium carbonate at moderately alkaline pH
title_fullStr Microbial methane production from calcium carbonate at moderately alkaline pH
title_full_unstemmed Microbial methane production from calcium carbonate at moderately alkaline pH
title_short Microbial methane production from calcium carbonate at moderately alkaline pH
title_sort microbial methane production from calcium carbonate at moderately alkaline ph
url https://doi.org/10.1038/s43247-025-02057-y
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