Lignite coal burning seam in the remote Altai Mountains harbors a hydrogen-driven thermophilic microbial community

Abstract Thermal ecosystems associated with underground coal combustion sites are rare and less studied than geothermal features. Here we analysed microbial communities of near-surface ground layer and bituminous substance in an open quarry heated by subsurface coal fire by metagenomic DNA sequencin...

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Autores principales: Vitaly V. Kadnikov, Andrey V. Mardanov, Denis A. Ivasenko, Dmitry V. Antsiferov, Alexey V. Beletsky, Olga V. Karnachuk, Nikolay V. Ravin
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Publicado: Nature Portfolio 2018
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Acceso en línea:https://doaj.org/article/56207671a76b49bbada3fd1393e0a072
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spelling oai:doaj.org-article:56207671a76b49bbada3fd1393e0a0722021-12-02T11:40:17ZLignite coal burning seam in the remote Altai Mountains harbors a hydrogen-driven thermophilic microbial community10.1038/s41598-018-25146-92045-2322https://doaj.org/article/56207671a76b49bbada3fd1393e0a0722018-04-01T00:00:00Zhttps://doi.org/10.1038/s41598-018-25146-9https://doaj.org/toc/2045-2322Abstract Thermal ecosystems associated with underground coal combustion sites are rare and less studied than geothermal features. Here we analysed microbial communities of near-surface ground layer and bituminous substance in an open quarry heated by subsurface coal fire by metagenomic DNA sequencing. Taxonomic classification revealed dominance of only a few groups of Firmicutes. Near-complete genomes of three most abundant species, ‘Candidatus Carbobacillus altaicus’ AL32, Brockia lithotrophica AL31, and Hydrogenibacillus schlegelii AL33, were assembled. According to the genomic data, Ca. Carbobacillus altaicus AL32 is an aerobic heterotroph, while B. lithotrophica AL31 is a chemolithotrophic anaerobe assimilating CO2 via the Calvin cycle. H. schlegelii AL33 is an aerobe capable of both growth on organic compounds and carrying out CO2 fixation via the Calvin cycle. Phylogenetic analysis of the large subunit of RuBisCO of B. lithotrophica AL31 and H. schlegelii AL33 showed that it belongs to the type 1-E. All three Firmicutes species can gain energy from aerobic or anaerobic oxidation of molecular hydrogen, produced as a result of underground coal combustion along with other coal gases. We propose that thermophilic Firmicutes, whose spores can spread from their original geothermal habitats over long distances, are the first colonizers of this recently formed thermal ecosystem.Vitaly V. KadnikovAndrey V. MardanovDenis A. IvasenkoDmitry V. AntsiferovAlexey V. BeletskyOlga V. KarnachukNikolay V. RavinNature PortfolioarticleMedicineRScienceQENScientific Reports, Vol 8, Iss 1, Pp 1-12 (2018)
institution DOAJ
collection DOAJ
language EN
topic Medicine
R
Science
Q
spellingShingle Medicine
R
Science
Q
Vitaly V. Kadnikov
Andrey V. Mardanov
Denis A. Ivasenko
Dmitry V. Antsiferov
Alexey V. Beletsky
Olga V. Karnachuk
Nikolay V. Ravin
Lignite coal burning seam in the remote Altai Mountains harbors a hydrogen-driven thermophilic microbial community
description Abstract Thermal ecosystems associated with underground coal combustion sites are rare and less studied than geothermal features. Here we analysed microbial communities of near-surface ground layer and bituminous substance in an open quarry heated by subsurface coal fire by metagenomic DNA sequencing. Taxonomic classification revealed dominance of only a few groups of Firmicutes. Near-complete genomes of three most abundant species, ‘Candidatus Carbobacillus altaicus’ AL32, Brockia lithotrophica AL31, and Hydrogenibacillus schlegelii AL33, were assembled. According to the genomic data, Ca. Carbobacillus altaicus AL32 is an aerobic heterotroph, while B. lithotrophica AL31 is a chemolithotrophic anaerobe assimilating CO2 via the Calvin cycle. H. schlegelii AL33 is an aerobe capable of both growth on organic compounds and carrying out CO2 fixation via the Calvin cycle. Phylogenetic analysis of the large subunit of RuBisCO of B. lithotrophica AL31 and H. schlegelii AL33 showed that it belongs to the type 1-E. All three Firmicutes species can gain energy from aerobic or anaerobic oxidation of molecular hydrogen, produced as a result of underground coal combustion along with other coal gases. We propose that thermophilic Firmicutes, whose spores can spread from their original geothermal habitats over long distances, are the first colonizers of this recently formed thermal ecosystem.
format article
author Vitaly V. Kadnikov
Andrey V. Mardanov
Denis A. Ivasenko
Dmitry V. Antsiferov
Alexey V. Beletsky
Olga V. Karnachuk
Nikolay V. Ravin
author_facet Vitaly V. Kadnikov
Andrey V. Mardanov
Denis A. Ivasenko
Dmitry V. Antsiferov
Alexey V. Beletsky
Olga V. Karnachuk
Nikolay V. Ravin
author_sort Vitaly V. Kadnikov
title Lignite coal burning seam in the remote Altai Mountains harbors a hydrogen-driven thermophilic microbial community
title_short Lignite coal burning seam in the remote Altai Mountains harbors a hydrogen-driven thermophilic microbial community
title_full Lignite coal burning seam in the remote Altai Mountains harbors a hydrogen-driven thermophilic microbial community
title_fullStr Lignite coal burning seam in the remote Altai Mountains harbors a hydrogen-driven thermophilic microbial community
title_full_unstemmed Lignite coal burning seam in the remote Altai Mountains harbors a hydrogen-driven thermophilic microbial community
title_sort lignite coal burning seam in the remote altai mountains harbors a hydrogen-driven thermophilic microbial community
publisher Nature Portfolio
publishDate 2018
url https://doaj.org/article/56207671a76b49bbada3fd1393e0a072
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AT nikolayvravin lignitecoalburningseamintheremotealtaimountainsharborsahydrogendriventhermophilicmicrobialcommunity
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