Microbial methane formation in deep aquifers of a coal-bearing sedimentary basin, Germany

Coal-bearing sediments are major reservoirs of organic matter potentially available for methanogenic subsurface microbial communities. In this study the specific microbial community inside lignite-bearing anoxic cenozoic sediments from a coal mine and its contribution to methanogenic hydrocarbon deg...

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Main Authors: Friederike eGruendger, Núria eJiménez, Thomas eThielemann, Nontje eStraaten, Tillmann eLüders, Hans H. Richnow, Martin eKrüger
Format: Article
Language:English
Published: Frontiers Media S.A. 2015-03-01
Series:Frontiers in Microbiology
Subjects:
Online Access:http://journal.frontiersin.org/Journal/10.3389/fmicb.2015.00200/full
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author Friederike eGruendger
Núria eJiménez
Thomas eThielemann
Nontje eStraaten
Tillmann eLüders
Hans H. Richnow
Martin eKrüger
author_facet Friederike eGruendger
Núria eJiménez
Thomas eThielemann
Nontje eStraaten
Tillmann eLüders
Hans H. Richnow
Martin eKrüger
author_sort Friederike eGruendger
collection DOAJ
description Coal-bearing sediments are major reservoirs of organic matter potentially available for methanogenic subsurface microbial communities. In this study the specific microbial community inside lignite-bearing anoxic cenozoic sediments from a coal mine and its contribution to methanogenic hydrocarbon degradation processes was investigated. The stable isotope signature of methane measured in groundwater and coal-rich sediment samples indicated methanogenic activity. Analysis of 16S rRNA gene sequences showed the presence of methanogenic Archaea, predominantly belonging to the orders Methanosarcinales and Methanomicrobiales, capable of acetoclastic or hydrogenotrophic methanogenesis. Furthermore, we identified fermenting, sulfate-, nitrate- and metal-reducing, or acetogenic Bacteria clustering within the phyla Proteobacteria, complemented by members of the classes Actinobacteria, and Clostridia. The indigenous microbial communities found in the groundwater as well as in the coal-rich sediments are able to degrade coal-derived organic components and to produce methane as the final product. Lignite-bearing sediments may be an important nutrient and energy source influencing larger compartments via groundwater transport.
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spelling doaj.art-d79b1e8db0de4a7c8a3a00d8334e98312022-12-21T18:41:15ZengFrontiers Media S.A.Frontiers in Microbiology1664-302X2015-03-01610.3389/fmicb.2015.00200129943Microbial methane formation in deep aquifers of a coal-bearing sedimentary basin, GermanyFriederike eGruendger0Núria eJiménez1Thomas eThielemann2Nontje eStraaten3Tillmann eLüders4Hans H. Richnow5Martin eKrüger6Federal Institue for Geosciences and Natural Resources (BGR)Federal Institue for Geosciences and Natural Resources (BGR)Federal Institue for Geosciences and Natural Resources (BGR)Federal Institue for Geosciences and Natural Resources (BGR)Helmholtz Center for Environmental HealthHelmholtz Centre for Environmental Research (UFZ)Federal Institue for Geosciences and Natural Resources (BGR)Coal-bearing sediments are major reservoirs of organic matter potentially available for methanogenic subsurface microbial communities. In this study the specific microbial community inside lignite-bearing anoxic cenozoic sediments from a coal mine and its contribution to methanogenic hydrocarbon degradation processes was investigated. The stable isotope signature of methane measured in groundwater and coal-rich sediment samples indicated methanogenic activity. Analysis of 16S rRNA gene sequences showed the presence of methanogenic Archaea, predominantly belonging to the orders Methanosarcinales and Methanomicrobiales, capable of acetoclastic or hydrogenotrophic methanogenesis. Furthermore, we identified fermenting, sulfate-, nitrate- and metal-reducing, or acetogenic Bacteria clustering within the phyla Proteobacteria, complemented by members of the classes Actinobacteria, and Clostridia. The indigenous microbial communities found in the groundwater as well as in the coal-rich sediments are able to degrade coal-derived organic components and to produce methane as the final product. Lignite-bearing sediments may be an important nutrient and energy source influencing larger compartments via groundwater transport.http://journal.frontiersin.org/Journal/10.3389/fmicb.2015.00200/fullCoalmethanogenesismethanogenic archaeafluvial depositsstable isotope fractionationCenozoic sediments
spellingShingle Friederike eGruendger
Núria eJiménez
Thomas eThielemann
Nontje eStraaten
Tillmann eLüders
Hans H. Richnow
Martin eKrüger
Microbial methane formation in deep aquifers of a coal-bearing sedimentary basin, Germany
Frontiers in Microbiology
Coal
methanogenesis
methanogenic archaea
fluvial deposits
stable isotope fractionation
Cenozoic sediments
title Microbial methane formation in deep aquifers of a coal-bearing sedimentary basin, Germany
title_full Microbial methane formation in deep aquifers of a coal-bearing sedimentary basin, Germany
title_fullStr Microbial methane formation in deep aquifers of a coal-bearing sedimentary basin, Germany
title_full_unstemmed Microbial methane formation in deep aquifers of a coal-bearing sedimentary basin, Germany
title_short Microbial methane formation in deep aquifers of a coal-bearing sedimentary basin, Germany
title_sort microbial methane formation in deep aquifers of a coal bearing sedimentary basin germany
topic Coal
methanogenesis
methanogenic archaea
fluvial deposits
stable isotope fractionation
Cenozoic sediments
url http://journal.frontiersin.org/Journal/10.3389/fmicb.2015.00200/full
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