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Plant roots but not hydrology control microbiome composition and methane flux in temperate fen mesocosms

Piecha, Marc (författare)
Department of Bacterial Physiology, Institute of Microbiology, Greifswald, Germany
Kreyling, Juergen (författare)
Experimental Plant Ecology, Institute of Botany and Landscape Ecology, Greifswald, Germany
Couwenberg, John (författare)
Experimental Plant Ecology, Institute of Botany and Landscape Ecology, Greifswald, Germany
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Pester, Michael (författare)
Department of Microorganisms, Leibniz Institute, German Collection of Microorganisms and Cell Cultures GmbH, Braunschweig, Germany; Institute of Microbiology, Technical University of Braunschweig, Braunschweig, Germany
Guenther, Anke (författare)
Landscape Ecology, Faculty of Agricultural and Environmental Sciences, University of Rostock, Rostock, Germany
Henningsen, Levke (författare)
Experimental Plant Ecology, Institute of Botany and Landscape Ecology, Greifswald, Germany
Weil, Micha (författare)
Department of Bacterial Physiology, Institute of Microbiology, Greifswald, Germany
Jurasinski, Gerald (författare)
Landscape Ecology, Faculty of Agricultural and Environmental Sciences, University of Rostock, Rostock, Germany; Peatland Science, University of Greifswald, Greifswald, Germany
Blume-Werry, Gesche, 1985- (författare)
Umeå universitet,Institutionen för ekologi, miljö och geovetenskap,Experimental Plant Ecology, Institute of Botany and Landscape Ecology, Greifswald, Germany
Urich, Tim (författare)
Department of Bacterial Physiology, Institute of Microbiology, Greifswald, Germany
Wang, Haitao (författare)
Department of Bacterial Physiology, Institute of Microbiology, Greifswald, Germany
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 (creator_code:org_t)
Elsevier, 2024
2024
Engelska.
Ingår i: Science of the Total Environment. - : Elsevier. - 0048-9697 .- 1879-1026. ; 940
  • Tidskriftsartikel (refereegranskat)
Abstract Ämnesord
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  • The rewetting of formerly drained peatlands can help to counteract climate change through the reduction of CO2 emissions. However, this can lead to resuming CH4 emissions due to changes in the microbiome, favoring CH4-producing archaea. How plants, hydrology and microbiomes interact as ultimate determinants of CH4 dynamics is still poorly understood. Using a mesocosm approach, we studied peat microbiomes, below-ground root biomass and CH4 fluxes with three different water level regimes (stable high, stable low and fluctuating) and four different plant communities (bare peat, Carex rostrata, Juncus inflexus and their mixture) over the course of one growing season. A significant difference in microbiome composition was found between mesocosms with and without plants, while the difference between plant species identity or water regimes was rather weak. A significant difference was also found between the upper and lower peat, with the difference increasing as plants grew. By the end of the growing season, the methanogen relative abundance was higher in the sub-soil layer, as well as in the bare peat and C. rostrata pots, as compared to J. inflexus or mixture pots. This was inversely linked to the larger root area of J. inflexus. The root area also negatively correlated with CH4 fluxes which positively correlated with the relative abundance of methanogens. Despite the absence or low abundance of methanotrophs in many samples, the integration of methanotroph abundance improved the quality of the correlation with CH4 fluxes, and methanogens and methanotrophs together determined CH4 fluxes in a structural equation model. However, water regime showed no significant impact on plant roots and methanogens, and consequently, on CH4 fluxes. This study showed that plant roots determined the microbiome composition and, in particular, the relative abundance of methanogens and methanotrophs, which, in interaction, drove the CH4 fluxes.

Ämnesord

NATURVETENSKAP  -- Biologi -- Ekologi (hsv//swe)
NATURAL SCIENCES  -- Biological Sciences -- Ecology (hsv//eng)

Nyckelord

Mesocosm
Methane
Methanogens
Microbiome
Plant root
Water regime

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