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Sökning: WFRF:(Milucka Jana)

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1.
  • Schorn, Sina, et al. (författare)
  • Persistent activity of aerobic methane-oxidizing bacteria in anoxic lake waters due to metabolic versatility
  • 2024
  • Ingår i: NATURE COMMUNICATIONS. - 2041-1723. ; 15:1
  • Tidskriftsartikel (refereegranskat)abstract
    • Lacustrine methane emissions are strongly mitigated by aerobic methane-oxidizing bacteria (MOB) that are typically most active at the oxic-anoxic interface. Although oxygen is required by the MOB for the first step of methane oxidation, their occurrence in anoxic lake waters has raised the possibility that they are capable of oxidizing methane further anaerobically. Here, we investigate the activity and growth of MOB in Lake Zug, a permanently stratified freshwater lake. The rates of anaerobic methane oxidation in the anoxic hypolimnion reached up to 0.2 mu M d-1. Single-cell nanoSIMS measurements, together with metagenomic and metatranscriptomic analyses, linked the measured rates to MOB of the order Methylococcales. Interestingly, their methane assimilation activity was similar under hypoxic and anoxic conditions. Our data suggest that these MOB use fermentation-based methanotrophy as well as denitrification under anoxic conditions, thus offering an explanation for their widespread presence in anoxic habitats such as stratified water columns. Thus, the methane sink capacity of anoxic basins may have been underestimated by not accounting for the anaerobic MOB activity. The occurrence of aerobic methane-oxidizing bacteria in anoxic environments is puzzling, as oxygen is thought to be required for methane oxidation. Here, Schorn et al. show that the methane assimilation activity of these bacteria is similar under hypoxic and anoxic conditions in a stratified lake, and the bacteria use fermentation-based methanotrophy as well as denitrification under anoxic conditions.
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2.
  • Wilson, Samuel T., et al. (författare)
  • Ideas and perspectives : A strategic assessment of methane and nitrous oxide measurements in the marine environment
  • 2020
  • Ingår i: Biogeosciences. - : Copernicus GmbH. - 1726-4170 .- 1726-4189. ; 17:22, s. 5809-5828
  • Tidskriftsartikel (refereegranskat)abstract
    • In the current era of rapid climate change, accurate characterization of climate-relevant gas dynamics – namely production, consumption, and net emissions – is required for all biomes, especially those ecosystems most susceptible to the impact of change. Marine environments include regions that act as net sources or sinks for numerous climate-active trace gases including methane (CH4) and nitrous oxide (N2O). The temporal and spatial distributions of CH4 and N2O are controlled by the interaction of complex biogeochemical and physical processes. To evaluate and quantify how these mechanisms affect marine CH4 and N2O cycling requires a combination of traditional scientific disciplines including oceanography, microbiology, and numerical modeling. Fundamental to these efforts is ensuring that the datasets produced by independent scientists are comparable and interoperable. Equally critical is transparent communication within the research community about the technical improvements required to increase our collective understanding of marine CH4 and N2O. A workshop sponsored by Ocean Carbon and Biogeochemistry (OCB) was organized to enhance dialogue and collaborations pertaining to marine CH4 and N2O. Here, we summarize the outcomes from the workshop to describe the challenges and opportunities for near-future CH4 and N2O research in the marine environment.
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