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Cable bacteria delay euxinia and modulate phosphorus release in coastal hypoxic systems.

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Area of Science:

  • Microbial ecology
  • Biogeochemistry
  • Environmental science

Background:

  • Cable bacteria are filamentous microbes with unique electron transport capabilities.
  • They thrive in seasonally hypoxic sediments, influencing iron and sulfur cycling.
  • Their metabolism dissolves iron sulfides (FeS), releasing ferrous iron (Fe2+).

Purpose of the Study:

  • To experimentally investigate the 'iron firewall hypothesis' proposed for cable bacteria.
  • To assess the role of cable bacteria in controlling hydrogen sulfide (H2S) and phosphorus (P) release from sediments.
  • To understand the seasonal impact of cable bacteria on coastal biogeochemical cycles.

Main Methods:

  • Collection of natural sediment cores from a seasonally hypoxic basin across three seasons.
  • Incubation of undisturbed sediment cores under anoxic conditions.
  • Monitoring of effluxes for hydrogen sulfide (H2S), dissolved iron (dFe), and phosphate (PO43-) over 140 days.

Main Results:

  • Sediment cores with active cable bacteria showed a significant stock of iron oxyhydroxides (FeOx).
  • This FeOx layer delayed the efflux of H2S for up to 102 days.
  • Evidence supports the role of cable bacteria in retaining H2S and modulating P release.

Conclusions:

  • Cable bacteria establish an 'iron firewall' that effectively prevents the release of H2S.
  • This mechanism plays a crucial role in regulating phosphorus release and preventing euxinia in coastal environments.
  • The findings highlight the ecological importance of cable bacteria in marine sediment biogeochemistry.