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Free keywords:
INTACT POLAR LIPIDS; MICROBIAL COMMUNITIES; FATTY-ACIDS; SP NOV.;
METHANOTROPHIC ARCHAEA; ELECTRON-TRANSFER; MUD VOLCANO; AMINO-ACIDS;
GEN. NOV.; OXIDATIONMicrobiology; anaerobic oxidation of methane; archaea; bacteria; heterotrophy; stable
isotope probing; lipid biomarkers;
Abstract:
Consortia of anaerobic methanotrophic archaea (ANME) and sulfate-reducing bacteria mediate the anaerobic oxidation of methane (AOM) in marine sediments. However, even sediment-free cultures contain a substantial number of additional microorganisms not directly related to AOM. To track the heterotrophic activity of these community members and their possible relationship with AOM, we amended meso- (37 degrees C) and thermophilic (50 degrees C) AOM cultures (dominated by ANME-1 archaea and their partner bacteria of the Seep-SRB2 clade or Candidatus Desulfofervidus auxilii) with L-leucine-3-C-13 (C-13-leu). Various microbial lipids incorporated the labeled carbon from this amino acid, independent of the presence of methane as an energy source, specifically bacterial fatty acids, such as iso and anteiso-branched C-15:0 and C-17:0, as well as unsaturated C-18:1 omega 9 and C-18:1 omega 7. In natural methane-rich environments, these bacterial fatty acids are strongly C-13-depleted. We, therefore, suggest that those fatty acids are produced by ancillary bacteria that grow on C-13-depleted necromass or cell exudates/lysates of the AOM core communities. Candidates that likely benefit from AOM biomass are heterotrophic bacterial members of the Spirochetes and Anaerolineae-known to produce abundant branched fatty acids and present in all the AOM enrichment cultures. For archaeal lipids, we observed minor C-13-incorporation, but still suggesting some C-13-leu anabolism. Based on their relatively high abundance in the culture, the most probable archaeal candidates are Bathyarchaeota, Thermoplasmatales, and Lokiarchaeota. The identified heterotrophic bacterial and archaeal ancillary members are likely key players in organic carbon recycling in anoxic marine sediments.
