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Geo-Marine Letters

, Volume 34, Issue 2–3, pp 269–280 | Cite as

Lipid biomarkers for anaerobic oxidation of methane and sulphate reduction in cold seep sediments of Nyegga pockmarks (Norwegian margin): discrepancies in contents and carbon isotope signatures

  • Nicolas Chevalier
  • Ioanna Bouloubassi
  • Alina Stadnitskaia
  • Marie-Hélène Taphanel
  • Jaap S. Sinninghe Damsté
Original

Abstract

Distributions and carbon isotopic compositions of microbial lipid biomarkers were investigated in sediment cores from the G11 and G12 pockmarks in the Nyegga sector of the Storegga Slide on the mid-Norwegian margin to explore differences in depth zonation, type and carbon assimilation mode of anaerobic methane-oxidizing archaea (ANMEs) and associated sulphate-reducing bacteria responsible for anaerobic oxidation of methane (AOM) in these cold seep environments. While the G11 site is characterised by black reduced sediments colonized by gastropods and Siboglinidae tubeworms, the G12 site has black reduced sediments devoid of fauna but surrounded by a peripheral occurrence of gastropods and white filamentous microbial mats. At both sites, bulk sediments contained abundant archaeal and bacterial lipid biomarkers substantially depleted in 13C, consisting mainly of isoprenoidal hydrocarbons and dialkyl glycerol diethers, fatty acids and non-isoprenoidal monoalkylglycerol ethers. At the G11 site, down-core profiles revealed that lipid biomarkers were in maximum abundance from 10 cm depth to the core bottom at 16 cm depth, associated with δ13C values of −57 to −136‰. At the G12 site, by contrast, lipid biomarkers were in high abundance in the upper 5 cm sediment layer, associated with δ13C values of −43 to −133‰. This suggests that, as expected from the benthic fauna characteristics of the sites, AOM takes place mainly at depth in the G11 pockmark but just below the seafloor in the G12 pockmark. These patterns can be explained largely by variable fluid flow rates. Furthermore, at both sites, a dominance of ANME-2 archaea accompanied by their bacterial partners is inferred based on lipid biomarker distributions and carbon isotope signatures, which is in agreement with recently published DNA analyses for the G11 pockmark. However, the present data reveal high discrepancies in the contents and δ13C values for both archaeal and bacterial lipid profiles, implying the possible involvement of at least two distinct AOM-related microbial consortia at the inferred AOM depth zonation of G11 and G12 pockmark sediments. In both sediment cores, the δ13C profiles for most archaeal lipids suggest a direct assimilation of dissolved inorganic carbon (DIC) in addition to methane by ANMEs (chemoautotrophy); constant and highly depleted δ13C profiles for PMI:3, an archaeal lipid biomarker presumably related to ANME-2, suggest a direct assimilation of 13C-depleted methane-derived carbon via AOM (methanotrophy). Evidently, the common approach of investigating lipid biomarker contents and δ13C signatures in cold seep sediments does not suffice to precisely discriminate between the carbon assimilation mode for each ANME archaeal group and associated bacteria. Rather, this needs to be combined with further specific labelling studies including different carbon sources (methane carbon, methane-derived organic intermediates and DIC) in order to unravel the metabolic pathways of each microbial consortium involved in AOM (ANME-1 vs. ANME-2 vs. ANME-3 archaeal group and associated bacteria).

Keywords

Dissolve Inorganic Carbon Carbon Isotopic Composition Methanotrophs Cold Seep Bacterial Lipid 
These keywords were added by machine and not by the authors. This process is experimental and the keywords may be updated as the learning algorithm improves.

Notes

Acknowledgments

This work was supported by the HERMES project funded by the European Commission’s Framework Six Programme, EC contract no. GOCE-CT-2005-511234, by a grant from the Ministry of Education (France) to Nicolas Chevalier, and by a VENI grant from the Netherlands Organization for Scientific Research (NWO) to Alina Stadnitskaia. We thank the scientific team of the VICKING cruise, the captain and crew of the R/V Pourquoi pas?, and Catherine Pierre for sediment sampling. Also gratefully acknowledged are the technical and scientific staff of the Department of Marine Organic Biogeochemistry at NIOZ. Constructive assessments by three anonymous reviewers and the editors proved useful in improving the paper.

Supplementary material

367_2014_363_MOESM1_ESM.pdf (330 kb)
ESM 1 (PDF 329 kb)

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Copyright information

© Springer-Verlag Berlin Heidelberg 2014

Authors and Affiliations

  • Nicolas Chevalier
    • 1
  • Ioanna Bouloubassi
    • 1
  • Alina Stadnitskaia
    • 2
  • Marie-Hélène Taphanel
    • 1
  • Jaap S. Sinninghe Damsté
    • 2
  1. 1.Laboratoire d’Océanographie et du Climat - Expérimentation et Approches Numériques (LOCEAN), CNRS UMR 7159, IPSLUniversité Pierre et Marie Curie, CC 100Paris cedex 05France
  2. 2.Department of Marine Organic BiogeochemistryNIOZ Royal Netherlands Institute for Sea ResearchDen BurgThe Netherlands

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