Microbial Diversity of Hydrothermal Sediments in the Guaymas Basin: Evidence for Anaerobic Methanotrophic Communities

  • Andreas Teske
    Biology Department
  • Kai-Uwe Hinrichs
    Geology and Geophysics Department, Woods Hole Oceanographic Institution
  • Virginia Edgcomb
    Marine Biological Laboratory, The Josephine Bay Paul Center for Comparative Molecular Biology and Evolution, Woods Hole, Massachusetts
  • Alvin de Vera Gomez
    Biology Department
  • David Kysela
    Marine Biological Laboratory, The Josephine Bay Paul Center for Comparative Molecular Biology and Evolution, Woods Hole, Massachusetts
  • Sean P. Sylva
    Geology and Geophysics Department, Woods Hole Oceanographic Institution
  • Mitchell L. Sogin
    Marine Biological Laboratory, The Josephine Bay Paul Center for Comparative Molecular Biology and Evolution, Woods Hole, Massachusetts

書誌事項

公開日
2002-04
権利情報
  • https://journals.asm.org/non-commercial-tdm-license
DOI
  • 10.1128/aem.68.4.1994-2007.2002
公開者
American Society for Microbiology

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説明

<jats:title>ABSTRACT</jats:title> <jats:p> Microbial communities in hydrothermally active sediments of the Guaymas Basin (Gulf of California, Mexico) were studied by using 16S rRNA sequencing and carbon isotopic analysis of archaeal and bacterial lipids. The Guaymas sediments harbored uncultured euryarchaeota of two distinct phylogenetic lineages within the anaerobic methane oxidation 1 (ANME-1) group, ANME-1a and ANME-1b, and of the ANME-2c lineage within the <jats:italic>Methanosarcinales</jats:italic> , both previously assigned to the methanotrophic archaea. The archaeal lipids in the Guaymas Basin sediments included archaeol, diagnostic for nonthermophilic euryarchaeota, and <jats:italic>sn</jats:italic> -2-hydroxyarchaeol, with the latter compound being particularly abundant in cultured members of the <jats:italic>Methanosarcinales</jats:italic> . The concentrations of these compounds were among the highest observed so far in studies of methane seep environments. The δ- <jats:sup>13</jats:sup> C values of these lipids (δ- <jats:sup>13</jats:sup> C = −89 to −58‰) indicate an origin from anaerobic methanotrophic archaea. This molecular-isotopic signature was found not only in samples that yielded predominantly ANME-2 clones but also in samples that yielded exclusively ANME-1 clones. ANME-1 archaea therefore remain strong candidates for mediation of the anaerobic oxidation of methane. Based on 16S rRNA data, the Guaymas sediments harbor phylogenetically diverse bacterial populations, which show considerable overlap with bacterial populations of geothermal habitats and natural or anthropogenic hydrocarbon-rich sites. Consistent with earlier observations, our combined evidence from bacterial phylogeny and molecular-isotopic data indicates an important role of some novel deeply branching bacteria in anaerobic methanotrophy. Anaerobic methane oxidation likely represents a significant and widely occurring process in the trophic ecology of methane-rich hydrothermal vents. This study stresses a high diversity among communities capable of anaerobic oxidation of methane. </jats:p>

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