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A carbonate corrosion experiment at a marine methane seep: The role of aerobic methanotrophic bacteria.
Cordova-Gonzalez, Alexmar; Birgel, Daniel; Wisshak, Max; Urich, Tim; Brinkmann, Florian; Marcon, Yann; Bohrmann, Gerhard; Peckmann, Jörn.
Afiliación
  • Cordova-Gonzalez A; Centrum für Erdsystemforschung und Nachhaltigkeit, Universität Hamburg, Institut für Geologie, Hamburg, Germany.
  • Birgel D; Centrum für Erdsystemforschung und Nachhaltigkeit, Universität Hamburg, Institut für Geologie, Hamburg, Germany.
  • Wisshak M; Senckenberg am Meer, Abteilung Meeresforschung, Wilhelmshaven, Germany.
  • Urich T; Center for Functional Genomics of Microbes, University of Greifswald, Institut für Mikrobiologie, Greifswald, Germany.
  • Brinkmann F; MARUM - Zentrum für Marine Umweltwissenschaften und Fachbereich Geowissenschaften, Universität Bremen, Bremen, Germany.
  • Marcon Y; MARUM - Zentrum für Marine Umweltwissenschaften und Fachbereich Geowissenschaften, Universität Bremen, Bremen, Germany.
  • Bohrmann G; MARUM - Zentrum für Marine Umweltwissenschaften und Fachbereich Geowissenschaften, Universität Bremen, Bremen, Germany.
  • Peckmann J; Centrum für Erdsystemforschung und Nachhaltigkeit, Universität Hamburg, Institut für Geologie, Hamburg, Germany.
Geobiology ; 21(4): 491-506, 2023 07.
Article en En | MEDLINE | ID: mdl-36775968
Methane seeps are typified by the formation of authigenic carbonates, many of which exhibit corrosion surfaces and secondary porosity believed to be caused by microbial carbonate dissolution. Aerobic methane oxidation and sulfur oxidation are two processes capable of inducing carbonate corrosion at methane seeps. Although the potential of aerobic methanotrophy to dissolve carbonate was confirmed in laboratory experiments, this process has not been studied in the environment to date. Here, we report on a carbonate corrosion experiment carried out in the REGAB Pockmark, Gabon-Congo-Angola passive margin, in which marble cubes were deployed for 2.5 years at two sites (CAB-B and CAB-C) with apparent active methane seepage and one site (CAB-D) without methane seepage. Marble cubes exposed to active seepage (experiment CAB-C) were found to be affected by a new type of microbioerosion. Based on 16S rRNA gene analysis, the biofilms adhering to the bioeroded marble mostly consisted of aerobic methanotrophic bacteria, predominantly belonging to the uncultured Hyd24-01 clade. The presence of abundant 13 C-depleted lipid biomarkers including fatty acids (n-C16:1ω8c , n-C18:1ω8c , n-C16:1ω5t ), various 4-mono- and 4,4-dimethyl sterols, and diplopterol agrees with the dominance of aerobic methanotrophs in the CAB-C biofilms. Among the lipids of aerobic methanotrophs, the uncommon 4α-methylcholest-8(14)-en-3ß,25-diol is interpreted to be a specific biomarker for the Hyd24-01 clade. The combination of textural, genetic, and organic geochemical evidence suggests that aerobic methanotrophs are the main drivers of carbonate dissolution observed in the CAB-C experiment at the REGAB pockmark.
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Texto completo: 1 Colección: 01-internacional Base de datos: MEDLINE Asunto principal: Sedimentos Geológicos / Metano Idioma: En Revista: Geobiology Asunto de la revista: BIOLOGIA Año: 2023 Tipo del documento: Article País de afiliación: Alemania Pais de publicación: Reino Unido
Texto completo
Añadir a Mi BVS
Imprimir
XML
PubMed Links
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Texto completo: 1 Colección: 01-internacional Base de datos: MEDLINE Asunto principal: Sedimentos Geológicos / Metano Idioma: En Revista: Geobiology Asunto de la revista: BIOLOGIA Año: 2023 Tipo del documento: Article País de afiliación: Alemania Pais de publicación: Reino Unido