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Geology; July 2008; v. 36; no. 7; p. 543-546; DOI: 10.1130/G24690A.1
© 2008 Geological Society of America
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A new constraint on the antiquity of anaerobic oxidation of methane: Late Pennsylvanian seep limestones from southern Namibia

Daniel Birgel1, Tobias Himmler2, André Freiwald2 and Jörn Peckmann3,*

1 MARUM–Center for Marine Environmental Sciences, Universität Bremen, 28334 Bremen, Germany
2 Geozentrum Nordbayern, FG Paläoumwelt, Universität Erlangen, 91054 Erlangen, Germany
3 MARUM–Center for Marine Environmental Sciences, Universität Bremen, 28334 Bremen, Germany

Correspondence: * E-mail: peckmann{at}uni-bremen.de.

Late Pennsylvanian seep limestones (ca. 300 Ma) enclosed in the Ganigobis shales in southern Namibia formed by microbial activity. The process that induced carbonate precipitation was the anaerobic oxidation of methane. The presence of 13C-depleted pentamethylicosane (PMI) (–113{per thousand}) and a mixture of crocetane and phytane (–112{per thousand}) in concert with similarly 13C-depleted pseudohomologous series of regular isoprenoids reveals that methanotrophic archaea oxidized methane anaerobically at the ancient seep site. Biphytane and a C39 pseudohomologue are other archaeal molecular fossils with {delta}13C values of –99{per thousand} and –97{per thousand}, respectively. The former presence of sulfate-reducing bacteria as the syntrophic partners of methanotrophic archaea in the anaerobic oxidation of methane is indicated by isotopically depleted iso- and anteiso-alkanes. These compounds most probably derive from non-isoprenoidal monoethers and diethers, synthates of sulfate-reducing bacteria. These findings show that anaerobic oxidation of methane is at least 300 m.y. old, extending the record of this process for ~140 m.y. As the molecular fossils of archaea and bacteria are preserved in a product of their own metabolic activity (i.e., methane-derived carbonates with {delta}13C values as low as –51{per thousand}), the syngenicity of molecular fossils and enclosing deposits is unambiguous. This reveals that microbially formed rocks can represent excellent archives for studying past biogeochemical processes.

Key Words: anaerobic oxidation • methane • archaea • sulfate-reducing bacteria • seeps • isoprenoids • limestones






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