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Science 9 August 2002:
Vol. 297. no. 5583, pp. 1013 - 1015
DOI: 10.1126/science.1072502

Reports

Microbial Reefs in the Black Sea Fueled by Anaerobic Oxidation of Methane

Walter Michaelis,1* Richard Seifert,1 Katja Nauhaus,2 Tina Treude,2 Volker Thiel,1 Martin Blumenberg,1 Katrin Knittel,2 Armin Gieseke,2 Katharina Peterknecht,1 Thomas Pape,1 Antje Boetius,3 Rudolf Amann,2 Bo Barker Jørgensen,2 Friedrich Widdel,2 Jörn Peckmann,4 Nikolai V. Pimenov,5 Maksim B. Gulin6

Massive microbial mats covering up to 4-meter-high carbonate buildups prosper at methane seeps in anoxic waters of the northwestern Black Sea shelf. Strong 13C depletions indicate an incorporation of methane carbon into carbonates, bulk biomass, and specific lipids. The mats mainly consist of densely aggregated archaea (phylogenetic ANME-1 cluster) and sulfate-reducing bacteria (Desulfosarcina/Desulfococcus group). If incubated in vitro, these mats perform anaerobic oxidation of methane coupled to sulfate reduction. Obviously, anaerobic microbial consortia can generate both carbonate precipitation and substantial biomass accumulation, which has implications for our understanding of carbon cycling during earlier periods of Earth's history.

1 Institute of Biogeochemistry and Marine Chemistry, University of Hamburg, Bundesstrasse 55, 20146 Hamburg, Germany.
2 Max Planck Institute for Marine Microbiology, Celsiusstrasse 1, 28359 Bremen, Germany.
3 Alfred Wegener Institute for Polar and Marine Research, 27515 Bremerhaven, and International University Bremen, 28725 Bremen, Germany.
4 Geowissenschaftliches Zentrum, University of Göttingen, Goldschmidtstrasse 3, 37077 Göttingen, Germany.
5 Institute of Microbiology, Russian Academy of Sciences, pr. 60-letiya Oktyabrya 7, k. 2, Moscow, 117811, Russia.
6 Institute of Biology of Southern Seas, National Academy of Sciences of Ukraine, pr. Nakhimova 2, Sevastopol, Ukraine.
*   To whom correspondence should be addressed. E-mail: michaelis{at}geowiss.uni-hamburg.de


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