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