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Microbial reefs in the Black Sea fueled by anaerobic oxidation of methane
Authors:Michaelis Walter  Seifert Richard  Nauhaus Katja  Treude Tina  Thiel Volker  Blumenberg Martin  Knittel Katrin  Gieseke Armin  Peterknecht Katharina  Pape Thomas  Boetius Antje  Amann Rudolf  Jørgensen Bo Barker  Widdel Friedrich  Peckmann Jörn  Pimenov Nikolai V  Gulin Maksim B
Institution:Institute of Biogeochemistry and Marine Chemistry, University of Hamburg, Bundesstrasse 55, 20146 Hamburg, Germany. michaelis@geowiss.uni-hamburg.de
Abstract: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.
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