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A novel, multi‐layered methanotrophic microbial mat system growing on the sediment of the Black Sea
Author(s) -
Krüger Martin,
Blumenberg Martin,
Kasten Sabine,
Wieland Andrea,
Känel Layla,
Klock JanHendrik,
Michaelis Walter,
Seifert Richard
Publication year - 2008
Publication title -
environmental microbiology
Language(s) - English
Resource type - Journals
SCImago Journal Rank - 1.954
H-Index - 188
eISSN - 1462-2920
pISSN - 1462-2912
DOI - 10.1111/j.1462-2920.2008.01607.x
Subject(s) - anaerobic oxidation of methane , authigenic , archaea , microbial mat , methane , sediment , biology , sulfide , geomicrobiology , environmental chemistry , extracellular polymeric substance , oceanography , ecology , biofilm , geology , bacteria , chemistry , microorganism , paleontology , environmental biotechnology , cyanobacteria , organic chemistry
Summary A novel microbially diverse type of 1‐ to 5‐cm‐thick mat performing anaerobic oxidation of methane (AOM) and covering several square metres of the seafloor was discovered in the Black Sea at 180 m water depth. Contrary to other AOM‐mat systems of the Black Sea these floating mats are not associated to free gas and are not stabilized by authigenic carbonates. However, supply of methane is ensured by the horizontal orientation of the mats acting as a cover of methane enriched fluids ascending from the underlying sediments. Thorough investigation of their community composition by molecular microbiology and lipid biomarkers, metabolic activities and elemental composition showed that the mats provide a clearly structured system with extracellular polymeric substances (EPS) building the framework of the mats. The top black zone, showing high rates of AOM (15 μmol g dw −1 day −1 ), was dominated by ANME‐2, while the following equally active pink layer was dominated by ANME‐1 Archaea . The lowest AOM activity (2 μmol g dw −1 day −1 ) and cell numbers were found in the greyish middle part delimited towards the sediment by a second pink, ANME‐1‐dominated and sometimes a black outer layer (ANME‐2). Our work clearly shows that the different microbial populations are established along defined chemical gradients such as methane, sulfate or sulfide.