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Formation of Siderite in Microbial Microcosms Derived from a Marine Sediment
Authors:Aysha Kamran  Dominik Schneider  Vladimir Roddatis  Volker Thiel
Institution:1. Institute of Microbiology and Genetics, University of Goettingen, Goettingen, Germany;2. Institute of Materials Physics, University of G?ttingen, Goettingen, Germany;3. Geobiology, Geoscience Centre, University of Goettingen, Goettingen, Germany
Abstract:Abstract

Exceptionally well-preserved fossils are frequently encased by carbonate concretions. The initial steps of their formation in marine and freshwater sediments are induced by microbial activity. The role of the involved microbial communities, however, is not well understood. In this study, siderite (FeCO3) formation in microbial microcosms is observed, with various fatty acyl compounds (lipids, surfactants) as substrates and Wadden Sea sediment samples as inocula. In actively growing microcosms, sulfate-reducing bacteria (the genus Desulfofrigus in particular) dominate the microbial community and submicroscopic siderite precipitates on bacterial cell surfaces were identified. We suggest that these biologically induced mineralization processes may, in the natural environment, initiate the formation of large concretions under suboxic conditions in coastal sediments.
Keywords:Fossilization  sulfate reduction  microbial community  siderite  biomineral  community structure  molecular ecology  sulfate reducing bacteria
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