Contribution of microbial mats to sedimentary surface structures |
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Authors: | Dr. Gisela Gerdes Marianne Claes Katharina Dunajtschik-Piewak Heike Riege Prof. Dr. Wolfgang E. Krumbein Prof. Dr. Hans-Erich Reineck |
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Affiliation: | (1) Marine Laboratory of the Institute for Chemistry and Biology of the Marine Environment, Carl von Ossietzky University, Schleusenstr. 16, D-26382 Wilhelmshaven, Germany;(2) Senckenberg Institute, Schleusenstr. 39A, D-36382 Wilhelmshaven;(3) Institute for Chemistry and Biology of the Marine Environment, Carl von Ossietzky University, Postfach 2503, D-2611 Oldenburg |
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Abstract: | Summary This paper summarizes studies of sedimentary surface structures in which microbial mats play a role. Intertidal/supratidal transitions of tidal flats of the North Sea coast, and shallow hypersaline water bodies of salterns (Bretagne, Canary and Balearic Islands), and Gavish Sabkha (Sinai) reveal a multitude of sedimentary surface structures which can be grouped and primary biologically controlled structures. Physically controlled surface structures include shrinkage cracks, erosion marks, deformation structures caused by water friction, gas pressure and mineral encrustation. Shrinkage cracks in microbial mats reveal the following features: (i) horizontally arranged cauliflower pattern that differs from the usually orthogonally regular crack morphology in clay, (ii) rounded edges and pillow-like thickening along the crack edges, caused by the growth of mats into the cracks. Criteria of erosion are pocket-like depressions and ripple marks on the thus exposed non-stabilized sand, and residual stacks of microbial mats. Deformation structures are due to water friction causing flotation of loosely attached microbial mats which fold and tear. Gas migration from deeper layers causes domal upheaval, protuberance structures, folds and “fairy rings”. Protuberance structures are caused by the rupture of gas domes and rapid escape of the enclosed gas. The sudden drop of pressure forces sediment to well up from below through the gas channels and to fill the internal hollow spaces of the domes. “Fairy rings” are horizontal ringshaped structures. Their center is the exit point of gas bubbles which escape from the substrate into the shallow water. The bubbles generate concentric waves which cause displacement of fine muddy sediments at the sediment-water interface Such gradual displacement guides mat-constructing microbes to grow concentrically. The “fairy rings” are crowned by pinnacle structures of bacterial and diatom origin. Pinnacles, “fairy rings” and pillow-like coatings of crack margins are biogenic structures which have to be genetically separated from purely physically controlled structures. |
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Keywords: | Microbial Mats Biostabilization Sedimentary Surface Structures Shrinkage Cracks Erosion Marks Deformation Structures Gas Upheaval Pinnacles Biogenic Structures Salterns Tidal Flats Recent |
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