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migration of the redox boundary to the sediment-water interface. Sediment trapping and precipitation of authigenic minerals are essential in the preservation of microbial constructions as a result of the organic matter that composed the original mat is rapidly degraded throughout burial and diagenesis, leaving little greater than the bodily and chemical properties related to the original mats ( Noffke et al. 2002 ). Chemical clues embrace the precipitation of authigenic silicates and pyrite, whereas later oxidation of iron sulfides may additionally outcome in the

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