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above the substrate ( Schieber 1999 , Petroff et al. 2010 ). Nonetheless, as deeper water environments are sometimes less influenced by fixed water motion, positive carbonaceous and wavy laminae have been urged as evidence of microbially induced constructions, similar to from the Miocene Monterey Shale ( Williams and Reimer 1983 , Williams 1984 ) and the Jurassic Jet Rock Shale ( ‘Brien 1990 ). While it is true that high quality laminae could kind by the trapping

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