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Four coarsening upward parasequences, ranging in thickness from 4 to 17m are present in an Upper Mannville (Aptian to early Albian) core from east central Alberta. These parasequences are composed of three main facies; mudstone, mudstone/sandstone, and bioturbated rippled sandstone. Based on sedimentological, ichnological, palynological, and geochemical data these parasequences are interpreted as crevasse splay deposits. A low diversity suite of trace fossils (Arenicolites, Chondrites, Gyrolithes, Monocraterion, Palaeophycus, Planolites, Skolithos, and Teichichnus) characterize these units. The ichnological character of these deposits is unique and represents a powerful tool in the delineation and interpretation of marginal marine environments.

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