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The Lower Cretaceous Viking Formation in the Crystal Field of south-central Alberta contains a thick (30m) sandstone body that has been interpreted as an incised valley fill. The incision surface is marked by a wide-spread Glossifungites -demarcated erosion surface that is penetrated by Diplocraterion and Arenicolites. Distinct trace fossil suites are recognizable above and below this surface. Open marine, distal offshore to lower shoreface suites are present below the surface, while, low diversity, brackish water suites characterize the sediments overlying the surface. A major lowstand of sea level that occurred approximately 97 m. y. ago is believed to be responsible for incisement of the estuarine valley, which was filled during rising sea level.

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