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The Paleocene–Eocene Chickaloon Formation of southern Alaska represents rapid deposition in a floodbasin setting, contains abundant and diverse fossil plant material, and spans the Paleocene–Eocene Thermal Maximum (PETM). Sedimentologic, lithofacies, and chemostratigraphic analyses of exposures of the Chickaloon Formation were conducted in order to provide a contextual framework for this, late Paleocene–early...
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