全球变化知识资源中心

High-frequency incised valley systems and subaerial exposure surfaces are prevalent in Aptian-aged units, having been documented in numerous basins around the world. In light of a growing body of palynological, geochemical and sedimentological evidence, a glacio-eustatic mechanism for their generation has been suggested, driven by the waxing and waning of polar ice caps. The densely-penetrated McMurray Formation of north-eastern Alberta, Canada, provides a unique opportunity to test for an Aptian glacio-eustatic signal within the Western Canadian Foreland Basin. This study combines detailed drill core description with wireline log-based stratigraphic analysis to map and evaluate a series of drainage networks located along the cratonic edge of the Western Canadian Foreland Basin. Four stratigraphically distinct composite channel-form bodies are documented across an area >14 000 km(2). Composite channel-form bodies are up to 50 km wide and locally exceed 70 m thick, subtending from upward-coarsening parasequence sets 2 to 12 m thick; bounding marine flooding surfaces are mappable over distances exceeding 280 km along the north-south trending basin. Detailed internal fill characterization of the four composite channel-form bodies suggests that three represent tidal-fluvial incised valley networks, and one represents a deltaic distributary system. At least six cycles of transgression and regression are apparent within the McMurray Formation stratigraphy. Recent biostratigraphic assessment has constrained deposition of the McMurray Formation between ca 125 Ma and 118 Ma, and periods on the order of 0 center dot 7 to 1 center dot 7 Ma are estimated for the mapped transgressive-regressive cycles. The high frequency nature of these Aptian sequences suggests that the sea-level oscillations recorded in McMurray Formation strata are consistent with a glacio-eustatic driver. Linking the internal stratigraphic architecture of the McMurray Formation with interpreted global cooling events and sea-level drops provides the first evidence of glacio-eustasy within Early Cretaceous strata of western Canada.