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Ocean Drilling Program data indicates a major compositional shift in debris flow deposits around 1.1 million years before present. The dataset, from Geoscience Australia, describes changes in the Lambert Glacier-Amery Ice Shelf drainage system during the late Neogene, including the deposition of a trough mouth fan prior to the Brunhes Matuyama Boundary (780 ka BP). It provides stratigraphic evidence for the evolution of ice discharge patterns and their interaction with climate cycles.
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