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- W2024361707 abstract "A 20 m long piston core from a basement ridge on the continental rise off southeastern Canada provides a 0.9 Ma record of distal continental margin sedimentation. Sediment sources are distinguished by sand and clay-sized mineralogy and detrital palynomorphs. They include detritus eroded from (a) northern Canadian Shield and lower Paleozoic rocks transported southward through the Labrador Sea, (b) the Grand Banks and (c) the Gulf of St Lawrence and Newfoundland. Isotopic stratigraphy allows correlation of glacial and interglacial stages with changes in sources and flux rates via different transport processes (nepheloid layer, ice-rafting and distal turbidity currents). The glacial history of southeastern Canada is interpreted from variation in the flux and type of detrital material, and correlation with other data from the continental margin. From stages 27 to 15, the Grand Banks formed a forested coastal plain; limited local glaciation may have occurred in stages 18 and 16. Tertiary regolith and Cretaceous clays were stripped from land areas in stages 14 and 12, culminating in the excavation of the Laurentian Channel late in stage 12. Extensive cold-based ice sheets are inferred for glacial stages 10, 8 and 6, with less severe glaciation in stages 4 and 2. Extent of this local Appalachian ice correlates poorly with global ice volumes." @default.
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- W2024361707 date "1994-01-01" @default.
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- W2024361707 title "A 1 Ma record of sediment flux south of the grand banks used to infer the development of glaciation in southeastern Canada" @default.
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- W2024361707 doi "https://doi.org/10.1016/0277-3791(94)90123-6" @default.
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