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Diatom and foraminiferal analyses of the Pleistocene turbidites in the Cascadia margin suggest that turbidite sediments originated mainly in the landward shelf area and were displaced to the present deep-sea site, which maintained a constant depth during this time. Abundant and highly fluctuating occurrences of shallowmarine and nonmarine diatoms may reflect the global glacioeustatic sea level changes in the Pleistocene.

Data report: diatom and foraminiferal assemblages in Pleistocene turbidite sediments from the Cascadia margin (IODP Expedition 311), northeast Pacific