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Foraminiferal assemblages in vibracored sediments within ~5 m of the seafloor document high-resolution sea-level fluctuations and confirm the complex Quaternary depositional history of the New Jersey margin. Biostratigraphic data have been integrated with ongoing 2-D/3-D high-resolution seismic analyses to interpret paleoenvironments of surficial stratigraphy beneath the modern middle-to-outer shelf...
Planktonic foraminifera and coccoliths were analyzed from six gravity cores obtained on a deep terrace located on the upper continental slope of the Gulf of Cadiz, between 400 and 700 m water depth. The lithology of these cores consists mainly of muds with some interbedded sandy or silty foraminifer-rich layers that have been reported as contourites originated by the action of the Mediterranean Outflowing...
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