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- W1785451360 abstract "Paleoslope models of foraminifera in the Upper Cretaceous of the New Jersey coastal plain are utilized to estimate paleobathymetric change during cycles of rising and falling sea level. The paleoslope method estimates change in sea level from the distribution of foraminiferal assemblages and species on a baseline parallel to the regional dip. The paleoslope is the restoration of the original depositional slope of the basin. The paleobathymetry of the foraminifera along the paleoslope is estimated from the gradient of the original depositional slope. Application of the paleoslope model to the Campanian of New Jersey indicates a maximum rise of..." @default.
- W1785451360 created "2016-06-24" @default.
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- W1785451360 date "1988-01-01" @default.
- W1785451360 modified "2023-09-27" @default.
- W1785451360 title "FORAMINIFERAL MODELING OF SEA-LEVEL CHANGE IN THE LATE CRETACEOUS OF NEW JERSEY" @default.
- W1785451360 doi "https://doi.org/10.2110/pec.88.01.0289" @default.
- W1785451360 hasPublicationYear "1988" @default.
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