Navesink Formation

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The Navesink Formation is a 66 to 70 mya greensand glauconitic marl and sand geological formation in New Jersey. It is known for its Cretaceous period fossil shell beds and dinosaur bones.[1]

Description

The Navesink Formation, named after Navesink, New Jersey, is typically found above the Mount Laurel Formation and under the Red Bank Formation. There is a 5 mya gap between the Navesink and Mount Laurel Formations.[2] The Navesink varies in depth from Script error: No such module "convert". to Script error: No such module "convert". across its range from Sandy Hook to Pennsville.[3][4]

The Navesink has the highest radon gas potential of the New Jersey geologic[5] formations.

Sites

There are several locations where the Navesink Formation is visible including Poricy Park in Middletown, New Jersey which has several exposures along Poricy Brook. There is also exposure in Big Brook Park in Marlboro, NJ.

Paleofauna

Dinosaurs
Color key
Taxon Reclassified taxon Taxon falsely reported as present Dubious taxon or junior synonym Ichnotaxon Ootaxon Morphotaxon
Notes
Uncertain or tentative taxa are in small text; crossed out taxa are discredited.
Genus Species Material Notes Images
Coelosaurus[6] C. antiquus Tibia An ornithomimid.
Diplotomodon[7] D. horrificus Tooth Indeterminate theropod.
Dryptosaurus[8] D. aquilunguis A large eutyrannosaur.
Hadrosaurus[9] H. foukii Caudal vertebrae A hadrosaurid.
"Hadrosaurus"[10] "H." minor Partial hindlimb, vertebrae, [and] ribs. Probably a basal hadrosaurid different from Hadrosaurus.[8]
Nodosauridae[8] Indeterminate Vertebra An indeterminate nodosaurid, possibly a new taxon.
Ornithomimosauria[11] Indeterminate End of metatarsal, end of tibia, pedal phalanges Ornithomimosaur part of "Laelaps" macropus.
"Teihivenator" Indeterminate Tibia fragments Informal genus of tyrannosauroid theropod. Might be a chimera of tyrannosauroid and ornithomimid remains.
Telmatornis T. priscus Possibly a charadriform.
Tyrannosauroidea[12] Indeterminate Tibia Tyrannosauroid part of "Laelaps" macropus. A small tyrannosauroid, possibly juvenile, closely related to Bistahieversor.
Tyrannosauroidea[13] Indeterminate Pedal phalanx A large tyrannosauroid possibly the same taxon as "Laelaps" macropus.

References

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  6. Baird D., and Horner, J., 1979, "Cretaceous dinosaurs of North Carolina", Brimleyana 2: 1–28
  7. "Table 5.1," in Weishampel, et al. (2004). Page 114.
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  9. "Table 20.1," in Weishampel, et al. (2004). Page 442.
  10. "Table 20.1," in Weishampel, et al. (2004). Page 441.
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