Navesink Formation
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] DescriptionThe 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 45 feet (14 m) to 65 feet (20 m) 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. SitesThere 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
Genus
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Species
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Material
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Notes
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Images
| Coelosaurus[6]
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C. antiquus
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Tibia
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An ornithomimid.
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| Diplotomodon[7]
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D. horrificus
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Tooth
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Indeterminate theropod.
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| Dryptosaurus[8]
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D. aquilunguis
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A large eutyrannosaur.
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| Hadrosaurus[9]
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H. foukii
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Caudal vertebrae
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A hadrosaurid.
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| "Hadrosaurus"[10]
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"H." minor
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Partial hindlimb, vertebrae, [and] ribs.
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Probably a basal hadrosaurid different from Hadrosaurus.[8]
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| Nodosauridae[8]
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Indeterminate
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Vertebra
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An indeterminate nodosaurid, possibly a new taxon.
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| Ornithomimosauria[11]
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Indeterminate
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End of metatarsal, end of tibia, pedal phalanges
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Ornithomimosaur part of "Laelaps" macropus.
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| "Teihivenator"
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Indeterminate
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Tibia fragments
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Informal genus of tyrannosauroid theropod. Might be a chimera of tyrannosauroid and ornithomimid remains.
| Telmatornis
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T. priscus
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Possibly a charadriform.
| Tyrannosauroidea[12]
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Indeterminate
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Tibia
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Tyrannosauroid part of "Laelaps" macropus. A small tyrannosauroid, possibly juvenile, closely related to Bistahieversor.
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| Tyrannosauroidea[13]
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Indeterminate
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Pedal phalanx
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A large tyrannosauroid possibly the same taxon as "Laelaps" macropus.
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| References
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