| Reference Type | Journal (article/letter/editorial) |
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| Title | Maastrichtian ammonites from the Hornerstown Formation in New Jersey |
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| Journal | Journal of Paleontology |
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| Authors | Kennedy, W. J. | Author |
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| Cobban, W. A. | Author |
| Year | 1996 (September) | Volume | 70 |
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| Issue | 5 |
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| Publisher | Cambridge University Press (CUP) |
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| DOI | doi:10.1017/s0022336000023842Search in ResearchGate |
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| Generate Citation Formats |
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| Mindat Ref. ID | 417121 | Long-form Identifier | mindat:1:5:417121:2 |
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| GUID | 0 |
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| Full Reference | Kennedy, W. J., Cobban, W. A. (1996) Maastrichtian ammonites from the Hornerstown Formation in New Jersey. Journal of Paleontology, 70 (5) 798-804 doi:10.1017/s0022336000023842 |
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| Plain Text | Kennedy, W. J., Cobban, W. A. (1996) Maastrichtian ammonites from the Hornerstown Formation in New Jersey. Journal of Paleontology, 70 (5) 798-804 doi:10.1017/s0022336000023842 |
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| In | (1996, September) Journal of Paleontology Vol. 70 (5) Cambridge University Press (CUP) |
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| Abstract/Notes | The base of the Paleocene Hornerstown Formation at the Inversand pit and certain other localities in New Jersey yields a diverse phosphatised fauna of Maastrichtian age, including the ammonites Pachydsicus (Neodesmoceras) mokotibensis Collignon, 1952, Sphenodiscus lobatus (Tuomey, 1854), Baculites spp., and Eubaculites carinatus (Morton, 1834). S. lobatus is known from the older Red Bank Sand and Tinton Sand in New Jersey; the other species are known only from the basal Hornerstown. Occurrences at the Inversand pit are regarded as either reworked or remainié, although details of Cretaceous/Paleocene boundary events have been destroyed by pervasive burrowing that pipes the Hornerstown down into the underlying Navesink Formation. |
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