Maastrichtian ammonites from the Hornerstown Formation in New Jersey
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 s...
| Main Authors: | , |
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| Format: | Journal article |
| Language: | English |
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1996
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| _version_ | 1826283434589290496 |
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| author | Kennedy, W Cobban, W |
| author_facet | Kennedy, W Cobban, W |
| author_sort | Kennedy, W |
| collection | OXFORD |
| description | 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 remainie, although details of Cretaceous/Paleocene boundary events have been destroyed by pervasive burrowing that pipes the Hornerstown down into the underlying Navesink Formation. |
| first_indexed | 2024-03-07T00:58:51Z |
| format | Journal article |
| id | oxford-uuid:8907502e-b4ae-41b7-94b9-2d9f56c3e35b |
| institution | University of Oxford |
| language | English |
| last_indexed | 2024-03-07T00:58:51Z |
| publishDate | 1996 |
| record_format | dspace |
| spelling | oxford-uuid:8907502e-b4ae-41b7-94b9-2d9f56c3e35b2022-03-26T22:21:39ZMaastrichtian ammonites from the Hornerstown Formation in New JerseyJournal articlehttp://purl.org/coar/resource_type/c_dcae04bcuuid:8907502e-b4ae-41b7-94b9-2d9f56c3e35bEnglishSymplectic Elements at Oxford1996Kennedy, WCobban, WThe 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 remainie, although details of Cretaceous/Paleocene boundary events have been destroyed by pervasive burrowing that pipes the Hornerstown down into the underlying Navesink Formation. |
| spellingShingle | Kennedy, W Cobban, W Maastrichtian ammonites from the Hornerstown Formation in New Jersey |
| title | Maastrichtian ammonites from the Hornerstown Formation in New Jersey |
| title_full | Maastrichtian ammonites from the Hornerstown Formation in New Jersey |
| title_fullStr | Maastrichtian ammonites from the Hornerstown Formation in New Jersey |
| title_full_unstemmed | Maastrichtian ammonites from the Hornerstown Formation in New Jersey |
| title_short | Maastrichtian ammonites from the Hornerstown Formation in New Jersey |
| title_sort | maastrichtian ammonites from the hornerstown formation in new jersey |
| work_keys_str_mv | AT kennedyw maastrichtianammonitesfromthehornerstownformationinnewjersey AT cobbanw maastrichtianammonitesfromthehornerstownformationinnewjersey |