BETA TEST - Fossil data and pages are very much experimental and under development. Please report any problems
Ragley Lumber #D1 well - 10685ft, Vermillion Parish, Louisiana, USA
| Lat/Long (Decimal) | 30,-92 |
|---|---|
| Co-ordinates Derivation | not explained |
| Given Location | Louisiana, United States |
| Mindat.org Region (for given coordinates) | Vermillion Parish, Louisiana, USA |
Collections
| Collection | Reference | Stratigraphic Name | Comments | Lithology | Age |
|---|---|---|---|---|---|
| Ragley Lumber #D1 well - 10524ft | Gregory W. A., Hart G. F. (1995) | Wilcox | Gregory and Hart (1995a, pollen and spores) do not recognize the Clairbornian in the core, but in Gregory and Hart (1995, dinoflagellates), they do. Both papers look at the same samples from the same core and derive different age assignments because they treat each independently. RAL elected to enter a uniform age assignment for both papers. | 56 - 33.9 Ma Paleogene | |
| Ragley Lumber #D1 well - 10633ft | Gregory W. A., Hart G. F. (1995) | Wilcox | Gregory and Hart (1995a, pollen and spores) do not recognize the Clairbornian in the core, but in Gregory and Hart (1995, dinoflagellates), they do. Both papers look at the same samples from the same core and derive different age assignments because they treat each independently. RAL elected to enter a uniform age assignment for both papers. | 56 - 33.9 Ma Paleogene | |
| Ragley Lumber #D1 well - 10685ft | Gregory W. A., Hart G. F. (1995) | Wilcox | Gregory and Hart (1995a, pollen and spores) do not recognize the Clairbornian in the core, but in Gregory and Hart (1995, dinoflagellates), they do. Both papers look at the same samples from the same core and derive different age assignments because they treat each independently. RAL elected to enter a uniform age assignment for both papers. | 56 - 33.9 Ma Paleogene | |
| Ragley Lumber #D1 well - 10704ft | Gregory W. A., Hart G. F. (1995) | Wilcox | Gregory and Hart (1995a, pollen and spores) do not recognize the Clairbornian in the core, but in Gregory and Hart (1995, dinoflagellates), they do. Both papers look at the same samples from the same core and derive different age assignments because they treat each independently. RAL elected to enter a uniform age assignment for both papers. | 56 - 33.9 Ma Paleogene | |
| Ragley Lumber #D1 well - 10721ft | Gregory W. A., Hart G. F. (1995) | Wilcox | Gregory and Hart (1995a, pollen and spores) do not recognize the Clairbornian in the core, but in Gregory and Hart (1995, dinoflagellates), they do. Both papers look at the same samples from the same core and derive different age assignments because they treat each independently. RAL elected to enter a uniform age assignment for both papers. | 56 - 33.9 Ma Paleogene | |
| Ragley Lumber #D1 well - 10757ft | Gregory W. A., Hart G. F. (1995) | Wilcox | Gregory and Hart (1995a, pollen and spores) do not recognize the Clairbornian in the core, but in Gregory and Hart (1995, dinoflagellates), they do. Both papers look at the same samples from the same core and derive different age assignments because they treat each independently. RAL elected to enter a uniform age assignment for both papers. | 56 - 33.9 Ma Paleogene | |
| Ragley Lumber #D1 well - 10809ft | Gregory W. A., Hart G. F. (1995) | Wilcox | Gregory and Hart (1995a, pollen and spores) do not recognize the Clairbornian in the core, but in Gregory and Hart (1995, dinoflagellates), they do. Both papers look at the same samples from the same core and derive different age assignments because they treat each independently. RAL elected to enter a uniform age assignment for both papers. | 56 - 33.9 Ma Paleogene | |
| Ragley Lumber #D1 well - 10832ft | Gregory W. A., Hart G. F. (1995) | Wilcox | Gregory and Hart (1995a, pollen and spores) do not recognize the Clairbornian in the core, but in Gregory and Hart (1995, dinoflagellates), they do. Both papers look at the same samples from the same core and derive different age assignments because they treat each independently. RAL elected to enter a uniform age assignment for both papers. | 56 - 33.9 Ma Paleogene | |
| Ragley Lumber #D1 well - 10868ft | Gregory W. A., Hart G. F. (1995) | Wilcox | Horizon sample from drill core. Gregory and Hart (1995a, pollen and spores) do not recognize the Clairbornian in the core, but in Gregory and Hart (1995, dinoflagellates), they do. Both papers look at the same samples from the same core and derive different age assignments because they treat each independently. RAL elected to enter a uniform age assignment for both papers. | siltstone | 56 - 33.9 Ma Paleogene |
| Ragley Lumber #D1 well - 10890ft | Gregory W. A., Hart G. F. (1995) | Wilcox | Horizon sample from drill core. Gregory and Hart (1995a, pollen and spores) do not recognize the Clairbornian in the core, but in Gregory and Hart (1995, dinoflagellates), they do. Both papers look at the same samples from the same core and derive different age assignments because they treat each independently. RAL elected to enter a uniform age assignment for both papers. | siltstone | 56 - 33.9 Ma Paleogene |
| Ragley Lumber #D1 well - 10914ft | Gregory W. A., Hart G. F. (1995) | Horizon sample from drill core. Gregory and Hart (1995a, pollen and spores) do not recognize the Clairbornian in the core, but in Gregory and Hart (1995, dinoflagellates), they do. Both papers look at the same samples from the same core and derive different age assignments because they treat each independently. RAL elected to enter a uniform age assignment for both papers. | siltstone | 56 - 33.9 Ma Paleogene | |
| Ragley Lumber #D1 well - 10935ft | Gregory W. A., Hart G. F. (1995) | Horizon sample from drill core. Gregory and Hart (1995a, pollen and spores) do not recognize the Clairbornian in the core, but in Gregory and Hart (1995, dinoflagellates), they do. Both papers look at the same samples from the same core and derive different age assignments because they treat each independently. RAL elected to enter a uniform age assignment for both papers. | siltstone | 56 - 33.9 Ma Paleogene | |
| Ragley Lumber #D1 well - 11083ft | Gregory W. A., Hart G. F. (1995) | Wilcox | Horizon sample from drill core. Gregory and Hart (1995a, pollen and spores) do not recognize the Clairbornian in the core, but in Gregory and Hart (1995, dinoflagellates), they do. Both papers look at the same samples from the same core and derive different age assignments because they treat each independently. RAL elected to enter a uniform age assignment for both papers. | siltstone | 56 - 33.9 Ma Paleogene |
| Ragley Lumber #D1 well - 11099ft | Gregory W. A., Hart G. F. (1995) | Horizon sample from drill core. Gregory and Hart (1995a, pollen and spores) do not recognize the Clairbornian in the core, but in Gregory and Hart (1995, dinoflagellates), they do. Both papers look at the same samples from the same core and derive different age assignments because they treat each independently. RAL elected to enter a uniform age assignment for both papers. | siltstone | 56 - 33.9 Ma Paleogene | |
| Ragley Lumber #D1 well - 11154ft | Gregory W. A., Hart G. F. (1995) | Wilcox | Horizon sample from drill core. Gregory and Hart (1995a, pollen and spores) do not recognize the Clairbornian in the core, but in Gregory and Hart (1995, dinoflagellates), they do. Both papers look at the same samples from the same core and derive different age assignments because they treat each independently. RAL elected to enter a uniform age assignment for both papers. | siltstone | 56 - 33.9 Ma Paleogene |
| Ragley Lumber #D1 well - 11254ft | Gregory W. A., Hart G. F. (1995) | Wilcox | Horizon sample from drill core. Gregory and Hart (1995a, pollen and spores) do not recognize the Clairbornian in the core, but in Gregory and Hart (1995, dinoflagellates), they do. Both papers look at the same samples from the same core and derive different age assignments because they treat each independently. RAL elected to enter a uniform age assignment for both papers. | siltstone | 56 - 33.9 Ma Paleogene |
| Ragley Lumber #D1 well - 11340ft | Gregory W. A., Hart G. F. (1995) | Horizon sample from drill core. Gregory and Hart (1995a, pollen and spores) do not recognize the Clairbornian in the core, but in Gregory and Hart (1995, dinoflagellates), they do. Both papers look at the same samples from the same core and derive different age assignments because they treat each independently. RAL elected to enter a uniform age assignment for both papers. | siltstone | 56 - 33.9 Ma Paleogene | |
| Ragley Lumber #D1 well - 11412ft | Gregory W. A., Hart G. F. (1995) | Horizon sample from drill core. Gregory and Hart (1995a, pollen and spores) do not recognize the Clairbornian in the core, but in Gregory and Hart (1995, dinoflagellates), they do. Both papers look at the same samples from the same core and derive different age assignments because they treat each independently. RAL elected to enter a uniform age assignment for both papers. | siltstone | 56 - 33.9 Ma Paleogene | |
| Ragley Lumber #D1 well - 11528ft | Gregory W. A., Hart G. F. (1995) | Wilcox | Horizon sample from drill core. Gregory and Hart (1995a, pollen and spores) do not recognize the Clairbornian in the core, but in Gregory and Hart (1995, dinoflagellates), they do. Both papers look at the same samples from the same core and derive different age assignments because they treat each independently. RAL elected to enter a uniform age assignment for both papers. | siltstone | 56 - 33.9 Ma Paleogene |
| Ragley Lumber #D1 well - 11602ft | Gregory W. A., Hart G. F. (1995) | Wilcox | Horizon sample from drill core. Gregory and Hart (1995a, pollen and spores) do not recognize the Clairbornian in the core, but in Gregory and Hart (1995, dinoflagellates), they do. Both papers look at the same samples from the same core and derive different age assignments because they treat each independently. RAL elected to enter a uniform age assignment for both papers. | siltstone | 56 - 33.9 Ma Paleogene |
| Ragley Lumber #D1 well - 11701 | Gregory W. A., Hart G. F. (1995) | Wilcox | Horizon sample from drill core. Gregory and Hart (1995a, pollen and spores) do not recognize the Clairbornian in the core, but in Gregory and Hart (1995, dinoflagellates), they do. Both papers look at the same samples from the same core and derive different age assignments because they treat each independently. RAL elected to enter a uniform age assignment for both papers. | siltstone | 56 - 33.9 Ma Paleogene |
| Ragley Lumber #D1 well - 11835ft | Gregory W. A., Hart G. F. (1995) | Wilcox | Horizon sample from drill core. Gregory and Hart (1995a, pollen and spores) do not recognize the Clairbornian in the core, but in Gregory and Hart (1995, dinoflagellates), they do. Both papers look at the same samples from the same core and derive different age assignments because they treat each independently. RAL elected to enter a uniform age assignment for both papers. | siltstone | 56 - 33.9 Ma Paleogene |
| Ragley Lumber #D1 well - 11928ft | Gregory W. A., Hart G. F. (1995) | Wilcox | Horizon sample from drill core. Gregory and Hart (1995a, pollen and spores) do not recognize the Clairbornian in the core, but in Gregory and Hart (1995, dinoflagellates), they do. Both papers look at the same samples from the same core and derive different age assignments because they treat each independently. RAL elected to enter a uniform age assignment for both papers. | siltstone | 56 - 33.9 Ma Paleogene |
| Ragley Lumber #D1 well - 12056ft | Gregory W. A., Hart G. F. (1995) | Wilcox | Horizon sample from drill core. Gregory and Hart (1995a, pollen and spores) do not recognize the Clairbornian in the core, but in Gregory and Hart (1995, dinoflagellates), they do. Both papers look at the same samples from the same core and derive different age assignments because they treat each independently. RAL elected to enter a uniform age assignment for both papers. | siltstone | 56 - 33.9 Ma Paleogene |
| Ragley Lumber #D1 well - 12139ft | Gregory W. A., Hart G. F. (1995) | Wilcox | Horizon sample from drill core. Gregory and Hart (1995a, pollen and spores) do not recognize the Clairbornian in the core, but in Gregory and Hart (1995, dinoflagellates), they do. Both papers look at the same samples from the same core and derive different age assignments because they treat each independently. RAL elected to enter a uniform age assignment for both papers. | siltstone | 56 - 33.9 Ma Paleogene |
| Ragley Lumber #D1 well - 12255ft | Gregory W. A., Hart G. F. (1995) | Wilcox | Horizon sample from drill core. Gregory and Hart (1995a, pollen and spores) do not recognize the Clairbornian in the core, but in Gregory and Hart (1995, dinoflagellates), they do. Both papers look at the same samples from the same core and derive different age assignments because they treat each independently. RAL elected to enter a uniform age assignment for both papers. | siltstone | 56 - 33.9 Ma Paleogene |
| Ragley Lumber #D1 well - 12292ft | Gregory W. A., Hart G. F. (1995) | Wilcox | Horizon sample from drill core. Gregory and Hart (1995a, pollen and spores) do not recognize the Clairbornian in the core, but in Gregory and Hart (1995, dinoflagellates), they do. Both papers look at the same samples from the same core and derive different age assignments because they treat each independently. RAL elected to enter a uniform age assignment for both papers. | siltstone | 56 - 33.9 Ma Paleogene |
| Ragley Lumber #D1 well - 12348ft | Gregory W. A., Hart G. F. (1995) | Wilcox | Horizon sample from drill core. Gregory and Hart (1995a, pollen and spores) do not recognize the Clairbornian in the core, but in Gregory and Hart (1995, dinoflagellates), they do. Both papers look at the same samples from the same core and derive different age assignments because they treat each independently. RAL elected to enter a uniform age assignment for both papers. | siltstone | 56 - 33.9 Ma Paleogene |
| Ragley Lumber #D1 well - 12472ft | Gregory W. A., Hart G. F. (1995) | Wilcox | Horizon sample from drill core. Gregory and Hart (1995a, pollen and spores) do not recognize the Clairbornian in the core, but in Gregory and Hart (1995, dinoflagellates), they do. Both papers look at the same samples from the same core and derive different age assignments because they treat each independently. RAL elected to enter a uniform age assignment for both papers. | siltstone | 56 - 33.9 Ma Paleogene |
| Ragley Lumber #D1 well - 12541ft | Gregory W. A., Hart G. F. (1995) | Wilcox | Horizon sample from drill core. Gregory and Hart (1995a, pollen and spores) do not recognize the Clairbornian in the core, but in Gregory and Hart (1995, dinoflagellates), they do. Both papers look at the same samples from the same core and derive different age assignments because they treat each independently. RAL elected to enter a uniform age assignment for both papers. | siltstone | 56 - 33.9 Ma Paleogene |
| Ragley Lumber #D1 well - 12687ft | Gregory W. A., Hart G. F. (1995) | Wilcox | Horizon sample from drill core. Gregory and Hart (1995a, pollen and spores) do not recognize the Clairbornian in the core, but in Gregory and Hart (1995, dinoflagellates), they do. Both papers look at the same samples from the same core and derive different age assignments because they treat each independently. RAL elected to enter a uniform age assignment for both papers. | siltstone | 56 - 33.9 Ma Paleogene |
| Ragley Lumber #D1 well - 12784ft | Gregory W. A., Hart G. F. (1995) | Wilcox | Horizon sample from drill core. Gregory and Hart (1995a, pollen and spores) do not recognize the Clairbornian in the core, but in Gregory and Hart (1995, dinoflagellates), they do. Both papers look at the same samples from the same core and derive different age assignments because they treat each independently. RAL elected to enter a uniform age assignment for both papers. | siltstone | 56 - 33.9 Ma Paleogene |
| Ragley Lumber #D1 well - 12855ft | Gregory W. A., Hart G. F. (1995) | Wilcox | Horizon sample from drill core. Gregory and Hart (1995a, pollen and spores) do not recognize the Clairbornian in the core, but in Gregory and Hart (1995, dinoflagellates), they do. Both papers look at the same samples from the same core and derive different age assignments because they treat each independently. RAL elected to enter a uniform age assignment for both papers. | siltstone | 56 - 33.9 Ma Paleogene |
| Ragley Lumber #D1 well - 12958ft | Gregory W. A., Hart G. F. (1995) | Wilcox | Horizon sample from drill core. Gregory and Hart (1995a, pollen and spores) do not recognize the Clairbornian in the core, but in Gregory and Hart (1995, dinoflagellates), they do. Both papers look at the same samples from the same core and derive different age assignments because they treat each independently. RAL elected to enter a uniform age assignment for both papers. | siltstone | 56 - 33.9 Ma Paleogene |
| Ragley Lumber #D1 well - 13020ft | Gregory W. A., Hart G. F. (1995) | Wilcox | Horizon sample from drill core. Gregory and Hart (1995a, pollen and spores) do not recognize the Clairbornian in the core, but in Gregory and Hart (1995, dinoflagellates), they do. Both papers look at the same samples from the same core and derive different age assignments because they treat each independently. RAL elected to enter a uniform age assignment for both papers. | siltstone | 56 - 33.9 Ma Paleogene |
| Ragley Lumber #D1 well - 13255ft | Gregory W. A., Hart G. F. (1995) | Wilcox | Horizon sample from drill core. Gregory and Hart (1995a, pollen and spores) do not recognize the Clairbornian in the core, but in Gregory and Hart (1995, dinoflagellates), they do. Both papers look at the same samples from the same core and derive different age assignments because they treat each independently. RAL elected to enter a uniform age assignment for both papers. | siltstone | 56 - 33.9 Ma Paleogene |
| Ragley Lumber #D1 well - 13319ft | Gregory W. A., Hart G. F. (1995) | Wilcox | Horizon sample from drill core. Gregory and Hart (1995a, pollen and spores) do not recognize the Clairbornian in the core, but in Gregory and Hart (1995, dinoflagellates), they do. Both papers look at the same samples from the same core and derive different age assignments because they treat each independently. RAL elected to enter a uniform age assignment for both papers. | siltstone | 56 - 33.9 Ma Paleogene |
| Ragley Lumber #D1 well - 13382ft | Gregory W. A., Hart G. F. (1995) | Wilcox | Horizon sample from drill core. Gregory and Hart (1995a, pollen and spores) do not recognize the Clairbornian in the core, but in Gregory and Hart (1995, dinoflagellates), they do. Both papers look at the same samples from the same core and derive different age assignments because they treat each independently. RAL elected to enter a uniform age assignment for both papers. | siltstone | 56 - 33.9 Ma Paleogene |
| Ragley Lumber #D1 well - 14007ft | Gregory W. A., Hart G. F. (1995) | Wilcox | Horizon sample from drill core. Gregory and Hart (1995a, pollen and spores) do not recognize the Clairbornian in the core, but in Gregory and Hart (1995, dinoflagellates), they do. Both papers look at the same samples from the same core and derive different age assignments because they treat each independently. RAL elected to enter a uniform age assignment for both papers. | siltstone | 56 - 33.9 Ma Paleogene |
| Ragley Lumber #D1 well - 14063ft | Gregory W. A., Hart G. F. (1995) | Wilcox | Horizon sample from drill core. Gregory and Hart (1995a, pollen and spores) do not recognize the Clairbornian in the core, but in Gregory and Hart (1995, dinoflagellates), they do. Both papers look at the same samples from the same core and derive different age assignments because they treat each independently. RAL elected to enter a uniform age assignment for both papers. | siltstone | 56 - 33.9 Ma Paleogene |
| Ragley Lumber #D1 well - 14251ft | Gregory W. A., Hart G. F. (1995) | Horizon sample from drill core. Gregory and Hart (1995a, pollen and spores) do not recognize the Clairbornian in the core, but in Gregory and Hart (1995, dinoflagellates), they do. Both papers look at the same samples from the same core and derive different age assignments because they treat each independently. RAL elected to enter a uniform age assignment for both papers. | siltstone | 56 - 33.9 Ma Paleogene | |
| Ragley Lumber #D1 well - 14359ft | Gregory W. A., Hart G. F. (1995) | Wilcox | Horizon sample from drill core. Gregory and Hart (1995a, pollen and spores) do not recognize the Clairbornian in the core, but in Gregory and Hart (1995, dinoflagellates), they do. Both papers look at the same samples from the same core and derive different age assignments because they treat each independently. RAL elected to enter a uniform age assignment for both papers. | siltstone | 56 - 33.9 Ma Paleogene |
| Ragley Lumber #D1 well - 14423ft | Gregory W. A., Hart G. F. (1995) | Wilcox | Horizon sample from drill core. Gregory and Hart (1995a, pollen and spores) do not recognize the Clairbornian in the core, but in Gregory and Hart (1995, dinoflagellates), they do. Both papers look at the same samples from the same core and derive different age assignments because they treat each independently. RAL elected to enter a uniform age assignment for both papers. | siltstone | 56 - 33.9 Ma Paleogene |
| Ragley Lumber #D1 well - 14445ft | Gregory W. A., Hart G. F. (1995) | Wilcox | Horizon sample from drill core. Gregory and Hart (1995a, pollen and spores) do not recognize the Clairbornian in the core, but in Gregory and Hart (1995, dinoflagellates), they do. Both papers look at the same samples from the same core and derive different age assignments because they treat each independently. RAL elected to enter a uniform age assignment for both papers. | siltstone | 56 - 33.9 Ma Paleogene |
| Ragley Lumber #D1 well - 14526ft | Gregory W. A., Hart G. F. (1995) | Wilcox | Horizon sample from drill core. Gregory and Hart (1995a, pollen and spores) do not recognize the Clairbornian in the core, but in Gregory and Hart (1995, dinoflagellates), they do. Both papers look at the same samples from the same core and derive different age assignments because they treat each independently. RAL elected to enter a uniform age assignment for both papers. | siltstone | 56 - 33.9 Ma Paleogene |
| Ragley Lumber #D1 well - 14544ft | Gregory W. A., Hart G. F. (1995) | Wilcox | Horizon sample from drill core. Gregory and Hart (1995a, pollen and spores) do not recognize the Clairbornian in the core, but in Gregory and Hart (1995, dinoflagellates), they do. Both papers look at the same samples from the same core and derive different age assignments because they treat each independently. RAL elected to enter a uniform age assignment for both papers. | siltstone | 56 - 33.9 Ma Paleogene |
| Ragley Lumber #D1 well - 14681ft | Gregory W. A., Hart G. F. (1995) | Wilcox | Horizon sample from drill core. Gregory and Hart (1995a, pollen and spores) do not recognize the Clairbornian in the core, but in Gregory and Hart (1995, dinoflagellates), they do. Both papers look at the same samples from the same core and derive different age assignments because they treat each independently. RAL elected to enter a uniform age assignment for both papers. | siltstone | 56 - 33.9 Ma Paleogene |
| Ragley Lumber #D1 well - 14747ft | Gregory W. A., Hart G. F. (1995) | Wilcox | Horizon sample from drill core. Gregory and Hart (1995a, pollen and spores) do not recognize the Clairbornian in the core, but in Gregory and Hart (1995, dinoflagellates), they do. Both papers look at the same samples from the same core and derive different age assignments because they treat each independently. RAL elected to enter a uniform age assignment for both papers. | siltstone | 56 - 33.9 Ma Paleogene |
| Ragley Lumber #D1 well - 14792ft | Gregory W. A., Hart G. F. (1995) | Wilcox | Horizon sample from drill core. Gregory and Hart (1995a, pollen and spores) do not recognize the Clairbornian in the core, but in Gregory and Hart (1995, dinoflagellates), they do. Both papers look at the same samples from the same core and derive different age assignments because they treat each independently. RAL elected to enter a uniform age assignment for both papers. | siltstone | 56 - 33.9 Ma Paleogene |
| Ragley Lumber #D1 well - 14914ft | Gregory W. A., Hart G. F. (1995) | Wilcox | Horizon sample from drill core. Gregory and Hart (1995a, pollen and spores) do not recognize the Clairbornian in the core, but in Gregory and Hart (1995, dinoflagellates), they do. Both papers look at the same samples from the same core and derive different age assignments because they treat each independently. RAL elected to enter a uniform age assignment for both papers. | siltstone | 56 - 33.9 Ma Paleogene |
Recorded Fossils
References
| Gregory W. A., Hart G. F. (1995) Distribution of pollen and spores in a subsurface marine Wilcox (Paleocene-Eocene) section in southwest Louisiana, Palynology 19, 1-43 |
Data courtesy of: PBDB: The Paleobiology Database, Creative Commons CC-BY licenced. , GBIF: the Global Biodiversity Information Facility, various licences, iDigBio, various licences, and EOL: The Encyclopedia of Life (Open Data Public Domain). Because fossils are made of minerals too!
