Translation and analysis of words by ChatGPT artificial intelligence
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ramiform$550828$ - translation to greek
 of the Illinois basin (1958) (20654535006).jpg?width=200)
![Preserved articulated association of conodont elements belonging to the species ''[[Archeognathus]] primus'' (Ordovician, North America)](https://commons.wikimedia.org/wiki/Special:FilePath/Archeognathus primus.png?width=200 "Preserved articulated association of conodont elements belonging to the species ''[[Archeognathus]] primus'' (Ordovician, North America)")
![Figures 1, 2. Conodonts from the Deer Valley Member of the Mauch Chunk Formation, Keystone quarry, Pa. This collection (93RS–79c) is from the lower 10 cm of the Deer Valley Member. Note the nonabraded, although slightly broken, conodont elements of the high-energy oolitic marine facies of the Deer Valley Member.<br>1. ''[[Kladognathus]] sp.'', Sa element, posterior view, X140 2. ''[[Cavusgnathus]] unicornis'', gamma morphotype, Pa element, lateral view, X140 <br>3–9. Conodonts from the uppermost Loyalhanna Limestone Member of the Mauch Chunk Formation, Keystone quarry, Pa. This collection (93RS–79b) is from the upper 10 cm of the Loyalhanna Member. Note the highly abraded and reworked aeolian forms. <br>3, 4. ''[[Kladognathus]] sp.'', Sa element, lateral views, X140 <br>5. ''[[Cavusgnathus]] unicornis'', alpha morphotype, Pa element, lateral view, X140 <br>6, 7. ''[[Cavusgnathus]] sp.'', Pa element, lateral view, X140 <br>8. ''[[Polygnathus]] sp.'', Pa element, upper view, reworked Late Devonian to Early Mississippian morphotype, X140 <br>9. ''[[Gnathodus]] texanus?'', Pa element, upper view, X140 <br>10–14. Conodonts from the basal 20 cm of the Loyalhanna Limestone Member of the Mauch Chunk Formation, Keystone quarry, Pa. (93RS–79a), and Westernport, Md. (93RS–67), note the highly abraded and reworked aeolian forms <br>10. ''[[Polygnathus]] sp.'', Pa element, upper view, reworked Late Devonian to Early Mississippian morphotype, 93RS–79a, X140 <br>11. ''Polygnathus sp.'', Pa element, upper view, reworked Late Devonian to Early Mississippian morphotype, 93RS–67, X140 <br>12. ''[[Gnathodus]] sp.'', Pa element, upper view, reworked Late Devonian(?) through Mississippian morphotype, 93RS–67, X140 <br>13. ''[[Kladognathus]] sp.'', M element, lateral views, 93RS–67, X140 <br>14. ''[[Cavusgnathus]] sp.'', Pa element, lateral view, 93RS–67, X140}}](https://commons.wikimedia.org/wiki/Special:FilePath/Conodonts.jpg?width=200 "Figures 1, 2. Conodonts from the Deer Valley Member of the Mauch Chunk Formation, Keystone quarry, Pa. This collection (93RS–79c) is from the lower 10 cm of the Deer Valley Member. Note the nonabraded, although slightly broken, conodont elements of the high-energy oolitic marine facies of the Deer Valley Member.<br>1. ''[[Kladognathus]] sp.'', Sa element, posterior view, X140 2. ''[[Cavusgnathus]] unicornis'', gamma morphotype, Pa element, lateral view, X140 <br>3–9. Conodonts from the uppermost Loyalhanna Limestone Member of the Mauch Chunk Formation, Keystone quarry, Pa. This collection (93RS–79b) is from the upper 10 cm of the Loyalhanna Member. Note the highly abraded and reworked aeolian forms. <br>3, 4. ''[[Kladognathus]] sp.'', Sa element, lateral views, X140 <br>5. ''[[Cavusgnathus]] unicornis'', alpha morphotype, Pa element, lateral view, X140 <br>6, 7. ''[[Cavusgnathus]] sp.'', Pa element, lateral view, X140 <br>8. ''[[Polygnathus]] sp.'', Pa element, upper view, reworked Late Devonian to Early Mississippian morphotype, X140 <br>9. ''[[Gnathodus]] texanus?'', Pa element, upper view, X140 <br>10–14. Conodonts from the basal 20 cm of the Loyalhanna Limestone Member of the Mauch Chunk Formation, Keystone quarry, Pa. (93RS–79a), and Westernport, Md. (93RS–67), note the highly abraded and reworked aeolian forms <br>10. ''[[Polygnathus]] sp.'', Pa element, upper view, reworked Late Devonian to Early Mississippian morphotype, 93RS–79a, X140 <br>11. ''Polygnathus sp.'', Pa element, upper view, reworked Late Devonian to Early Mississippian morphotype, 93RS–67, X140 <br>12. ''[[Gnathodus]] sp.'', Pa element, upper view, reworked Late Devonian(?) through Mississippian morphotype, 93RS–67, X140 <br>13. ''[[Kladognathus]] sp.'', M element, lateral views, 93RS–67, X140 <br>14. ''[[Cavusgnathus]] sp.'', Pa element, lateral view, 93RS–67, X140}}")
![Complete element set of the conodont ''[[Hindeodus parvus]]''](https://commons.wikimedia.org/wiki/Special:FilePath/Hindeodus elements.jpg?width=200 "Complete element set of the conodont ''[[Hindeodus parvus]]''")
![Life restoration of ''[[Promissum pulchrum]]''](https://commons.wikimedia.org/wiki/Special:FilePath/Promissum NT small.jpg?width=200 "Life restoration of ''[[Promissum pulchrum]]''")
![Panderodus unicostatus]]''](https://commons.wikimedia.org/wiki/Special:FilePath/A body fossil of a Panderodus unicostatus (Branson & Mehl, 1933) from the Waukesha Lagerstätte of Wisconsin, USA.png?width=200 "Panderodus unicostatus]]''")
![Fossils of ''[[Typhloesus]]'', at one time considered the first conodont body fossil.](https://commons.wikimedia.org/wiki/Special:FilePath/Typhloesus fossils 2022.jpg?width=200 "Fossils of ''[[Typhloesus]]'', at one time considered the first conodont body fossil.")
Definition
Wikipedia
 of the Illinois basin (1958) (20654535006).jpg?width=120)
Conodonts (Greek kōnos, "cone", + odont, "tooth") are an extinct group of agnathan (jawless) vertebrates resembling eels, classified in the class Conodonta. For many years, they were known only from their tooth-like oral elements, which are usually found in isolation and are now called conodont elements. Knowledge about soft tissues remains limited. They existed in the world's oceans for over 300 million years, from the Cambrian to the beginning of the Jurassic. Conodont elements are widely used as index fossils, fossils used to define and identify geological periods. The animals are also called Conodontophora (conodont bearers) to avoid ambiguity.
