Dollymae
| Dollymae Temporal range: Tournaisian | |
|---|---|
| Scientific classification | |
| Kingdom: | Animalia |
| Phylum: | Chordata |
| Class: | †Conodonta |
| Genus: | †Dollymae Hass, 1959[1] |
| Species | |
| |
Dollymae is an extinct genus of conodonts.[2][3]
Use in stratigraphy
The Tournaisian, the oldest age of the Mississippian (also known as Lower Carboniferous) contains eight conodont biozones, one of which is the zone of Dollymae bouckaerti.
References
- ↑ Conodonts from the Chappel limestone of Texas. Wilbert H. Hass, 1959
- ↑ The origin and evolution of the middle Dinantian conodont genera Doliognathus, Dollymae, Scaliognathus, and Staurognathus, and related forms. Ronald L. Austin and Eric Groessens, Annales de la Société géologique de Belgique, Volume 95 (1972), Fascicule 2, pages 229-238 (URL, retrieved 24 April 2016)
- ↑ Les conodontes du Tournaisien supérieur de la Belgique: note préliminaire. E Groessens, 1971, Service Géologique de Belgique
External links
- Dollymae at the Encyclopedia of Life
- Dollymae at fossilworks.org (retrieved 3 July 2016)
This article is issued from Wikipedia - version of the 7/9/2016. The text is available under the Creative Commons Attribution/Share Alike but additional terms may apply for the media files.