Doliognathus

Doliognathus; Temporal range: Lower Carboniferous PreꞒ Ꞓ O S D C P T J K Pg N
Scientific classification
Kingdom:	Animalia
Phylum:	Chordata
Class:	†Conodonta
Order:	†Prioniodinida
Family:	†Bactrognathidae
Genus:	†Doliognathus; Branson and Mehl, 1941
Species
	†Doliognathus excavata; †Doliognathus latus[1];

Doliognathus is an extinct genus of conodonts in the family Bactrognathidae from the Middle Dinantian (Lower Carboniferous).[2] It is a genus of multielement conodonts.[3]

References

Deep water facies of the Lisburne Group, west-central Brooks Range, Alaska.Dumoulin, J. A., et al, 1992 Proceedings International Conference on Arctic Margins:U.S. Dept. of Interior Minerals Mgt. Service MMS 94-0040. 77-82.
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 [En ligne], Volume 95 (1972), Fascicule 2, 229 - 238 (URL, retrieved 24 April 2016)
Phylogeny of the Multielement Conodont Genera Bactrognathus, Doliognathus and Staurognathus. Karl M. Chauff, Journal of Paleontology, Vol. 59, No. 2 (Mar., 1985), pages 299-309 (Stable URL, retrieved 22 April 2016)

External links

Doliognathus at fossilworks.org (retrieved 22 April 2016)

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[1] Deep water facies of the Lisburne Group, west-central Brooks Range, Alaska.Dumoulin, J. A., et al, 1992 Proceedings International Conference on Arctic Margins:U.S. Dept. of Interior Minerals Mgt. Service MMS 94-0040. 77-82.

[2] 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 [En ligne], Volume 95 (1972), Fascicule 2, 229 - 238 (URL, retrieved 24 April 2016)

[3] Phylogeny of the Multielement Conodont Genera Bactrognathus, Doliognathus and Staurognathus. Karl M. Chauff, Journal of Paleontology, Vol. 59, No. 2 (Mar., 1985), pages 299-309 (Stable URL, retrieved 22 April 2016)