Concordia (genus)

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Concordia
Temporal range: Late Carboniferous, 300 Ma
Scientific classification e
Kingdom: Animalia
Phylum: Chordata
Class: Reptilia
Family: Captorhinidae
Genus: †Concordia
Müller & Reisz, 2005
Species:
† C. cunninghami
Binomial name
Concordia cunninghami
Müller & Reisz, 2005
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Concordia is an extinct genus of Late Carboniferous captorinid known from Greenwood County, Kansas of the United States.[1]

Description

Concordia is known from the holotype KUVP 8702a&b, well preserved skull in dorsal view along with its counterpart, a partial preserved braincase in ventral view, and from the referred specimen KUVP 96/95, well preserved skull in ventral view and a poorly preserved dorsal counterpart. It was collected in the Hamilton Quarry, from the Calhouns Shale Formation of the Shawnee Group, dating to the Virgilian stage (or alternatively late Kasimovian to early Gzhelian stage) of the Late Pennsylvanian Series, about 300 million years ago. Concordia was originally thought to be the basalmost known member of Captorhinidae.[1] A novel phylogenic study of primitive reptile relationships by Müller & Reisz in 2006 recovered Thuringothyris as a sister taxon of the Captorhinidae, and therefore, by definition, Thuringothyris represents the basalmost known captorhinid.[2] The same results were obtained in later phylogenic analyses.[3][4] Concordia is still the earliest known captorhinid as all other captorhinid taxa are known only from Permian deposits.[2]

Etymology

Concordia was first named by Johannes Müller and Robert R. Reisz in 2005 and the type species is Concordia cunninghami. The generic name is derived from the Latin concordia, meaning "unity" or "harmony". The specific name honors Christopher R. Cunningham for studying this taxon as part of his PhD thesis on the Hamilton Quarry.[1]

References

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  2. 2.0 2.1 Muller, J. and Reisz, R.R. (2006). "The phylogeny of early eureptiles: Comparing parsimony and Bayesian approaches in the investigation of a basal fossil clade." Systematic Biology, 55(3):503-511. doi:10.1080/10635150600755396
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