Jump to content

Cargninia: Difference between revisions

From Wikipedia, the free encyclopedia
Content deleted Content added
m WPCleaner (v0.99) Repairing link to disambiguation page - (You can help) - Generic name
No edit summary
Line 18: Line 18:
}}
}}


'''''Cargninia''''' is an [[extinct]] [[genus]] of [[basal (phylogenetics)|basal]] [[Lepidosauria|lepidosaur]] from the Late [[Triassic]] period. It lived during the [[late Triassic]] [[period (geology)|period]] ([[Carnian]] to [[Norian]] stage) in what is now [[Faxinal do Soturno]], [[Rio Grande do Sul]], southern [[Brazil]]. It is known from the [[holotype]] UFRGS&nbsp;PV&nbsp;1027&nbsp;T, a partial [[dentary]], recovered from the middle section of the [[Caturrita Formation]]. ''Cargninia'' was named by [[José Fernando Bonaparte]], César Leandro Schultz, Marina Bento Soares and Agustín G. Martinelli in [[2010 in paleontology|2010]] and the [[type species]] is ''Cargninia enigmatica''. The [[name of a biological genus|generic name]] honors [[Padre Daniel Cargnin]], a Brazilian fossil collector, and the [[specific name]] means “enigmatic” in reference to the basal position within the Lepidosauria.<ref name="BonaparteFauna">{{Cite journal|author=José Fernando Bonaparte, César Leandro Schultz, Marina Bento Soares and Agustín G. Martinelli |year=2010 |title=La Fauna local de faxinal do soturno, Triasico tardio de Rio Grande do Sul, Brasil |url=http://www.sbpbrasil.org/revista/edicoes/13_3/233a246_La%20fauna%20local.pdf |journal=Revista Brasileira de Paleontologia |volume=13 |issue=3 |pages=233–246 |doi=10.4072/rbp.2010.3.07}}</ref>
'''''Cargninia''''' is an [[extinct]] [[genus]] of [[basal (phylogenetics)|basal]] [[Lepidosauria|lepidosaur]] from the Late [[Triassic]] period. It lived during the [[late Triassic]] [[period (geology)|period]] ([[Carnian]] to [[Norian]] stage) in what is now [[Faxinal do Soturno]], [[Rio Grande do Sul]], southern [[Brazil]]. It is known from the [[holotype]] UFRGS&nbsp;PV&nbsp;1027&nbsp;T, a partial [[dentary]], recovered from the middle section of the [[Caturrita Formation]]. ''Cargninia'' was named by [[José Fernando Bonaparte]], César Leandro Schultz, Marina Bento Soares and Agustín G. Martinelli in [[2010 in paleontology|2010]] and the [[type species]] is ''Cargninia enigmatica''. The [[name of a biological genus|generic name]] honors [[Daniel Cargnin]] priest, a Brazilian fossil collector, and the [[specific name]] means “enigmatic” in reference to the basal position within the Lepidosauria.<ref name="BonaparteFauna">{{Cite journal|author=José Fernando Bonaparte, César Leandro Schultz, Marina Bento Soares and Agustín G. Martinelli |year=2010 |title=La Fauna local de faxinal do soturno, Triasico tardio de Rio Grande do Sul, Brasil |url=http://www.sbpbrasil.org/revista/edicoes/13_3/233a246_La%20fauna%20local.pdf |journal=Revista Brasileira de Paleontologia |volume=13 |issue=3 |pages=233–246 |doi=10.4072/rbp.2010.3.07}}</ref>


==References==
==References==

Revision as of 15:07, 29 May 2011

Cargninia
Temporal range: Late Triassic, Carnian–Norian
Scientific classification
Kingdom:
Phylum:
Class:
Subclass:
Infraclass:
Superorder:
Genus:
Cargninia

Bonaparte et al., 2010
Species

C. enigmatica Bonaparte et al., 2010 (type)

Cargninia is an extinct genus of basal lepidosaur from the Late Triassic period. It lived during the late Triassic period (Carnian to Norian stage) in what is now Faxinal do Soturno, Rio Grande do Sul, southern Brazil. It is known from the holotype UFRGS PV 1027 T, a partial dentary, recovered from the middle section of the Caturrita Formation. Cargninia was named by José Fernando Bonaparte, César Leandro Schultz, Marina Bento Soares and Agustín G. Martinelli in 2010 and the type species is Cargninia enigmatica. The generic name honors Daniel Cargnin priest, a Brazilian fossil collector, and the specific name means “enigmatic” in reference to the basal position within the Lepidosauria.[1]

References

  1. ^ José Fernando Bonaparte, César Leandro Schultz, Marina Bento Soares and Agustín G. Martinelli (2010). "La Fauna local de faxinal do soturno, Triasico tardio de Rio Grande do Sul, Brasil" (PDF). Revista Brasileira de Paleontologia. 13 (3): 233–246. doi:10.4072/rbp.2010.3.07.{{cite journal}}: CS1 maint: multiple names: authors list (link)