Raibliania: Difference between revisions
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'''''Raibliania''''' is an extinct genus of [[Tanystropheidae|tanystropheid]] [[Archosauromorpha|archosauromorph]] discovered in the [[Calcare del Predil Formation]] in [[Italy]].<ref name=Dallavecchia2020>{{Cite journal|author=Fabio Marco Dalla Vecchia |year=2020 |title=''Raibliania calligarisi'' gen. n., sp. n., a new tanystropheid (Diapsida, Tanystropheidae) from the Upper Triassic (Carnian) of northeastern Italy |journal=Rivista Italiana di Paleontologia e Stratigrafia |volume=126 |issue=1 |pages=197–222 |doi=10.13130/2039-4942/13041 }}</ref> It lived during the [[Carnian]] stage of the [[Late Triassic]] and it was related to ''[[Tanystropheus]]''. ''Raibliania'' is distinct from ''Tanystropheus'' due to some distinct features of the cervical vertebrae and teeth.<ref name=Dallavecchia2020 /> The [[type species]] is '''''Raibliania calligarisi''''', named in 2020. The [[holotype]] ( |
'''''Raibliania''''' is an extinct genus of [[Tanystropheidae|tanystropheid]] [[Archosauromorpha|archosauromorph]] discovered in the [[Calcare del Predil Formation]] in [[Italy]].<ref name=Dallavecchia2020>{{Cite journal|author=Fabio Marco Dalla Vecchia |year=2020 |title=''Raibliania calligarisi'' gen. n., sp. n., a new tanystropheid (Diapsida, Tanystropheidae) from the Upper Triassic (Carnian) of northeastern Italy |journal=Rivista Italiana di Paleontologia e Stratigrafia |volume=126 |issue=1 |pages=197–222 |doi=10.13130/2039-4942/13041 }}</ref> It lived during the [[Carnian]] stage of the [[Late Triassic]] and it was related to ''[[Tanystropheus]]''. ''Raibliania'' is distinct from ''Tanystropheus'' due to some distinct features of the cervical vertebrae and teeth.<ref name=Dallavecchia2020 /> The [[type species]] is '''''Raibliania calligarisi''''', named in 2020. The [[holotype]] (MFSN 27532) consists of a partial post-cranial skeleton, with the known elements including [[Vertebra|vertebrae]] ([[sacrum|sacral]], [[Cervical vertebrae|cervical]] and [[dorsal (anatomy)|dorsal]]; sans caudal), a single [[tooth]], several [[Rib cage|ribs]], [[gastralia]] and parts of the [[pelvis]] ([[ilium (bone)|ilium]] and [[pubis (bone)|pubis]]). |
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In their 2024 description of ''[[Dinocephalosaurus]]'' material, Spiekman ''et al''. suggested that the ''Raibliania'' fossil material may actually be referrable to ''[[Tanystropheus]]'', due to notable similarities between skeletons of the two taxa. The results of their [[phylogenetic analysis]], which included both ''Raibliania'' and ''Tanystropheus'' spp., are shown in the [[cladogram]] below:<ref name="Dinocephalosaurus2024">{{Cite journal |last1=Spiekman |first1=Stephan N. F. |last2=Wang |first2=Wei |last3=Zhao |first3=Lijun |last4=Rieppel |first4=Olivier |last5=Fraser |first5=Nicholas C. |last6=Li |first6=Chun |date=2024-02-23 |title=''Dinocephalosaurus orientalis'' Li, 2003: a remarkable marine archosauromorph from the Middle Triassic of southwestern China |journal=Earth and Environmental Science Transactions of The Royal Society of Edinburgh |language=en |pages=1–33 |doi=10.1017/S175569102400001X |issn=1755-6910}}</ref> |
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|{{clade |
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|1=''[[Jesairosaurus]]'' |
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|2={{clade |
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|1=''[[Protorosaurus]]'' |
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|2={{clade |
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|1=''[[Prolacerta]]'' |
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|2={{clade |
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|1=[[Crocopoda]] |
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|2={{clade |
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|1=[[Dinocephalosauridae]] |
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|2={{clade |
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|1=''[[Fuyuansaurus]]'' |
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|label2=[[Tanystropheidae]] |
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|2={{clade |
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|1={{clade |
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|1=''[[Macrocnemus bassanii]]'' |
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|2={{clade |
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|1=''Macrocnemus fuyuanensis'' |
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|2={{clade |
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|1=''Macrocnemus obristi'' |
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|2=''[[Elessaurus]]'' }} }} }} |
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|3={{clade |
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|1={{clade |
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|1=''[[Amotosaurus]]'' |
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|2=''[[Ozimek volans|Ozimek]]'' }} |
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|3={{clade |
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|1=''[[Sclerostropheus]]'' |
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|2=''[[Langobardisaurus]]'' |
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|3=[[AMNH]] FARB 7206 {{small|(an unnamed ''Tanytrachelos''-like tanystropheid from [[New Jersey]])}} |
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|4=''[[Tanytrachelos]]'' |
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|5=''[[Gracilicollum]]'' |
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|6={{clade |
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|1=''[[Tanystropheus]] hydroides'' |
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|2=GMPKU P 1527 {{small|(''T.'' cf. ''hydroides'')}} |
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|3={{clade |
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|1=''Tanystropheus longobardicus'' |
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|2='''''Raibliania''''' |
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}} }} }} }} }} }} }} }} }} }} }}|label1=[[Archosauromorpha]]}} |
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==References== |
==References== |
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Revision as of 23:12, 23 February 2024
| Raibliania Temporal range: Late Triassic,
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| Photograph of the holotype (top) and line drawing (bottom) | |
Scientific classification 
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| Domain: | Eukaryota |
| Kingdom: | Animalia |
| Phylum: | Chordata |
| Class: | Reptilia |
| Clade: | Archosauromorpha |
| Family: | †Tanystropheidae |
| Genus: | †Raibliania Dalla Vecchia, 2020 |
| Type species | |
| †Raibliania calligarisi Dalla Vecchia, 2020
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Raibliania is an extinct genus of tanystropheid archosauromorph discovered in the Calcare del Predil Formation in Italy.[1] It lived during the Carnian stage of the Late Triassic and it was related to Tanystropheus. Raibliania is distinct from Tanystropheus due to some distinct features of the cervical vertebrae and teeth.[1] The type species is Raibliania calligarisi, named in 2020. The holotype (MFSN 27532) consists of a partial post-cranial skeleton, with the known elements including vertebrae (sacral, cervical and dorsal; sans caudal), a single tooth, several ribs, gastralia and parts of the pelvis (ilium and pubis).
In their 2024 description of Dinocephalosaurus material, Spiekman et al. suggested that the Raibliania fossil material may actually be referrable to Tanystropheus, due to notable similarities between skeletons of the two taxa. The results of their phylogenetic analysis, which included both Raibliania and Tanystropheus spp., are shown in the cladogram below:[2]
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References
- ^ a b Fabio Marco Dalla Vecchia (2020). "Raibliania calligarisi gen. n., sp. n., a new tanystropheid (Diapsida, Tanystropheidae) from the Upper Triassic (Carnian) of northeastern Italy". Rivista Italiana di Paleontologia e Stratigrafia. 126 (1): 197–222. doi:10.13130/2039-4942/13041.
- ^ Spiekman, Stephan N. F.; Wang, Wei; Zhao, Lijun; Rieppel, Olivier; Fraser, Nicholas C.; Li, Chun (2024-02-23). "Dinocephalosaurus orientalis Li, 2003: a remarkable marine archosauromorph from the Middle Triassic of southwestern China". Earth and Environmental Science Transactions of The Royal Society of Edinburgh: 1–33. doi:10.1017/S175569102400001X. ISSN 1755-6910.
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