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dc.contributor.author
Haluza, Alejandro
dc.contributor.author
Canale, Juan Ignacio
dc.date.available
2016-02-01T17:07:05Z
dc.date.issued
2013-04
dc.identifier.citation
Haluza, Alejandro; Canale, Juan Ignacio; A partial pterosaur ulna from the Candeleros Formation (Neuquén Group), Late Cretaceous of Argentina; Fundación de Historia Natural "Félix de Azara"; Historia Natural; 3; 1; 4-2013; 5-12
dc.identifier.issn
0326-1778
dc.identifier.uri
http://hdl.handle.net/11336/3932
dc.description.abstract
The proximal portion of the left ulna of a pterosaur is described. The specimen comes from the Candeleros Formation (Cenomanian), Neuquén Group, at Cabo Alarcón, Neuquén province, Argentina. The analysis of this new specimen allows the re-interpretation of a previously described pterosaur tibia founded at Los Catutos locality, Neuquén (MOZ 2280 P) as a proximal ulna. The new material belongs to a medium-sized pterosaur, considerably larger than previously recorded pterosaurs from this geological unit. The analysis of correlation between ulnar length-pes length in well-known pterodactyloid pterosaurs shows that the new ulna matches well with the inferred size of the Pteraichnus isp. trackmaker recorded from the same formation.
dc.description.abstract
The proximal portion of the left ulna of a pterosaur is described. The specimen comes from the Candeleros Formation (Cenomanian), Neuquén Group, at Cabo Alarcón, Neuquén province, Argentina. The analysis of this new specimen allows the re-interpretation of a previously described pterosaur tibia founded at Los Catutos locality, Neuquén (MOZ 2280 P) as a proximal ulna. The new material belongs to a medium-sized pterosaur, considerably larger than previously recorded pterosaurs from this geological unit. The analysis of correlation between ulnar length-pes length in well-known pterodactyloid pterosaurs shows that the new ulna matches well with the inferred size of the Pteraichnus isp. trackmaker recorded from the same formation.
dc.format
application/pdf
dc.language.iso
eng
dc.publisher
Fundación de Historia Natural "Félix de Azara"
dc.rights
info:eu-repo/semantics/openAccess
dc.rights.uri
https://creativecommons.org/licenses/by-nc-sa/2.5/ar/
dc.subject
Pterosauria
dc.subject
Cretaceous
dc.subject
Neuquen Group
dc.subject
Candeleros Formation
dc.subject
Argentina
dc.subject.classification
Paleontología
dc.subject.classification
Ciencias de la Tierra y relacionadas con el Medio Ambiente
dc.subject.classification
CIENCIAS NATURALES Y EXACTAS
dc.title
A partial pterosaur ulna from the Candeleros Formation (Neuquén Group), Late Cretaceous of Argentina
dc.title
Una ulna parcial de Pterosauria de la Formación Candeleros (Grupo Neuquén), Cretácico tardío de Argentina
dc.type
info:eu-repo/semantics/article
dc.type
info:ar-repo/semantics/artículo
dc.type
info:eu-repo/semantics/publishedVersion
dc.date.updated
2016-03-30 10:35:44.97925-03
dc.journal.volume
3
dc.journal.number
1
dc.journal.pagination
5-12
dc.journal.pais
Argentina
dc.journal.ciudad
Ciudad Autónoma de Buenos Aires
dc.conicet.avisoEditorial
No se permite la reproducción parcial o total, el almacenamiento, el
alquiler, la transmisión o la transformación de esta revista, en cualquier forma o por cualquier medio, sea electrónico o
mecánico, mediante fotocopias, digitalización u otros métodos, sin el permiso previo y escrito del editor. Su infracción está
penada por las leyes 11.723 y 25.446.
dc.description.fil
Fil: Haluza, Alejandro. Provincia del Neuquén. Municipalidad de Villa El Chocón. Museo Paleontológico "Ernesto Bachmann"; Argentina
dc.description.fil
Fil: Canale, Juan Ignacio. Provincia del Neuquén. Municipalidad de Villa El Chocón. Museo Paleontológico "Ernesto Bachmann"; Argentina. Consejo Nacional de Investigaciones Científicas y Técnicas; Argentina
dc.journal.title
Historia Natural
dc.relation.alternativeid
info:eu-repo/semantics/altIdentifier/url/http://www.fundacionazara.org.ar/img/revista-historia-natural/tomo-05/historia-natural-2013-1-art-01.pdf
dc.relation.alternativeid
info:eu-repo/semantics/altIdentifier/issn/0326-1778
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