Plesiosaurs (diapsida, sauropterygia) from late cretaceous (late campanian-early maastrichtian) marginal marine environments from north Patagonia

During the late Campanian and early Maastrichtian, Northern Patagonia suffered the first stage of the Atlantic marine ingression that reached the Neuquén Basin. The Allen and La Colonia formations show the early stages of this change, and were deposited in a complex association of marginal marine en...

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Autor: O'gorman, Jose Patricio
Formato: artículo
Estado:Versión publicada
Fecha de publicación:2015
País:Argentina
Recursos:Consejo Nacional de Investigaciones Científicas y Técnicas
Repositorio:CONICET Digital (CONICET)
Idioma:inglés
OAI Identifier:oai:ri.conicet.gov.ar:11336/55343
Acesso em linha:http://hdl.handle.net/11336/55343
Access Level:acceso abierto
Palavra-chave:Elasmosauridae
Polycotylidae
Cretácico Tardío
Patagonia
Sulcusuchus erraini
https://purl.org/becyt/ford/1.5
https://purl.org/becyt/ford/1
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oai_identifier_str oai:ri.conicet.gov.ar:11336/55343
network_acronym_str AR
network_name_str Argentina
repository_id_str
dc.title.none.fl_str_mv Plesiosaurs (diapsida, sauropterygia) from late cretaceous (late campanian-early maastrichtian) marginal marine environments from north Patagonia
Plesiosaurios (diapsida, sauropterygia) del cretácico tardío (campaniano tardío-maastrichtiano temprano) de ambientes marino-marginales del norte de Patagonia
title Plesiosaurs (diapsida, sauropterygia) from late cretaceous (late campanian-early maastrichtian) marginal marine environments from north Patagonia
spellingShingle Plesiosaurs (diapsida, sauropterygia) from late cretaceous (late campanian-early maastrichtian) marginal marine environments from north Patagonia
O'gorman, Jose Patricio
Elasmosauridae
Polycotylidae
Cretácico Tardío
Patagonia
Sulcusuchus erraini
https://purl.org/becyt/ford/1.5
https://purl.org/becyt/ford/1
title_short Plesiosaurs (diapsida, sauropterygia) from late cretaceous (late campanian-early maastrichtian) marginal marine environments from north Patagonia
title_full Plesiosaurs (diapsida, sauropterygia) from late cretaceous (late campanian-early maastrichtian) marginal marine environments from north Patagonia
title_fullStr Plesiosaurs (diapsida, sauropterygia) from late cretaceous (late campanian-early maastrichtian) marginal marine environments from north Patagonia
title_full_unstemmed Plesiosaurs (diapsida, sauropterygia) from late cretaceous (late campanian-early maastrichtian) marginal marine environments from north Patagonia
title_sort Plesiosaurs (diapsida, sauropterygia) from late cretaceous (late campanian-early maastrichtian) marginal marine environments from north Patagonia
dc.creator.none.fl_str_mv O'gorman, Jose Patricio
author O'gorman, Jose Patricio
author_facet O'gorman, Jose Patricio
author_role author
dc.subject.none.fl_str_mv Elasmosauridae
Polycotylidae
Cretácico Tardío
Patagonia
Sulcusuchus erraini
https://purl.org/becyt/ford/1.5
https://purl.org/becyt/ford/1
topic Elasmosauridae
Polycotylidae
Cretácico Tardío
Patagonia
Sulcusuchus erraini
https://purl.org/becyt/ford/1.5
https://purl.org/becyt/ford/1
description During the late Campanian and early Maastrichtian, Northern Patagonia suffered the first stage of the Atlantic marine ingression that reached the Neuquén Basin. The Allen and La Colonia formations show the early stages of this change, and were deposited in a complex association of marginal marine environments, including coastal and marine deposits (i.e., flood plains, estuaries and lagoons). The plesiosaurs from the Allen and La Colonia formations included at least three species, each with a distinctive morphotype, representing a high diversity in the Late Cretaceous. The only species that preserved cranial material, Sulcusuchus erraini Gasparini and Spalleti, is a strange polycotylid characterized by the presence of deep grooves in the rostrum and mandible. The other two species correspond to aristonectine and non-aristonectine elasmosaurids. The former are distinguished by relatively large skulls and a high number of teeth compared to other elasmosaurids, whereas the non-aristonectine elasmosaurids are characterized by their relatively small body sizes, despite being adult specimens.
publishDate 2015
dc.date.none.fl_str_mv 2015-11
dc.type.none.fl_str_mv info:eu-repo/semantics/article
info:eu-repo/semantics/publishedVersion
http://purl.org/coar/resource_type/c_6501
info:ar-repo/semantics/articulo
format article
status_str publishedVersion
dc.identifier.none.fl_str_mv http://hdl.handle.net/11336/55343
O'gorman, Jose Patricio; Plesiosaurs (diapsida, sauropterygia) from late cretaceous (late campanian-early maastrichtian) marginal marine environments from north Patagonia; Asociación Paleontológica Argentina; Publicación Electrónica de la Asociación Paleontológica Argentina; 1; 11-2015; 187-195
2469-0228
CONICET Digital
CONICET
url http://hdl.handle.net/11336/55343
identifier_str_mv O'gorman, Jose Patricio; Plesiosaurs (diapsida, sauropterygia) from late cretaceous (late campanian-early maastrichtian) marginal marine environments from north Patagonia; Asociación Paleontológica Argentina; Publicación Electrónica de la Asociación Paleontológica Argentina; 1; 11-2015; 187-195
2469-0228
CONICET Digital
CONICET
dc.language.none.fl_str_mv eng
language eng
dc.relation.none.fl_str_mv info:eu-repo/semantics/altIdentifier/doi/10.5710/PEAPA.13.05.2015.105
info:eu-repo/semantics/altIdentifier/url/http://www.peapaleontologica.org.ar/index.php/peapa/article/view/105
dc.rights.none.fl_str_mv info:eu-repo/semantics/openAccess
https://creativecommons.org/licenses/by-nc-sa/2.5/ar/
eu_rights_str_mv openAccess
rights_invalid_str_mv https://creativecommons.org/licenses/by-nc-sa/2.5/ar/
dc.format.none.fl_str_mv application/pdf
application/pdf
dc.publisher.none.fl_str_mv Asociación Paleontológica Argentina
publisher.none.fl_str_mv Asociación Paleontológica Argentina
dc.source.none.fl_str_mv reponame:CONICET Digital (CONICET)
instname:Consejo Nacional de Investigaciones Científicas y Técnicas
instname_str Consejo Nacional de Investigaciones Científicas y Técnicas
reponame_str CONICET Digital (CONICET)
collection CONICET Digital (CONICET)
repository.name.fl_str_mv CONICET Digital (CONICET) - Consejo Nacional de Investigaciones Científicas y Técnicas
repository.mail.fl_str_mv dasensio@conicet.gov.ar; lcarlino@conicet.gov.ar
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spelling Plesiosaurs (diapsida, sauropterygia) from late cretaceous (late campanian-early maastrichtian) marginal marine environments from north PatagoniaPlesiosaurios (diapsida, sauropterygia) del cretácico tardío (campaniano tardío-maastrichtiano temprano) de ambientes marino-marginales del norte de PatagoniaO'gorman, Jose PatricioElasmosauridaePolycotylidaeCretácico TardíoPatagoniaSulcusuchus errainihttps://purl.org/becyt/ford/1.5https://purl.org/becyt/ford/1During the late Campanian and early Maastrichtian, Northern Patagonia suffered the first stage of the Atlantic marine ingression that reached the Neuquén Basin. The Allen and La Colonia formations show the early stages of this change, and were deposited in a complex association of marginal marine environments, including coastal and marine deposits (i.e., flood plains, estuaries and lagoons). The plesiosaurs from the Allen and La Colonia formations included at least three species, each with a distinctive morphotype, representing a high diversity in the Late Cretaceous. The only species that preserved cranial material, Sulcusuchus erraini Gasparini and Spalleti, is a strange polycotylid characterized by the presence of deep grooves in the rostrum and mandible. The other two species correspond to aristonectine and non-aristonectine elasmosaurids. The former are distinguished by relatively large skulls and a high number of teeth compared to other elasmosaurids, whereas the non-aristonectine elasmosaurids are characterized by their relatively small body sizes, despite being adult specimens.Durante el Campaniano tardío y el Maastrichtiano temprano el norte de la Patagonia sufrió la primera etapa de la ingresión marina atlántica, que alcanzó la Cuenca Neuquina. Las formaciones Allen y La Colonia evidencian las primeras etapas de este cambio, habiéndose depositado en una asociación de ambientes irregulares que incluyen depósitos marino-marginales (es decir de llanuras mareales, estuarios y lagunas costeras). Los plesiosaurios de las formaciones Allen y La Colonia incluyen al menos tres especies, cada una con un morfotipo distintivo, lo que representa una alta diversidad hacia fines del Cretácico. La única especie con material craneano preservado es Sulcusuchus erraini Gasparini y Spalleti, un extraño policotílido caracterizado por la presencia de profundos surcos en el rostro y la mandíbula. Las otras dos especies corresponden a elasmosáuridos aristonectinos, caracterizados por tener cráneos relativamente grandes y elevado número de dientes comparados con otros elasmosáuridos y a elasmosáuridos no aristonectinos, que se destacan por su relativo pequeño tamaño, a pesar de tratarse de ejemplares adultos.Fil: O'gorman, Jose Patricio. Consejo Nacional de Investigaciones Científicas y Técnicas; Argentina. Universidad Nacional de La Plata. Facultad de Ciencias Naturales y Museo. División Paleontología Vertebrados; ArgentinaAsociación Paleontológica Argentina2015-11info:eu-repo/semantics/articleinfo:eu-repo/semantics/publishedVersionhttp://purl.org/coar/resource_type/c_6501info:ar-repo/semantics/articuloapplication/pdfapplication/pdfhttp://hdl.handle.net/11336/55343O'gorman, Jose Patricio; Plesiosaurs (diapsida, sauropterygia) from late cretaceous (late campanian-early maastrichtian) marginal marine environments from north Patagonia; Asociación Paleontológica Argentina; Publicación Electrónica de la Asociación Paleontológica Argentina; 1; 11-2015; 187-1952469-0228CONICET DigitalCONICETenginfo:eu-repo/semantics/altIdentifier/doi/10.5710/PEAPA.13.05.2015.105info:eu-repo/semantics/altIdentifier/url/http://www.peapaleontologica.org.ar/index.php/peapa/article/view/105info:eu-repo/semantics/openAccesshttps://creativecommons.org/licenses/by-nc-sa/2.5/ar/reponame:CONICET Digital (CONICET)instname:Consejo Nacional de Investigaciones Científicas y Técnicas2024-05-08T13:50:59Zoai:ri.conicet.gov.ar:11336/55343instacron:CONICETInstitucionalhttp://ri.conicet.gov.ar/Organismo científico-tecnológicoNo correspondehttp://ri.conicet.gov.ar/oai/requestdasensio@conicet.gov.ar; lcarlino@conicet.gov.arArgentinaNo correspondeNo correspondeNo correspondeopendoar:34982024-05-08 13:51:00.087CONICET Digital (CONICET) - Consejo Nacional de Investigaciones Científicas y Técnicasfalse
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