Dental evolution in Neophanomys (Rodentia, Octodontidae) from the late Miocene of central Argentina

Autores
Verzi, Diego Hector; Vieytes, Emma Carolina; Montalvo, Claudia Inés
Año de publicación
2011
Idioma
inglés
Tipo de recurso
artículo
Estado
versión publicada
Descripción
The evolutionary pattern of the molar morphology of the small caviomorph (Octodontidae) Neophanomys from the late Miocene Cerro AzulFormation of central Argentina is analyzed. Two new species (chronomorphs) are recognized, which constitute an anagenetically evolving lineagewith a gradual and directional pattern of increasing molar hypsodonty. Dental changes related to increasing hypsodonty are comparable to those ofthe octodontid lineage Chasichimys also recovered from the Cerro Azul Formation. However, Neophanomys shows comparatively less variation ingross morphology and there are no evidences that this lineage achieved euhypsodonty. In contrast, important changes in enamel microstructure(schmelzmuster) are observed among different populations of Neophanomys, supporting the hypothesis that these changes can occur at leastpartially independently from modifications in dental gross morphology. The patterns of dental evolution detected in the Neophanomys andChasichimys-Xenodontomys lineages and the unequivocal polarity of the changes involved, related to increasing hypsodonty, reinforce thehypothesis that chronological differences exist among late Miocene outcroppings of Cerro Azul Formation in central Argentina.
Fil: Verzi, Diego Hector. Universidad Nacional de La Plata. Facultad de Ciencias Naturales y Museo. División Zoología de Vertebrados. Sección de Mastozoología; Argentina. Consejo Nacional de Investigaciones Científicas y Técnicas. Centro Científico Tecnológico Conicet - La Plata; Argentina
Fil: Vieytes, Emma Carolina. Universidad Nacional de La Plata. Facultad de Ciencias Naturales y Museo. División Zoología de Vertebrados. Sección de Mastozoología; Argentina. Consejo Nacional de Investigaciones Científicas y Técnicas. Centro Científico Tecnológico Conicet - La Plata; Argentina
Fil: Montalvo, Claudia Inés. Universidad Nacional de La Pampa; Argentina. Consejo Nacional de Investigaciones Científicas y Técnicas; Argentina
Materia
BIOCHRONOLOGY
LATE MIOCENE
MOLAR EVOLUTION
OCTODONTIDAE
SCHMELZMUSTER
Nivel de accesibilidad
acceso abierto
Condiciones de uso
https://creativecommons.org/licenses/by-nc-sa/2.5/ar/
Repositorio
CONICET Digital (CONICET)
Institución
Consejo Nacional de Investigaciones Científicas y Técnicas
OAI Identificador
oai:ri.conicet.gov.ar:11336/196462

id CONICETDig_72fa679e72645359588c1251c8aa4c2d
oai_identifier_str oai:ri.conicet.gov.ar:11336/196462
network_acronym_str CONICETDig
repository_id_str 3498
network_name_str CONICET Digital (CONICET)
spelling Dental evolution in Neophanomys (Rodentia, Octodontidae) from the late Miocene of central ArgentinaÉvolution dentaire chez les Neophanomys (Rodentia, Octodontidae) du Miocène tardif d’Argentine centraleVerzi, Diego HectorVieytes, Emma CarolinaMontalvo, Claudia InésBIOCHRONOLOGYLATE MIOCENEMOLAR EVOLUTIONOCTODONTIDAESCHMELZMUSTERhttps://purl.org/becyt/ford/1.5https://purl.org/becyt/ford/1The evolutionary pattern of the molar morphology of the small caviomorph (Octodontidae) Neophanomys from the late Miocene Cerro AzulFormation of central Argentina is analyzed. Two new species (chronomorphs) are recognized, which constitute an anagenetically evolving lineagewith a gradual and directional pattern of increasing molar hypsodonty. Dental changes related to increasing hypsodonty are comparable to those ofthe octodontid lineage Chasichimys also recovered from the Cerro Azul Formation. However, Neophanomys shows comparatively less variation ingross morphology and there are no evidences that this lineage achieved euhypsodonty. In contrast, important changes in enamel microstructure(schmelzmuster) are observed among different populations of Neophanomys, supporting the hypothesis that these changes can occur at leastpartially independently from modifications in dental gross morphology. The patterns of dental evolution detected in the Neophanomys andChasichimys-Xenodontomys lineages and the unequivocal polarity of the changes involved, related to increasing hypsodonty, reinforce thehypothesis that chronological differences exist among late Miocene outcroppings of Cerro Azul Formation in central Argentina.Fil: Verzi, Diego Hector. Universidad Nacional de La Plata. Facultad de Ciencias Naturales y Museo. División Zoología de Vertebrados. Sección de Mastozoología; Argentina. Consejo Nacional de Investigaciones Científicas y Técnicas. Centro Científico Tecnológico Conicet - La Plata; ArgentinaFil: Vieytes, Emma Carolina. Universidad Nacional de La Plata. Facultad de Ciencias Naturales y Museo. División Zoología de Vertebrados. Sección de Mastozoología; Argentina. Consejo Nacional de Investigaciones Científicas y Técnicas. Centro Científico Tecnológico Conicet - La Plata; ArgentinaFil: Montalvo, Claudia Inés. Universidad Nacional de La Pampa; Argentina. Consejo Nacional de Investigaciones Científicas y Técnicas; ArgentinaElsevier France-Editions Scientifiques Medicales Elsevier2011-10info:eu-repo/semantics/articleinfo:eu-repo/semantics/publishedVersionhttp://purl.org/coar/resource_type/c_6501info:ar-repo/semantics/articuloapplication/pdfapplication/pdfapplication/pdfhttp://hdl.handle.net/11336/196462Verzi, Diego Hector; Vieytes, Emma Carolina; Montalvo, Claudia Inés; Dental evolution in Neophanomys (Rodentia, Octodontidae) from the late Miocene of central Argentina; Elsevier France-Editions Scientifiques Medicales Elsevier; Geobios; 44; 6; 10-2011; 621-6330016-6995CONICET DigitalCONICETenginfo:eu-repo/semantics/altIdentifier/url/https://www.sciencedirect.com/science/article/abs/pii/S0016699511000817info:eu-repo/semantics/altIdentifier/doi/10.1016/j.geobios.2011.02.008info:eu-repo/semantics/openAccesshttps://creativecommons.org/licenses/by-nc-sa/2.5/ar/reponame:CONICET Digital (CONICET)instname:Consejo Nacional de Investigaciones Científicas y Técnicas2025-09-03T10:00:34Zoai:ri.conicet.gov.ar:11336/196462instacron: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:34982025-09-03 10:00:35.121CONICET Digital (CONICET) - Consejo Nacional de Investigaciones Científicas y Técnicasfalse
dc.title.none.fl_str_mv Dental evolution in Neophanomys (Rodentia, Octodontidae) from the late Miocene of central Argentina
Évolution dentaire chez les Neophanomys (Rodentia, Octodontidae) du Miocène tardif d’Argentine centrale
title Dental evolution in Neophanomys (Rodentia, Octodontidae) from the late Miocene of central Argentina
spellingShingle Dental evolution in Neophanomys (Rodentia, Octodontidae) from the late Miocene of central Argentina
Verzi, Diego Hector
BIOCHRONOLOGY
LATE MIOCENE
MOLAR EVOLUTION
OCTODONTIDAE
SCHMELZMUSTER
title_short Dental evolution in Neophanomys (Rodentia, Octodontidae) from the late Miocene of central Argentina
title_full Dental evolution in Neophanomys (Rodentia, Octodontidae) from the late Miocene of central Argentina
title_fullStr Dental evolution in Neophanomys (Rodentia, Octodontidae) from the late Miocene of central Argentina
title_full_unstemmed Dental evolution in Neophanomys (Rodentia, Octodontidae) from the late Miocene of central Argentina
title_sort Dental evolution in Neophanomys (Rodentia, Octodontidae) from the late Miocene of central Argentina
dc.creator.none.fl_str_mv Verzi, Diego Hector
Vieytes, Emma Carolina
Montalvo, Claudia Inés
author Verzi, Diego Hector
author_facet Verzi, Diego Hector
Vieytes, Emma Carolina
Montalvo, Claudia Inés
author_role author
author2 Vieytes, Emma Carolina
Montalvo, Claudia Inés
author2_role author
author
dc.subject.none.fl_str_mv BIOCHRONOLOGY
LATE MIOCENE
MOLAR EVOLUTION
OCTODONTIDAE
SCHMELZMUSTER
topic BIOCHRONOLOGY
LATE MIOCENE
MOLAR EVOLUTION
OCTODONTIDAE
SCHMELZMUSTER
purl_subject.fl_str_mv https://purl.org/becyt/ford/1.5
https://purl.org/becyt/ford/1
dc.description.none.fl_txt_mv The evolutionary pattern of the molar morphology of the small caviomorph (Octodontidae) Neophanomys from the late Miocene Cerro AzulFormation of central Argentina is analyzed. Two new species (chronomorphs) are recognized, which constitute an anagenetically evolving lineagewith a gradual and directional pattern of increasing molar hypsodonty. Dental changes related to increasing hypsodonty are comparable to those ofthe octodontid lineage Chasichimys also recovered from the Cerro Azul Formation. However, Neophanomys shows comparatively less variation ingross morphology and there are no evidences that this lineage achieved euhypsodonty. In contrast, important changes in enamel microstructure(schmelzmuster) are observed among different populations of Neophanomys, supporting the hypothesis that these changes can occur at leastpartially independently from modifications in dental gross morphology. The patterns of dental evolution detected in the Neophanomys andChasichimys-Xenodontomys lineages and the unequivocal polarity of the changes involved, related to increasing hypsodonty, reinforce thehypothesis that chronological differences exist among late Miocene outcroppings of Cerro Azul Formation in central Argentina.
Fil: Verzi, Diego Hector. Universidad Nacional de La Plata. Facultad de Ciencias Naturales y Museo. División Zoología de Vertebrados. Sección de Mastozoología; Argentina. Consejo Nacional de Investigaciones Científicas y Técnicas. Centro Científico Tecnológico Conicet - La Plata; Argentina
Fil: Vieytes, Emma Carolina. Universidad Nacional de La Plata. Facultad de Ciencias Naturales y Museo. División Zoología de Vertebrados. Sección de Mastozoología; Argentina. Consejo Nacional de Investigaciones Científicas y Técnicas. Centro Científico Tecnológico Conicet - La Plata; Argentina
Fil: Montalvo, Claudia Inés. Universidad Nacional de La Pampa; Argentina. Consejo Nacional de Investigaciones Científicas y Técnicas; Argentina
description The evolutionary pattern of the molar morphology of the small caviomorph (Octodontidae) Neophanomys from the late Miocene Cerro AzulFormation of central Argentina is analyzed. Two new species (chronomorphs) are recognized, which constitute an anagenetically evolving lineagewith a gradual and directional pattern of increasing molar hypsodonty. Dental changes related to increasing hypsodonty are comparable to those ofthe octodontid lineage Chasichimys also recovered from the Cerro Azul Formation. However, Neophanomys shows comparatively less variation ingross morphology and there are no evidences that this lineage achieved euhypsodonty. In contrast, important changes in enamel microstructure(schmelzmuster) are observed among different populations of Neophanomys, supporting the hypothesis that these changes can occur at leastpartially independently from modifications in dental gross morphology. The patterns of dental evolution detected in the Neophanomys andChasichimys-Xenodontomys lineages and the unequivocal polarity of the changes involved, related to increasing hypsodonty, reinforce thehypothesis that chronological differences exist among late Miocene outcroppings of Cerro Azul Formation in central Argentina.
publishDate 2011
dc.date.none.fl_str_mv 2011-10
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/11336/196462
Verzi, Diego Hector; Vieytes, Emma Carolina; Montalvo, Claudia Inés; Dental evolution in Neophanomys (Rodentia, Octodontidae) from the late Miocene of central Argentina; Elsevier France-Editions Scientifiques Medicales Elsevier; Geobios; 44; 6; 10-2011; 621-633
0016-6995
CONICET Digital
CONICET
url http://hdl.handle.net/11336/196462
identifier_str_mv Verzi, Diego Hector; Vieytes, Emma Carolina; Montalvo, Claudia Inés; Dental evolution in Neophanomys (Rodentia, Octodontidae) from the late Miocene of central Argentina; Elsevier France-Editions Scientifiques Medicales Elsevier; Geobios; 44; 6; 10-2011; 621-633
0016-6995
CONICET Digital
CONICET
dc.language.none.fl_str_mv eng
language eng
dc.relation.none.fl_str_mv info:eu-repo/semantics/altIdentifier/url/https://www.sciencedirect.com/science/article/abs/pii/S0016699511000817
info:eu-repo/semantics/altIdentifier/doi/10.1016/j.geobios.2011.02.008
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
application/pdf
dc.publisher.none.fl_str_mv Elsevier France-Editions Scientifiques Medicales Elsevier
publisher.none.fl_str_mv Elsevier France-Editions Scientifiques Medicales Elsevier
dc.source.none.fl_str_mv reponame:CONICET Digital (CONICET)
instname:Consejo Nacional de Investigaciones Científicas y Técnicas
reponame_str CONICET Digital (CONICET)
collection CONICET Digital (CONICET)
instname_str Consejo Nacional de Investigaciones Científicas y Técnicas
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
_version_ 1842269646880768000
score 13.13397