A new Dasypodini armadillo (Xenarthra: Cingulata) from San Gregorio Formation, Pliocene of Venezuela: affinities and biogeographic interpretations

Autores
Cordeiro de Castro, Mariela; Carlini, Alfredo Armando; Sánchez, Rodolfo; Sánchez-Villagra, Marcelo R.
Año de publicación
2014
Idioma
inglés
Tipo de recurso
artículo
Estado
versión publicada
Descripción
We describe Pliodasypus vergelianus gen. et sp. nov., a Dasypodini armadillo from the middle Pliocene of Venezuela (Vergel Member, San Gregorio Formation). Although scarce, the remains are remarkable because of their geochronologic proximity to the main phase of Great American Biotic Interchange (GABI). The cladistic analysis conducted reveals that Pliodasypus groups with Dasypus and both are sister taxa of Propraopus, whereas Anadasypus is at a basal position. With respect to the records of tribe Dasypodini, after its oldest representative (Anadasypus, middle and late Miocene), the chronologically subsequent form is Pl. vergelianus (middle Pliocene), followed by Dasypus bellus in higher northern latitudes (late Pliocene), and then by widespread occurrences in the Pleistocene of North America (D. bellus) and South America (Propraopus, Dasypus punctatus, and Dasypus novemcinctus). Thus, we infer that Dasypus differentiated in the late Pliocene at low latitudes in the northern South America. It leads to two alternative hypotheses of dispersal: (a) some early Dasypus remained cryptically in South America until the Pleistocene, whereas others dispersed to North America between 2.2 and 2.7 Ma, or (b) they dispersed to North America subsequently to the emersion of the Panamanian isthmus and D. bellus differentiated there; later, during the Pleistocene, D. bellus entered South America and experienced speciation. The same process of re-ingression has been proposed to other xenarthrans, breaking with the traditional assumption that the GABI was unidirectional.
Facultad de Ciencias Naturales y Museo
Materia
Ciencias Naturales
Xenarthra
Cingulata
Dasypodidae
Pliodasypus
Pliocene
Venezuela
Nivel de accesibilidad
acceso abierto
Condiciones de uso
http://creativecommons.org/licenses/by-nc-sa/4.0/
Repositorio
SEDICI (UNLP)
Institución
Universidad Nacional de La Plata
OAI Identificador
oai:sedici.unlp.edu.ar:10915/134786

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spelling A new Dasypodini armadillo (Xenarthra: Cingulata) from San Gregorio Formation, Pliocene of Venezuela: affinities and biogeographic interpretationsCordeiro de Castro, MarielaCarlini, Alfredo ArmandoSánchez, RodolfoSánchez-Villagra, Marcelo R.Ciencias NaturalesXenarthraCingulataDasypodidaePliodasypusPlioceneVenezuelaWe describe <i>Pliodasypus vergelianus</i> gen. et sp. nov., a Dasypodini armadillo from the middle Pliocene of Venezuela (Vergel Member, San Gregorio Formation). Although scarce, the remains are remarkable because of their geochronologic proximity to the main phase of Great American Biotic Interchange (GABI). The cladistic analysis conducted reveals that <i>Pliodasypus</i> groups with <i>Dasypus</i> and both are sister taxa of <i>Propraopus</i>, whereas <i>Anadasypus</i> is at a basal position. With respect to the records of tribe Dasypodini, after its oldest representative (<i>Anadasypus</i>, middle and late Miocene), the chronologically subsequent form is <i>Pl. vergelianus</i> (middle Pliocene), followed by <i>Dasypus bellus</i> in higher northern latitudes (late Pliocene), and then by widespread occurrences in the Pleistocene of North America (<i>D. bellus</i>) and South America (<i>Propraopus</i>, <i>Dasypus punctatus</i>, and <i>Dasypus novemcinctus</i>). Thus, we infer that <i>Dasypus</i> differentiated in the late Pliocene at low latitudes in the northern South America. It leads to two alternative hypotheses of dispersal: (a) some early <i>Dasypus</i> remained cryptically in South America until the Pleistocene, whereas others dispersed to North America between 2.2 and 2.7 Ma, or (b) they dispersed to North America subsequently to the emersion of the Panamanian isthmus and <i>D. bellus</i> differentiated there; later, during the Pleistocene, <i>D. bellus</i> entered South America and experienced speciation. The same process of re-ingression has been proposed to other xenarthrans, breaking with the traditional assumption that the GABI was unidirectional.Facultad de Ciencias Naturales y Museo2014-02info:eu-repo/semantics/articleinfo:eu-repo/semantics/publishedVersionArticulohttp://purl.org/coar/resource_type/c_6501info:ar-repo/semantics/articuloapplication/pdf77-86http://sedici.unlp.edu.ar/handle/10915/134786enginfo:eu-repo/semantics/altIdentifier/issn/1432-1904info:eu-repo/semantics/altIdentifier/issn/0028-1042info:eu-repo/semantics/altIdentifier/doi/10.1007/s00114-013-1131-5info:eu-repo/semantics/altIdentifier/pmid/24414134info:eu-repo/semantics/openAccesshttp://creativecommons.org/licenses/by-nc-sa/4.0/Creative Commons Attribution-NonCommercial-ShareAlike 4.0 International (CC BY-NC-SA 4.0)reponame:SEDICI (UNLP)instname:Universidad Nacional de La Platainstacron:UNLP2025-10-15T11:23:47Zoai:sedici.unlp.edu.ar:10915/134786Institucionalhttp://sedici.unlp.edu.ar/Universidad públicaNo correspondehttp://sedici.unlp.edu.ar/oai/snrdalira@sedici.unlp.edu.arArgentinaNo correspondeNo correspondeNo correspondeopendoar:13292025-10-15 11:23:48.102SEDICI (UNLP) - Universidad Nacional de La Platafalse
dc.title.none.fl_str_mv A new Dasypodini armadillo (Xenarthra: Cingulata) from San Gregorio Formation, Pliocene of Venezuela: affinities and biogeographic interpretations
title A new Dasypodini armadillo (Xenarthra: Cingulata) from San Gregorio Formation, Pliocene of Venezuela: affinities and biogeographic interpretations
spellingShingle A new Dasypodini armadillo (Xenarthra: Cingulata) from San Gregorio Formation, Pliocene of Venezuela: affinities and biogeographic interpretations
Cordeiro de Castro, Mariela
Ciencias Naturales
Xenarthra
Cingulata
Dasypodidae
Pliodasypus
Pliocene
Venezuela
title_short A new Dasypodini armadillo (Xenarthra: Cingulata) from San Gregorio Formation, Pliocene of Venezuela: affinities and biogeographic interpretations
title_full A new Dasypodini armadillo (Xenarthra: Cingulata) from San Gregorio Formation, Pliocene of Venezuela: affinities and biogeographic interpretations
title_fullStr A new Dasypodini armadillo (Xenarthra: Cingulata) from San Gregorio Formation, Pliocene of Venezuela: affinities and biogeographic interpretations
title_full_unstemmed A new Dasypodini armadillo (Xenarthra: Cingulata) from San Gregorio Formation, Pliocene of Venezuela: affinities and biogeographic interpretations
title_sort A new Dasypodini armadillo (Xenarthra: Cingulata) from San Gregorio Formation, Pliocene of Venezuela: affinities and biogeographic interpretations
dc.creator.none.fl_str_mv Cordeiro de Castro, Mariela
Carlini, Alfredo Armando
Sánchez, Rodolfo
Sánchez-Villagra, Marcelo R.
author Cordeiro de Castro, Mariela
author_facet Cordeiro de Castro, Mariela
Carlini, Alfredo Armando
Sánchez, Rodolfo
Sánchez-Villagra, Marcelo R.
author_role author
author2 Carlini, Alfredo Armando
Sánchez, Rodolfo
Sánchez-Villagra, Marcelo R.
author2_role author
author
author
dc.subject.none.fl_str_mv Ciencias Naturales
Xenarthra
Cingulata
Dasypodidae
Pliodasypus
Pliocene
Venezuela
topic Ciencias Naturales
Xenarthra
Cingulata
Dasypodidae
Pliodasypus
Pliocene
Venezuela
dc.description.none.fl_txt_mv We describe <i>Pliodasypus vergelianus</i> gen. et sp. nov., a Dasypodini armadillo from the middle Pliocene of Venezuela (Vergel Member, San Gregorio Formation). Although scarce, the remains are remarkable because of their geochronologic proximity to the main phase of Great American Biotic Interchange (GABI). The cladistic analysis conducted reveals that <i>Pliodasypus</i> groups with <i>Dasypus</i> and both are sister taxa of <i>Propraopus</i>, whereas <i>Anadasypus</i> is at a basal position. With respect to the records of tribe Dasypodini, after its oldest representative (<i>Anadasypus</i>, middle and late Miocene), the chronologically subsequent form is <i>Pl. vergelianus</i> (middle Pliocene), followed by <i>Dasypus bellus</i> in higher northern latitudes (late Pliocene), and then by widespread occurrences in the Pleistocene of North America (<i>D. bellus</i>) and South America (<i>Propraopus</i>, <i>Dasypus punctatus</i>, and <i>Dasypus novemcinctus</i>). Thus, we infer that <i>Dasypus</i> differentiated in the late Pliocene at low latitudes in the northern South America. It leads to two alternative hypotheses of dispersal: (a) some early <i>Dasypus</i> remained cryptically in South America until the Pleistocene, whereas others dispersed to North America between 2.2 and 2.7 Ma, or (b) they dispersed to North America subsequently to the emersion of the Panamanian isthmus and <i>D. bellus</i> differentiated there; later, during the Pleistocene, <i>D. bellus</i> entered South America and experienced speciation. The same process of re-ingression has been proposed to other xenarthrans, breaking with the traditional assumption that the GABI was unidirectional.
Facultad de Ciencias Naturales y Museo
description We describe <i>Pliodasypus vergelianus</i> gen. et sp. nov., a Dasypodini armadillo from the middle Pliocene of Venezuela (Vergel Member, San Gregorio Formation). Although scarce, the remains are remarkable because of their geochronologic proximity to the main phase of Great American Biotic Interchange (GABI). The cladistic analysis conducted reveals that <i>Pliodasypus</i> groups with <i>Dasypus</i> and both are sister taxa of <i>Propraopus</i>, whereas <i>Anadasypus</i> is at a basal position. With respect to the records of tribe Dasypodini, after its oldest representative (<i>Anadasypus</i>, middle and late Miocene), the chronologically subsequent form is <i>Pl. vergelianus</i> (middle Pliocene), followed by <i>Dasypus bellus</i> in higher northern latitudes (late Pliocene), and then by widespread occurrences in the Pleistocene of North America (<i>D. bellus</i>) and South America (<i>Propraopus</i>, <i>Dasypus punctatus</i>, and <i>Dasypus novemcinctus</i>). Thus, we infer that <i>Dasypus</i> differentiated in the late Pliocene at low latitudes in the northern South America. It leads to two alternative hypotheses of dispersal: (a) some early <i>Dasypus</i> remained cryptically in South America until the Pleistocene, whereas others dispersed to North America between 2.2 and 2.7 Ma, or (b) they dispersed to North America subsequently to the emersion of the Panamanian isthmus and <i>D. bellus</i> differentiated there; later, during the Pleistocene, <i>D. bellus</i> entered South America and experienced speciation. The same process of re-ingression has been proposed to other xenarthrans, breaking with the traditional assumption that the GABI was unidirectional.
publishDate 2014
dc.date.none.fl_str_mv 2014-02
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info:eu-repo/semantics/altIdentifier/pmid/24414134
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Creative Commons Attribution-NonCommercial-ShareAlike 4.0 International (CC BY-NC-SA 4.0)
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