Una breve revisión crítica del origen de los roedores sigmodontinos, con énfasis en datos paleontológicos

Most of the contemporary debate about the origin and early diversi cation of sigmodontine rodents, the most diverse living subfamily of cricetids, is based on the analysis of molecular evidence. In order to promote interest and highlight the importance of fossil evidence, we conducted a critical rev...

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Detalles Bibliográficos
Autores: Ronez, Christophe, Martin, Robert A., Kelly, Thomas S., Barbiere, Franck, Pardiñas, Ulises Francisco J.
Tipo de recurso: artículo
Estado:Versión publicada
Fecha de publicación:2021
País:Argentina
Institución:Consejo Nacional de Investigaciones Científicas y Técnicas
Repositorio:CONICET Digital (CONICET)
Idioma:español
OAI Identifier:oai:ri.conicet.gov.ar:11336/213310
Acceso en línea:http://hdl.handle.net/11336/213310
Access Level:acceso abierto
Palabra clave:CRICETIDAE
MIOCENE
NEOTOMINAE
PLIOCENE
SIGMODONTINAE
https://purl.org/becyt/ford/1.7
https://purl.org/becyt/ford/1
Descripción
Sumario:Most of the contemporary debate about the origin and early diversi cation of sigmodontine rodents, the most diverse living subfamily of cricetids, is based on the analysis of molecular evidence. In order to promote interest and highlight the importance of fossil evidence, we conducted a critical review of the paleontological record for this group of rodents. Thus, the Mio-Pliocene genera that have been associated directly or indirectly with the origin of the Sigmodontinae are reviewed. Although Honeymys (Oklahoma and Nebraska, USA, Clarendonian, late Miocene) has been tentatively associated with the origin of the Sigmodontinae, the oldest reliable records for the subfamily in North America are around 5 Ma, if Prosigmodon is considered a sigmodontine (a hypothesis not free of controversy). For South America, poorly-known and fragmentary evidence suggests a first occurrence of sigmodontines towards the late Huayquerian (latest Miocene), although the oldest assemblage with some diversity is from the Montehermosan (early Pliocene). For both North and South America, the most relevant findings, their refined chronological locations, as well as a detail of the main taxonomic problems associated with each one, are discussed. All this information is integrated, in a final section, with that derived from molecular phylogenies. As a guide for future phylogenetic studies based on molecular evidence, several fossils are suggested for calibrations.