The first rodent from the Mariño Formation (Miocene) at Divisadero Largo (Mendoza, Argentina) and its biochronological implications

A new significant mammal fossil from the Mariño Formation in the area of Divisadero Largo (Mendoza, Argentina) is described herein. The material consists of a mandibular fragment with the right series p4-m3 of the rodent Scleromys sp. It is compared with the Santacrucian species S. osbornianus Amegh...

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Autores principales: Cerdeño Serrano, María Esperanza, Vucetich, María Guiomar
Formato: Articulo
Lenguaje:Inglés
Publicado: 2007
Materias:
Acceso en línea:http://sedici.unlp.edu.ar/handle/10915/110296
Aporte de:
id I19-R120-10915-110296
record_format dspace
institution Universidad Nacional de La Plata
institution_str I-19
repository_str R-120
collection SEDICI (UNLP)
language Inglés
topic Paleontología
Rodents
Mariño Formation
Early Miocene
Mendoza
Argentina
Roedores
Formación Mariño
Mioceno Temprano
spellingShingle Paleontología
Rodents
Mariño Formation
Early Miocene
Mendoza
Argentina
Roedores
Formación Mariño
Mioceno Temprano
Cerdeño Serrano, María Esperanza
Vucetich, María Guiomar
The first rodent from the Mariño Formation (Miocene) at Divisadero Largo (Mendoza, Argentina) and its biochronological implications
topic_facet Paleontología
Rodents
Mariño Formation
Early Miocene
Mendoza
Argentina
Roedores
Formación Mariño
Mioceno Temprano
description A new significant mammal fossil from the Mariño Formation in the area of Divisadero Largo (Mendoza, Argentina) is described herein. The material consists of a mandibular fragment with the right series p4-m3 of the rodent Scleromys sp. It is compared with the Santacrucian species S. osbornianus Ameghino and S. angustus Ameghino, and with S.quadrangulatus Kramarz from the Pinturas Formation, all of them from the Santa Cruz Province. At the same time, the studied fossil presents a combination of characters that differ from those species: more transverse molars, with anterior wall slightly curved, lower degree of hypsodonty and smaller size. However, due to the great morphological variation within Scleromys, a specific determination is not provided based on a sole specimen. The presence of this genus, together with the previously studied mesotheriine, supports an early Miocene age for the middle member of the Mariño Formation.
format Articulo
Articulo
author Cerdeño Serrano, María Esperanza
Vucetich, María Guiomar
author_facet Cerdeño Serrano, María Esperanza
Vucetich, María Guiomar
author_sort Cerdeño Serrano, María Esperanza
title The first rodent from the Mariño Formation (Miocene) at Divisadero Largo (Mendoza, Argentina) and its biochronological implications
title_short The first rodent from the Mariño Formation (Miocene) at Divisadero Largo (Mendoza, Argentina) and its biochronological implications
title_full The first rodent from the Mariño Formation (Miocene) at Divisadero Largo (Mendoza, Argentina) and its biochronological implications
title_fullStr The first rodent from the Mariño Formation (Miocene) at Divisadero Largo (Mendoza, Argentina) and its biochronological implications
title_full_unstemmed The first rodent from the Mariño Formation (Miocene) at Divisadero Largo (Mendoza, Argentina) and its biochronological implications
title_sort first rodent from the mariño formation (miocene) at divisadero largo (mendoza, argentina) and its biochronological implications
publishDate 2007
url http://sedici.unlp.edu.ar/handle/10915/110296
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