A New Chronology for Middle Eocene-Early Miocene South American Land Mammal Ages

Cenozoic South American Land Mam- mal Ages (SALMAs) have historically been correlated to the geologic time scale using 40 Ar/ 39 Ar dating and magnetostratigraphy. At Gran Barranca (68.7°W, 45.7°S)—one of South America's key areas for constraining SALMAs—existing radioisotopic ages have uncerta...

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Autores principales: Dunn, Regan E., Madden, Richard H., Kohn, Matthew J., Schmitz, Mark D., Strömberg, Caroline A.E., Carlini, Alfredo Armando, Re, Guillermo Hector, Crowley, James L.
Formato: Articulo
Lenguaje:Inglés
Publicado: 2013
Materias:
Acceso en línea:http://sedici.unlp.edu.ar/handle/10915/132105
Aporte de:
id I19-R120-10915-132105
record_format dspace
institution Universidad Nacional de La Plata
institution_str I-19
repository_str R-120
collection SEDICI (UNLP)
language Inglés
topic Paleontología
Mammal
South America
Eocene–early Miocene
spellingShingle Paleontología
Mammal
South America
Eocene–early Miocene
Dunn, Regan E.
Madden, Richard H.
Kohn, Matthew J.
Schmitz, Mark D.
Strömberg, Caroline A.E.
Carlini, Alfredo Armando
Re, Guillermo Hector
Crowley, James L.
A New Chronology for Middle Eocene-Early Miocene South American Land Mammal Ages
topic_facet Paleontología
Mammal
South America
Eocene–early Miocene
description Cenozoic South American Land Mam- mal Ages (SALMAs) have historically been correlated to the geologic time scale using 40 Ar/ 39 Ar dating and magnetostratigraphy. At Gran Barranca (68.7°W, 45.7°S)—one of South America's key areas for constraining SALMAs—existing radioisotopic ages have uncertainties of up to 4 m.y. To better con- strain the ages of mammalian assemblages, we employed high-precision (±<40 k.y.) U-Pb dating using single zircon crystals. We dated nine tuffs from the Sarmiento Formation containing middle Eocene-early Miocene faunas (Barrancan, Mustersan, Tinguiriri- can, Deseadan, Colhuehuapian, and "Pin- turan"). The new dates span from 39.861 ± 0.037 Ma to 19.041 ± 0.027 Ma. The La Can- cha Tuff, occurring within the Tinguirirican faunal level yielded an age of 33.581 ± 0.015 Ma, confi rming that the Vera Member con- tains the only fossiliferous geologic section encompassing the Eocene-Oligocene transi- tion in the Southern Hemisphere. The pre- Deseadan fauna, La Cantera, is ≤30.77 Ma, the age of the Colhuehuapian is expanded to 21.1-20.1 Ma, and the Pinturan may be as old as ca. 19 Ma. The new U-Pb dates confi rm that at- mospheric temperatures and vegetation remained constant across the Eocene- Oligocene transition in Patagonia and that hypsodonty occurred in South American un- gulates much earlier than on any other conti- nent. Additionally, refi nement of the SALMA boundaries will eventually provide the con- text necessary to compare faunal transitions across continents, although currently too much data are missing to allow such compar- isons. Finally, the new ages provide a high- resolution age model from which hypotheses about rates of environmental and evolution- ary change at Gran Barranca can be tested.
format Articulo
Articulo
author Dunn, Regan E.
Madden, Richard H.
Kohn, Matthew J.
Schmitz, Mark D.
Strömberg, Caroline A.E.
Carlini, Alfredo Armando
Re, Guillermo Hector
Crowley, James L.
author_facet Dunn, Regan E.
Madden, Richard H.
Kohn, Matthew J.
Schmitz, Mark D.
Strömberg, Caroline A.E.
Carlini, Alfredo Armando
Re, Guillermo Hector
Crowley, James L.
author_sort Dunn, Regan E.
title A New Chronology for Middle Eocene-Early Miocene South American Land Mammal Ages
title_short A New Chronology for Middle Eocene-Early Miocene South American Land Mammal Ages
title_full A New Chronology for Middle Eocene-Early Miocene South American Land Mammal Ages
title_fullStr A New Chronology for Middle Eocene-Early Miocene South American Land Mammal Ages
title_full_unstemmed A New Chronology for Middle Eocene-Early Miocene South American Land Mammal Ages
title_sort new chronology for middle eocene-early miocene south american land mammal ages
publishDate 2013
url http://sedici.unlp.edu.ar/handle/10915/132105
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