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Published April 7, 2012 | public
Journal Article

Middle Eocene rodents from Peruvian Amazonia reveal the pattern and timing of caviomorph origins and biogeography

Abstract

The long-term isolation of South America during most of the Cenozoic produced a highly peculiar terrestrial vertebrate biota, with a wide array of mammal groups, among which caviomorph rodents and platyrrhine primates are Mid-Cenozoic immigrants. In the absence of indisputable pre-Oligocene South American rodents or primates, the mode, timing and biogeography of these extraordinary dispersals remained debated. Here, we describe South America's oldest known rodents, based on a new diverse caviomorph assemblage from the late Middle Eocene (approx. 41 Ma) of Peru, including five small rodents with three stem caviomorphs. Instead of being tied to the Eocene/Oligocene global cooling and drying episode (approx. 34 Ma), as previously considered, the arrival of caviomorphs and their initial radiation in South America probably occurred under much warmer and wetter conditions, around the Mid-Eocene Climatic Optimum. Our phylogenetic results reaffirm the African origin of South American rodents and support a trans-Atlantic dispersal of these mammals during Middle Eocene times. This discovery further extends the gap (approx. 15 Myr) between first appearances of rodents and primates in South America.

Additional Information

We thank the IRD-PeruPetro Convention Programme, the Canaan Shipibo Native Community and Maple Gas Peru S.A. for access to the field, J.-L. Hartenberger, F. Delsuc, M. Steiper and O. Bertrand for fruitful discussion, P. Baby, M. Roddaz, C. Gautheron, Y. Calderón and L. Quiroz for help with fieldwork, F. Leite and D. Carvajal for their work on pollen, and C. Cazevieille (Centre de Ressources en Imagerie Cellulaire, Montpellier) for access to a scanning electron microscope facility. We are much indebted to R. Cifelli for having edited this article, as well as to C. de Muizon and E. F. Seiffert for their constructive remarks on an earlier version of the manuscript. P.-O.A. was supported by CNRS 'Eclipse 2', CNRS 'Paleo2' and Toulouse University 'SPAM'; L.M. and M.J.O. were supported by ANR-08-JCJC-0017 (PALASIAFRICA); G.B. and T.M. were supported by Alexander von Humboldt-Foundation, Bonn. Publication ISEM 2011-126.

Additional details

Created:
August 22, 2023
Modified:
October 25, 2023