Article ID Journal Published Year Pages File Type
4466057 Palaeogeography, Palaeoclimatology, Palaeoecology 2015 17 Pages PDF
Abstract

•We report the most complete Pleistocene avifauna from southern South America.•This is the first South American assemblage from a clear interstadial event (MIS3).•We infer similar habitats during MIS3 in Pampas and post-LGM stadials in SE Brazil.•Late Pleistocene oscillations may have played a more impact on the NW avifaunas.

In the present paper we report the most complete fossil avifauna from the southern cone of South America. The specimens here described were collected in the Paso Otero locality, at the middle stream of the Quequén Grande River, Pampean Region (Buenos Aires Province, Argentina). The fossiliferous levels belong to the La Chumbiada Member of Luján Formation (37,800 ± 2300 yr BP, late Pleistocene). The assemblage is represented by 60 specimens belonging to at least 22 taxa. The radiocarbon age indicates that Paso Otero birds represent the oldest late Pleistocene avifauna known from the South American continent and the first coming from a clear interstadial event (MIS3). Available evidence indicates similar environmental conditions during the MIS3 interstadial in the Pampean Region of Argentina and the post-Last Glacial Maximum stadials in southeastern Brazil. The absence of significant extinction events in the latest Pleistocene–early Holocene avifaunas of Brazil and Argentina suggests that the main avifaunal composition along southeastern continental lowlands may not be affected by the cyclic retraction and extension of open environments. On the contrary, the fossil record of Peru and Ecuador demonstrates that a large number of taxa, including aquatic and predatory-scavenger birds, have gone extinct along Andean environments at the Pacific coast, and late Pleistocene climatic oscillations may have played a more dramatic impact in these avian communities.

Related Topics
Physical Sciences and Engineering Earth and Planetary Sciences Earth-Surface Processes
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