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Please use this identifier to cite or link to this item: http://hdl.handle.net/10362/4596

Título: Paleoclimatic and paleobiological correlations by mammal faunas from Southern America and SW Europe
Autor: Alberdi, M. T.
Bonadonna, F. P.
Cerdeño, E.
Leone, G.
Longinelli, A.
Prado, J. L.
Sánchez, B.
Tonni, E. P.
Palavras-chave: Correlation
Mammals
Paleoclimatology
Geochemistry
Neogene
Issue Date: 1992
Resumo: The preliminary results of a research dealing with the study of global changes in the last 5 Ma by correlations of continental records between the Northern and the Southern Hemispheres (SW Europe and Argentina, respectively) are reported. The first analyses of the evolutionary patterns point out, in Argentina, two different turnover times: the first one is characterized by a high percentage of mammalautochthonous extinctions placed in the span of time between the last Chapadmalalan and the first Ensenadan faunas, around 2.5-2.3 Ma. It is possible to identify a high percentage of new immigrant genera from North America in the first turnover, while the second one, associated to the "last Pleistocene megafaunal extinctions", probably occurred at the beginning of the "Glacial Pleistocene", around 1.0-0.8 Ma. The oxygen isotope composition of phosphate from fossil mammal bones was measured to have a better climatic resolution from faunal elements of two hemispheres and to compare them by results as quantitative as possible. The preliminary efforts are brought out on fourteen deposits from SE Spain. Isotopic and chemical results strongly suggest the existence of a relation between the oxygen isotope composition in various skeletal components and the taphonomic processes of a single deposit. The variations of 0180 in the mammal teeth of Equidae from SE Spain suggest a shift towards a colder environment from the older one, Huelago, to more recent deposits, as well as from Venta Micena to Fuensanta in agreement with the transition from the Middle to the Upper Villafranchian, around 2.5 Ma, and the transition between the "Preglacial" to the "Glacial" Pleistocene, around 1.9-0.8 Ma.
Descrição: Proceedings of the 1" R.C.A.N.S. Congress, Lisboa, October 1992
URI: http://hdl.handle.net/10362/4596
Appears in Collections:FCT: DCT - Ciências da Terra

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