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Although the extinct Quaternary megafauna is widely recorded in northeastern Brazil, geochronological studies carried out on its fossiliferous deposits are still scarce. In this study, Electron Spin Resonance (ESR) was applied to date 12 tooth fragments of Toxodon platensis (Mammalia, Notoungulata) collected in the tank deposit of Lago do Rumo, Baixa Grande, state of Bahia, Brazil. The results obtained in the geochronological analysis performed here reveal ages from around 60 ka to 34 ka for T. platensis in Lagoa do Rumo; and, considering the integration data in the paleontological literature, our results evidence the largest time-averaging ever recorded for tank deposits: around 51 thousand years. • Twelve teeth of Toxodon platensis from Brazilian Northeast were dated using Electron Spin Resonance. • Absolute dating revealed fossils of Toxodon platensis ranging from around 60 ky to 34 ky. • Considering the literature, time-averaging in Lagoa do Rumo is around 51 thousand years. [ABSTRACT FROM AUTHOR]

We applied the ESR (Electron Spin Resonance) dating method to fossils of Notiomastodon platensis (two teeth) and Toxodontinae (two teeth) found in the fossiliferous deposit of Lajedão do Patrício, João Dourado, State of Bahia, Brazil, to identify the period of formation of this fossil accumulation. Neutron Activation Analysis was applied to determine the concentrations of the main radioisotopes in enamel, dentine and sediment. The ages found for N. platensis are 16.8 ± 2.6 ka and 12.5 ± 2.3 ka, while the ages for Toxodontinae are 9.6 ± 1 ka and 9.1 ± 1 ka. The results for Notiomastodon. platensis and Toxodontinae are similar to other fossiliferous of Brazil. The estimated maximum time-averaging for Lajedão do Patrício is 11.3 ka, indicating a long period of accumulation of skeletal remains, attributed to resedimentation and reworking. The crossing between the period of formation of fossil assemblage Lajedão do Patrício and ages of climatic variations diponible in paleoclimatic curves produced for the Quaternary of northeastern Brazil indicates different climatic and environmental conditions during the formation of the deposit. • Dating Electron Spin Resonance (ESR) Notiomastodon platensis and Toxodontiane from the Quaternary of Northeast Brazil. • Notiomastodon platensis are 16.8 ± 2.6 ka and 12.5 ± 2.3 ka, and Toxodontinae 9.6 ± 1 ka and 9.1 ± 1 ka. • Maximum time-averaging for Lajedão do Patrício is 11.3 ka, indicating a long period of accumulation. • Comparison of Lajedão do Patrício and paleoclimatic curves different climatic and environmental conditions. [ABSTRACT FROM AUTHOR]