Isotopic paleoecology (δ13C) from mammals from IUIU/BA and paleoenvironmental reconstruction (δ13C, δ18O) for the Brazilian intertropical region through the late Pleistocene. (15th August 2020)

• Record Type: Journal Article
• Authors: Dantas, Mário André Trindade; Missagia, Rafaela Velloso; Dutra, Rodrigo Parisi; Raugust, Tiago; Silva, Leandro Antônio da; Delicio, Maria Paula; Renó, Rodolfo; Cherkinsky, Alexander
• Is Part Of: Quaternary science reviews. Volume 242(2020)
• Publication Date: 2020-08-15
• Subjects: Megafauna -- Quaternary -- Carbon and oxygen isotopes -- Paleoenvironment -- Diet; Geology, Stratigraphic -- Quaternary -- Periodicals; Stratigraphie -- Quaternaire -- Périodiques; 551.79
• DOI: 10.1016/j.quascirev.2020.106469
• Languages: English
• ISSNs: 0277-3791

Abstract

Abstract: Stable isotopes of carbon and oxygen of fossil specimens are widely used for paleoecological and paleoenvironmental inferences, and there has been an effort to better understand the isotopic paleoecology and chronology of herbivores that inhabited the Brazilian Intertropical Region during the late Quaternary. In the present work, new radiocarbon datings and carbon and oxygen isotopes data for Eremotherium laurillardi, Notiomastodon platensis, Tapirus terrestris, Tayassu pecari, and Mazama gouazoubira are presented, from specimens that lived on Iuiu county (Toca Fria and Jatobá caves), state of Bahia, in the Brazilian Intertropical Region. E. laurillardi was dated as of ∼32 ka BP, representing the oldest direct dating for this species in the Brazilian Intertropical Region, while N. platensis was dated as of ∼25 ka BP. Fossils of the extant species T. pecari, M. gouazoubira, and T. terrestris presented radiocarbon ages of ∼23 ka BP, ∼21 ka BP, and ∼15 ka BP, respectively, showing that some of these species lived in Iuiu during the Last Glacial Maximum. According to our analyses, T. terrestris was the only specialist ( δ 13 C = −11.0‰; p i C3 = 0.76; B A = 0.49), whereas the remaining taxa were generalists mixed-feeders ( δ 13 C = −1.3 to −10.0‰; p i C3 = 0.24 to 0.69; B A > 0.58). The paleoenvironment reconstruction in Iuiu and other localities in BIR, during ∼32 ka BP to ∼15 ka BP, allow us to suggest that the dry arboreal to open Savanna habitats (rich in grass and shrubs) were the most common environment. Highlights: Radiocarbon datings for extant and extinct taxa from Brazilian Intertropical Region. Unpublished isotopic data for Pleistocenic mammals from Bahia, Brazil. Paleoenvironmental reconstruction for six late Pleistocene localities from BIR.