@Article{SallesPTGRSOHCS:2016:QuCaSt,
               author = "Salles, Leandro O. and Perini, Fernando A. and Toledo, Peter Mann 
                         de and Guedes, Patricia G. and Ramos, Renato R. C. and Strikis, 
                         Nicolas M. and Oliveira, Luiz Flamarion B. and Hofmann, Gabriel S. 
                         and Calvo, Emilio M. and Stafford Junior, Thomas W.",
          affiliation = "{Universidade Federal do Rio de Janeiro (UFRJ)} and {Universidade 
                         Federal de Minas Gerais (UFMG)} and {Instituto Nacional de 
                         Pesquisas Espaciais (INPE)} and {Universidade Federal do Rio de 
                         Janeiro (UFRJ)} and {Universidade Federal do Rio de Janeiro 
                         (UFRJ)} and {Universidade Federal Fluminense (UFF)} and 
                         {Universidade Federal do Rio de Janeiro (UFRJ)} and {Centro 
                         Universit{\'a}rio La Salle} and {Universidade Federal do Rio de 
                         Janeiro (UFRJ)} and {Aarhus University}",
                title = "A new record of a scelidotheriine ground sloth (Xenarthra, 
                         Mylodontidae) from Central Brazil: quaternary cave stratigraphy, 
                         taxonomy and stable isotopes",
              journal = "Palaeogeography, Palaeoclimatology, Palaeoecology",
                 year = "2016",
               volume = "461",
                pages = "253--260",
                month = "Nov.",
             keywords = "Central Brazil, karst of Serra da Mesa, cave stratigraphy, 
                         megafauna, Scelidotheriinae, microvertebrate associations, 
                         Isotopes.",
             abstract = "An upper fourth molariform of a Scelidotheriine ground sloth is 
                         reported from Cameiro Cave, which is located in the karstic region 
                         of Serra da Mesa (Goias). In this limestone cave the tooth was 
                         found at the base of a depositional sequence, associated with a 2 
                         m thick debris flows deposit, which is covered by the lowest 
                         carbonate crust dated at approximately 200,000 yr BP. Detailed 
                         morphological description, stable isotope data and stratigraphic 
                         context are provided. This represents the first megafauna record 
                         for this region of Central Brazil, where this record is found in 
                         direct association with a diverse microvertebrate fauna.",
                  doi = "10.1016/j.palaeo.2016.08.032",
                  url = "http://dx.doi.org/10.1016/j.palaeo.2016.08.032",
                 issn = "0031-0182",
             language = "en",
           targetfile = "salles_new][.pdf",
        urlaccessdate = "07 maio 2024"
}