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Mammalian fossils from Gruta do Ioio cave and past of the Chapada Diamantina, northeastern Brazil, using taphonomy, radiocarbon dating and paleoecology

dc.contributor.authorEltink, Estevan
dc.contributor.authorCastro, Mariela
dc.contributor.authorMontefeltro, Felipe Chinaglia [UNESP]
dc.contributor.authorTrindade Dantas, Mario Andre
dc.contributor.authorScherer, Carolina Saldanha
dc.contributor.authorOliveira, Paulo Victor de
dc.contributor.authorLanger, Max Cardoso
dc.contributor.institutionUniv Fed Vale Sao Francisco
dc.contributor.institutionUniversidade Federal de Goiás (UFG)
dc.contributor.institutionUniversidade Estadual Paulista (Unesp)
dc.contributor.institutionUniversidade Federal da Bahia (UFBA)
dc.contributor.institutionUniv Fed Reconcavo Bahia
dc.contributor.institutionUniv Fed Piaui
dc.contributor.institutionUniversidade de São Paulo (USP)
dc.date.accessioned2020-12-10T19:51:17Z
dc.date.available2020-12-10T19:51:17Z
dc.date.issued2020-03-01
dc.description.abstractGruta do Ioio is a cave part of Iraquara carstic system (Salitre Formation, Una Group). Located in the region of the Chapada Diamantina, northeastern Brazil, this partially submerged cave has yielded abundant fossil remains that until now included Siluriformes, an alligatorid crocodilian and a set of mammals, such as representatives of Mustelidae, Rodentia and Chiroptera. Besides the record of Palaeolama major (Camelidae), Pecari tajacu (Tayassuidae), both yielded from subaquatic site, Puma concolor, Leopardus pardalis (Felidae), Chrysocyon brachyurus (Canidae), and a Didelphidae indet. were yielded from newly described subaerial site. Taphonomic features, such as weathering, transport, breakage, bones and taxonomic representation, demonstrate that bioestrationomic and fossildiagenetic conditions varies between fossiliferous accumulations in the cave, and differences are still observed in the same fossil-bearing site (subaerial). The radiocarbon ages indicate the occurrence of Leopardus pardalis at 30,351-30,862 yr cal BP, Palaeolama major at 24,854-25,379 yr cal BP and Pecari tajacu at 8170-8336 yr cal BP. It extends the time range of Gruta do 1oi6 fossils from the Late Pleistocene to the Early-Middle Holocene, encompassing the Last Glacial Maximum. Paleoecological inferences provided by stable isotopes (delta C-13) suggest great proportion of diets based on C-3 plants along the trophic levels, suggesting a denser forest environment and more humid conditions in the region of Gruta do Ioio cave during the Quaternary. The record of taxa, such as Myocastor coypus (a semiaquatic rodent currently distributed in subtropical and temperate South America) and Chrysocyon brachyurus (a typical dweller of open grasslands) shows that past landscape, composed by forests and/or savannic vegetations, contrasts with xeric arboreal scrubland that currently covers the area.en
dc.description.affiliationUniv Fed Vale Sao Francisco, Colegiado Ecol, Senhor Do Bonfim, BA, Brazil
dc.description.affiliationUniv Fed Goias, Dept Ciencias Biol, Catalao, Go, Brazil
dc.description.affiliationUniv Estadual Paulista, Dept Biol & Zootecnia, Ilha Solteira, SP, Brazil
dc.description.affiliationUniv Fed Bahia, Lab Ecol & Geociencias, Vitoria Da Conquista, BA, Brazil
dc.description.affiliationUniv Fed Reconcavo Bahia, Ctr Ciencias Agr Ambientais & Biol, Cruz Das Almas, BA, Brazil
dc.description.affiliationUniv Fed Piaui, Curso Ciencias Biol, Picos, PI, Brazil
dc.description.affiliationUniv Sao Paulo, Lab Paleontol Ribeirao Preto, Ribeirao Preto, SP, Brazil
dc.description.affiliationUnespUniv Estadual Paulista, Dept Biol & Zootecnia, Ilha Solteira, SP, Brazil
dc.description.sponsorshipFundação de Amparo à Pesquisa do Estado de São Paulo (FAPESP)
dc.description.sponsorshipPrimeiros Projetos PROPe UNESP
dc.description.sponsorshipUNIVASF
dc.description.sponsorshipIdFAPESP: 2014/03825-3
dc.description.sponsorshipIdPrimeiros Projetos PROPe UNESP: 730
dc.description.sponsorshipIdUNIVASF: PRPPGI - PC 860/2017
dc.format.extent16
dc.identifierhttp://dx.doi.org/10.1016/j.jsames.2019.102379
dc.identifier.citationJournal Of South American Earth Sciences. Oxford: Pergamon-elsevier Science Ltd, v. 98, 16 p., 2020.
dc.identifier.doi10.1016/j.jsames.2019.102379
dc.identifier.issn0895-9811
dc.identifier.lattes9313332827151714
dc.identifier.orcid0000-0001-6519-8546
dc.identifier.urihttp://hdl.handle.net/11449/196635
dc.identifier.wosWOS:000517664800047
dc.language.isoeng
dc.publisherElsevier B.V.
dc.relation.ispartofJournal Of South American Earth Sciences
dc.sourceWeb of Science
dc.subjectFossils
dc.subjectLimestone Cave
dc.subjectStable Isotopes
dc.subjectRadiocarbon Dating
dc.subjectTaphonomy
dc.subjectChapada Diamantina
dc.subjectQuaternary
dc.titleMammalian fossils from Gruta do Ioio cave and past of the Chapada Diamantina, northeastern Brazil, using taphonomy, radiocarbon dating and paleoecologyen
dc.typeArtigo
dcterms.licensehttp://www.elsevier.com/about/open-access/open-access-policies/article-posting-policy
dcterms.rightsHolderElsevier B.V.
dspace.entity.typePublication
unesp.author.lattes9313332827151714[3]
unesp.author.orcid0000-0001-6519-8546[3]
unesp.departmentBiologia e Zootecnia - FEISpt

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