Please use this identifier to cite or link to this item: https://cir.cenieh.es/handle/20.500.12136/2674
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dc.contributor.authorLouys, Julien-
dc.contributor.authorDuval, Mathieu-
dc.contributor.authorPrice, Gilbert J.-
dc.contributor.authorWestaway, Kira-
dc.contributor.authorZaim, Yahdi-
dc.contributor.authorRizal, Yan-
dc.contributor.authorPuspaningrum, Mika R.-
dc.contributor.authorTrihascaryo, Agus-
dc.contributor.authorBreitenbach, Sebastian F. M.-
dc.contributor.authorKwiecien, Ola-
dc.contributor.authorCai, Yanjun-
dc.contributor.authorHiggins, Penny-
dc.contributor.authorAlbers, Paul C. H.-
dc.contributor.authorVos, John de-
dc.contributor.authorRoberts, Patrick-
dc.date.accessioned2022-06-01T13:58:13Z-
dc.date.issued2022-04-
dc.identifier.citationPhilosophical Transactions of the Royal Society B-Biological Sciences, 2022, 377(1849), 20200494es_ES
dc.identifier.issn0962-8436-
dc.identifier.issn1471-2970-
dc.identifier.urihttp://cir.cenieh.es/handle/20.500.12136/2674-
dc.description.abstractSome of the earliest evidence for the presence of modern humans in rainforests has come from the fossil deposits of Lida Ajer in Sumatra. Two human teeth from this cave were estimated to be 73–63 thousand years old, which is significantly older than some estimates of modern human migration out of Africa based on genetic data. The deposits were interpreted as being associated with a rainforest environment based largely on the presence of abundant orangutan fossils. As well as the main fossil-bearing chamber, fossil-bearing passages are present below a sinkhole, although the relationship between the different fossil deposits has only been tenuously established. Here, we provide significant new sedimentological, geochronological and palaeoecological data aimed at reconstructing the speleological and environmental history of the cave and the clastic and fossil deposits therein. Our data suggest that the Lida Ajer fossils were deposited during Marine Isotope Stage 4, with fossils from the lower passages older than the main fossil chamber. Our use of stable carbon and oxygen isotope analyses of mammalian tooth enamel demonstrates that early humans probably occupied a closed-canopy forest very similar to those present in the region today, although the fossil orangutans may have occupied a slightly different niche.es_ES
dc.description.sponsorshipThis work was supported by the Australian Research Council (FT160100450); a Spanish Ramón y Cajal Fellowship (RYC2018-025221-I); the European Research Council (starter grant PANTROPOCENE (no. 850709)); and the Max Planck Society. Permission for the research was granted by the Indonesian government–RISTEK Foreign Research Permit (Louys 2483/FRP/E5/Dit.KI/V/2018). M.D. is grateful to María Jesús Alonso Escarza, Javier Iglesias Cibanal, David Martínez Asturias and Leticia Miguens Rodríguez, CENIEH, for technical support throughout the ESR dating analytical procedure. K.W. is grateful to Kaushal Tewari for technical support throughout the OSL dating procedure.es_ES
dc.language.isoenes_ES
dc.publisherThe Royal Societyes_ES
dc.rightsinfo:eu-repo/semantics/openAccesses_ES
dc.rightsAttribution 4.0 International (CC BY 4.0)*
dc.rights.urihttps://creativecommons.org/licenses/by/4.0/*
dc.subjectEarly humanses_ES
dc.subjectPleistocenees_ES
dc.subjectRainforestes_ES
dc.subjectSoutheast Asiaes_ES
dc.subjectFossilses_ES
dc.titleSpeleological and environmental history of Lida Ajer cave, western Sumatraes_ES
dc.typeArticlees_ES
dc.identifier.doi10.1098/rstb.2020.0494-
dc.relation.publisherversionhttps://doi.org/10.1098/rstb.2020.0494es_ES
dc.date.available2022-06-01T13:58:13Z-
Appears in Collections:Datación por Resonancia Paramagnética Electrónica
Geocronología y Geología



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