Por favor, use este identificador para citar o enlazar este ítem: https://cir.cenieh.es/handle/20.500.12136/2540
Registro completo de metadatos
Campo DC Valor Lengua/Idioma
dc.contributor.authorSmith, Holly Ellen-
dc.contributor.authorPrice, Gilbert J.-
dc.contributor.authorDuval, Mathieu-
dc.contributor.authorWestaway, Kira E.-
dc.contributor.authorZaim, Jahdi-
dc.contributor.authorRizal, Yan-
dc.contributor.authorAswan, Aswan-
dc.contributor.authorPuspaningrum, Mika R.-
dc.contributor.authorTrihascaryo, Agus-
dc.contributor.authorStewart, Mathew-
dc.contributor.authorLouys, Julien-
dc.date.accessioned2021-09-13T15:37:06Z-
dc.date.issued2021-11-
dc.identifier.citationQuaternary International, 2021, 603, 40-63es_ES
dc.identifier.issn1040-6182-
dc.identifier.urihttp://cir.cenieh.es/handle/20.500.12136/2540-
dc.description.abstractNgalau Gupin is a broad karstic cave system in the Padang Highlands of western Sumatra, Indonesia. Abundant fossils, consisting of mostly isolated teeth from small-to large-sized animals, were recovered from breccias cemented on the cave walls and unconsolidated sediments on the cave floor. Two loci on the walls and floors of Ngalau Gupin, named NG-A and NG-B respectively, are studied. We determine that NG-B most likely formed as a result of the erosion and redeposition of material from NG-A. The collection reveals a rich, diverse Pleistocene faunal assemblage (Proboscidea, Primates, Rodentia, Artiodactyla, Perissodactyla, Carnivora) largely analogous to extant fauna in the modern rainforests of Sumatra. The hippopotamid Hexaprotodon represents the only globally extinct taxon in deposits from Sumatra and the first record of this animal from the island. This fossil assemblage is dated using combined U-series/ESR dating analyses of several teeth that yield a finite age of between ~160 and ~115 ka, depending on the modalities of the dose rate evaluation. Moreover, a direct U-series age estimate of ~70 ka is obtained on the Hexaprotodon specimen, providing a minimum age constraint for the fossil that is compatible with the combined U-series/ESR results. These results suggest that the faunal assemblage at Ngalau Gupin correlates with late MIS 6 or early MIS 5. Ngalau Gupin likely reflects the formation of a fossil assemblage with two primary taphonomic pathways: a prime-aged dominated macrofauna component initially produced by carnivores but subsequently accumulated by porcupines and transported to the cave, and a microfauna component likely accumulated by small carnivores. Decalcification of the cemented deposit has further resulted in loss of fossil and other sedimentary material. This site adds important new chronologically constrained fossil mammal data for the Pleistocene record of Sumatra, an island relatively poorly investigated for Southeast Asia.es_ES
dc.description.sponsorshipThis study was funded by Australian Research Council (ARC) Future Fellowship (FF) FT160100450 granted to J.L. Aspects of the combined U-series/ESR analyses have been funded by the Australian Research Council Future Fellowship Grant FT150100215 and the Spanish Ramón y Cajal Fellowship RYC2018-025221-I granted to M.D. H.S's Postgraduate & Research Scholarships were provided by the Australian Research Centre for Human Evolution, Griffith University, Brisbane.es_ES
dc.language.isoenes_ES
dc.publisherElsevieres_ES
dc.rightsinfo:eu-repo/semantics/openAccesses_ES
dc.rightsAtribución-NoComercial-SinDerivadas 3.0 Estados Unidos de América*
dc.rights.urihttp://creativecommons.org/licenses/by-nc-nd/3.0/us/*
dc.subjectTaxonomyes_ES
dc.subjectTaphonomyes_ES
dc.subjectCavees_ES
dc.subjectPleistocenees_ES
dc.subjectSoutheast Asiaes_ES
dc.subjectHexaprotodones_ES
dc.subjectESR and U-series datinges_ES
dc.titleTaxonomy, taphonomy and chronology of the Pleistocene faunal assemblage at Ngalau Gupin Cave, Sumatraes_ES
dc.typeArticlees_ES
dc.identifier.doi10.1016/j.quaint.2021.05.005-
dc.relation.publisherversionhttps://doi.org/10.1016/j.quaint.2021.05.005es_ES
dc.date.available2021-09-13T15:37:06Z-
Aparece en las colecciones: Datación por Resonancia Paramagnética Electrónica
Geocronología y Geología
Laboratorio de Geología



Este ítem está sujeto a una licencia Creative Commons Licencia Creative Commons Creative Commons