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Authordc.contributor.authorLópez Mendoza, Patricio 
Authordc.contributor.authorCartajena Fasting, María Isabel 
Authordc.contributor.authorCarabias, Diego 
Authordc.contributor.authorPrevosti, Francisco J. 
Authordc.contributor.authorMaldonado, Antonio 
Authordc.contributor.authorFlores Aqueveque, Valentina Alejandra 
Admission datedc.date.accessioned2018-07-26T15:01:34Z
Available datedc.date.available2018-07-26T15:01:34Z
Publication datedc.date.issued2018
Cita de ítemdc.identifier.citationQuaternary International 463 (2018) 153-160es_ES
Identifierdc.identifier.other10.1016/j.quaint.2016.08.017
Identifierdc.identifier.urihttps://repositorio.uchile.cl/handle/2250/150302
Abstractdc.description.abstractSite GNL Quintero 1 (GNLQ1), located nearshore at Quintero bay in the central coast of Chile (32 degrees S), is the only documented Late Pleistocene drowned terrestrial site along the Pacific coast of South America. During the last decade, through underwater archaeological operations conducted at GNLQ1, several clusters of shallowly buried bone deposits were documented and excavated, revealing a well preserved high-resolution in situ context. Taxonomic analysis of the faunal assemblage recovered yielded at least 26 individuals comprising extinct Camelidae, Cervidae, Equidae, Mylodontidae, and Xenarthra as well as Canidae, Myocastoridae, Octodontidae, Cricetidae, among others. By conducting stable isotope analyses (delta C-13(ap) and delta O-18(ap))on mammalian bioapatite, we aim to perform a first characterization of the GNLQ1 taxa paleoecology and carry out paleoenvironmental inferences. Regional records for the Last Glacial Maximum (LGM) suggest lower sea surface temperatures and more humid climatic conditions for Central Chile. Isotopic data obtained suggests a landscape of mixed vegetation areas, in good agreement with the sedimentary context of the fossil remains and a preliminary Quintero paleolandscape model: a wetland environment developed under semiarid conditions prior to post-glacial sea level rise, with GNLQ1 located > 6 km inland as the paleoshoreline was further out on the continental shelf.es_ES
Patrocinadordc.description.sponsorshipGNL Quintero S.A Project Fondecyt 11121543 CONICET PICT 2011-309 2015-966 ANPCyT PIP 2011-164 NC120066es_ES
Lenguagedc.language.isoenes_ES
Publisherdc.publisherElsevieres_ES
Type of licensedc.rightsAttribution-NonCommercial-NoDerivs 3.0 Chile*
Link to Licensedc.rights.urihttp://creativecommons.org/licenses/by-nc-nd/3.0/cl/*
Sourcedc.sourceQuaternary Internationales_ES
Keywordsdc.subjectLate Pleistocenees_ES
Keywordsdc.subjectMammalses_ES
Keywordsdc.subjectPaleoecologyes_ES
Keywordsdc.subjectStable isotopeses_ES
Keywordsdc.subjectContinental shelfes_ES
Keywordsdc.subjectCentral Chilees_ES
Títulodc.titleReconstructing drowned terrestrial landscapes. Isotopic paleoecology of a late Pleistocene extinct faunal assemblage: site GNL Quintero 1 (GNLQ1) (32 degrees S, central Chile)es_ES
Document typedc.typeArtículo de revista
Catalogueruchile.catalogadortjnes_ES
Indexationuchile.indexArtículo de publicación ISIes_ES


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Attribution-NonCommercial-NoDerivs 3.0 Chile
Except where otherwise noted, this item's license is described as Attribution-NonCommercial-NoDerivs 3.0 Chile