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Authordc.contributor.authorLabarca, Rafael 
Authordc.contributor.authorGonzález Guarda, Erwin 
Authordc.contributor.authorLizama Catalán, Álvaro 
Authordc.contributor.authorVillavicencio, Natalia A. 
Authordc.contributor.authorAlarcón Muñoz, Jhonatan 
Authordc.contributor.authorSuazo Lara, Felipe 
Authordc.contributor.authorOyanadel Urbina, Pablo 
Authordc.contributor.authorSoto Huenchumán, Paula 
Authordc.contributor.authorSalazar, Christian 
Authordc.contributor.authorSoto Acuña, Sergio 
Authordc.contributor.authorBuldrini, Karina E. 
Admission datedc.date.accessioned2020-07-02T17:21:13Z
Available datedc.date.available2020-07-02T17:21:13Z
Publication datedc.date.issued2020
Cita de ítemdc.identifier.citationQuaternary Science Reviews 238 (2020) 106282es_ES
Identifierdc.identifier.other10.1016/j.quascirev.2020.106282
Identifierdc.identifier.urihttps://repositorio.uchile.cl/handle/2250/175757
Abstractdc.description.abstractThe Laguna de Tagua Tagua has yielded two important late Pleistocene archaeological sites, Taguatagua 1 and Taguatagua 2, in which a clear early human exploitation of megafauna has been recorded. Particularly in Taguatagua 1 (TT-1), here re-dated around 12,600 cal yr BP, an abundant small faunal assemblage was also recovered, which had not been previously studied in detail. Here we report the first comprehensive taxonomic and taphonomic analysis of this site. We identified 28 different taxa, including mollusks, fish, anurans, reptiles, birds, marsupials, rodents, carnivores, gomphotheres, horses and cervids, making this the richest late Pleistocene site in Chile so far. Among these, sixteen taxa are new for the Chilean late Pleistocene. Birds are the richest group, with ten taxa, followed by rodents with eight taxa. Most of the species currently inhabit the area, but we identified some locally extirpated taxa, together with extinct taxa (exclusively megamammals). Taphonomic analysis suggests a very complex depositional scenario, mostly related to lake-level oscillations which covered and exposed a mainly natural deposited small faunal assemblage. So far, we detected human-made modifications exclusively in horse and cervid bones. Current habitat requirements of the extant fauna, as well as dietary reconstruction of extinct fauna, suggest a highly variable climate and vegetation during the formation of TT-1 since taxa with preferences from semiarid to humid/wooded environments were identified. These results can be related to the changes from cold/wet to dry/warm conditions documented during the Pleistocene - Holocene transition.es_ES
Patrocinadordc.description.sponsorshipAnanuca Foundation Comision Nacional de Investigacion Cientifica y Tecnologica (CONICYT) CONICYT FONDECYT 11170919 3170706 Proyecto Anillo (PIA-ANID, Chile) ACT-172099es_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 Science Reviewses_ES
Keywordsdc.subjectPleistocenees_ES
Keywordsdc.subjectSouth Americaes_ES
Keywordsdc.subjectMegafaunaes_ES
Keywordsdc.subjectSmall faunaes_ES
Keywordsdc.subjectTaphonomyes_ES
Keywordsdc.subjectPaleoenvironmentes_ES
Títulodc.titleTaguatagua 1: New insights into the late Pleistocene fauna, paleoenvironment, and human subsistence in a unique lacustrine context in central Chilees_ES
Document typedc.typeArtículo de revistaes_ES
dcterms.accessRightsdcterms.accessRightsAcceso Abierto
Catalogueruchile.catalogadorlajes_ES
Indexationuchile.indexArtículo de publicación ISI
Indexationuchile.indexArtículo de publicación SCOPUS


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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