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The Oldowan of Zarqa Valley, Northern Jordan

dc.contributor.authorParenti, Fabio
dc.contributor.authorVarejao, Filipe Giovanini
dc.contributor.authorScardia, Giancarlo [UNESP]
dc.contributor.authorOkumura, Mercedes
dc.contributor.authorAraujo, Astolfo
dc.contributor.authorGuedes, Carlos Conforti Ferreira
dc.contributor.authorNeves, Walter Alves
dc.contributor.institutionUniv Fed Parana
dc.contributor.institutionIst Italiano Paleontol Umana
dc.contributor.institutionUniv Fed Ouro Preto
dc.contributor.institutionUniversidade Estadual Paulista (UNESP)
dc.contributor.institutionUniversidade de São Paulo (USP)
dc.date.accessioned2025-04-29T19:14:45Z
dc.date.issued2024-01-20
dc.description.abstractThe fluvial Dawqara Formation, upper Zarqa Valley, eastern side of Jordan Valley, is chronologically constrained between 2.52 and 1.98 Ma. Several artifact-bearing outcrops display a core and flake industry, with no handaxes nor planned flaking. Herein, we describe 40 artifacts from section 334 Lower, the earliest archeological site of the formation and one of the oldest Oldowan complexes outside Africa. Despite the occurrence of basalt rocks, all artifacts were made on chert cobbles displaying various degrees of abrasion due to fluvial transport. The industry is represented by 30 flakes and 10 cores and choppers, preferentially obtained on chert cobbles with massive-fan form, unifacially and bifacially flaked. Most of the flakes present plain or cortical platforms and show on their dorsal faces a unipolar production scheme. Eighteen flakes, from unipolar or undetermined cores, exhibit a discontinuous retouch, defining a denticulated or convex margin. The assemblage is compared to Oldowan or lower Acheulean complexes in and outside Africa, pointing to a rapid spread of unknown hominins with this flaking technology, possibly ascribable to an early Homo clade.en
dc.description.affiliationUniv Fed Parana, Ctr Estudos & Pesquisas Arqueol, Dept Antropol, Rua Bom Jesus 650, BR-80035010 Curitiba, PR, Brazil
dc.description.affiliationIst Italiano Paleontol Umana, Piazza Ruggero Bonghi 2, I-03012 Anagni, FR, Italy
dc.description.affiliationUniv Fed Ouro Preto, Escola Minas, Dept Geol, Campos Morro Cruzeiro S-N Bauxita, BR-35400000 Ouro Preto, MG, Brazil
dc.description.affiliationUniv Estadual Paulista, Inst Geociencias & Ciencias Exatas, Ave 24-A,1515 Bela Vista, BR-13506700 Rio Claro, SP, Brazil
dc.description.affiliationUniv Sao Paulo, Dept Genet & Biol Evolut, R Matao,277 Butanta, BR-05508090 Sao Paulo, SP, Brazil
dc.description.affiliationUniv Sao Paulo, Museu Arqueol & Etnol, Ave Prof Almeida Prado 1466 Butanta, BR-05508070 Sao Paulo, SP, Brazil
dc.description.affiliationUniv Fed Parana, Dept Geol, Ave Cel Francisco H St,S-N Jardim Americas, BR-81270460 Curitiba, PR, Brazil
dc.description.affiliationUniv Sao Paulo, Inst Estudos Avancados, R Anfiteatro,513 Butanta, BR-05508060 Sao Paulo, SP, Brazil
dc.description.affiliationUnespUniv Estadual Paulista, Inst Geociencias & Ciencias Exatas, Ave 24-A,1515 Bela Vista, BR-13506700 Rio Claro, SP, Brazil
dc.description.sponsorshipCoordenao de Aperfeioamento de Pessoal de Nvel Superior
dc.format.extent26
dc.identifierhttp://dx.doi.org/10.1007/s41982-023-00168-6
dc.identifier.citationJournal Of Paleolithic Archaeology. London: Springernature, v. 7, n. 1, 26 p., 2024.
dc.identifier.doi10.1007/s41982-023-00168-6
dc.identifier.urihttps://hdl.handle.net/11449/302513
dc.identifier.wosWOS:001145432400001
dc.language.isoeng
dc.publisherSpringer
dc.relation.ispartofJournal Of Paleolithic Archaeology
dc.sourceWeb of Science
dc.subjectEarly Pleistocene
dc.subjectOldowan
dc.subjectTaphonomy
dc.subjectLithic technology
dc.subjectZarqa Valley
dc.subjectOut of Africa
dc.titleThe Oldowan of Zarqa Valley, Northern Jordanen
dc.typeArtigopt
dcterms.licensehttp://www.springer.com/open+access/authors+rights?SGWID=0-176704-12-683201-0
dcterms.rightsHolderSpringer
dspace.entity.typePublication
unesp.author.orcid0000-0002-5833-5925[1]
unesp.author.orcid0000-0002-3776-9476[2]
unesp.author.orcid0000-0003-3710-7197[3]
unesp.campusUniversidade Estadual Paulista (UNESP), Instituto de Geociências e Ciências Exatas, Rio Claropt

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