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Exploring the Later Stone Age at a micro-scale: new high-resolution excavations at Wonderwerk Cave

dc.contributor.authorRhodes, Sara
dc.contributor.authorGoldberg, Paul
dc.contributor.authorEcker, Michaela
dc.contributor.authorHorwitz, Liora Kolska
dc.contributor.authorBoaretto, Elisabetta
dc.contributor.authorChazan, Michael
dc.date.accessioned2022-03-11T12:06:17Z
dc.date.available2022-03-11T12:06:17Z
dc.date.issued2022
dc.description.abstractIn 2018, we initiated renewed excavation of the Later Stone Age (LSA) deposits at Wonderwerk Cave. Here we describe the goals and initial results of the first two seasons of excavation, including the first micromorphological description of these deposits. We employed a small-scale excavation technique to emphasize precision recording and limit the destruction of sensitive deposits. Our preliminary results indicate that meaningful patterns in material culture records and paleoecological proxy materials can be derived from such investigations. Bioturbation of the LSA deposits is widespread in our micromorphological samples, suggesting that some postdepositional movement of the sediment occurred but did not impact overall stratigraphic integrity. This is supported by the radiocarbon chronology (derived from various material records), which indicates that this movement had a limited effect on the material record. Three technocomplexes (the Kuruman/Oakhurst, Wilton, and Historic) were identified in the new Wonderwerk lithic material record, alongside increasing evidence for a period of intensified use and/or occupation of the site during the Wilton - a pattern previously identified by the F. Thackeray's and A. Thackeray's 1970s excavations. New radiocarbon ages support previous determinations placing the timing of this intensification at ca. 6200 years cal BP. Faunal and ostrich eggshell records also support previous findings, confirming an anthropogenic origin for the faunal remains and suggesting that different pathways of OES bead production were employed at the site at different times. The presence of herbivore dung and associated spherulites in a micromorphology thin section provides a new potential line of evidence to support the Thackeray's tentative suggestion for sheep herding at the site ca. 2000 years BP. While this evidence is far from conclusive, it suggests that the Wonderwerk Cave LSA record may have a role to play in resolving the timing of the adoption of sheep by hunter-gatherers on the Ghaap Plateau. Our work on the LSA at Wonderwerk Cave serves as a touchstone within the more regionally focused Northern Cape Archaeology and Ecology Project (NCAEP) - an international and interdisciplinary research project studying the LSA paleoenvironment of the South African arid interior. Ultimately, NCAEP is designed to produce a multi-proxy diachronic climatic record of the Northern Cape firmly situated within new and existing radiocarbon chronologies.pt_PT
dc.description.versioninfo:eu-repo/semantics/publishedVersionpt_PT
dc.identifier.doi10.1016/j.quaint.2021.10.004pt_PT
dc.identifier.issn1040-6182
dc.identifier.urihttp://hdl.handle.net/10400.1/17669
dc.language.isoengpt_PT
dc.peerreviewedyespt_PT
dc.publisherElsevierpt_PT
dc.subjectLater Stone Agept_PT
dc.subjectNorthern Capept_PT
dc.subjectWiltonpt_PT
dc.subjectMicroarchaeologypt_PT
dc.subjectMicromorphologypt_PT
dc.subjectWonderwerk Cavept_PT
dc.titleExploring the Later Stone Age at a micro-scale: new high-resolution excavations at Wonderwerk Cavept_PT
dc.typejournal article
dspace.entity.typePublication
oaire.citation.endPage145pt_PT
oaire.citation.startPage126pt_PT
oaire.citation.titleQuaternary Internationalpt_PT
oaire.citation.volume614pt_PT
person.familyNameRhodes
person.givenNameSara
person.identifier.ciencia-idC41A-E5EA-D62E
person.identifier.orcid0000-0001-7328-4663
rcaap.rightsrestrictedAccesspt_PT
rcaap.typearticlept_PT
relation.isAuthorOfPublicationb14f41c8-6c9e-43f6-83b2-9dbea65677e0
relation.isAuthorOfPublication.latestForDiscoveryb14f41c8-6c9e-43f6-83b2-9dbea65677e0

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