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Continuity, Variability and the Nature of Technological Change During the Late Pleistocene at Klipfonteinrand Rockshelter in the Western Cape, South Africa

  • Marika LowEmail author
Original Article

Abstract

This paper discusses the late Pleistocene lithic sequence at Klipfonteinrand (KFR) rockshelter in the eastern Cederberg of the Western Cape. A characteristically Robberg technological system associated with the production of small silcrete blades from small cores was in place at the site by ~ 22 ka (thousand years ago) with a hornfels-dominant, non-microlithic Oakhurst system replacing it ~ 16 ka. Key technological differences in lithic material selection, artifact size, form, and techniques relating to the manufacturing process itself are apparent between early and later components within the Robberg, and between the Robberg and Oakhurst more broadly. Results suggest that technological change during the late Pleistocene was a fluid process involving continual modifications within the broad regional technological system. Variation during the Robberg occurred within a constrained range and the nature of change through the sequence was overall relatively gradual. The KFR data contributes to the emerging picture of the Robberg as temporally, spatially, and technologically complex with nuanced variation at a very fine scale of analysis.

Keywords

Robberg Lithic technology Klipfonteinrand South Africa Variability Technological change 

Résumé

Cet article caractérise la séquence lithique du pléistocène supérieur provenant du Klipfonteinrand Rockshelter (KFR) situé dans la région du Cederberg oriental (Cap-Occidental). Le système technologique de Robberg est. ici associé à la production de petites lames de silcrète faites à partir de petits noyaux qui étaient sur le site il y a environ 22 ka (il y a mille ans). Ce système est. par la suite remplacé par celui d’Oakhurst étant non microlitique à dominante cornéenne à une date relativement précoce ~16 ka. Les principales différences technologiques dans la sélection des matériaux lithiques, la taille ou la forme des artéfacts et des techniques relatives au processus de fabrication sont apparentes entre les composantes précoces et postérieures du système de Robberg et, plus généralement, entre Robberg et Oakhurst. Les résultats suggèrent que le changement technologique vers la fin du pléistocène était un processus fluide impliquant des modifications continuelles au sein d’un plus large système technologique étant en place à ce moment-là. Durant le système de Robberg, la variation s'est produite et a été contrainte par la nature du changement effectuer à travers la séquence qui était dans l'ensemble relativement graduelle. Les données de KFR contribuent à l'image émergente du système de Robberg se définissant comme complexe temporellement, spatialement et technologiquement avec une variation nuancée relative à la nature du changement technologique apparente sur une échelle plus réduite.

Notes

Acknowledgements

Funding for research at Klipfonteinrand comes from the Australian Research Council grant DP#1092445 or DE130100068 awarded to Alex Mackay. My research has been conducted with the additional support of the Australian Government Research Training Program Scholarship and by grants from the Centre for Archaeological Science and the University of Wollongong. Thank you to Alex Mackay and Sam Lin for comments on the earlier drafts. Thanks particularly to Sam Lin for his guidance and patience in providing advice and assistance with the statistical analyses performed in this study. Thanks to Shane Hourigan for producing the locational figure and to Mélissa Verrier for translating the abstract into French. Thanks also to the Archaeology department at the University of Cape Town for providing lab space.

Compliance with Ethical Standards

Conflict of Interest

The author declares no conflict of interest.

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Copyright information

© Springer Science+Business Media, LLC, part of Springer Nature 2019

Authors and Affiliations

  1. 1.Centre for Archaeological Science, School of Earth and Environmental SciencesUniversity of WollongongWollongongAustralia

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