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Diversity and significance of core preparation in the Developed Oldowan technology: reconstructing the flaking processes at SHK and BK (Middle‐Upper Bed II, Olduvai Gorge, Tanzania)
Author(s) -
SánchezYustos Policarpo,
DiezMartín Fernando,
DomínguezRodrigo Manuel,
Duque Javier,
Fraile Cristina,
Baquedano Enrique,
Mabulla Audax
Publication year - 2017
Publication title -
boreas
Language(s) - English
Resource type - Journals
SCImago Journal Rank - 0.95
H-Index - 74
eISSN - 1502-3885
pISSN - 0300-9483
DOI - 10.1111/bor.12237
Subject(s) - acheulean , flake , olduvai gorge , geology , debitage , knapping , taphonomy , lithic technology , paleontology , paleoanthropology , archaeology , geography , pleistocene , fishery , biology
Core preparation has been documented in Developed Oldowan assemblages dated between 1.5–1.3 Ma. However, its correct identification and significance is a matter of debate. In order to shed light on this issue, this paper attempts to reconstruct the flake production processes of the lithic assemblages currently recovered in SHK and BK at Olduvai Gorge (Tanzania). The methodological approach applied for the study of these two classical Developed Oldowan sites is based on the analysis and classification of flaking cores through detailed diacritical and technological descriptions, regardless of aprioristic morphological considerations. The flake production processes identified in both assemblages exhibit great technological homogeneity. The most remarkable difference between them is linked with divergences in flake size production. Core rotation and elongation of the perimeter of the flaked surface were the main technical actions implemented to manage core reduction, and seem to be related to reduction intensity. Core preparation, specifically striking platform preparation, was also applied, but to a minor extent, and was linked with a more effective management of blank reduction. It was not carried out through rigid technical and geometric schemes, and the products obtained were not predetermined. Nevertheless, its mere presence in Developed Oldowan sites is very suggestive, as it confirms a strong relationship between the Developed Oldowan and early Acheulean assemblages.

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