2021
DOI: 10.1371/journal.pone.0254603
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Tracing the spatial imprint of Oldowan technological behaviors: A view from DS (Bed I, Olduvai Gorge, Tanzania)

Abstract: DS (David’s site) is one of the new archaeological sites documented in the same paleolandscape in which FLK 22 was deposited at about 1.85 Ma in Olduvai Gorge. Fieldwork in DS has unearthed the largest vertically-discrete archaeological horizon in the African Pleistocene, where a multi-cluster anthropogenic accumulation of fossil bones and stone tools has been identified. In this work we present the results of the techno-economic study of the lithic assemblage recovered from DS. We also explore the spatial mag… Show more

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Cited by 20 publications
(5 citation statements)
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References 126 publications
(215 reference statements)
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“…However, first generation flakes are more common in volcanic rocks (21.1%) than in quartzite (5.4%). In general lavas are more prone to cortical retention (54.5% of volcanic rocks retain some dorsal cortex versus 18.6% of quartzite), a trait that might support the idea that second and third generation volcanic flakes could have been taken off-site more easily (Diez-Martı ´n et al, 2021). In line with the previous statement, cortical butts are more common in lavas than in quartzite (26 versus 7%).…”
supporting
confidence: 75%
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“…However, first generation flakes are more common in volcanic rocks (21.1%) than in quartzite (5.4%). In general lavas are more prone to cortical retention (54.5% of volcanic rocks retain some dorsal cortex versus 18.6% of quartzite), a trait that might support the idea that second and third generation volcanic flakes could have been taken off-site more easily (Diez-Martı ´n et al, 2021). In line with the previous statement, cortical butts are more common in lavas than in quartzite (26 versus 7%).…”
supporting
confidence: 75%
“…This percentage is in contradiction with the data provided by the core sample, where quartzite cores only represent a mean of 24.73% (sd = 6). Overrepresentation of quartzite flakes and deficit of volcanic flakes represents a consistent pattern in Bed I sites (Brantingham, 1998;Kimura, 2002;Leakey, 1975;McNabb, 1998;Potts, 1988) and might be related to: a) a longer life of volcanic cutting edges (Key et al, 2020) and consequently more intense circulation of volcanic flakes across the landscape (Brantingham, 1998;Diez-Martı ´n et al, 2021); b) the specific crystallographic traits of Naibor Soit quartzite (coarse-grained structure and abundant cleavage planes) that accelerate reduction and promote a faster and more intensive reduction of cores (Potts, 1988). Less controlled quartzite response to breakage might account for significant amounts of quartzite waste in the ZP sites, particularly in the case of FLK 22.…”
mentioning
confidence: 97%
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“…Relative spatial distributions and artifact cluster significances were assessed with the relative risk function. Artifact spatial correlations were evaluated with the nearest neighbor equality function 109 , 110 . Analyses were performed using the R spatstat package 111 , 112 .…”
Section: Methodsmentioning
confidence: 99%
“…Ma) (Table 1; Figure 4) manufactured >1,400 artefacts from quartzite, basalt, phonolite, gneiss, chert, and hyaline quartz, with igneous rocks contributing more than five times the total weight of quartzite (Diez-Martín et al 2021). The difference in raw material weight, in combination with techno-typological data, indicate that hominins at DS preferentially utilised volcanic rocks for flake production and percussion activities, and these materials were likely provisioned from indeterminate fluvial channels to the south (Diez-Martín et al 2021).…”
Section: Oldowan Raw Materials Provisioningmentioning
confidence: 99%