Simulating Lithic Assemblage Composition and Its Relationship to Mobility
Author(s): Matthew Barrett; Simon Holdaway
Year: 2023
Summary
This is an abstract from the "Variability: A Reassessment of Its Meaning, Afforded Range, and the Relation to Process" session, at the 88th annual meeting of the Society for American Archaeology.
Artifact density and techno-morphological form distribution in lithic assemblages are often used to make inferences about mobility. However, the relationship between such observations and mobility strategies varies with socio-natural contexts, leading to contrasting interpretations of the same data. To overcome such indeterminacy, we investigate the physical movement of artifacts as a proxy for the movement of people. An exploratory agent-based simulation indicates how different combinations of lithic reduction, reuse, selection, and transport affect assemblage composition, modeled using nodules of raw material (cores) and the pieces of stone struck from them (flakes). The simulated artifact distributions serve as hypotheses that are tested with empirical data from two surface stone artifact assemblages from semiarid Australia: one low-density record dating to the late Pleistocene, where raw material is not locally available; and one higher-density record from the late Holocene from a context of raw material abundance. These records should exhibit differences in formational processes and the use of stone. However, thought of in relation to the simulation outcomes, similarities in place use are suggested for both records, with a similar set of simple processes responsible for the emergent patterning observed.
Cite this Record
Simulating Lithic Assemblage Composition and Its Relationship to Mobility. Matthew Barrett, Simon Holdaway. Presented at The 88th Annual Meeting of the Society for American Archaeology. 2023 ( tDAR id: 473155)
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Keywords
Geographic Keywords
AUSTRALIA
Spatial Coverage
min long: 111.797; min lat: -44.465 ; max long: 154.951; max lat: -9.796 ;
Record Identifiers
Abstract Id(s): 36940.0