The mineralogy and structure of use-wear polish on chert

Abstract Polished edges of archaeological stone tools are commonly investigated to obtain information on the tools’ uses in prehistory. Yet to this day, it remains unclear what exactly such polishes are and how they form. Answering these questions should allow the elaboration of new interpretative m...

Full description

Bibliographic Details
Main Authors: Patrick Schmidt, Alice Rodriguez, Kaushik Yanamandra, Rakesh K. Behera, Radu Iovita
Format: Article
Language:English
Published: Nature Publishing Group 2020-12-01
Series:Scientific Reports
Online Access:https://doi.org/10.1038/s41598-020-78490-0
id doaj-b0d4303c35694a4c9d24420e5b6d5e8a
record_format Article
spelling doaj-b0d4303c35694a4c9d24420e5b6d5e8a2020-12-13T12:30:28ZengNature Publishing GroupScientific Reports2045-23222020-12-011011910.1038/s41598-020-78490-0The mineralogy and structure of use-wear polish on chertPatrick Schmidt0Alice Rodriguez1Kaushik Yanamandra2Rakesh K. Behera3Radu Iovita4Department of Early Prehistory and Quaternary Ecology, Eberhard Karls University of TübingenAnthrotopography Laboratory, Center for the Study of Human Origins, Department of Anthropology, New York UniversityComposite Materials and Mechanics Laboratory, Mechanical and Aerospace Engineering Department, New York University, Tandon School of EngineeringComposite Materials and Mechanics Laboratory, Mechanical and Aerospace Engineering Department, New York University, Tandon School of EngineeringDepartment of Early Prehistory and Quaternary Ecology, Eberhard Karls University of TübingenAbstract Polished edges of archaeological stone tools are commonly investigated to obtain information on the tools’ uses in prehistory. Yet to this day, it remains unclear what exactly such polishes are and how they form. Answering these questions should allow the elaboration of new interpretative methods based on objective measurements. Two major competing hypotheses of polish formation have been proposed: abrasion and the formation of a thin amorphous film on the chert or flint surface. We employ reflectance infrared spectroscopy, a technique particularly sensitive to thin amorphous films, to investigate these two hypotheses. We found no added amorphous layer that would have formed upon friction against bone, antler, ivory or wood. Our observations suggest polish formation by abrasion, notwithstanding previous claims of added amorphous surface structures. This has implications for our understanding of the physical processes taking place during friction of chert and flint against different materials. Our results also open the possibility to propose new pathways for identifying different use-wear processes, based on the degree of abrasion.https://doi.org/10.1038/s41598-020-78490-0
collection DOAJ
language English
format Article
sources DOAJ
author Patrick Schmidt
Alice Rodriguez
Kaushik Yanamandra
Rakesh K. Behera
Radu Iovita
spellingShingle Patrick Schmidt
Alice Rodriguez
Kaushik Yanamandra
Rakesh K. Behera
Radu Iovita
The mineralogy and structure of use-wear polish on chert
Scientific Reports
author_facet Patrick Schmidt
Alice Rodriguez
Kaushik Yanamandra
Rakesh K. Behera
Radu Iovita
author_sort Patrick Schmidt
title The mineralogy and structure of use-wear polish on chert
title_short The mineralogy and structure of use-wear polish on chert
title_full The mineralogy and structure of use-wear polish on chert
title_fullStr The mineralogy and structure of use-wear polish on chert
title_full_unstemmed The mineralogy and structure of use-wear polish on chert
title_sort mineralogy and structure of use-wear polish on chert
publisher Nature Publishing Group
series Scientific Reports
issn 2045-2322
publishDate 2020-12-01
description Abstract Polished edges of archaeological stone tools are commonly investigated to obtain information on the tools’ uses in prehistory. Yet to this day, it remains unclear what exactly such polishes are and how they form. Answering these questions should allow the elaboration of new interpretative methods based on objective measurements. Two major competing hypotheses of polish formation have been proposed: abrasion and the formation of a thin amorphous film on the chert or flint surface. We employ reflectance infrared spectroscopy, a technique particularly sensitive to thin amorphous films, to investigate these two hypotheses. We found no added amorphous layer that would have formed upon friction against bone, antler, ivory or wood. Our observations suggest polish formation by abrasion, notwithstanding previous claims of added amorphous surface structures. This has implications for our understanding of the physical processes taking place during friction of chert and flint against different materials. Our results also open the possibility to propose new pathways for identifying different use-wear processes, based on the degree of abrasion.
url https://doi.org/10.1038/s41598-020-78490-0
work_keys_str_mv AT patrickschmidt themineralogyandstructureofusewearpolishonchert
AT alicerodriguez themineralogyandstructureofusewearpolishonchert
AT kaushikyanamandra themineralogyandstructureofusewearpolishonchert
AT rakeshkbehera themineralogyandstructureofusewearpolishonchert
AT raduiovita themineralogyandstructureofusewearpolishonchert
AT patrickschmidt mineralogyandstructureofusewearpolishonchert
AT alicerodriguez mineralogyandstructureofusewearpolishonchert
AT kaushikyanamandra mineralogyandstructureofusewearpolishonchert
AT rakeshkbehera mineralogyandstructureofusewearpolishonchert
AT raduiovita mineralogyandstructureofusewearpolishonchert
_version_ 1724384686715699200