Bone Fractures under the Microscope. An Experimental Approach to Mid-Upper Paleolithic Faunal Remains
The result's identifiers
Result code in IS VaVaI
<a href="https://www.isvavai.cz/riv?ss=detail&h=RIV%2F68081731%3A_____%2F22%3A00567320" target="_blank" >RIV/68081731:_____/22:00567320 - isvavai.cz</a>
Alternative codes found
RIV/68081758:_____/22:00567320 RIV/62690094:18460/22:50019722
Result on the web
<a href="https://www.sav.sk/index.php?lang=sk&doc=journal-list&part=article_response_page&journal_article_no=29515" target="_blank" >https://www.sav.sk/index.php?lang=sk&doc=journal-list&part=article_response_page&journal_article_no=29515</a>
DOI - Digital Object Identifier
<a href="http://dx.doi.org/10.31577/szausav.2022.69.10" target="_blank" >10.31577/szausav.2022.69.10</a>
Alternative languages
Result language
angličtina
Original language name
Bone Fractures under the Microscope. An Experimental Approach to Mid-Upper Paleolithic Faunal Remains
Original language description
Bone fragmentation results from different natural processes or various activities employed by several taphonomic agents. However, it may also represent direct evidence of deliberate human activity connected to the exploitation of animal resources throughout the Paleolithic period. Extensive long mammal bone fragmentation research resulted in last decades into description of individual fracture characteristics reflecting the background of fragmentation process (Johnson 1985, Outram 2001). The features combine macroscopic traits such as angle, an outline, and surface texture of the fracture. However, as the experimental works show, the response of bone on a gross scale is in great extent given by microstructure and its state of preservation directly correlating with the biomechanical properties (Currey 2012, Gifford-Gonzales 2018). The paper aims on testing (1) whether the microscopic features correlate with described macroscale differences or even (2) are able to distinguish features with macroscopic overlaps but of different origin. We have thus tested and applied two microscopic methods on two experimental assemblages with documented fragmentation conditions. By the scanning electron microscopy (SEM) we observed irregularities and micro-fractures in bone fracture surface (FS). They proved to be in certain aspect specific for a given state of bone preservation. Transmitted light microscopy mapped the abundance of micro-cracking, its characteristic features in relation to bone preservation and specific way of fragmentation. The histological thin-sections (HTS) revealed a variety of micro-cracking penetrating the FS, but they did not prove any differentiating pattern among observed experimental sets. A range of different surface profiles was documented, the profile morphology seems to be characteristic for individual bone preservation states. If compared to macroscopic method (FFI), the study of microscopic features in their presented extent did not allow us to differentiate further between fractures. Finally, we undertook an example application of the macroscopic fracture analysis on settlement areas from the Gravettian site Pavlov I (Czech Republic) and we discuss the potential of suggested micro-methods in taphonomic analysis dealing with animal body manipulation and exploitation.
Czech name
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Czech description
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Classification
Type
J<sub>imp</sub> - Article in a specialist periodical, which is included in the Web of Science database
CEP classification
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OECD FORD branch
60102 - Archaeology
Result continuities
Project
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Continuities
I - Institucionalni podpora na dlouhodoby koncepcni rozvoj vyzkumne organizace
Others
Publication year
2022
Confidentiality
S - Úplné a pravdivé údaje o projektu nepodléhají ochraně podle zvláštních právních předpisů
Data specific for result type
Name of the periodical
Študijné zvesti Archeologického ústavu Slovenskej akadémie vied
ISSN
0560-2793
e-ISSN
—
Volume of the periodical
69
Issue of the periodical within the volume
2
Country of publishing house
CZ - CZECH REPUBLIC
Number of pages
18
Pages from-to
187-204
UT code for WoS article
000925144300001
EID of the result in the Scopus database
2-s2.0-85151485314