Evidence map›Paper›PMID 33206671›Full record

ArticlePloS one2020

Introducing platform surface interior angle (PSIA) and its role in flake formation, size and shape.

Shannon P McPherron, Aylar Abdolahzadeh, Will Archer, Annie Chan, Igor Djakovic, Tamara Dogandžić, George M Leader, Li Li, Sam Lin, Matthew Magnani and 3 more

Open access · goldAbstract read
In one paragraph

Article in PloS one, 2020. The graph could read no effect estimate from its abstract, so it casts no vote on the map. Cited by 6 papers.

0numbers the graph read from it
0cells of the map it votes in
6citing papers in PubMed
13.8field-weighted citation impact, top 2% of its field
1 · What the graph read from it

What it found

Each row is one number read from the abstract, on the scale the paper reported it, with its interval. Left of the dashed line favours the treatment, right favours the comparator. Under each row is the sentence it came from. New to these charts? A ten-minute tutorial.

The abstract states no effect estimate the extractor could read, or names no intervention and outcome on the map, so this paper lights no cell and moves no belief. It is still indexed, cited and linked below.

2 · The registry

The trial behind it

Trials whose registry record cites this paper, or whose number appears in the abstract. A trial that started after this paper was published is citing it as background, not reporting it.

Neither the registry nor the abstract names a trial number. If this is a trial report, that itself is worth knowing.

3 · Its place in the literature

Who cites it

6 citing papers in PubMed, 19 citations in OpenAlex.

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4 · The record

Corrections and comments

PubMed lists nothing against this paper. Absence here is not a guarantee, only a check that was made.

5 · Who and what money

Authors and funding

13 authors at 8 institutions in 5 countries.

Shannon P McPherronDepartment of Human Evolution, Max Planck Institute for Evolutionary Anthropology, Leipzig, Germany.ORCID 0000-0002-2063-468X
Aylar AbdolahzadehDepartment of Anthropology, University of Pennsylvania, Philadelphia, Pennsylvania, United States of America.
Will ArcherDepartment of Human Evolution, Max Planck Institute for Evolutionary Anthropology, Leipzig, Germany.
Annie ChanDepartment of Asian Studies, Ludwig-Maximilians-Universität München, Munich, Germany.ORCID 0000-0002-4435-3209
Igor DjakovicDepartment of Archaeology, University of Leiden, Leiden, The Netherlands.
Tamara DogandžićDepartment of Human Evolution, Max Planck Institute for Evolutionary Anthropology, Leipzig, Germany.ORCID 0000-0001-9354-9761
George M LeaderDepartment of Anthropology, University of Pennsylvania, Philadelphia, Pennsylvania, United States of America.
Li LiDepartment of Early Prehistory and Quaternary Ecology, Eberhard Karls University of Tübingen, Tübingen, Germany.
Sam LinCentre for Archaeological Science, School of Earth, Atmospheric and Life Sciences, University of Wollongong, Wollongong, Australia.ORCID 0000-0001-6834-2646
Matthew MagnaniDepartment of Anthropology, Harvard University, Cambridge, Massachusetts, United States of America.
Jonathan ReevesDepartment of Early Prehistory and Quaternary Ecology, Eberhard Karls University of Tübingen, Tübingen, Germany.
Zeljko RezekDepartment of Human Evolution, Max Planck Institute for Evolutionary Anthropology, Leipzig, Germany.
Marcel WeissDepartment of Human Evolution, Max Planck Institute for Evolutionary Anthropology, Leipzig, Germany.
Max Planck Institute for Evolutionary Anthropology · DEUniversity of Tübingen · DECentre de Recherches Linguistiques sur l'Asie Orientale · FRCollege of New Jersey · USHarvard University · USNational Museum · ZAUniversity of Pennsylvania · USUniversity of Wollongong · AU

Funding

European Research Council 714658
6 · The paper itself

Abstract

Four ways archaeologists have tried to gain insights into how flintknapping creates lithic variability are fracture mechanics, controlled experimentation, replication and attribute studies of lithic assemblages. Fracture mechanics has the advantage of drawing more directly on first principles derived from physics and material sciences, but its relevance to controlled experimentation, replication and lithic studies more generally has been limited. Controlled experiments have the advantage of being able to isolate and quantify the contribution of individual variables to knapping outcomes, and the results of these experiments have provided models of flake formation that when applied to the archaeological record of flintknapping have provided insights into past behavior. Here we develop a linkage between fracture mechanics and the results of previous controlled experiments to increase their combined explanatory and predictive power. We do this by documenting the influence of Herztian cone formation, a constant in fracture mechanics, on flake platforms. We find that the platform width is a function of the Hertzian cone constant angle and the geometry of the platform edge. This finding strengthens the foundation of one of the more influential models emerging from the controlled experiments. With additional work, this should make it possible to merge more of the experimental results into a more comprehensive model of flake formation.

Indexed as

Mechanical PhenomenaGlassModels, Theoretical

Identifiers

PMID33206671
PMCPMC7673556
OpenAlexW3101121888

What OpenQuestion holds

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LicenceCC BY
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Registered trials

None linked

Read under generation 80e0d062 · epoch 390. Bibliography from PubMed, PubMed Central and OpenAlex; grants from NIH RePORTER; trial links from ClinicalTrials.gov; estimates, votes and beliefs from the OpenQuestion graph.