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The late middle Palaeolithic occupation of Abri du Maras (Layer 1, Neronian, southeast France): integrating lithic analyses, ZooMS and radiocarbon dating to reconstruct Neanderthal hunting behaviour

Ruebens, K. ORCID: https://orcid.org/0000-0002-5621-5786, Sinet-Mathiot, V., Talamo, S., Smith, G. M., Welker, F., Hublin, J.-J. and McPherron, S. P. (2022) The late middle Palaeolithic occupation of Abri du Maras (Layer 1, Neronian, southeast France): integrating lithic analyses, ZooMS and radiocarbon dating to reconstruct Neanderthal hunting behaviour. Journal of Palaeolithic Archaeology, 5. 4. ISSN 2520-8217

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To link to this item DOI: 10.1007/s41982-022-00113-z

Abstract/Summary

The exact strategies and technologies underlying Neanderthal hunting events remain open for debate with lithic points being sparse across the European Middle Palaeolithic. An exception is the Neronian entity in southeast France, defned by ventrally retouched Soyons points. This study contextualises one of the largest Neronian assemblages, layer 1 at Abri du Maras. Our lithic analyses focussed on attributes described as indicative of projectile use or hafting to contextualise the morphometric and technological characteristics of the pointed implements at an assemblage level. We found that retouched points were made on a variety of blank types (including Levallois, laminar and discoidal faking techniques) and ventral retouch is present across diferent artefact types (including points, scrapers and denticulates). Next, these lithic data were compared to similar typo-technological data recorded on a sample from the recently excavated and well-contextualised point-rich layer 4.1 of Abri du Maras (MIS-3). Zooarchaeology by Mass Spectrometry (ZooMS) was applied to 280 faunal remains from layer 1 and indicated signifcant proportions of equids, bovids, cervids and reindeer. Carnivore remains and carnivore modifcations are absent, while human bone surface modifcations are present across a variety of species. Five bones had sufcient collagen for radiocarbon dating but returned dates younger than expected (ca. 41–31 ka cal BP). Finally, we place Abri du Maras layer 1 in its broader regional context and discuss its relation to other Neronian assemblages and more general problematics inherent to studying material from old excavations.

Item Type:Article
Refereed:Yes
Divisions:No Reading authors. Back catalogue items
Science > School of Archaeology, Geography and Environmental Science > Department of Archaeology
ID Code:116060
Publisher:Springer

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