Middle Neolithic fluorites in Northern France and Belgium: Characterization, sourcing and methodological limitations

•Fluorite pearls characterize Middle Neolithic sites in Belgium and Northern France.•Fluorite associated to Michelsberg culture, Spiere group and northern Chassean.•Raw fluorite mainly derives from Dinantian limestones of Central Belgium.•Source(s) for Neolithic fluorite differs from Upper Palaeolit...

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Veröffentlicht in:Journal of archaeological science, reports reports, 2023-06, Vol.49, p.103980, Article 103980
Hauptverfasser: Goemaere, Eric, Vanmontfort, Bart, Bonjean, Dominique, Bosquet, Dominique, Bostyn, Françoise, Cayol, Nicolas, Colas, Caroline, Collet, Hélène, Delbey, Thomas, Delye, Emmanuel, Golitko, Mark, Jadin, Ivan, Jungels, Cécile, Leroy-Langelin, Emmanuelle, Monchablon, Cécile, Praud, Ivan
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Sprache:eng
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Zusammenfassung:•Fluorite pearls characterize Middle Neolithic sites in Belgium and Northern France.•Fluorite associated to Michelsberg culture, Spiere group and northern Chassean.•Raw fluorite mainly derives from Dinantian limestones of Central Belgium.•Source(s) for Neolithic fluorite differs from Upper Palaeolithic fluorite.•Sr isotopes ratio is a method allowing to trace the source of fluorite.•Interpretation of REEs curves must be used with caution. Ornaments and fragments of fluorite have been found at sixteen Neolithic sites in Belgium and Northern France, mainly Middle Neolithic sites associated with the Michelsberg culture and the Spiere and Chassean groups. These sites are located in a large geographical area representing different types of sites and various geological backgrounds. One of the aims of this study is to identify where this mineral could have been quarried in the Neolithic and compare the possible source(s) with those used during the Palaeolithic. A survey of some Neolithic fluorite occurrences in Belgium and Northern France was conducted and the origins of this mineral investigated by means of geochemical Rare Earth Elements and Sr-isotopic analysis. We also explore the limitations of isotopic 87Sr/86Sr and REE ratios for analysis of fluorite. Results show that Neolithic fluorite originates from different local and regional sources, mainly the Dinantian limestones/dolostones of the Ardennes Allochthon, in contrast to the use of silicified Givetian limestones of the Calestian Band near Givet (France) during the Magdalenian. The Neolithic fluorite that is studied in this paper is found exclusively at settlement sites whereas elsewhere, fluorite comes exclusively from funerary contexts.
ISSN:2352-409X
2352-4103
DOI:10.1016/j.jasrep.2023.103980