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Preservation of δ13C signatures in oak charred wood: Application to the “forest” of Notre-Dame de Paris

•Inter- and intra-annual δ13C is preserved despite heating above 500 °C.•Laser ablation was applied on charred wood to study very narrow rings.•Charcoals from Notre-Dame can be used to reconstruct paleoenvironmental conditions. The fire of the Notre-Dame de Paris’s cathedral (NDP) in 2019 brought a...

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Published in:Journal of archaeological science, reports reports, 2025-02, Vol.61, Article 104894
Main Authors: Rocha, Eva, Dufraisse, Alexa, Rinne-Garmston, Katja T., Sahlstedt, Elina, Mendez-Millan, Mercedes, Nguyen Tu, Thanh Thuy, Girardclos, Olivier, Lemoine, Michel, Ghavidel, Amir, Terrei, Lucas, Collin, Anthony, Bellot-Gurlet, Ludovic, Delarue, Frédéric
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Language:English
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Summary:•Inter- and intra-annual δ13C is preserved despite heating above 500 °C.•Laser ablation was applied on charred wood to study very narrow rings.•Charcoals from Notre-Dame can be used to reconstruct paleoenvironmental conditions. The fire of the Notre-Dame de Paris’s cathedral (NDP) in 2019 brought a unique opportunity to study the past environmental conditions in the region during the High Middle Ages through the charred oak beams of the “Forest” (name given to its framework). However, as a preamble, there is a need to evaluate the preservation of the stable carbon isotope signatures (δ13C) in response to changes in molecular composition, occurring with carbonisation. To this end, experimental studies were conducted on modern and NDP oak wood at both inter- and intra-annual levels. Laser ablation was used for the first time on burnt wood. Results show that regardless of the charring duration, at temperatures above 500 °C, carbonisation‑induced 13C fractionation shows a consistent decrease (Δ13C) of approximately 1 ‰ relative to uncharred values. Despite a slight decrease in variance, a strong and significant correlation (rmean = 0.9, p 
ISSN:2352-409X
2352-4103
DOI:10.1016/j.jasrep.2024.104894