• Aucun résultat trouvé

Charring-induced fractionation of δ13C and δ15N in cotton (Gossypium arboreum) seeds: implications for reconstructing archaeological environments

N/A
N/A
Protected

Academic year: 2021

Partager "Charring-induced fractionation of δ13C and δ15N in cotton (Gossypium arboreum) seeds: implications for reconstructing archaeological environments"

Copied!
1
0
0

Texte intégral

(1)

Charring-induced fractionation of δ13C and δ15N in cotton

(Gossypium arboreum) seeds: implications for reconstructing

archaeological environments

Saskia E. Ryan1Charlène Bouchaud1, 2, 3Elena Peláez AndéricaChristopher Viot4Antoine Zazzo1 1AASPE - Archéozoologie, archéobotanique : sociétés, pratiques et environnements

2CNRS - Centre National de la Recherche Scientifique

3MNHN - Muséum national d'Histoire naturelle

4UMR AGAP - Amélioration génétique et adaptation des plantes méditerranéennes et tropicales

Abstract :

The ancient diffusion of cotton (Gossypium sp.) across the Old World is one of the most outstanding examples of social, environmental, technical and economic entanglement. The various trajectories of cotton products, including raw and processed seeds and fibres, are relevant markers of the circulation of knowledge, goods and people. However, understanding cotton diffusion in the past is limited by the fact that cotton products could have been produced locally and/or imported from different regions. Furthermore, cotton seeds and to a lesser extent, cotton fibres, are generally only found in charred form in archaeological contexts and this can be problematic as in some cases, the charring of plant remains results in an offset of the biogenic isotope values. In this study, the isotope composition of modern uncharred and experimentally charred cotton seeds that were grown in irrigated fields in Seville, Spain and greenhouses in Montpellier, France, was measured to establish the range of isotope fractionation that takes places across several parameters (temperature range: 50, 100, 150, 200, 225, 250, 275, 300, 325 and 350°C; time range: 2, 4, 8 and 16 hours). The results provide information on the extent to which carbonization effects measured δ13C and δ15N values and if such values can be used successfully to reconstruct the nature of the local growing environment.

Saskia E. Ryan, Charlène Bouchaud, Elena Peláez Andérica, Christopher Viot, Antoine Zazzo (2019) Charring-induced fractionation of δ13C and δ15N in cotton (Gossypium arboreum) seeds: implications for reconstructing archaeological environments. 18th of the International Workgroup for Palaeoethnobotany, Jun 2019, Lecce, Italy. 2019 (poster) ⟨hal-02336202⟩

Liens :

https://hal.archives-ouvertes.fr/hal-02336202v1

https://hal.archives-ouvertes.fr/hal-02950477

Références

Documents relatifs

To obtain a more thorough characterization of the genetic diversity of cotton, we used the CottonSNP63K array to analyze a total of 395 cotton samples provided by the NCGC

  The aims of this study was therefore to characterize the level of water contamination in the Tanjona via trace metals concentrations and stables isotopes (δ 13 C

However, for monogastric animals, the high fibre content and the presence of gossypol are limiting factors and, since cotton seeds contain more fibre and free gossypol than

The genetic structure observed in a broad collection of cottons representing a vast region of Mesoamerica, Central America, the eastern Caribbean, and even Pacific islands

For a given chromosome, QTLs within the same broad trait category (thus possibly including different, but cor- related traits, like ML, UHML and UQLw in case of fiber length

The French Cotton Germplasm Collection, which was founded in Montpellier (France) in 1978, conserves 3070 accessions belonging to 5 tetraploid species and 27 diploid

These plants were once more �bundant when native people traditionally grew perennial cotton which was regenerated either by seed or by allowing new plantlets to

Significance of spatial and temporal variations of stable isotope values (δ 13 C and δ 15 N) of coral host tissues and stable isotope differences between coral host tissues and