North and South in Medieval Iberia: A historical and environmental estimate through isotopic analyses
Metadatos
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Martín Alonso, José Francisco; Laffranchi, Zita; Milella, Marco; Coppola Bove, L.; Mena-Sánchez, Luis; Jiménez Brobeil, Sylvia AlejandraEditorial
Plos One
Fecha
2024-06-05Referencia bibliográfica
Martín-Alonso JF, Laffranchi Z, Milella M, Coppola-Bove L, Mena-Sánchez LA, Jiménez-Brobeil SA (2024) North and South in Medieval Iberia: A historical and environmental estimate through isotopic analyses. PLoS ONE 19(6): e0304313. https://doi.org/10.1371/journal.pone.0304313
Patrocinador
Research project "Health and nutrition in populations of the Southeast of al-Andalus" (Ref. PID2019-107654-GB-100) funded by the Ministry of Science and Innovation of the Spanish GovernmentResumen
The Middle Ages in the Iberian Peninsula is a period of special interest for studying the relationship
of climate change with historical and socioeconomic processes. Between the 8th
and 15th centuries AD, the Peninsula was characterized not only by complex political, cultural,
and social transitions but also by major variations in the climate. The objective of this
study was to examine differences in diet and mobility between distinct populations of the
Peninsula and explore the possible relationship of diet, mobility, and culture with environmental
variables and geographical settings. For this purpose, we obtained stable isotopic
ratios of carbon and oxygen (δ13C and δ18O) from the enamel apatite of first upper incisors
from 145 individuals at eight archeological sites that represent both Christian and Islamic
communities and both rural and urban social settings. Results revealed a dietary difference
between Christian and Islamic populations, observing a greater contribution of C4 plants,
possibly sorghum, in the diet of the latter, especially in a rural setting. The disparity in oxygen
isotopic ratios between populations from the North and South of the Peninsula is consistent
with modern climatic differences between these regions. In this line, intraregional
variability in oxygen isotopic ratios may hint at diachronic occupation phases under varying
climatic conditions. The few isotopic outliers in our sample suggest overall low mobility
levels.