The Grotta d’Oriente, on the island of Favignana (Egadi, Sicily) has yielded a series of burials and human remains attributable to the final Epigravettian and Mesolithic. The Epigravettian burial, known as Oriente A, is characterised by funerary equipment consisting of perforated shells and a pebble with traces of red ochre. This site is one of the rare cases in which there is evidence of the use of ochre in a funerary context in Sicily and therefore the archaeological reconstruction requires the chemical-mineralogical characterization of this pigment using SEM, EDS, XRD, FORS and Raman spectroscopy. The comparative analysis of this pigment with a series of Terra Rossa from Favignana and other areas of Sicily has demonstrated that the Oriental A ochre does not derive from these sediments. This study shows the importance of applying different analysis methods for the characterization of ochres to try to define their origin.
Vita G., Saladino M.L., Armetta F., Sineo L. (2024). Geochemical and mineralogical characterization on an ochre residue adhering to a pebble found in the Oriente A Epigravettian burial, in the Grotta d’Oriente of Favignana (Egadi, Italy). ARCHAEOLOGICAL AND ANTHROPOLOGICAL SCIENCES, 16(10) [10.1007/s12520-024-02084-4].
Geochemical and mineralogical characterization on an ochre residue adhering to a pebble found in the Oriente A Epigravettian burial, in the Grotta d’Oriente of Favignana (Egadi, Italy)
Vita G.;Saladino M. L.;Armetta F.;Sineo L.
2024-10-01
Abstract
The Grotta d’Oriente, on the island of Favignana (Egadi, Sicily) has yielded a series of burials and human remains attributable to the final Epigravettian and Mesolithic. The Epigravettian burial, known as Oriente A, is characterised by funerary equipment consisting of perforated shells and a pebble with traces of red ochre. This site is one of the rare cases in which there is evidence of the use of ochre in a funerary context in Sicily and therefore the archaeological reconstruction requires the chemical-mineralogical characterization of this pigment using SEM, EDS, XRD, FORS and Raman spectroscopy. The comparative analysis of this pigment with a series of Terra Rossa from Favignana and other areas of Sicily has demonstrated that the Oriental A ochre does not derive from these sediments. This study shows the importance of applying different analysis methods for the characterization of ochres to try to define their origin.File | Dimensione | Formato | |
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