4.7 Article

Calcium antimonate: A new discovery in colour palette of Paestum wall paintings

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MICROCHEMICAL JOURNAL
卷 168, 期 -, 页码 -

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ELSEVIER
DOI: 10.1016/j.microc.2021.106401

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Microscopy; Spectroscopy; Calcium antimonate; Funerary wall paintings; Paestum

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A multi-analytical approach was used to study Paestum funerary slabs, confirming intentional use of calcium antimonate in paintings and limited pigments were used by ceramic painters. Various mineral pigments were identified, with green earth, Egyptian blue, hematite, and red ochre being frequently used. The study sheds light on the techniques and materials used in the ancient Lucanian funerary art.
During a restoration and diagnostic campaigns carried out on Paestum funerary slabs belonging to the Lucanian funerary art, calcium antimonate (CaSb2O6) was detected for the first time in the pictorial layers. This artificial pigment, widely employed as opacifier both in ancient glass and glaze covering clay objects, was found in the wall paintings, regardless of the colour, supporting the hypothesis of an intentional addition of calcium antimonate to the pigments and the involvement of ceramic painters. A multi-analytical approach was performed on 32 funerary slabs (6th-3rd century BCE), currently located at the National Archaeological Museum of Paestum (Italy) using both polarized light microscopy and environmental scanning electron microscopy equipped with energy dispersive X-ray spectrometer, micro X-ray fluorescence, micro Raman spectroscopy, Fourier Transform Infrared spectroscopy and powder X-ray diffraction. The results confirmed the use of a limited number of pigments, usually applied with fresco technique, although in many cases the stratigraphy of the painted layer showed morphology of mezzo fresco technique, but no organic binders were found. The hues of vegetal decorations were obtained using green earth, sometimes Egyptian blue mixed with yellow ochre, carbon and bone blacks, and orpiment. The alteration of green earth and other ironcontaining pigments are likely responsible for the discolouration of the original hues. In red paints, hematite and red ochre are frequently associated with ilmenite, a typical volcanic mineral. Egyptian blue was used in blue paints while in black paints it was mixed with carbon and bone black pigments.

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