文摘
?A physicochemical characterisation of a selected group of late Roman amphorae was carried out using x-ray diffraction spectrometry, flame atomic absorption and emission spectroscopy as well as petrographic polarisation microscopy. Most of these amphorae were found in underwater environments on both coasts of the Straits of Gibraltar: Ceuta and Cadiz (Spain). A multivariate statistical study of the obtained data for 99 samples and 21 variables (Si, Al, Ca, Mg, K, Na, Fe, Mn, Ti, Cr, Cu, Ni, Pb, Zn, calcite, quartz, dolomite, orthoclase, plagioclase, phyllosilicates and gypsum) was performed. Relations among amphorae that shared a similar composition were established by factor analysis. As a result, amphorae coming from Cadiz showed a different composition than those coming from Ceuta. This is demonstrated by the increase in concentration of certain chemical elements, such as Cu, Cr and Ca. This fact supports the archaeological hypothesis that some amphorae of South-Hispanic typology found in Ceuta were produced locally, although there is no proof of the existence of kilns in this area. On the other hand, neither the different typologies nor the food stored or transported in these amphorae seem to affect the mineralogical and chemical composition of the ceramic pastes. However, their porosity contributes to the enrichment in trace elements and salt contents in those samples that had been in marine underwater contexts for a large period of time.