Abstract

The origins of the silver trade across the Mediterranean, and the role of the Phoenicians in this phenomenon, remain contentious. This is partly because of difficulties encountered when trying to assign archaeological silver to its geological sources. Here we present a reanalysis of Iron Age silver hoards in the southern Levant, which demonstrates not only that recycling of silver was widespread in the Early and Late Iron Age, but that the components of this mixed silver originated from the Aegean, Anatolia and the western Mediterranean. An assessment of lead isotope analyses combined with compositional data allows the identification of mixing lines based on gold levels in the silver and the Pb crustal age (or, more loosely, geological age) of the ore from which the silver originated. It is shown that, from as early as the 11th century BC, these mixed silver signatures derive from the Taurus mountains in Anatolia, from Iberia and an unknown source—with Sardinia as an additional possibility—and Laurion in Greece in the Late Iron Age. In contrast to copper, which was deliberately alloyed with silver, gold appears to have been mixed unintentionally, through the melting down of silver objects with gold parts. It is suggested that vertical mixing lines (with constant Pb crustal age but variable Au), may indicate the melting down and mixing of silver in times of unrest, both here and in other contexts. Gold and lead concentrations in the silver indicate that native silver from Iberia was most likely used in the Early Iron Age, suggesting that the first people to convey silver to the southern Levant were not miners but traders who had acquired silver directly from the indigenous Bronze Age inhabitants of Iberia. However, evidence of the exploitation of jarosite also supports that silver ore mining and cupellation was ongoing in Iberia at a similar time, and continued in the Late Iron Age—potentially a result of technological transfer from the East. In essence, the western Mediterranean origin of the silver in these Early Iron Age southern Levantine hoards supports an emerging picture of Mediterranean interactions and trade relations in the increasingly bright Dark Ages (c. 1200–800 BC).

Highlights

  • In terms of geographical and chronological distributions, the largest identified concentration of silver hoards in the ancient Near East is in the Iron Age of the southern Levant (Thompson 2003)

  • The combination of estimated crustal ages based on lead isotope analyses and gold concentrations in ancient silver makes it possible to identify groups of objects that are likely to derive from the same source or batch, and allows the identification of mixing lines between groups

  • Mixing lines suggest that the Late Iron Age silver found at Miqne-Ekron and Ein Gedi was sourced from the Laurion and a much older ore with a signature commensurate with jarosite ores in Iberia

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Summary

Introduction

In terms of geographical and chronological distributions, the largest identified concentration of silver hoards in the ancient Near East is in the Iron Age of the southern Levant (Thompson 2003). Silver exhibiting crustal ages around 380 Ma was probably derived from silver from different Spanish sources: low gold, low lead and crustal ages commensurate with Iberia indicate a native silver source (as used by the indigenous Late Bronze Age/Early Iron Age inhabitants of Iberia), whereas higher levels of gold and lead are potentially the consequence of smelting jarosite ores Both types of silver appear to have ended up in the Early Iron Age hoards, which suggests that cupellation was a process used to acquire silver in Iberia from at least the late 11th century BC

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