Abstract

Over the last 60 years, much analytical research has sought to determine the ore sources of ancient Greek silver artefacts. Lead isotopic analysis has played a key role in this endeavor. While most studies so far have limited their search to places mentioned in historical sources, the present study takes a different approach by first identifying Ag-bearing ore sources in the Aegean world based on their geological characteristics and then using Pb isotopes to determine whether they were exploited in antiquity. To this end, we have geolocated, sampled, and measured high-precision Pb isotopic compositions of 17 Ag-bearing mineralizations in Greece for which we have evidence of ancient mining activity, and a further 10 exhibiting minor Ag occurrences that may also have been exploited in ancient times. We found that Pb model ages provide better discrimination of ore sources than the more conventional plots of raw Pb isotope data.Our study establishes Lavrion, northeast Chalkidiki, Pangaeon, Thasos, Siphnos, Palaea Kavala, Angistron, and south Euboea as the most important ancient silver mining districts in Greece. Two previously undiscovered ancient mining areas in Pelion and in the Kroussia mountain range are also documented. The latter may be identified with ancient Mount Dysoron, from which King Alexander I of Macedon reportedly extracted the fabulous sum of a talent of silver per day. For the first time, we isotopically differentiate some of the mining districts in Thraco-Macedonia, and show that the mines of Thasos include geologically different silver-bearing ore sources. We further identify the hitherto unrealized importance of Euboean silver mines and demonstrate that they isotopically overlap those of Siphnos, with major implications for our understanding of ancient Greek history.

Highlights

  • Understanding metal production and circulation in antiquity is directly related to our 35 knowledge of ore sources, but, for the most part, these are uncertain

  • The ancient mining areas closest to the Plaka granodiorite are at Ari and Dimoliaki with numerous adits and shafts that explore the contact between the Lavrion schists and Pounta marble (Fig. 3b)

  • We have provided new high-precision Pb isotopic data from samples obtained from the 405 known ancient mining territories in Greece with the intention of providing a useful tool for silver artefact provenance studies

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Summary

Introduction

Understanding metal production and circulation in antiquity is directly related to our 35 knowledge of ore sources, but, for the most part, these are uncertain. Lead isotopic analysis (LIA) has long been widely used for Pb-Cu-Ag-bearing ore deposits to assign provenances to copper/lead/silver artefacts as it has proved to be the most reliable analytical technique for 45 providing coherent provenance signatures, especially in coin provenance studies (Gentner et al, 1978; Gale, 1979; Chamberlain and Gale, 1980; Gale et al, 1980; Wagner et al, 1980; Wagner and Weisgerber, 1985; Artioli et al, 2020; Killick et al, 2020). A major study of Greek ore deposits published by Gale et al (1980) for Lavrion, the Cyclades, and northern Greece, as well as many silver coinages, using different Pb isotopic ratios has underpinned most subsequent historical understandings of silver extraction and usage in archaic Greek coin production

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