Настоящая публикация посвящена обобщению результатов аналитических исследований боспорского монетного серебра, выполненных методом изотопного анализа Pb, и вопросу эволюции источников поступления серебра на территорию Боспора в период с V–IV вв. до н.э. по II–III вв. н.э. Pb-изотопные характеристики монетного серебра, происходящего с территории Боспора (https://www.archaeolog.ru/ru/data/isoarchmet-iaras), сравнивались с новейшими данными, полученными для монетного серебра Великой Греции, Карфагена и Рима, что позволило уточнить круг регионов добычи серебра, поступавшего на территорию Боспора в разные хронологические периоды. Так, на раннем этапе монетной чеканки Боспора использовалось серебро из месторождений Лавриона, п-ва Халкидики и Родопских гор. В отличие от греческого монетного серебра, доля месторождений п-ва Халкидики и Родопских гор в боспорской чеканке значительно превышает долю серебра из рудников Лавриона. В период III–I вв. до н.э. боспорская чеканка работала на этом же «старом» серебре, но встречается сырье и из другого источника, сходного с источником для монетного серебра Карфагена (Иберийский п-в); римского монетного серебра на территории Боспора это время пока не фиксируется. В период II–III вв. н.э. основным источником монетного серебра на Боспоре являются римские рудники, расположенные в Дакии (регион Роша Монтанэ); встречается также серебро, добытое на римских рудниках Иберии и Центрального Французского массива.
Боспор, Великая Греция, Карфаген, Рим, монеты, серебро, изотопный анализ Pb, рудные источники
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