Lead Isotopic Characteristics and Metal Sources for the Jewelry in the Medieval Rural Settlements from the Suzdal Region (Kievan Rus’)

Datos Bibliográficos

ID23199798
AutoresAndrey V Chugaev, А В Чугаев (0000-0002-0528-3965, Institute of Geology of Ore Deposits Petrography Mineralogy and Geochemistry), Stephen Merkel (0000-0001-8730-6923, Deutsches Bergbau-Museum Bochum), Stephen W Merkel, Irina E Zaytseva (0000-0003-3577-421X, Institute of Archaeology)
Año2021
Volumen25
Número2
Páginas101-125
Fecha de publicación2021-05-07
Peer ReviewedSí
Open AccessSí
TipoARTICLE
RevistaMETALLA (JOURNAL)
Identificadores de la revistaISSN: 0947-6229 • E-ISSN: 2749-6430
EditorialUniversitatsbibliothek der Ruhr-Universitat Bochum (PUBLISHER)
DOI10.46586/metalla.v25.2019.i2.101-125
OpenAlexW4285467250
IdiomaEN
Citas recibidas9
Referencias citadas16

The article considers the results of the study of lead isotope composition of 38 non-ferrous artifacts discovered at medieval rural sites of the Suzdal Region (Kievan Rus’). The copper-alloy, silver and pewter artifacts were compared with reference data from geographically and temporally diverse medieval artifacts and ore deposits and revealed differing source regions and supply networks within and between metal types. The identification in some cases was difficult due to the conformity of the lead isotopic composition of deposits of some regions. The copper-alloys, represented mostly by crosses made of high-tin bronze, show close isotopic parallels to contemporary copper alloys from Southern Scandinavia, Westphalia and Lower Saxony. Since the copper alloys contain significant quantities of lead, this lead may have entered the metal by alloying with lead-tin alloys, by smelting mixed copper-lead ore, or through haphazard alloying with lead. The lead isotope ratios for nearly all copper alloys are consistent with deposits in Cornwall and Devon and remobilized ore from the Rhenish Massif. For silver and lead-tin alloy objects, lead isotope analyses point to wide ranging sources. Most silver objects are consistent with mid-to-late 10th century silver stocks circulating in the Baltic area and 10th century Volga-Bulgar silver dirham imitations probably representing mixtures of 9th-10th century Islamic silver. The silver shows a heavy reliance on 10th century mixed stocks and there are little indications of Central and Western European silver, which was common in the 11th century Baltic region. The pewter and lead, however, indicate other sources. Lead isotope ratios are consistent with sources connected to Mediterranean and Baltic networks, some being consistent with sources in England, but it is possible that the lead found in some pewter objects could come from the Olkusz lead district in southern Poland.

Bronze · Copper · Geochemistry · Lead (geology) · Massif · Metallurgy · Smelting · Tin · Eurasian Exchange Networks · Geology · Historical and Archaeological Studies · Materials Science · Metallurgy and Cultural Artifacts