Abstract
Analysis of prehistoric copper and bronze in the Caucasus was performed previously on thousands of objects with arc optical emission spectroscopy (OES). While arc OES is no longer widely used in archaeometry, LA-ICP-MS has shown great promise for isotopic and chemical analysis of ancient copper and bronze artifacts. In order to explore the effectiveness of LA-ICP-MS for the characterization of materials in a large group of ancient copper-based metalwork from the South Caucasus, we analyzed 48 metal artifacts from the Horom necropolis and 16 from the Karashamb necropolis, at Idaho State University’s Center for Archaeology, Materials and Applied Spectroscopy (CAMAS). These artifacts had been recovered from burials dating to the late second–early first millennium bc, a period noted for the use of a variety of copper alloy mixtures, including antimony bronze (which is very unusual at this early period in Europe and Asia). The metal artifacts from Horom had been previously analyzed by arc OES at the Institute of Archaeology and Ethnography in Yerevan, Armenia. This provided the opportunity to compare the performance of arc OES with LA-ICP-MS for analysis of variations in the use of copper alloys in ancient metal artifacts. In addition to LA-ICP-MS, EDS was used to analyze major elements, especially the proportion of copper in relation minor and trace elements that were measured with LA-ICP-MS. Besides unalloyed copper, the alloys detected by EDS and arc OES included mixtures with arsenic, tin, lead and antimony. More alloys were detected in the assemblage by LA-ICP-MS and EDS than with arc OES. This may be because copper levels were measured by EDS allowing the results for all elements to be normalized in proportion to copper. Normalization of results was therefore not possible with arc OES, which is another advantage of using LA-ICP-MS together with EDS.
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Notes
- 1.
The majority of these analyses are summarized by Chernykh (1992).
- 2.
In addition to the OES results, additional points of comparison are available from XRF and neutron activation analysis of samples from other copper and bronze artifacts from Armenia that were collected previously by Meliksetian and colleagues (Meliksetian et al. 2003a, b; Meliksetian et al. 2007; Meliksetian and Pernicka 2010). However, these are discussed only in passing here since those analyses were not conducted on the same objects as those described in this chapter.
- 3.
These ores are more difficult to smelt into metallic copper than the weathered oxide ores that would have been encountered earlier in the upper levels of deposits.
- 4.
In other projects using other techniques, copper, bronze, antimony and lead artifacts as well as Armenian copper ores have been analyzed at the Curt-Englehorn Zentrum, Mannheim (Meliksetian et al. 2003a, b; Meliksetian et al. 2007; Meliksetian and Pernicka 2010). Other ongoing archaeometallurgical research in the South Caucasus includes investigations of ancient gold mining in Georgia by Stöllner, Gambashidze, and Hauptmann (Hauptmann et al. 2010; Hauptmann and Klein 2009), and research recently initiated on the Sotk mine and neighboring sites in Armenia under the direction of Ernst Pernicka.
- 5.
By three of us: Dudgeon, Tromp, and Peterson.
- 6.
A closer examination of the dating and periodization of the Horom metalwork is beyond the scope of the present discussion.
- 7.
SRM B10 and B12 are from the Centre de Développement des Industries de Mise en Forme des Matériaux, France, and 51.13-4, 71.32-4 are from the Bureau of Analysed Samples Ltd, England.
- 8.
Another strategy for dealing with heterogeneity in a situation in which it is not possible to remove samples for SEM-EDS visualization, such as analysis through the corroded surface of a bronze, might be to sample numerous points and to average the results. However, it is not possible to say how many points would be sufficient in a given case.
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Acknowledgments
We are grateful to Aram Gevorkyan (Institute for Archaeology and Ethnography, Yerevan, Armenia) for providing the results of Arc OES analysis of metalwork from Horom presented in Table 8.4. Some of the results discussed here were presented at the Archaeometallurgy in Europe III conference (June 28–July 1, 2011) at the Deutsches-Bergbau Museum, Bochum, Germany (Peterson et al. 2011), and were the subject of a poster displayed at the 2011 Annual Meeting of the Society for American Archaeology in Sacramento, California (Meredith et al. 2011). This research was sponsored by the American Councils for International Education and the National Councils for Eurasian and East European Research, through a National Endowment for the Humanities International Collaborative Research Fellowship in 2009–2010 for Collaborative Investigations of Early Mining and Metal Production on the Armenian Plateau, ca. 7000–800 bce (David Peterson, PI). Additional support was provided by Idaho State University’s Faculty Research Committee (2009–2010) and Humanities and Social Sciences Research Committee (2010). Laure Dussubieux (Field Museum of Natural History, Chicago) graciously provided copper and bronze standards utilized in the LA-ICP-MS analysis. The objects analyzed were recovered in excavations at Horom directed by Ruben Badalyan and O. K. Agekyan in 1987–1989 (Badalyan and Agekyan 1991). Many thanks to Idaho State University Anthropology students Adam Clegg for preparation of Fig. 8.2, and Bradley Paige for Fig. 8.3.
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Peterson, D.L., Dudgeon, J.V., Tromp, M., Bobokhyan, A. (2016). LA-ICP-MS Analysis of Prehistoric Copper and Bronze Metalwork from Armenia. In: Dussubieux, L., Golitko, M., Gratuze, B. (eds) Recent Advances in Laser Ablation ICP-MS for Archaeology. Natural Science in Archaeology. Springer, Berlin, Heidelberg. https://doi.org/10.1007/978-3-662-49894-1_8
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