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instrumental techniques applied to mineralogy and geochemistry

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Radiogenic iso<strong>to</strong>pes <strong>and</strong> their applications within a range of scientific fields 123<br />

FIGURE 5. Lead iso<strong>to</strong>pe data of Cu-tacks from the Bavaria wreckage <strong>and</strong> some reference fields<br />

(after Van Duiwenvoorde, 2008).<br />

Mints <strong>and</strong> coins form another group of objects which have been successfully<br />

provenanced by lead iso<strong>to</strong>pes. Silver coins often carry a substantial amount of lead<br />

which follows from the circumstance that argentiferous lead ores often are used for<br />

silver production. Laser ablation ICP-MS analyses of Roman silver coins were reported<br />

<strong>to</strong> have been used for assessing the trade <strong>and</strong> exchange of metals <strong>and</strong> ores (Pointing et<br />

al., 2003).<br />

Tracing the life s<strong>to</strong>ry of humans (" you are what you eat")<br />

Archaeologists, interested in how people have moved between inhabited regions,<br />

may benefit from applying Sr iso<strong>to</strong>pes in their work. The reason is that different regions,<br />

characterized by different geology, tend <strong>to</strong> have quite distinct Sr iso<strong>to</strong>pic signatures or<br />

finger-prints. Taken Sr iso<strong>to</strong>pes as an example, there is principally a 1:1 relationship<br />

between bedrock, soil, plants <strong>and</strong> other organisms higher up in the food chain which can<br />

be explained as follows. The strontium iso<strong>to</strong>pe signature of the bedrock is controlled by<br />

geological fac<strong>to</strong>rs – the soil inherits the iso<strong>to</strong>pic signature of the weathered bedrock – the

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