Abstract
The discovery of excess ^(107)Ag (^(107)Ag*) was made in a IVB iron meteorite ten years ago. The ^(107)Ag* anomaly is inferred to be due to decay of ^(107)pd (t_(1/2)=6.5 10^6 y) and appears to provide a chronometer for the timescale of early planet formation and differentiation.
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