Nonstoichiometric grains with depletions of magnesium and silicon (rel
ative to oxygen) and inclusions of iron-nickel metal and iron-rich sul
fides have been identified in interplanetary dust particles from comet
s. These chemical anomalies accumulate in grains exposed to ionizing r
adiation. The grains, known as GEMS (glass with embedded metal and sul
fides), were irradiated before the accretion of comets, and their infe
rred exposure ages, submicrometer sizes, and ''amorphous'' silicate st
ructures are consistent with those of interstellar silicate grains. Th
e measured compositional trends suggest that chemical (as well as isot
opic) anomalies can be used to identify presolar interstellar componen
ts in primitive meteoritic materials.