We study spectroscopically determined iron abundances of 640 solar-type stars to search for the signature of accreted iron-rich material. We Ðnd that the metallicity [Fe/H] of a subset of 466 main-sequence stars, when plotted as a function of stellar mass, mimics the pattern seen in lithium abundances in open clusters. Using Monte Carlo models, we Ðnd that, on average, these stars appear to have accreted D0.5 of iron while on the main-sequence. A consistency check is provided by a much smaller sample of M1 9 stars in the Hertzsprung gap, which are slightly evolved and the convection zones of which are signiÐ-cantly more massive ; they have lower average [Fe/H], and their metallicity shows no clear variation with stellar mass. We argue that our Sun is likely to have accreted a similar amount of iron ; in this respect, most systems resemble ours rather than the currently known extrasolar planetary systems. These Ðndings suggest that terrestrial-type material is common around solar-type stars.