A survey of the structure and mineral composition of leaf idioblasts in the Cecropiaceae was conducted. In all six genera of the family, idioblasts usually occur as trichomes or enlarged epidermal cells and nearly always accumulate Si, in marked contrast to the idioblasts of other members of the Urticales, which mostly possess cystoliths containing abundant Ca and Si. The horizontally elongate, mineralized structures ofPoikilospermum, reported formerly as “cystoliths” also contain mainly Si and little Ca. Six genera of Cecropiaceae share a common character in accumulating abundant Si in idioblasts of the leaf epidermis, while lacking cystoliths composed of abundant Ca and Si.