A survey of the structure and mineral composition of leaf idioblasts i
n the Cecropiaceae was conducted. In all six genera of the family, idi
oblasts usually occur as trichomes or enlarged epidermal cells and nea
rly always accumulate Si, in marked contrast to the idioblasts of othe
r members of the Urticales, which mostly possess cystoliths containing
abundant Ca and Si. The horizontally elongate, mineralized structures
of Poikilospermum, reported formerly as ''cystoliths'' also contain m
ainly Si and little Ca. Six genera of Cecropiaceae share a common char
acter in accumulating abundant Si in idioblasts of the leaf epidermis,
while lacking cystoliths composed of abundant Ca and Si.