Biomineralizing organisms use organic molecules to generate species-specifi
c mineral patterns. Here, we describe the chemical structure of long-chain
polyamines (up to 20 repeated units), which represent the main organic cons
tituent of diatom biosilica. These substances are the longest polyamine cha
ins found in nature and induce rapid silica precipitation from a silicic ac
id solution. Each diatom is equipped with a species-specific set of polyami
nes and silica-precipitating proteins, which are termed silaffins. Differen
t morphologies of precipitating silica can be generated by polyamines of di
fferent chain lengths as well as by a synergistic action of long-chain poly
amines and silaffins.