We have studied the precipitation of short DNA molecules by the polyca
tions spermidine, spermine, and cobalthexamine. The addition of these
cations to a DNA solution leads first to the precipitation of the DNA;
further addition resolubilizes the DNA pellet. The multivalent salt c
oncentration required for resolubilization is essentially independent
of the DNA concentration (between 1 mu g/ml and 1 mg/ml) and of the mo
novalent cation concentration present in the DNA solution (up to 100 m
M). The DNA aggregates are anisotropic; those obtained in the presence
of the polyamines spermidine and spermine generally contain a cholest
eric liquid crystalline phase that flows spontaneously. In contrast th
is phase is never seen in the presence of cobalthexamine. We propose t
hat the ability of polyamines to condense DNA in fluid structures is a
n essential feature of their biological functions.