Guanine quarters are readily formed by guanine nucleotides and guanine-rich
oligonucleotides in the presence of certain monovalent and divalent cation
s. The quadruplexes composed of these quartets are of interest for their po
tential roles in vivo, their relatively frequent appearance in oligonucleot
ides derived from in vitro selection, and their inhibition of template dire
cted RNA polymerization under proposed prebiotic conditions. The requiremen
t of cation coordination for the stabilization of G quartets makes understa
nding cation-quadruplex interactions an essential step towards a complete u
nderstanding of G quadruplex formation. We have used (NH4+)-N-15 as a probe
of cation coordination by the four G quarters of the DNA bimolecular quadr
uplex [d(G(4)T(4)G(4))](2), formed from oligonucleotides with the repeat se
quence found in Oxytricha nova telomeres. H-1 and N-15 heteronuclear NMR sp
ectroscopy has allowed the direct localization of monovalent cation binding
sites in the solution state and the analysis of cation movement between th
e binding sites. These experiments show that [d(G(4)T(4)G(4))](2) coordinat
es three ammonium ions, one in each of two symmetry related sites and one o
n the axis of symmetry of the dimeric molecule. The NH4+ move along the cen
tral axis of the quadruplex between these sites and the solution, reminisce
nt of an ion channel. The residence time of the central ion is determined t
o be 250 ms. The (NH4+)-N-15 is shown to be a valuable probe of monovalent
cation binding sites and dynamics. (C) 1999 Academic Press.