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Figure 3.7 Sodium ion localization within G-quadruplexes as revealed by X-ray crystal struc-
tures of d[(TG 4 T) 4 ] with eight strands forming two sets of four G-quartets 157
Figure 3.7, multiple cation coordination geometries are possible and observed (see
below).
The determination of G-quadruplex crystal structures of d[(TG 4 T) 4 ] has pro-
vided a detailed view of cation coordination that is unmatched by other DNA
structures. 157 The X-ray crystal structure of d[(TG 4 T) 4 ] was refi ned to a resolution
of 0.95 Å (PDB ID 352D). This crystal structure confi rmed that d(TG 4 T) forms a
tetramolecular parallel-stranded G-quadruplex in the presence of Na + ions (Figure
3.8 a). 157 The asymmetric unit of the d[(TG 4 T) 4 ] crystal consists of four G-
quadruplexes, with two quadruplexes being coaxially stacked in a 5
orientation,
such that a continuous stack of eight G-quartets is formed. 157,246 Seven Na + ions are
coordinated along the axial channel formed by the O6 atoms of eight G-quartets
(Figure 3.8a). Close inspection of the crystal structure reveals that the central Na +
in this channel is positioned equidistant between the planes of two stacked G-quar-
tets. The coordination geometry of this particular Na + is bipyrimidal, with eight
equidistant guanine O6 atoms. Na + ions located away from this central position are
displaced incrementally further from this perfect symmetrical bipyrimidal coordina-
tion. At the ends of this channel, terminal Na + ions are in fact located in the planes
of the end G-quartets, coordinated by the carbonyl groups of only four guanine
residues (Figure 3.8a). Displacement of the Na + ions from the central eight-coordi-
nate geometry to the in-plane four-coordinate geometry is believed to arise from
electrostatic repulsion between adjacent Na + ions. The mutual repulsion of Na + ions
along the central axis of the G-quadruplex has also been hypothesized to be the
origin of an out of plane bending observed for the terminal G-quartets of the eight
stacked quartets. 157
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