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quadruplex crystal structures (Figure 3.9b). All K + ions have full occupancy. The
average K + - K + distance is 3.38 Å. All three G-quadruplexes have three octahedrally
coordinated K + cations that are located equidistant between the planes of two adja-
cent G-quartets, with each K + and eight O6 atoms forming a square antiprismatic
arrangement. The outer K + ions are located within the loops, where they also achieve
octahedral coordination with the outer G-quartet O6 carbonyl oxygen atoms and
the O2 atoms from the adjacent thymine bases, together with two oxygen atoms
provided by water molecules. These potassium ions have only slightly increased
mobilities (i.e. thermal factors) compared to the three central K + ions. 99
The crystal structure of the Tl + form of the d[(G 4 T 4 G 4 ) 2 ] has been solved to
1.55 Å resolution (PDB ID 2HBN). 129 This G - quadruplex contains fi ve Tl + ions
(Figure 3.9d). The relative positions of these fi ve cations are very similar to those
found in the K + crystal structure. The average distance between Tl + ions is 3.6 Å .
Three Tl + ions are spread between adjacent G-quartet planes. They are coordinated
by eight oxygens (one O6 from each of the surrounding guanines). Two Tl + ions are
coordinated in each of the two thymine loops (Figure 3.9d). They are coordinated
by four guanine O6 atoms from the outer G-quartet plane and two thymine carbonyl
groups. A water molecule was identifi ed and located within the thymine loops and
in close proximity to the loop-associated Tl + ion. 129
3.7.2 NMR Studies
Ammonium ions have been shown to stabilize G-quartets to an extent that is similar
to that observed for Na + . 5,125 Hud and Feigon et al. used this fact to exploit 15 NH 4 +
ion as a solution-state probe of monovalent cation coordination sites. 162,248 These
authors used 1 H - 1 H and 1 H - 15 N NMR correlation experiments to localize 15 NH 4 +
ions within the bimolecular G-quadruplex d[(G 4 T 4 G 4 ) 2 ]. Dipole - dipole interactions
(ROE) between the protons of the bound 15 NH 4 + ions and G-imino protons revealed
that d[(G 4 T 4 G 4 ) 2 ] coordinates three 15 NH 4 + ions within its symmetric architecture
(Figure 3.9e). In fact, only two distinct chemical shift environments were detected
for bound 15 NH 4 + ions. One of them was assigned to the two symmetry-related outer
sites, while the other was in the centre of the bimolecular G-quadruplex structure.
The observed ROE cross-peak intensities also revealed that 15 NH 4 + ions in
d[(G 4 T 4 G 4 ) 2 ] are positioned equidistant between stacked G-quartets (Figure
3.9 e). 162,176
NMR spectroscopy has also been used to monitor the competition between
Na + and 15 NH 4 + ions for coordination within G-quadruplexes at specifi c sites. For
the G-quadruplex formed by d(G 4 T 4 G 4 ) in the presence of 15 NH 4 Cl, Na + ions were
shown to replace 15 NH 4 + ions at all three of the above mentioned outer- and inner-
binding sites as the NaCl concentration is increased. 163 Moreover, Na + ions pre-
ferentially replace 15 NH 4 + ions coordinated at the inner site of d[(G 4 T 4 G 4 ) 2 ]
quadruplexes. 163
The 11 - mer d(G 3 T 4 G 4 ), a single base deletion of d(G 4 T 4 G 4 ), has been shown by
NMR spectroscopy to fold into an unusual asymmetric, bimolecular structure in the
presence of 15 NH 4 + , K + and Na + ions (Figure 3.6b). 244 Multinuclear NMR studies
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