Structural transition from antiparallel to parallel G-quadruplex of d(G4T4G4) induced by Ca2+.

Guanine quadruplex (G-quadruplex) structures are formed by guanine-rich oligonucleotides. Because of their in vivo and in vitro importance, numerous studies have been demonstrated that the structure and stability of the G-quadruplex are dependent on the sequence of oligonucleotide and environmental conditions such as existing cations. Previously, we quantitatively investigated the divalent cation effects on the antiparallel G-quadruplex of d(G4T4G4), and found that Ca2+ induces a structural transition from the antiparallel to parallel G-quadruplex, and finally G-wire formation. In the present study, we report in detail the kinetic and thermodynamic analyses of the structural transition induced by Ca2+ using stopped-flow apparatus, circular dichroism, size-exclusion chromatography (SEC) and atomic force microscopy. The quantitative parameters showed that at least two Ca2+ ions were required for the transition. The kinetic parameters also indicated that d(G4T4G4) underwent the transition through multiple steps involving the Ca2+ binding, isomerization and oligomerization of d(G4T4G4). The parallel-stranded G-wire structure of d(G4T4G4), which is a well controlled alignment of numerous DNA strands with G-quartets, as the final product induced by Ca2+, was observed using SEC and atomic force microscopy. These results provide insight into the mechanism of the structural transition and G-wire formation and are useful for constructing a nanomaterial regulated by Ca2+.