| Literature DB >> 32081872 |
Roberta Rocca1,2, Ferruccio Palazzesi3, Jussara Amato4, Giosuè Costa1,2, Francesco Ortuso1,2, Bruno Pagano4, Antonio Randazzo4, Ettore Novellino4, Stefano Alcaro1,2, Federica Moraca5,6,7, Anna Artese8,9.
Abstract
An increasingly comprehension of the folding intermediate states of DNA G-quadruplexes (G4s) is currently an important scientific challenge, especially for the human telomeric (h-tel) G4s-forming sequences, characterized by a highly polymorphic nature. Despite the G-triplex conformation was proposed as one of the possible folding intermediates for the antiparallel and hybrid h-tel G4s, for the parallel h-tel topology with an all-anti guanine orientation, a vertical strand-slippage involving the G-triplets was proposed in previous works through microseconds-long standard molecular dynamics simulations (MDs). Here, in order to get further insights into the vertical strand-slippage and the folding intermediate states of the parallel h-tel G4s, we have carried out a Well-Tempered Metadynamics simulation (WT-MetaD), which allowed us to retrieve an ensemble of six G4s having two/G-tetrad conformations derived by the G-triplets vertical slippage. The insights highlighted in this work are aimed at rationalizing the mechanistic characterisation of the parallel h-tel G4 folding process.Entities:
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Year: 2020 PMID: 32081872 PMCID: PMC7035250 DOI: 10.1038/s41598-020-59774-x
Source DB: PubMed Journal: Sci Rep ISSN: 2045-2322 Impact factor: 4.379
Figure 1Schematic representation of: (A) the three planes of the G-tetrad core typical of G4s; (B) the G-triplet; (C) the vertical slippage movement involving the G-triplet, which leads the formation of G4s having one G-triad and two/G-tetrad planes. For clarity, the G-triad residues are depicted with solid gray lines, while the guanine residues of the two/G-tetrad planes that are not involved in the G-triplet slippage are shown as dashed gray lines.
Figure 23D structures and schematic representations of the slipped ensemble structures found in the basin C from the reweighted FES. (a) 2d conformation derived from the vertical slippage of the second G-triplet (G8:G9:G10) towards the 3′-end position. (b) 3d conformation characterized by the slippage of the third G-triplet (G14:G15:G16) towards the 3′-end position. (c) 3u structure formed by the slippage of the third G-triplet (G14:G15:G16) towards the 5′-end position. (d) 4d conformation in which the fourth G-triplet (G20:G21:G22) moves towards the 3′-end position. (e,f) 24d and 34d conformations derived from the simultaneous slippage of the fourth G-triplet (G20:G21:G22) with the second (G8:G9:G10) and the third (G14:G15:G16) G-triplets, respectively. For clarity, the G-triplets not involved in the vertical slippage are shown in transparency with dashed gray lines. The red arrows point out the direction of the movement.
G-triplets residues involved in the vertical slippage for each structure found in the basin C. The guanine residues forming the two G-tetrad planes and the G-triads are also reported.
| Basin C structures | Slipped G-Triplet Residues | Two G-tetrads residues | G-triad residues |
|---|---|---|---|
5′-G8:G9:G10-3′ | G3: G4: | G2:G14:G20 | |
5′-G14:G15:G16-3′ | G3:G9: G4:G10: | G2:G8:G20 | |
3′-G16:G15:G14-5′ | G2:G8: G3:G9: | G4:G10:G22 | |
5′-G20:G21:G22-3′ | G3:G9:G15: G4:G10:G16: | G2:G8:G14 | |
5′-G8:G9:G10-3′ 5′-G20:G21:G22-3′ 5′→3′ | G3: G4: | No G-triad | |
5′-G14:G15:G16-3′ 5′-G20:G21:G22-3′ | G3:G9: G4:G10: | No G-triad |
Free energy values with the standard deviation of each slipped conformation found in the basin C, calculated after the reweighting procedure.
| Structure | Free Energy* ( |
|---|---|
| 14.6 ± 3.6 | |
| 16.0 ± 7.7 | |
| 28.2 ± 11.1 | |
| 13.0 ± 5.1 | |
| 34.6 ± 3.6 | |
| 13.0 ± 2.1 |
Figure 3The best geometrical stability of the “open” G-triad of 4d structure. (A) 3D structures (upper panel) of the G-triad (G2:G8:G14) belonging to 4d conformation, with two water molecules network (nw) (upper panel) and one water bridge between G14 and A1 (lower panel), both miming the G16 slipped residue (B) In the upper panel, plot showing the RMSd trend calculated during the MDs on the G-triad at 5′-end, formed by G2:G8:G14 residues (dark-green line). In the lower panel, the plot shows the number of contacts between K+ ion and the guanines O6 oxygen atoms (black line) and the number of contacts between bulk water (nw) and the G8 and G20 residues (red line) during the MDs.
Figure 4(A) Native gel electrophoresis analysis of h-tel23 (lane 1) and h-tel (lane 2) prepared in 20 mM potassium phosphate buffer (pH 7.0) containing 70 mM KCl, 0.2 mM EDTA, and 40% PEG200. Lane 3: bromophenol blue. CD spectra of (B) h-tel23 and (C) h-tel in 40% PEG200 containing K+-buffer as a function of temperature (from 10 to 100 °C with temperature increase of 5 °C); and normalized CD melting curves of (D) h-tel23 and (E) h-tel obtained by following changes of CD signal at 265 (black) and 295 (red) nm.