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computer modeling in molecular biology.pdf

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5 Modell<strong>in</strong>g Nucleic Acids 125rotations about the short and long axis of the base pair). In standard RNA helices,the values of those parameters are 15.9" and 0", respectively. The values averagedover the last 50 ps of simulation are -24.3' and 18.7', respectively. The change <strong>in</strong>sign of the <strong>in</strong>cl<strong>in</strong>ation parameter is particularly strik<strong>in</strong>g and difficult to rationalize.Despite those unexpla<strong>in</strong>ed structural deformations, the analysis of the hydrationof the RNA fragment was highly <strong>in</strong>structive. Cones of hydration around eachanionic phosphate oxygen (Figure 5-13) were systematically observed, as well aswater bridges connect<strong>in</strong>g successive phosphate groups with lifetimes around 10 psand more. The structur<strong>in</strong>g power of the ribose 02' atom on the polar environmentwas also apparent <strong>in</strong> the simulations, s<strong>in</strong>ce the 02' preferentially accepts hydrogenbond<strong>in</strong>g from water <strong>in</strong>stead of be<strong>in</strong>g a hydrogen donor. The organized hydration <strong>in</strong>the shallow groove of RNA helices and around unusual base pairs, like G-U pairs,already discussed on the basis of crystallographic results [45] could be describedmore precisely. The active structur<strong>in</strong>g role of water molecules is not restricted tohelical regions, s<strong>in</strong>ce very organized water networks were observed <strong>in</strong> the anticodonloop, <strong>in</strong>volv<strong>in</strong>g especially the pseudourid<strong>in</strong>e 32 and the methyl guanos<strong>in</strong>e 37P3

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