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computer modeling in molecular biology.pdf

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116 E. WesthoJ C. Rub<strong>in</strong>-Carrez, and K Fritsch5.9 Choice of CounterionsThe importance of ions for the stabilization of deoxy- and ribonucleic acids, has longbeen recognized. The theoretical treatment of specific ion b<strong>in</strong>d<strong>in</strong>g is difficult. Whendiscuss<strong>in</strong>g metal ion b<strong>in</strong>d<strong>in</strong>g to nucleotide ligands two limit<strong>in</strong>g cases are usually considered:(a) site b<strong>in</strong>d<strong>in</strong>g with a direct coord<strong>in</strong>ation of the metal ion to ligands of thenucleotide, lead<strong>in</strong>g to the formation of <strong>in</strong>ner-sphere complexes after partial dehydrationof the metal ion; (b) ion atmosphere b<strong>in</strong>d<strong>in</strong>g where<strong>in</strong> the metal ions with their<strong>in</strong>tact hydration shells <strong>in</strong>teract <strong>in</strong>directly through water molecules with thenucleotides, form<strong>in</strong>g outer-sphere complexes [30]. The k<strong>in</strong>etics of magnesium b<strong>in</strong>d<strong>in</strong>gto polynucleotides have been well studied 1311 and follow the preced<strong>in</strong>g structuraldescription. First, an outer-sphere complex is formed with a rate close to thelimit of diffusion control. In a second step, one or more water molecules exchangewith ligand of the polynucleotide lead<strong>in</strong>g to <strong>in</strong>ner-sphere complexation with a ratedeterm<strong>in</strong>ed by the process of water dissociation, around 100000 per second formagnesium and 1000 times faster for calcium ions. The second step was observedonly with short oligoriboadenylates, <strong>in</strong>dicat<strong>in</strong>g that <strong>in</strong>ner-sphere complexation requiresparticular conformations of the nucleotide cha<strong>in</strong>s and the presence of theaden<strong>in</strong>e base and of the ribose hydroxyl group 02’.nYo features observed <strong>in</strong> crystal structures appear <strong>in</strong>terest<strong>in</strong>g [lo] (Figure 5-7).First, the ion is rarely bound directly to the phosphate anionic oxygen atoms <strong>in</strong>ribonucleotide complexes, but more often <strong>in</strong> deoxynucleotide complexes. Direct contactto nucleic acid ligands occur ma<strong>in</strong>ly at N7 of pur<strong>in</strong>es and at anionic oxygenatoms while fully hydrated ions <strong>in</strong>teract as often with the bases as with the sugarphosphatebackbone. Secondly, often one or two water molecules of the ion hydrationshell are common to two ions so that they share an apex or an edge of the coord<strong>in</strong>ationspheres (two such sodium ions are separated by 3.3 to 3.8 A). While watermolecules are weakly held to sodium ions (they exchange at the diffusion-controlledvalue and have thus residency times on the ion around the nanosecond), watermolecules are held more strongly to magnesium ions. The very high rate constantsfor magnesium ions association to polynucleotides <strong>in</strong>dicate “outer sphere” complexation.Therefore, not surpris<strong>in</strong>gly, crystal structures of nucleotides and polynucleotidesreveal “<strong>in</strong>ner sphere” complexation with sodium ions and “outersphere” complexation with magnesium ions. However, while magnesium b<strong>in</strong>d<strong>in</strong>g tobases <strong>in</strong> helices appears to be preferentially of the “outer sphere” type, b<strong>in</strong>d<strong>in</strong>g tophosphate groups occur <strong>in</strong> loops and bends of the sugar-phophate backbone and isoften of the “<strong>in</strong>ner sphere” type.As counterions, we have favored the use of ammonium ions. First, its tetrahedralstereochemistry resembles that of water and its geometry as well as its empiricalparameters have been determ<strong>in</strong>ed [32]. Secondly, as described above, other types ofcounterions possess coord<strong>in</strong>ated water molecules (e. g. the octahedral arrangement

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