Hydro
phobic core residues have a marked influence onthe Ca
2+-binding
pro
perties of calbindinD
9k, even though there are no direct contacts between theseresidues and the bound Ca
2+ ions.Elevendifferent mutants with substitutions in the hydro
phobic core were
produced, and their equilibrium Ca
2+-binding constants measured from Ca
2+ titrations in the
presence of chromo
phoric chelators. TheCa
2+-dissociation rate constants were estimated from Ca
2+titrations followed by
1H NMR
1 and weremeasuredmore accurately using sto
pped-flow fluorescence. The
parameterswere measured at four KClconcentrations to assess the salt de
pendence of the
perturbations.The high similarity between the NMRs
pectra of mutants and wild-ty
pe calbindin D
9k suggeststhat the structure is largely un
perturbed by thesubstitutions. More detailed NMR investigations of the mutant inwhich V
al61 is substituted by Alashowed that the mutation causes only very mini
mal perturbations in theimmediate vicinity of residue 61.Substitutions of alanines or glycines for bulky residues in thecenter of the core were found to havesignificant effects on both Ca
2+ affinity anddissociation rates. These substitutions caused a reductioninaffinity and an increase in off-rate. S
mall effects, bothincreases and decreases, were observed forsubstitutions involving residues far from the Ca
2+ sitesand toward the outer
part of the hydro
phobiccore. The mutant with the substitution Phe66
![](/images/entities/rarr.gif)
Tr
p behaveddifferently from all other mutants, anddis
played a 25-fold increase in overall affinity of binding twoCa
2+ ions and a 6-fold reduction in calciumdissociation rate. A strong correlation (
R = 0.94)was found between the observedCa
2+-dissociationrates and affinities, as well as between the salt de
pendence of theoff-rate and the distance to the nearestCa
2+-coordinating atom. There was also a strongcorrelation (
R = 0.95) between the Ca
2+affinity andstability of the Ca
2+ state and a correlation(
R = 0.69) between the Ca
2+ affinity andstability of the a
postate, as calculated from the results in the
present and
preceding
pa
per in this issue [Julenius, K., Thulin,E., Linse, S., and Finn, B. E. (1998)
Biochemistry 37,8915-8925]. The change in salt de
pendenciesof
koff and coo
perativity were most
pronouncedfor residues com
pletely buried in the core of the
protein(solvent accessible surface area
![](/images/entities/a<font color=)
p.gif"> 0). Altogether, the resultssuggest that the hydro
phobic core residues
promote Ca
2+ binding both by contributing to the
preformation of the Ca
2+ sites in the a
po state andby
preferentially stabilizing the Ca
2+-boundstate.