G. Hajipour et al. / Bioorg. Med. Chem. 7 (1999) 887±894
893
rate-limiting. The value of 2 for product release is
the product of an inverse isotope eect of 2 and a
normal isotope eect of 4. The inverse isotope
eect of 2 is exactly similar to that for substrate
entry into the active site: we take it to arise from a
sulfhydryl addition±elimination equilibrium at the
allosteric site coupled to active-site opening and
closing, with rate-limiting departure of acetalde-
hyde from the active site during an open period.
Concurrent with the export of acetaldehyde is the
import of a proton required in the stoichiometry,
and this process generates a normal isotope eect
of 4.
j is about unity. The inverse isotope eect on {ko1 ko3/
(k +k )} which should approximate that for oxidant
entry into the active site is therefore 1.7Â1.5=2.6.
o2
o3
Conclusion
The oxidative-diversion reaction of the SCPDC-pyr-
uvate system by the oxidant dichlorophenolindophenol
appears to occur by entry of the oxidant into the active
site with a second-order rate constant k /K and sol-
ox ox
vent isotope eect very similar to that for the binding of
pyruvate to the active site. The solvent isotope eect
arises from sulfhydryl addition at the allosteric site,
coupled to opening of access to the active site. This
process is required for admission of the oxidant to the
active site, as well as the normal substrate pyruvate and
the abnormal substrate ¯uoropyruvate.
A proton-inventory study has also been carried out for
the solvent isotope eect of 1.9 (Table 2) seen with
1
¯
uoropyruvate.2 In this case, there is no contribution of
an inverse isotope eect and if such an eect is required
for product release in the ¯uoropyruvate reaction, then
product release must be a rapid, non-rate-limiting pro-
cess. The proton inventory is consistent with two steps
that are about equally rate-limiting, one with no solvent
isotope eect and the other with a normal solvent iso-
tope eect of about 3.4. The former may be ¯uoride
elimination, the latter either ketonization of the elim-
ination product to generate acetyl-ThDP or hydrolysis
of acetyl-ThDP, each of the two contributing processes
The ®rst-order rate constant rate kox re¯ects a quite
slow release of the hydrophobic product of oxidative
diversion DH , also with an inverse solvent isotope
2
eect arising sulfhydryl addition at the allosteric site,
coupled to opening of the active site to permit product
departure.
The inverse isotope eects for both oxidant entry into
the active site and reduced-product exit from the active
site are therefore readily reconciled with the model of
allosteric regulation according to which sulfhydryl
addition by Cys-221 to the keto group of a pyruvate or
other ketone at the allosteric site drives a rapid open-
ing±closing of access to the active site. It is less easy to
see how the observations can be reconciled with a model
for regulation according to which events at the allosteric
site eect reorganization of the catalytic machinery at
the active site.
�
1
occurring with a rate constant of about 88 s . If actual
release of acetate occurs with a rate constant similar to
that for acetaldehyde release in the normal catalytic
�
1
cycle (640 s ), then it is about sevenfold faster than the
rate-limiting steps.
In the oxidative-diversion reaction, the inverse isotope
eect of around 2 is most easily explained if it is
assumed that product release, coupled to sulfhydryl
addition at the allosteric site, is now rate-limiting.
However, unless some unusual eect is at work, the rate
of acetate release cannot be rate-limiting here because
its rate constant in the ¯uoropyruvate reaction is much
Experimental
�
1
larger than the observed rate constant of 44 s , whereas
the observed rate constant in the oxidative diversion
Materials. Thiamin diphosphate hydrochloride (`cocar-
boxylase'), buers, salts, and NADH were purchased
from Sigma, standard solutions, anhydrous citric acid
from Fisher, sodium citrate dihydrate and magnesium
sulfate (anhydrous) from J. T. Baker. Deuterium oxide
was obtained from Aldrich (99.9% D). Sodium pyr-
uvate was obtained from Sigma in 99% pure crystalline
form.
�
1
reaction is only 11 s . This leaves only the release of
DH . It does seem likely that this hydrophobic dye
2
molecule may have such a large anity for the active
site that it departs less frequently by about 60-fold than
the polar acetate molecule. We therefore suggest that
the rate-limiting event for kox is release of DH , coupled
2
to sulfhydryl addition at the allosteric site, which pro-
duces the inverse isotope eect.
Enzyme. Pyruvate decarboxylase (EC 4.1.1.1) from
Saccharomyces cerevisiae (speci®c activity 12±14 units/
mg) was purchased from Sigma, suspended in a solution
of 5% glycerol, 3.2 M ammonium sulfate, 5 mM potas-
sium phosphate, 1 mM magnesium acetate, 0.5 mM
EDTA, and 25 FM ThDP, pH 6.5.
The isotope eects on k/K are all inverse, in agreement
with the view that this constant is determined by events
during, or subsequent to, the entry of substrate or oxi-
dizing agent into the active site during an open period in
the rapid open±closed cycling driven by reversible addi-
tion of Cys-221 to pyruvate at the allosteric site. It
should be noted that the true inverse isotope eect for
oxidant entry in oxidative diversion may be larger than
2,6-Dichlorophenolindophenol (D). Obtained from
Sigma, dissolved in 1 M HCl, and extracted into ether.
The sodium salt was re-extracted into 2% sodium
bicarbonate solution and precipitated with sodium
chloride. The precipitate was washed with sodium chlo-
the measured value of 1.7 for k /K . The rate constant
ox ox
k /K is given by {ko1 k /(k +k )}{k /(k +k )}j
ox ox
o3
o2
o3
c5
c3
c5
where, as has been noted, the second factor is about 1/2
in protium oxide and about 1/3 in deuterium oxide and
ꢀ
ride solution, dried at 100 C, and stored in a dessicator.