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(a) highly
electrophilic oxo
H
H
Cl
nucleophilic attack
O
O
Ca
O
O
Mn V
O
Mn IV
Mn IV
Mn IV
O
(b)
H
H
Cl
oxyl radical
attack
O
O
Ca
O
O
Mn IV
O
Mn IV
Mn IV
Mn IV
O
FIGURE 16.4
(a,b) Possible mechanisms for formation of dioxygen during the S4-S0 transition.
(Adapted rom Barber, 2008 .)
FIGURE 16.5
The protein fold of Mn- or Fe-SODs (left) and the active site (right).
(From Miller, 2004 . Copyright 2004 with permission from
Elsevier.)
Catalases play an important protective role, catalysing the disproportionation of toxic hydrogen peroxide into O 2
and H 2 O. In contrast to the haem-containing catalases, which are ubiquitous in aerobic organisms, a broad range of
microorganisms, living in microaerophilic (almost oxygen-free) environments, including the lactic acid bacteria , 3
have catalases which have a dinuclear manganese centre in their active site ( Figure 16.6 ) ( Wu et al., 2004 ). These
'alternative' catalases are 4-helix bundle proteins, with the di-Mn centre located in themiddle of the
helical bundle.
The disproportionation of hydrogen peroxide is thermodynamically favourable; however, rapid reaction
requires a two-electron catalyst. For haem catalases, this is achieved by cycling between Fe III and Fe IV porphyrin
a
3. We mentioned earlier that this family of bacteria has adapted to its environment to function without iron, using Co and Mn instead.
 
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