Towards elucidation of the proton-coupled electron transfer reaction mechanism in manganese superoxide dismutase through disruption of the dimer interface — ASN Events

Towards elucidation of the proton-coupled electron transfer reaction mechanism in manganese superoxide dismutase through disruption of the dimer interface (#157)

Jatnika Hermawan 1 , Trevor S. Loo 1 , Gill Norris 1 , Sarah A. Kessans 2 , Renwick C.J. Dobson 2 , Geoffrey B. Jameson 1
  1. Institute of Fundamental Sciences, Massey University, Palmerston North, New Zealand
  2. Biomolecular Interactions Centre and School of Biological Sciences, University of Canterbury, Christchurch, New Zealand

The ubiquitous superoxide dismutases (SODs) are critical on protecting the cell against a toxic radical anion, superoxide. SODs catalyse the disproportionation of superoxide to molecular oxygen and hydrogen peroxide in a mechanism that involves proton-coupled electron-transfer (PCET). SODs are known as the fastest enzyme with the largest kcat/Km of any known enzyme. Manganese SOD (MnSOD) from Escherichia coli is known to be fully fully active only as a homodimer. To gain insights into the mechanism of the PCET reaction mechanism, a potentially key residue Ser126 at the conserved but asymmetric dimer interface of the MnSOD from E. coli was mutated to Asp with the initial intent to generate a monomeric species. The expression was carried out in E. coli QC781, a SOD-deficient strain, transformed by pDT1-5 containing a sodA locus. 

Mutation of Ser126 significantly reduces the superoxide dismutase activities to 6 % and 5% of those of the wild-type enzyme at pH 7.8 and 6.0, respectively. Sedimentation velocity analysis indicated a dimeric species at pH 7.8, which becomes partially dissociated at pH 6.0. X-ray diffraction studies on crystals prepared at pH 8.7 (1.65 Ǻ) and pH 6.7 (1.56 Ǻ) show different space groups. The tightly packed symmetrical dimer interface is preserved but exhibited a considerable disorder at pH 6.7. The structural analyses of MnSOD S126D by exploring possible changes in water structure provide new information to examine the hypothesis of the Glu170 bridge as a proton shuttle in an outer-sphere mechanism for proton delivery to the nascent peroxo species.