The first crystal structure of an inorganic pyrophosphatase
(S-PPase) from an archaebacterium, the thermophile Sulfolobus
acidocaldarius, has been solved by molecular replacement
and refined to an R-factor of 19.7% at 2.7 Å.
S-PPase is a D3 homohexameric protein with one
Mg2+ per active site in a position similar to,
but not identical with, the first activating metal in mesophilic
pyrophosphatases (PPase). In mesophilic PPases, Asp65,
Asp70, and Asp102 coordinate the Mg2+, while
only Asp65 and Asp102 do in S-PPase, and the Mg2+
moves by 0.7 Å. S-PPase may therefore be deactivated
at low temperature by mispositioning a key metal ion.
The monomer S-PPase structure is very similar to that of
Thermus thermophilus (T-PPase) and Escherichia
coli (E-PPase), root-mean-square deviations around
1 Å/Cα. But the hexamer structures of S- and
T-PPase are more tightly packed and more similar to each
other than they are to that of E-PPase, as shown by the
increase in surface area buried upon oligomerization. In
T-PPase, Arg116 creates an interlocking ionic network to
both twofold and threefold related monomers; S-PPase has
hydrophilic interactions to threefold related monomers
absent in both E- and T-PPase. In addition, the thermostable
PPases have about 7% more hydrogen bonds per monomer than
E-PPase, and, especially in S-PPase, additional ionic interactions
anchor the C-terminus to the rest of the protein. Thermostability
in PPases is thus due to subtle improvements in both monomer
and oligomer interactions.