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The central domain contains a [Fe4S4] cluster coordinated by four conserved cysteine residues.
In complex 2, each Zn II) ion is coordinated by four different L2 to form a undulated sheet.
The Cu and Zn atoms are coordinated by four IMI molecules and construct rectangular and tetrahedral configurations, respectively.
There are two types of cobalt environments: Co(1) is coordinated by four oxygen atoms from four carboxyl groups and two nitrogen atoms which are all from pdc2.
The structure determination reveals that the cobalt II) ions, bridged by bpee and coordinated by four water molecules, give rise to covalently linked 1D polymeric chain.
The crystallographic structures of the silica minerals, except stishovite, are three-dimensional arrays of linked tetrahedrons, each consisting of a silicon atom coordinated by four oxygen atoms.
Similar(12)
M2 is coordinated by six oxygen atoms.
The latter is uniquely coordinated by three carbonmonoxide (CO) and two cyanide (CN−) ligands.
Co is coordinated by six IMI molecules and forms an octahedral structure.
Therefore, each oxygen is coordinated by two A, one B, and one silicon cation (see figure).
The two copper ions in the conserved active site, CuA and CuB, are coordinated by six histidine residues5,6,7.
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