A REDOR ssNMR Investigation of the Role of an N-Terminus Lysine in R5 Silica Recognition.

Diatoms are unicellular algae that construct cell walls called frustules by the precipitation of silica, using special proteins that order the silica into a wide variety of nanostructures. The diatom species Cylindrotheca fusiformis contains proteins called silaffins within its frustules, which are believed to assemble into supramolecular matrices that serve as both accelerators and templates for silica deposition. Studying the properties of these biosilicification proteins has allowed the design of new protein and peptide systems that generate customizable silica nanostructures, with potential generalization to other mineral systems. It is essential to understand the mechanisms of aggregation of the protein and its coprecipitation with silica. We continue previous investigations into the peptide R5, derived from silaffin protein sil1p, shown to independently catalyze the precipitation of silica nanospheres in vitro. We used the solid-state NMR technique 13C{29Si} and 15N{29Si} REDOR to investigate the structure and interactions of R5 in complex with coprecipitated silica. These experiments are sensitive to the strength of magnetic dipole-dipole interactions between the 13C nuclei in R5 and the 29Si nuclei in the silica and thus yield distance between parts of R5 and 29Si in silica. Our data show strong interactions and short internuclear distances of 3.74 ± 0.20 Å between 13C═O Lys3 and silica. On the other hand, the Cα and Cß nuclei show little or no interaction with 29Si. This selective proximity between the K3 C═O and the silica supports a previously proposed mechanism of rapid silicification of the antimicrobial peptide KSL (KKVVFKVKFK) through an imidate intermediate. This study reports for the first time a direct interaction between the N-terminus of R5 and silica, leading us to believe that the N-terminus of R5 is a key component in the molecular recognition process and a major factor in silica morphogenesis.

Probing the self-association, intermolecular contacts, and folding propensity of amelogenin.

Amelogenins are an intrinsically disordered protein family that plays a major role in the development of tooth enamel, one of the most highly mineralized materials in nature. Monomeric porcine amelogenin possesses random coil and residual secondary structures, but it is not known which sequence regions would be conformationally attractive to potential enamel matrix targets such as other amelogenins (self-assembly), other matrix proteins, cell surfaces, or biominerals. To address this further, we investigated recombinant porcine amelogenin (rP172) using "solvent engineering" techniques to simultaneously promote native-like structure and induce amelogenin oligomerization in a manner that allows identification of intermolecular contacts between amelogenin molecules. We discovered that in the presence of 2,2,2-trifluoroethanol (TFE) significant folding transitions and stabilization occurred primarily within the N- and C-termini, while the polyproline Type II central domain was largely resistant to conformational transitions. Seven Pro residues (P2, P127, P130, P139, P154, P157, P162) exhibited conformational response to TFE, and this indicates these Pro residues act as folding enhancers in rP172. The remaining Pro residues resisted TFE perturbations and thus act as conformational stabilizers. We also noted that TFE induced rP172 self-association via the formation of intermolecular contacts involving P4-H6, V19-P33, and E40-T58 regions of the N-terminus. Collectively, these results confirm that the N- and C-termini of amelogenin are conformationally responsive and represent potential interactive sites for amelogenin-target interactions during enamel matrix mineralization. Conversely, the Pro, Gln central domain is resistant to folding and this may have important functional significance for amelogenin.

Evidence of mineralization activity and supramolecular assembly by the N-terminal sequence of ACCBP, a biomineralization protein that is homologous to the acetylcholine binding protein family.

Several biomineralization proteins that exhibit intrinsic disorder also possess sequence regions that are homologous to nonmineral associated folded proteins. One such protein is the amorphous calcium carbonate binding protein (ACCBP), one of several proteins that regulate the formation of the oyster shell and exhibit 30% conserved sequence identity to the acetylcholine binding protein sequences. To gain a better understanding of the ACCBP protein, we utilized bioinformatic approaches to identify the location of disordered and folded regions within this protein. In addition, we synthesized a 50 AA polypeptide, ACCN, representing the N-terminal domain of the mature processed ACCBP protein. We then utilized this polypeptide to determine the mineralization activity and qualitative structure of the N-terminal region of ACCBP. Our bioinformatic studies indicate that ACCBP consists of a ten-stranded beta-sandwich structure that includes short disordered sequence blocks, two of which reside within the primarily helical and surface-accessible ACCN sequence. Circular dichroism studies reveal that ACCN is partially disordered in solution; however, ACCN can be induced to fold into an alpha helix in the presence of TFE. Furthermore, we confirm that the ACCN sequence is multifunctional; this sequence promotes radial calcite polycrystal growth on Kevlar threads and forms supramolecular assemblies in solution that contain amorphous-appearing deposits. We conclude that the partially disordered ACCN sequence is a putative site for mineralization activity within the ACCBP protein and that the presence of short disordered sequence regions within the ACCBP fold are essential for function.