Faculty Bibliography

Intracrystalline modification of calcium carbonates by macromolecules is a fascinating process that offers insights into potential pathways for modifying the material properties of inorganic solids. Recently, we reported on the induction of intracrystalline nanoporosities within calcite by the nacre layer intracrystalline protein, AP7 (Haliotis rufescens). In this report we revisited this AP7-mediated phenomenon and tracked time-dependent intracrystalline porosity formation during in vitro mineralization using FIB/SEM serial milling. We find that AP7 induces intracrystalline nanoporosities as early as 1 min of elapsed assay time. Quantitation of pore regions confirms that average cross-sectional volume (ACSV), average void volume (AVV), and percent porosity parameters increase over time, leading to the formation of porous calcite crystals with a high surface-to-volume ratio. FIB serial milling, SEM imaging, and 3-D tomography revealed the presence of unexpected semicontinuous channels and cavities in the subsurface regions of a representative 60 min assay crystal. The random locations of these intracrystalline features are limited to the top and sides of the calcite crystal, which correspond to the sites of AP7 protein phase deposition during mineral formation. This random porosity distribution was also documented for protein-containing voids within nacre aragonite tablets in situ. In some instances we observed geometric relationships between adjacent channels and cavities. Interestingly, all three IUPAC-defined material porosity categories (micro-, meso-, and macro-) were represented in the AP7-treated crystals. Thus, the deposition of AP7 protein phases onto calcite surfaces induces surface nanoparticle nucleation and subsurface multiscale intracrystalline porosities and interconnected channels.

Amelogenin protein has the potential to interact with other enamel matrix proteins, mineral, and cell surfaces. We investigated the interactions of recombinant amelogenin rP172 with small unilamellar vesicles as model membranes, toward the goal of understanding the mechanisms of amelogenin-cell interactions during amelogenesis. Dynamic light scattering (DLS), fluorescence spectroscopy, circular dichroism (CD), and nuclear magnetic resonance (NMR) were used. In the presence of phospholipid vesicles, a blue shift in the Trp fluorescence emission maxima of rP172 was observed (∼334 nm) and the Trp residues of rP172 were inaccessible to the aqueous quencher acrylamide. DLS studies indicated complexation of rP172 and phospholipids, although the possibility of fusion of phospholipids following amelogenin addition cannot be ruled out. NMR and CD studies revealed a disorder-order transition of rP172 in a model membrane environment. Strong fluorescence resonance energy transfer from Trp in rP172 to DNS-bound-phospholipid was observed, and fluorescence polarization studies indicated that rP172 interacted with the hydrophobic core region of model membranes. Our data suggest that amelogenin has ability to interact with phospholipids and that such interactions may play key roles in enamel biomineralization as well as reported amelogenin signaling activities.

n16 is a framework protein family associated with biogenic mineral stabilization, thought to operate at three key interfaces in nacre: protein/β-chitin, protein/protein, and protein/CaCO3. The N-terminal half of this protein, n16N, is known to be active in conferring this mineral stabilization and organization. While some details relating to the stabilization and organization of the mineral are known, the molecular mechanisms that underpin these processes are not yet established. To provide these molecular-scale details, here we explore current hypotheses regarding the possible subdomain organization of n16N, as related to these three interfaces in nacre, by combining outcomes of Replica Exchange with Solute Tempering molecular dynamics simulations with NMR experiments, to investigate the conformational ensemble of n16N in solution. We verify that n16N lacks a well-defined secondary structure, both with and without the presence of Ca(2+) ions, as identified from previous experiments. Our data support the presence of three different, functional subdomains within n16N. Our results reveal that tyrosine, chiefly located in the center of the peptide, plays a multifunctional role in stabilizing conformations of n16N, for intrapeptide and possibly interpeptide interactions. Complementary NMR spectroscopy data confirm the participation of tyrosine in this stabilization. The C-terminal half of n16N, lacking in tyrosine and highly charged, shows substantive conformational diversity and is proposed as a likely site for nucleation of calcium carbonate. Finally, dominant structures from our predicted conformational ensemble suggest the presentation of key residues thought to be critical to the selective binding to β-chitin surfaces.

The mollusk shell nacre layer integrates mineral phases with macromolecular components such as intracrystalline proteins. However, the roles performed by intracrystalline proteins in calcium carbonate nucleation and subsequent postnucleation events (e.g., organization of mineral deposits) in the nacre layer are not known. We find that AP7, a nacre intracrystalline C-RING protein, self-assembles to form amorphous protein oligomers and films on mica that further assemble into larger aggregates or phases in the presence of Ca(2+). Using solution nuclear magnetic resonance spectroscopy, we determine that the protein assemblies are stabilized by interdomain interactions involving the aggregation-prone T31-N66 C-terminal C-RING domain but are destabilized by the labile nature of the intrinsically disordered D1-T19 AA N-terminal sequence. Thus, the dynamic, amorphous nature of the AP7 assemblies can be traced to the molecular behavior of the N-terminal sequence. Using potentiometric methods, we observe that AP7 protein phases prolong the time interval for prenucleation cluster formation but neither stabilize nor destabilize ACC clusters. Time-resolved flow cell scanning transmission electron microscopy mineralization studies confirm that AP7 protein phases delay the onset of nucleation and assemble and organize mineral nanoparticles into ring-shaped branching clusters in solution. These phenomena are not observed in protein-deficient assays. We conclude that C-RING AP7 protein phases modulate the time period for early events in nucleation and form strategic associations with forming mineral nanoparticles that lead to mineral organization.

We report an interesting phenomenon whereby a framework mollusk shell nacre protein, n16.3, facilitates a two-stage crystal growth process. This protein forms phases that permit initial calcite growth, then via direct contact introduce textured mineral overgrowth to these core crystals in a directional fashion, and, create subsurface nanoporosities within these crystals. This phenomenon is an example of crystal modification and assembly directed by a biomineralization protein phase and we believe this framework protein-driven process is important for the assembly of the nacre shell layer. Similar phase-based approaches could be used to engineer a variety of inorganic crystals for technological applications. This journal is © the Partner Organisations 2014.

We report an interesting process whereby the formation of nanoparticle assemblies on and nanoporosities within calcite crystals is directed by an intrinsically disordered C-RING mollusk shell nacre protein, AP7. Under mineralization conditions, AP7 forms protein phases that direct the nucleation of ordered calcite nanoparticles via a repetitive protein phase deposition process onto calcite crystals. These organized nanoparticles are separated by gaps or spaces that become incorporated into the forming bulk crystal as nanoporosities. This is an unusual example of organized nanoparticle biosynthesis and mineral modification directed by a C-RING protein phase.

Adsorption behavior of a gold binding peptide was experimentally studied to achieve kinetics and thermodynamics parameters toward understanding of the binding of an engineered peptide onto a solid metal surface. The gold-binding peptide, GBP1, was originally selected using a cell surface display library and contains 14 amino acid residues. In this work, single- and three-repeats of GBP1 were used to assess the effects of two parameters: molecular architecture versus secondary structure on adsorption on to gold substrate. The adsorption measurements were carried out using surface plasmon resonance (SPR) spectroscopy at temperatures ranging from 10 to 55 °C. At all temperatures, two different regimes of peptide adsorption were observed, which, based on the model, correspond to two sets of thermodynamics values. The values of enthalpy, ΔH(ads), and entropy, ΔS(ads), in these two regimes were determined using the van't Hoff approach and Gibbs-Helmholtz relationship. In general, the values of enthalpy for both peptides are negative indicating GBP1 binding to gold is an exothermic phenomenon and that the binding of three repeat gold binding peptide (3l-GBP1) is almost 5 times tighter than that for the single repeat (l-GBP1). More intriguing result is that the entropy of adsorption for the 3l-GBP1 is negative (-43.4 ± 8.5 cal/(mol K)), while that for the l-GBP1 is positive (10.90 ± 1.3 cal/(mol K)). Among a number of factors that synergistically contribute to the decrease of entropy, long-range ordered self-assembly of the 3l-GBP1 on gold surface is the most effective, probably through both peptide-solid and peptide-peptide intermolecular interactions. Additional adsorption experiments were conducted in the presence of 2,2,2-trifluoroethanol (TFE) to determine how the conformational structures of the biomolecules responded to the environmental perturbation. We found that the peptides differ in their conformational responses to the change in solution conditions; while l-GBP does not fold in the presence of TFE, 3l-GBP1 adopted two types of secondary structure (β-strand, α-helix) and that peptide's binding to the solid is enhanced by the presence of low percentages of TFE solvent. Not only do these kinetics and thermodynamics results provide adsorption behavior and binding of genetically engineered peptides for inorganics (GEPI), but they could also provide considerable insights into fundamental understanding peptide molecular recognition and their selective specificity for the solids. Moreover, comprehensive work described herein suggests that multiple repeat forms of the solid binding peptides possess a conformational component that can be exploited to further tailor affinity and binding of a given sequence to a solid material followed by ordered assembly as a convenient tool in future practical applications.

Amelogenin, the major extracellular matrix protein of developing tooth enamel is intrinsically disordered. Through its interaction with other proteins and mineral, amelogenin assists enamel biomineralization by controlling the formation of highly organized enamel crystal arrays. We used circular dichroism (CD), dynamic light scattering (DLS), fluorescence, and NMR spectroscopy to investigate the folding propensity of recombinant porcine amelogenin rP172 following its interaction with SDS, at levels above critical micelle concentration. The rP172-SDS complex formation was confirmed by DLS, while an increase in the structure moiety of rP172 was noted through CD and fluorescence experiments. Fluorescence quenching analyses performed on several rP172 mutants where all but one Trp was replaced by Tyr at different sequence regions confirmed that the interaction of amelogenin with SDS micelles occurs via the N-terminal region close to Trp25 where helical segments can be detected by NMR. NMR spectroscopy and structural refinement calculations using CS-Rosetta modeling confirm that the highly conserved N-terminal domain is prone to form helical structure when bound to SDS micelles. Our findings reported here reveal interactions leading to significant changes in the secondary structure of rP172 upon treatment with SDS. These interactions may reflect the physiological relevance of the flexible nature of amelogenin and its sequence specific helical propensity that might enable it to structurally adapt with charged and potential targets such as cell surface, mineral, and other proteins during enamel biomineralization. (c) 2013 Wiley Periodicals, Inc. Biopolymers 101: 525-535, 2014.

The mollusk shell is a complex biological material that integrates mineral phases with organic macromolecular components such as proteins. The role of proteins in the formation of the nacre layer (aragonite mineral phase) is poorly understood, particularly with regard to the organization of mineral deposits within the protein extracellular matrix and the identification of which proteins are responsible for this task. We report new experiments that provide insight into the role of the framework nacre protein, n16.3 (Pinctada fucata), as an organizer or assembler of calcium carbonate mineral clusters. Using a combination of biophysical techniques, we find that recombinant n16.3 (r-n16.3) oligomerizes to form amorphous protein films and particles that possess regions of disorder and mobility. These supramolecular assemblies possess an intrinsically disordered C-terminal region (T64-W98) and reorganize in the presence of Ca(2+) ions to form clustered protein oligomers. This Ca(2+)-induced reorganization leads to alterations in the molecular environments of Trp residues, the majority of which reside in putative aggregation-prone cross-beta strand regions. Potentiometric Ca(2+) titrations reveal that r-n16.3 does not significantly affect the formation of prenucleation clusters in solution, and this suggests a role for this protein in postnucleation mineralization events. This is verified in subsequent in vitro mineralization assays in which r-n16.3 demonstrates its ability to form gel-like protein phases that organize and cluster nanometer-sized single-crystal calcite relative to protein-deficient controls. We conclude that the n16 nacre framework proteome creates a protein gel matrix that organizes and dimensionally limits mineral deposits. This process is highly relevant to the formation of ordered, nanometer-sized nacre tablets in the mollusk shell.

The Japanese pearl oyster (Pinctada fucata) n16 framework matrix protein is an integral part of the growth and formation of the mollusk shell biomineralization mechanism. It is a required component of the extracellular matrix with a dual mineralization role, as an anchor component to synchronize the assembly of the beta-chitin and N-series, Pif-series protein extracellular matrix for aragonite formation and as a regulator of aragonite formation itself. However, the mechanism by which this protein controls aragonite formation is not understood. Here, we investigate the mineralization potential and kinetics of the 30 AA N-terminal portion of the n16 protein, n16N. This sequence has been demonstrated to form either vaterite or aragonite depending upon conditions. Using in situ potentiometric titration methods, we find that n16N is indeed responsible for the self-assembly characteristics found in vivo and in vitro but is not involved with active Ca²⁺ binding or mineral nucleation processes. Upon the basis of time- and peptide concentration-dependent sampling of mineral deposits that form in solution, we find that n16N is responsible for controlling where mineralization occurs in bulk solution. This protein sequence acts as a molecular spacer that organizes the mineralization space and promotes the formation of mineral constituents that contain ACC, vaterite, and aragonite. Without the concerted action of the n16N assemblage, unregulated calcite formation occurs exclusively. Thus, the n16 protein provides the regulation needed to have the characteristic polymorph, crystalline orientations, and related mechanical properties associated to the microstructure of mollusk shells. © 2014 American Chemical Society.