No abstract

The formation of the mollusk nacre layer involves the assembly and organization of mineral nanoparticles into fracture-toughened mesoscale-sized aragonite tablets that possess intracrystalline nanoporosities. At least one nacre protein family, known as the framework proteome, is strategically located as part of a macromolecular coating around each nacre tablet and is believed to participate in tablet formation. Here, we report new studies of a recombinant form (rPif97) of a unique Japanese pearl oyster (Pinctada fucata) nacre framework biomineralization protein, Pif97. This unique protein possesses both a von Willlebrand factor type A domain (vWA, F23-Y161) and a Peritrophin A chitin-binding domain (PAC, E234-D298). rPif97 self-associates or aggregates to form amorphous protein phases that organize both amorphous and single-crystal calcium carbonate nanoparticles in vitro. Further, in the presence of nucleating calcite crystals, rPif97 protein phases deposit onto these crystals and become occluded over time, forming nanochambers within the crystal interior. The formation of these mineral-modifying amorphous protein phases is linked to the presence of intrinsic disorder and amyloid-like cross-β-strand aggregation-prone regions, and three-dimensional modeling indicates that both the vWA and PAC domains are accessible for intermolecular interactions. Thus, the vWA- and PAC-containing Pif97 protein exhibits key functionalities that would allow its participation in mollusk nacre layer tablet assembly and porosity formation.

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 Ca2+. 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.

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-β 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.

A nacre protein, n16.3, forms phases that introduce textured mineral overgrowth and subsurface nanoporosities within calcite crystals.