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Lattice Shrinkage by Incorporation of Recombinant Starmaker-Like Protein within Bioinspired Calcium Carbonate Crystals
Authors:Mirosława Różycka  Ismael Coronado  Katarzyna Brach  Joanna Olesiak-Bańska  Marek Samoć  Mirosław Zarębski  Jerzy Dobrucki  Maciej Ptak  Eva Weber  Dr. Iryna Polishchuk  Dr. Boaz Pokroy  Jarosław Stolarski  Prof. Andrzej Ożyhar
Affiliation:1. Department of Biochemistry, Faculty of Chemistry, Wroclaw University of Science and Technology, Wroclaw, 50-370 Poland;2. Institute of Paleobiology, Polish Academy of Sciences, Warsaw, 00-818 Poland;3. Advanced Materials Engineering and Modelling Group, Faculty of Chemistry, Wroclaw University of Science and Technology, Wroclaw, 50-370 Poland;4. Department of Cell Biophysics, Faculty of Biochemistry, Biophysics and Biotechnology, Jagiellonian University, Krakow, 30-387 Poland;5. Institute of Low Temperature and Structure Research, Polish Academy of Sciences, Wroclaw, 50-422 Poland;6. Department of Materials Science and Engineering and the Russell Berrie Nanotechnology Institute, Technion Israel Institute of Technology, Haifa, 32000 Israel
Abstract:
The biological mediation of mineral formation (biomineralization) is realized through diverse organic macromolecules that guide this process in a spatial and temporal manner. Although the role of these molecules in biomineralization is being gradually revealed, the molecular basis of their regulatory function is still poorly understood. In this study, the incorporation and distribution of the model intrinsically disordered starmaker-like (Stm-l) protein, which is active in fish otoliths biomineralization, within calcium carbonate crystals, is revealed. Stm-l promotes crystal nucleation and anisotropic tailoring of crystal morphology. Intracrystalline incorporation of Stm-l protein unexpectedly results in shrinkage (and not expansion, as commonly described in biomineral and bioinspired crystals) of the crystal lattice volume, which is described herein, for the first time, for bioinspired mineralization. A ring pattern was observed in crystals grown for 48 h; this was composed of a protein-enriched region flanked by protein-depleted regions. It can be explained as a result of the Ostwald-like ripening process and intrinsic properties of Stm-l, and bears some analogy to the daily growth layers of the otolith.
Keywords:biominerals  calcium  crystal growth  proteins  X-ray diffraction
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