Supporting Information Available In vitro labeling of hydroxyapatite minerals by an engineered protein Esra Yucaa,b,c, Ayten Yazgan Karatasa, Urartu Ozgur Safak Sekera,c, Mustafa Gungormusc, Gizem Dinler-Doganaya, Mehmet Sarikayaa,c and Candan Tamerlera,c* a Department of Molecular Biology, Genetics and Biotechnology, Istanbul Technical University, Istanbul, Turkey, b Department of Biology, Yıldız Technical University, Istanbul, Turkey, c Department of Materials Science and Engineering, University of Washington, Seattle, Washington, USA Quartz Crystal Microbalance-Dissipation (QCM-D) Experiments: The QCM-D measures the change in the frequency and the dissipation following the crystal is excited under electrical power (Hook et al. 2001; Hook et al. 1998). By comparing the frequency change at different overtones, one can comment on the elasticity of the film adsorbed on the sensor surface. Proteins can be considered as polymers with water holding capacities. Upon adsorption on a solid surface, the proteins are able to capture water and form a viscoelastic film. Depending on the change in the dissipation of the adsorbed layer, one can make assumptions about how dense the adsorbed film is. In this section, we provide the dissipation changes monitored in our studies. The dissipation change for both of the proteins is very small in our case (Supplementary Figure 1). This may imply that the amount of water held by proteins is very small upon adsorption. We therefore can assume that a rigid protein film was formed on the 1 resonator surface. This is also in agreement with the fact that, GFP is quiet rigid with its beta sheet dominated barrel like structure. Supplementary Figure 1. Dissipation change (black) and frequency change (blue) for GFPHABP1 and GFP-HABP2 In calculations, Sauerbrey equation can be used to convert the frequency change (Δf) to the mass load. Sauerbrey equation assumes that the film adsorbed on the sensor surface is rigid, coupled 2 with the sensor and oscillating with the same frequency. By using this approach, mass deposited on the surface can be calculated using the following equation (Sauerbrey 1959): Equation 1 where m is the mass deposited, C is the mass sensitivity constant and f is the frequency change of the sensor and n is the overtone number. However this equation is not valid and applicable for the soft and elastic films. In our case the film may not be fully coupled with the resonator (sensor), even though there is only a small possibility of dissipation throughout adsorption. In this case the change in the deposited mass can be defined with a correction in the Sauerbery equation as shown in equation 2 (Domack et al. 1997; Fredriksson et al. 1998; Granstaff and Martin 1994; Martin et al. 1991; Voinova et al. 1999, Kankare 2002): Equation 2 where is deposited mass on resonator surface, is the resonance of the given overtone, is the change in the resonance frequency upon mass deposition on the resonator, of quartz, solution, is thickness of resonator, is the density is the density of medium in our case it is protein density of the protein film adsorbed on to the surface, solution, is angular frequency of oscillator, and is the viscosity of the protein is shear modulus. 3 Monitoring time wise mineralization Supplementary Figure 2: The ability of GFPuv-HABP1 construct to monitor the time wise mineralization was tested on minerals forming on glass slides. An alkaline phosphatase based mineralization model (Gungormus et al. 2008) was used for time wise monitoring the biomineralization. Before the examination by optical microscopy, scanning electron microscopy (SEM) and fluorescent microscopy, a calcium phosphate layer was formed on glass cover slides. At the end of each time point (0.5, 2, 8 and 24 hours), the glass slides were taken out and the mineral covered area on glass slides was calculated using Metamorph v7.5 image processing software (Molecular Devices, USA). Optical microscopy results showed that the amount of mineral on the glass slides has increased in a linear fashion. 4 TEM and Electron Diffraction Characterization of the HA minerals Supplementary Figure 3: TEM micrographs of the synthetic HA used for fluorescent binding characterization and the HA synthesized on a glass slide to monitor the mineral formation in vitro. The corresponding selected area electron diffraction (SAED) patterns are shown in the insets. The synthesized particles were collected by scraping off the mineral from the glass slides using a plastic toothpick. 5 SUPPLEMENTARY REFERENCES Domack A, Prucker O, Ruhe J, Johannsmann D. 1997. Swelling of a polymer brush probed with a quartz crystal resonator. Physical Review E 56(1):680-689. Fredriksson C, Kihlman S, Rodahl M, Kasemo B. 1998. The piezoelectric quartz crystal mass and dissipation sensor: A means of studying cell adhesion. Langmuir 14(2):248-251. Granstaff VE, Martin SJ. 1994. Characterization of a Thickness-Shear Mode Quartz Resonator with Multiple Nonpiezoelectric Layers. Journal of Applied Physics 75(3):1319-1329. Hook F, Kasemo B, Nylander T, Fant C, Sott K, Elwing H. 2001. Variations in coupled water, viscoelastic properties, and film thickness of a Mefp-1 protein film during adsorption and cross-linking: A quartz crystal microbalance with dissipation monitoring, ellipsometry, and surface plasmon resonance study. Analytical Chemistry 73(24):5796-5804. 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