Methods: High-resolution synchrotron radiation was used to collect 2D X-ray diffraction images across whole tooth crowns of intact sections of mature and partially mature enamel. The texture direction and magnitude were determined by interrogating the intensity pattern around the Debye ring of the 002 reflection to construct maps of the local orientation and magnitude of texture.
Results: Texture direction maps indicate a similar pattern of crystallite orientations in both mature and immature enamel; however the degree of texture was generally found to vary less in the immature enamel as compared to the fully mature enamel when observing a track from tooth surface to enamel-dentine junction.
Conclusion: Our results indicate that the differences in texture in mature and immature enamel can be quantified using synchrotron X-ray diffraction. Due to the complex growth patterns in enamel mineralization we have observed significant inter- and intra-tooth heterogeneities in enamel texture, therefore it will be necessary to characterize a larger number of tooth specimens in order to establish the precise texture markers of maturation.