4.7 Article

Intrafibrillar mineral may be absent in dentinogenesis imperfecta type II (DI-II)

Journal

JOURNAL OF DENTAL RESEARCH
Volume 80, Issue 6, Pages 1555-1559

Publisher

AMER ASSOC DENTAL RESEARCH
DOI: 10.1177/00220345010800061501

Keywords

dentin; dentinogenesis imperfecta; mineralization; small angle scattering; synchroton radiation

Funding

  1. NIDCR NIH HHS [P01 DE09859] Funding Source: Medline

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High-resolution synchrotron radiation computed tomography (SRCT) and small-angle x-ray scattering (SAXS) were performed on normal and dentinogenesis imperfecta type II (DI-II) teeth. The SRCT showed that the mineral concentration was 33% lower on average in the DI-II dentin with respect to normal dentin. The SAXS spectra from normal dentin exhibited low-angle diffraction peaks at harmonics of 67.6 nm, consistent with nucleation and growth of the apatite phase within gaps in the collagen fibrils (intrafibrillar mineralization). In contrast, the low-angle peaks were almost non-existent in the DI-II dentin. Crystallite thickness was independent of location in both DI-II and normal dentin, although the crystallites were significantly thicker in DI-II dentin (6.8 nm [SD = 0.5] vs. 5.1 run [SD = 0.6]). as determined The shape factor of the crystallites, by SAXS, showed a continuous progression in normal dentin from roughly one-dimensional (needle-like) near the pulp to two-dimensional (plate-like) near the dentin-enamel junction. The crystallites in DI-II dentin, on the other hand, remained needle-like throughout. The above observations are consistent with an absence of intrafibrillar mineral in DI-II dentin.

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