| Literature DB >> 35156182 |
W Eugene Roberts1, Jonathan E Mangum2, Paul M Schneider3.
Abstract
PURPOSE OF REVIEW: Compare noninfectious (part I) to infectious (part II) demineralization of bones and teeth. Evaluate similarities and differences in the expression of hard tissue degradation for the two most common chronic demineralization diseases: osteoporosis and dental caries. RECENTEntities:
Keywords: Cost-effective; Dental caries; Healthcare; Remineralization; Wellness; White spot lesion
Mesh:
Year: 2022 PMID: 35156182 PMCID: PMC8930953 DOI: 10.1007/s11914-022-00723-0
Source DB: PubMed Journal: Curr Osteoporos Rep ISSN: 1544-1873 Impact factor: 5.096
Fig. 1Based on the evidence reviewed, a schematic diagram of a plaque-coated enamel surface shows the principal stages of enamel pathophysiology relative to demineralization, remineralization and infectious dental caries. The superficial layer of plaque is aerobic, while the inner layer adjacent to the enamel surface is anaerobic. Enamel rods are separated by inter-rod substance (I) which has a more porous crystalline structure which allows percolation of fluoride to produce fluorapatite (FA). It is hypothesized that the inter-rod concentration of FA (cyan color gradient) is greatest near the oral surface and decreases with depth. Under anaerobic conditions, S. Mutans produces the lactic acid that facilitates active demineralization. Progressive caries preferentially demineralized the rods (HA prisms). From the left, black enamel rods depict stages of the pathophysiology: (1) intact rod, (2) active surface demineralization, (3) arrested lesion remineralized with HA, (4) arrested lesion remineralized with FA, and (5–7) active carious infection. See text for details
Fig. 2In a 2D section, a WSL is viewed from above as a white discoloration surrounded by intact enamel that reveals the subsurface location of a demineralized space >400μm in depth. It is hypothesized that mineralized inter-rod substance (asterisk) is less susceptible to demineralization because of natural FA formation via intercrystalline percolation. As the FA gradient decreased with depth, the active carious lesions progress laterally and coalesce to form a demineralization space. The lesion is invisible until it reaches a depth of ~400μm when light diffraction is adequate for the demineralized space to be visualized as a subsurface WSL. Evidence suggests the superficial remineralized porous enamel layer is a product of residual enamel not destroyed by the initial surface demineralization that is supplemented by remineralization via calcium (Ca++), PO4, and OH− moving toward the surface (black arrows). The source of the ions for remineralization is from HA destruction by the active carious lesion at the base of the demineralized space. See text for details