H. Tohda et al., TRANSMISSION ELECTRON-MICROSCOPY OF CEMENTUM CRYSTALS CORRELATED WITHCA AND F DISTRIBUTION IN NORMAL AND CARIOUS HUMAN ROOT SURFACES, Journal of dental research, 75(3), 1996, pp. 949-954
Root-surface caries, like enamel caries, develops as a subsurface type
of mineral loss. Very Little is known about the composition of the su
rface zone covering the body of the lesion, and the ultrastructure and
composition of carious cementum are not known. The aim of this study
was to correlate the ultrastructure and arrangement of the cementum cr
ystals with the distribution of fluoride and calcium in root cementum
from human teeth with sound, unexposed, or exposed root surfaces as we
ll as in early stages of root-surface caries. Microradiographically, u
nexposed specimens showed a relatively homogeneous mineral distributio
n contrasting with the formation of an apparently highly mineralized s
urface layer in exposed and, in particular, in carious cementum. The e
lectron-probe findings showed a substantial fluoride peak correspondin
g to the surface layers in carious tissues in particular, whereas the
calcium profile in the surface did not reflect the apparent increase i
n mineralization. A substantial increase in size of the cementum cryst
als was found in specimens with formation of the fluoride-rich, well-m
ineralized surface zone. The crystal lattice intervals when observed a
long the (001) plane showed a hydroxyapatite spacing. The findings ind
icated that a significant crystal growth can be achieved in human ceme
ntum concomitant with fluoride accumulation.