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Root Surface Anomalies INTERMEDIATE BIFURCATIONAL RIDGE

Оглавление

Intermediate bifurcational ridge (IBR) is defined as a distinct ridge running across the bifurcation in a mesiodistal direction.10 It originates from the mesial surface of the distal root at about 2 mm from the height of the furcation area and ends high up on the distal surface of the mesial root by merging within the root concavity.10 Histologic evaluation of IBRs has shown that these developmental anomalies are formed mostly by dentin but also contained cementum.10

Everett et al reported that among 328 extracted mandibular first molars, the prevalence of IBRs was 73%.10 This finding was confirmed by two other studies that revealed a presence of IBRs in 70% and 76.8% of extracted first molars.68,124 Moreover, Hou and Tsai found that IBRs are highly associated with CEPs (63.2%) and Class III furcations (25.3%).55

Periodontics

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