Balboni Armand L, Estenson Thomas L, Reidenberg Joy S, Bergemann Andrew D, Laitman Jeffrey T
Center for Anatomy and Functional Morphology, Mount Sinai School of Medicine, 1 Gustave L. Levy Place, New York, NY 10029, USA.
Anat Rec A Discov Mol Cell Evol Biol. 2005 Jan;282(1):38-48. doi: 10.1002/ar.a.20149.
The petro-occipital fissure (POF) lies within a critical interface of cranial growth and development in the posterior cranial fossa. The relationships between skeletal and soft tissues make this region especially important for examining biomechanical and basic biologic forces that may mold the cranial base and contribute to significant clinicopathologies associated with the structures located near the POF. Therefore, this study investigates the POF in adults in both preserved human cadavers and dried crania in order to determine if developmental changes can be observed and, if so, their value in age assessment as a model system for describing normal morphogenesis of the POF. This study demonstrates that tissue within the POF undergoes characteristic changes in ossification with age, the onset of which is considerably later than that of other synchondroses of the cranial base. Statistically, there is a moderate to strong correlation between age and stage of ossification within the POF. Further, male crania were observed to reach greater degrees of ossification at a younger age than female crania and that individual asymmetry in ossification of the tissue within the POF was not uncommon. An understanding of the basic temporal biological processes of the POF may yield insight into the development of clinicopathologies in this region of the cranial base.
岩枕裂(POF)位于颅后窝颅骨生长发育的关键界面内。骨骼与软组织之间的关系使得该区域对于研究可能塑造颅底并导致与岩枕裂附近结构相关的重大临床病理的生物力学和基本生物学力尤为重要。因此,本研究对保存的人类尸体和干燥颅骨中的成年人岩枕裂进行了研究,以确定是否能观察到发育变化,若能观察到,则确定其在年龄评估中的价值,作为描述岩枕裂正常形态发生的模型系统。本研究表明,岩枕裂内的组织会随着年龄增长发生特征性的骨化变化,其开始时间比颅底其他软骨结合处要晚得多。从统计学角度来看,年龄与岩枕裂内的骨化阶段之间存在中度至强相关性。此外,观察到男性颅骨比女性颅骨在更年轻的时候达到更高程度的骨化,并且岩枕裂内组织骨化的个体不对称并不罕见。对岩枕裂基本时间生物学过程的理解可能有助于深入了解颅底该区域临床病理的发展。