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Neuroradiology Case of the WeekCase 302 Scott Rudzinski, Virendra Kumar, MD, and P-L Westesson, MD, PhD, DDSClinical Presentation: The patient is a 9-year-old female with known osteogenesis imperfecta presenting with back pain and progressing scoliosis. Imaging Findings: The T5, T6 and T8 vertebral bodies show slight decrease in height, approximately 30%. No evidence of any marrow edema seen. These are suggestive of old compression. The T7 vertebral body shows slight decrease in height with focal marrow edema seen as hypointense signals on T1 which appears hyperintense on T2 and fat suppressed images and shows mild enhancement from the post-contrast images especially in the upper part. This is suggestive of acute nature. There is evidence of scoliosis noted in the midthoracic region with slight convexity towards the right.
Diagnosis: Vertebral compression fractures in osteogenesis imperfecta Discussion: Osteogenesis imperfecta (OI) is an inherited disorder of connective tissue that manifests as osseous fragility, blue sclera, hearing loss, hypermobile joints, and easy bruisability. OI is caused by mutations in the genes that codify for type I procollagen, ultimately producing defective type I collagen. Type I collagen, which is found in the bones, organ capsules, fascia, cornea, sclera, tendons, meninges and dermis, constitutes 30% of the human body by weight. The prevalence of OI is estimated to be 1 per 20,000 live births, but the mild form is underdiagnosed, and the actual prevalence may be higher than this. Patients with OI may present at anytime during their life from in utero to adulthood, depending on severity of disease. The most widely used classification system developed by Sillence is as follows:
Diagnosis is aided by collagen synthesis analysis and DNA mutation analysis after clinical presentation and radiography raises suspicion. There is decreased bone mineral density in OI, but degree varies greatly. Histologically the width of the cortex and the volume of cancellous bone are decreased in all types of OI. References:
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