Occipitocervical dislocation (or occipitoatlantal dislocation) results from the disruption of the joint between the skull and the spine. Usually, this only results from high energy injuries such as motor vehicle accidents. It is more common in children, and children are more likely to survive such an injury. It has an extremely high mortality – as much as 80% or more.
The skull articulates with the spine by both bony and ligamentous structures. At the base of the skull are two regions of thickened bone known as the occipital condyles. The condyles are seated on the lateral masses of the C1 vertebra forming the bony componentof the craniovertebral junction. C1 is also known as the atlas. The principal ligamentous contribution to the occipitocervical articulation is from the alar ligaments. These originate from the basion and insert on the odontoid process of C2.
A high index of suspicion for occipitoatlantal dislocation should be maintained in all instances of high energy injuries. Radiographic findings are not always obvious, and therefore special attention should always be payed to the OC junction. Careful inspection of the anatomic relationships is mandatory. Subluxation of the occipital condyles may be identified on sagittal CT reconstructions. If the alignment is not correct or the joint space is increased, the joint should be presumed unstable. Other indices that should be checked in suspicious cases are the BDI and the BAI.
If there is any malalignment, patients need to be managed with extreme caution. OC disassociations can be extremely unstable. The majority of patients with OC dislocations present with incomplete spinal cord injuries, although they may also have a normal neurologic examination. Complete injuries are presumed to be universally fatal.
Children with minimal displacement may be considered for treatment in a halo-vest. All other patients should be managed with occipitocervical fusion.