Introduction

We present a 20-year-old boy with pneumocephalus after direct blow to the left occiput and review the literature briefly. Clivus is an uncommon site for skull base fracture. Population based studies show that clivus fracture occurs most commonly in pedestrians involved in traffic accidents.  The extent and type of fracture depends on the trajectory and magnitude of the trauma [1-8]. Longitudinal and oblique fractures are suggested as the more devastating types in different studies [2]. There was an oblique clivus fracture (CVF) with sphenooccipital dehiscence but the patient had no neurological deficit. We would like to suggest this type of skull base fracture to be included in the classification skull base fractures.

Case report

A 20-year-old man was brought to our level 1 trauma center with severe headache after a direct blow to the head on the left side of the occiput. He was conscious, oriented and had a good memory of the moment of the injury. We found a superficial laceration of the scalp on the left occiput and no rhinorrhea or ottrrhagia. The neurological examination was completely normal, and the patient had fluent, clear speech. A head CT scan revealed diffuse pneumocephalous with the pattern of the gyri. Paranasal sinuses were filled with cerebro-spinal fluid (Figure 1). There was a linear skull base fracture, extending from the left petrous bone, crossing the sphenooccipital synchondrosis and extending to the roof of orbit on the right side (Figure 1). The fracture line traversed the sphenoid sinus, the right anterior clinoid process and the right sphenoid wing also. No insult to the internal carotid artery (ICA) or vertebral and basilar arteries were detected in CTV.  Patient was admitted to the intensive care unit and treated with complete bed rest and continuous high concentration oxygen mask. The pneumocephalus decreased remarkably and patient was transferred to the ward after three days.  He was discharged home after seven days and was asymptomatic when last visited after 3 months. Appropriate informed consent is taken from the patient and is present in the file.

Fig. 1 White arrow in the middle showing the horizontal and vertical fracture lines and dehiscence of the clivus with axial subluxation to the left (a). Fracture line is demarcated using white arrow starting from the base of the right mastoid bone coming to the lateral and mid clivus (b). Arrows showing fractured left anterior clinoid process in figures (c). Extension of the fracture line to the left orbital plate and sphenoid wing (a, b). 3D reconstruction of the skull base region shows whole the fracture line shaded to highlight the CVF all along the skull base (d).

Discussion

Clivus is a thick part of the occipital bone that forms a gradual sloping process at the anterior most portion of the basilar occipital bone at its junction with the sphenoid bone via ‘spheno-occipital synchondrosis’ and the petrosal part of the temporal bone on each side [1]. The cartilaginous connection between the clivus and the body of sphenoid is ossified in the adolescence up to the age of 15 and skull is more prone for clivus dehiscence in childhood [5,6]. Our case was a 20-year-old man.

Fracture of the clivus is a rare event and is seen only in 0.21% - 0.56% of traumatic head injuries. The trauma is usually a blunt one with compressive nature. The compressive pattern of the trajectory of the trauma or vector of the force is of main importance in development of CVF in most of the reported cases [4]. In our patient the fracture occurred due to a direct blunt trauma to the left Asterion. The vector of the force created an oblique line of fracture that extended from the left petrous bone to the sphenooccipital synchondrosis, then to the right anterior clinoid process and crossed to the roof of the right orbit (Figures 1A, B, C, D). The sphenoid and the ethmoid sinuses were also smashed by the vector of force passing through the skull base in this case.

 Corradino et al., [2] 1990, classified clival fractures to longitudinal, horizontal and oblique shapes. Wrinckler-Schwarts A et al., [8] subdivided the fracture types according to the extent of bonny damage. Neither of the authors’ classifications nor the existing literature can describe the CVFs in a convincing way for each case. That is one of the main reasons to present this case of ours with diastatic/displaced CVF as a very rare event and as a sample to be included in further multicentral studies for classification of CVFs.

The reported morbidity and mortality rate have been between 24% and 31% in different studies [3,4]. One of the theories to explain the death at the scene of traumatic brain injuries (TBI) after clivus fracture is that, the basilar artery may be crushed by the separated bone fragments [1]. Direct or indirect trauma to the cranial nerves can explain the neurological deficits usually occurring in such cases. In our case, a unilateral blunt trauma which was not severe enough to cause brain parenchymal damage, lead into this rare type of sphenooccipital dehiscence without any morbidity. We highlighted the main take away message of this case which can be important for neuro-trauma surgeons and radiologists.

In conclusion, a rare case of CVF is presented to be enrolled in the classification list of the clival fractures.

Declarations:

The ethics committee of Sina Hospital approved resenting the data of the file of the patient in this report.

No grant, financial support or funding for any of the authors.

Appropriate informed consent is taken from the patient and is present in the file.

All the authors contributed in preparation of the manuscript equally.

Conflict of Interest: The authors declare that they have no competing interests. 

Table 1. Showing the list of other cases of skull base fracture with sufficient information to be compared to our case.