Lateral midfoot pain

Computed tomography of the patient’s left ankle demonstrated two areas of ossification separated by a 2-cm gap along the course of the peroneus longus tendon. Two proximal ossicles were located distal to the peroneal tubercle of the calcaneus and one was inferior to the cuboid. The most proximal ossicle was completely corticated, but the two lower ossicles represented halves of one large ossicle with absence of cortex on the exposed ends of the bone. There was also fluid density within the tendon and edema of the subcutaneous fat adjacent to the common peroneal tendon sheath. This is analogous to the split ossicle sign that may be seen on radiographs. AnMRI examination performed 2 days later revealed a complete rupture of the peroneus longus tendon. Attached to each end of the tendon was a portion of the distal ossicle of a bipartite or fused multipartite os peroneum. The patient was taken to the operating room for repair of the torn tendon 13 days later. Surgery confirmed a large amount of fluid in the sheath at the tendinous rupture and two osseous fragments separated by intervening fibrosis. The os peroneum is usually located at or distal to the calcaneocuboid joint, or within the cuboid tunnel of the cuboid, but can occasionally articulate with the distal lateral calcaneus [1]. It is stabilized by four connective tissue bands that extend to the cuboid, fifth metatarsal base, plantar fascia, and the peroneus brevis tendon [1]. The incidence in the population varies from 5 % to 20 % but the incidence of multipartite ossicles is less clear, since it appears to increase with age owing to the formation of lamellar bone surrounding areas of metaplastic ossification [2]. Diagnosing a fractured os peroneum may be a challenge radiographically. One reason for this is that the fracture can appear either as a division in a solitary ossicle or as diastasis through a multipartite ossicle [3–7]. If the rupture of the tendon occurs away from the ossicle, there can be migration of the ossicle without its fragmentation [8, 9]. In this situation, prior radiographs can be useful since migration may not be evident if only minimal retraction is present. If a previously solitary ossicle appears multipartite at follow-up, or if a multipartite ossicle demonstrates diastasis between fragments, the diagnosis can be rendered with confidence. Irregularity of the margins of the fragments without sclerosis should raise the index of suspicion for an acute fracture [10]. Ultimately, MRI remains the best modality for further evaluating patients with persistent focal pain from a non-displaced fracture, although bone scintigraphy is also useful when MRI is not available. The peroneus longus muscle is responsible for pronation, eversion, and plantar flexion of the foot [8, 9]. The peroneus longus tendon is most susceptible to injury at the cuboid notch owing to a change in its course as the tendon heads toward the first metatarsal base [11, 12]. There have been several mechanisms proposed to explain the occurrence of a fracture of an os peroneum. The two most commonly proposed mechanisms are either direct trauma to the midfoot or violent dorsiflexion of the ankle and foot [7, 8, 10]. A less common mechanism is eversion against a supinated foot and ankle [6]. The case presentation can be found at doi: 10.1007/s00256-014-1933-3