Unicameral bone cyst
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Unicameral bone cysts (UBC), also known as simple bone cysts, are common benign non-neoplastic lucent bony lesions that are seen mainly in childhood and typically remain asymptomatic. They account for the S (simple bone cyst) in FEGNOMASHIC, the commonly used mnemonic for lytic bone lesions.
They are usually found in children in the 1st and 2nd decades (65% in teenagers) and are more common in males (M:F ~ 2-3:1) 2,6. Active unicameral bone cysts occur most frequently between the ages of 1 and 10 years.
These lesions are usually asymptomatic and found incidentally, although pain, swelling and stiffness of the adjacent joint also occur. The most frequent presentation is due to complications by pathological fracture. 1,2,6.
When uncomplicated by fracture the cysts contain clear serosanguineous fluid surrounded by a thin fibrous membranous lining. It is thought to arise as a defect during bone growth that fills with fluid, resulting in the expansion and thinning of the overlying bone.
During the active phase, the cyst remains adjacent to the growth plate. As the lesion becomes inactive it migrates away from the growth plate (normal bone is formed between it and the growth plate) and it gradually resolves 3,5.
They are typically intramedullary and active cysts are found in the metaphysis of long bones, abutting the growth plate 1. Locations include 1,2,5:
- proximal humerus: most common 50-60%
- proximal femur: 30%
- other long bones
- occurrence elsewhere is relatively uncommon, and usually occurs in adults
As bone growth progresses the cyst loses its connection to the physis migrating into the diaphysis and subsequently healing. UBCs can be rarely seen in adults in unusual locations such as in the talus, calcaneus, or the iliac wing.
Unicameral bone cysts are well defined geographic lucent lesions with a narrow zone of transition, mostly seen in skeletally immature patients, which are centrally located and show a thin sclerotic margin in the majority of cases with no periosteal reaction or soft tissue component. They sometimes expand the bone with thinning of the endosteum without any breach of the cortex unless there is a pathologic fracture. Prominent ridges of bone can appear as pseudotrabeculation on x-ray but in fact, UBC is usually unilocular. Rarely, they are truly multi-loculated 3.
If there is a fracture through this lesion a dependent bony fragment may be seen, and this is known as the fallen fragment sign.
CT and MRI
CT and MRI add little to the diagnosis, however, can be helpful in eliminating other entities that can potentially mimic a simple bone cyst (see differential diagnosis below).
MR signal characteristics for an uncomplicated lesion include:
- T1: low signal
- T2: high signal
Usually, there are no fluid-fluid levels unless there has been a complication with hemorrhage.
Unicameral bone cyst on bone scintigraphy tends to appear as foci of photopenia (cold spot). This is referred to as the doughnut sign which results in increased uptake peripherally and a photopenic center. However, a pathological fracture would cause an increased radioisotope activity.
Treatment and prognosis
Intervention is usually not required for an asymptomatic lesion. If large and threatening to fracture, or causing deformity then an intralesional steroid injection can be performed 3-5. If fractured the bone usually heals normally 5. In some instances, surgery with curettage and bone grafting is required.
History and etymology
Unicameral bone cysts were initially described by the German pathologist Rudolf Virchow in 1891 8,9.
General imaging differential considerations include:
- intraosseous lipoma
- fibrous dysplasia
- eosinophilic granuloma (EG)
- giant cell tumor of bone: usually older, extending to the articular surface
- non ossifying fibroma: eccentric, cortical base
- haemophilic pseudotumor (intraosseous)
- aneurysmal bone cyst (ABC): usually eccentric
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