A massive calcification and ossification of the transverse sinus and the neighbouring dura mimicking meningioma
© Xu et al.; licensee BioMed Central Ltd. 2013
Received: 30 April 2013
Accepted: 9 October 2013
Published: 11 October 2013
Although small calcifications of the dura and the transverse sinus occur frequently, large, single intracranial calcifications originating from the transverse sinus and the neighbouring dura are rare.
A 47-year-old man was admitted to the hospital for a right occipital headache that had persisted for two weeks. There was no neurological deficit. Normal skull X-ray and computed tomography (CT) scans revealed an irregular, calcified, intracranial lesion of approximately 4.4 × 4.0 × 2.5 cm in volume in the right occipital region. Via surgery, a bone-hard, poorly vascularised, pink mass originating from the right transverse sinus and the convex dura of the right cerebellar hemisphere, as well as the cerebellar tentorium, was completely removed. Pathological examination yielded a diagnosis of fibrous connective tissue with hyaline degeneration, calcification and ossification with no indication of neoplasia or inflammation.
We report a rare case of massive calcification and ossification of the transverse sinus and the neighbouring dura mimicking meningioma. Degenerative calcification and ossification may serve as a rare differential diagnosis of diseases, such as meningiomas, in the transverse sinus and the neighbouring dura.
KeywordsIntracranial calcification Intracranial ossification Transverse sinus Dura
Intracranial calcification may occur physiologically or pathologically and may be observed in asymptomatic individuals. Clinical assessment and laboratory investigations are required to determine whether these changes are physiological, idiopathic, neoplastic, inflammatory, traumatic, caused by metabolic disease, or manifestations of a generalised disease, such as hyperparathyroidism, vitamin D toxicity, Aicardi-Goutières syndrome, cerebroretinal microangiopathy with calcifications, COL4A1-related disease, Degos disease, Krabbe disease, Alexander disease, mitochondrial disease, tetrasomy 15, Hutchinson-Gilford progeria syndrome or chronic renal failure [1–3].
Certain intracranial tumours, especially oligodendrogliomas and craniopharyngiomas, tend to undergo calcification. Tumour calcifications were observed in approximately 83% of craniopharyngiomas  and 40% of intracranial oligodendrogliomas . Approximately 22 to 62% of benign meningiomas were reported to contain calcification, while nearly all malignant meningiomas lacked any calcification [6–8]. Metaplastic meningioma is a rare subtype of benign meningiomas, which encompass a broad range of tumour subtypes depending on the mesenchymal differentiation involved. Myxoid, osseous, cartilaginous, lipomatous, and xanthomatous subtypes are classified in this group . Tang et al.  reported clinicopathological analysis of 15 metaplastic meningiomas, of which 12 tumours were homogenously enhanced and three tumours were heterogeneously enhanced based on contrast MR imaging. The primary location was the dural tissue in approximately 6% of intracranial chondrosarcomas, but radiological examinations principally revealed bone destruction and variable calcification, as well as involvement of neuronal and vascular structures .
Calcifications can also develop in chronic subdural haematomas . Dural arteriovenous fistulas with cortical venous reflux may present with calcification in the cortico-medullary junction at the bottom of the cerebral sulci, resulting from chronic venous congestion with impaired perfusion of the involved parenchyma . Cases of idiopathic intracranial dural and optic nerve/sheath calcifications have also been reported .
Intracranial physiological calcifications are a common occurrence, found in approximately 35.2% of the adult population . The majority of physiological calcifications appeared in the pineal/habenular region (71%-80%) [15, 16], the choroid plexus region (12%-66.2%) [15, 16], or the petroclinoid ligament region (8%)  or as tentorium cerebella, sagittal sinus, or falx cerebri calcifications (7.3%) , vascular calcifications (6.6%) , basal ganglia calcifications (0.8%) , or lens and other non-defined calcifications (0.9%) . Calcification in the choroid plexus region and the petroclinoid ligament region is typically bilateral . All types of calcifications are increased in older patients, except for lens and other non-defined calcifications. Intracranial physiological calcifications are unaccompanied by any evidence of disease and have no demonstrable pathologic cause. They are often due to calcium or, in certain cases, iron, deposition in the blood vessels of different structures of the brain. CT scan is the most sensitive means of detecting these calcifications . Picht et al.  reported a giant intracerebral choroid plexus calcification, measuring approximately 3 × 3 × 4 cm in the right temporal region, which might have had a physiological cause, such as dystrophic calcium salt deposition. In this study, we report on the case of a 47-year-old male patient with a calcified intracranial mass approximately 4.4 × 4.0 × 2.5 cm in volume originating from the transverse sinus and the neighbouring dura. Histological examination demonstrated degenerative alterations, including calcification and ossification, with no evidence of neoplasia or inflammation. The potential mechanism is discussed.
A 47-year-old man was admitted to our hospital in September 2011 with complaints of intermittent episodes of mild to moderate headache in the right occipital region without nausea or vomiting for two weeks. The neurological examination was normal. The past history revealed hypertension for five years, which was well controlled using oral antihypertensive drugs, and there were no associated systemic complications, such as increased intracranial pressure, intracranial infection or hypercalcaemia.
Magnetic resonance (MR) examination was performed using a 1.5-T imager. T1- and T2-weighted images were obtained before and after administration of gadopentetate dimeglumine. A blur nodule was delineated in the right transverse sinus and cerebellar tentorium, protruding into the posterior cranial fossa and compressing the right cerebellar hemisphere. The lesion showed mixed low and equal signal intensity on T1-weighted images, and mixed low and high signal intensity on T2-weighted images. The lesion displayed irregular linear contrast enhancement only in its dural periphery. A magnetic resonance venogram (MRV) revealed that there was no detectable venous flow in the right transverse sinus and the right sigmoid sinus (Figure 1).
Normal levels of parathormone, serum calcium and phosphorus excluded diagnoses of hypercalcaemia and hypoparathyroidism.
The clinical course after surgery was uneventful. No neurological deficit developed. Following discharge, the patient followed up regularly. His preoperative right occipital headache subsided completely.
The cause of the calcification and ossification of the transverse sinus and neighbouring dura in the present case is not clear. The presence of a calcified meningioma was suspected preoperatively, but the pathologic examination provided no indication of neoplasia or inflammation. Additionally, it did not support calcification of the transverse sinus thrombosis, which characteristically would be located within the sinus . The probable cause might have been physiological degeneration, as the pathologic examination of the mass only revealed degenerative alterations, including the fibrous connective tissue with hyaline degeneration, calcification and ossification. Hyperblastosis of the neighbouring cerebellar glial tissue might have been caused by a response induced by the long-term compression of the mass. As there was total occlusion of right transverse sinus and the patient did not exhibit increased intracranial pressure, the degenerative course should have been long-term enough for the compensation of intracranial venous drainage via the collateral circulation. The identification of the calcified intracranial mass was in fact incidental to the examination pertaining to the patient’s intermittent episodes of mild to moderate headache in the right occipital region, as his headache had only persisted for two weeks. Degenerative calcification and ossification cannot develop in such a short period. The cause of the postoperative disappearance of his headache might have been partially psychological because he no longer had any anxiety regarding the intracranial mass. Nevertheless, if the diagnosis of degenerative calcification and ossification could be considered preoperatively, conservative observation might have been an option. To the best of our knowledge, this is the first description of a case of massive degenerative calcification and ossification originating from the transverse sinus and the neighbouring dura mimicking meningioma.
We report a rare case of massive calcification and ossification of the transverse sinus and neighbouring dura mimicking meningioma. Degenerative calcification and ossification may serve as a rare differential diagnosis for diseases, such as meningiomas, in the transverse sinus and the neighbouring dura.
Written informed consent was obtained from the patient for publication of this case report and any accompanying images. A copy of the written consent is available for review by the Editor-in-Chief of this journal.
Magnetic resonance venogram.
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