CRANIUM BIFIDUM PARIETAL FORAMINA |
Cranium bifidum
Cranium bifidum is a
defect in the fusion of the cranial bone. Cranium bifidum occurs in the
midline, and is most common in the occipital region. If meninges and CSF
herniate through the defect, it is called a meningocele. If meninges and
cerebral tissue protrude, it is called an encephalocele .
The most benign type - Persistent
parietal foramina or persistent wide fontanelle:
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The
parietal foramina can be transmitted as an autosomal dominant trait via a gene
located on the short arm of chromosome 11. The condition is sometimes called
"Caitlin marks," after the family for which it was described. Both
parietal foramina and a persistent anterior fontanelle are generally asymptomatic.
The intact skin and absent herniation of brain or meninges
differentiates it from a cephalocele.
Cranium bifidum such as
an encephalocele is much more serious.
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Encephaloceles
are thought to occur when the anterior neuropore fails to close during days
26-28 of gestation.
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Incidence
of this anomaly is 10% of the incidence of spina bifida cystica. In the United
States, approximately 80% of lesions are found on the dorsal surface of the
skull, with most near the occipital bone.
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In
contradistinction, most encephaloceles in Asia are ventral and involve the
frontal bone.
- In the Philippines and other Pacific countries, incidence of anterior encephaloceles that present as hypertelorism, obstructed nares, anterior skull masses, and cleft palate, among other presentations, is high.
In most lesions, the sac that has herniated through a midline skull defect is covered with epithelium.
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