Orthokeratosis
Orthokeratosis is a term used in dermatology to describe a condition where the stratum corneum layer of the skin is composed of fully differentiated keratinocytes.
Overview[edit | edit source]
Orthokeratosis is characterized by the presence of anucleate squamous cells in the stratum corneum. This is a normal finding in the epidermis of the skin, but can also be seen in certain pathological conditions such as psoriasis, lichen planus, and actinic keratosis.
Pathology[edit | edit source]
In orthokeratosis, the stratum corneum is thickened due to the accumulation of anucleate squamous cells. This is in contrast to parakeratosis, where the stratum corneum is composed of nucleated squamous cells. The presence of orthokeratosis can be confirmed through a skin biopsy and subsequent histopathological examination.
Clinical Significance[edit | edit source]
Orthokeratosis is often associated with a variety of skin conditions. In psoriasis, it is seen as part of the characteristic "psoriasiform" epidermal hyperplasia. In lichen planus, orthokeratosis occurs in areas of epidermal thickening known as "Wickham's striae". In actinic keratosis, orthokeratosis is seen in areas of sun-damaged skin.
See Also[edit | edit source]
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