| Summary: | The end-product of epidermal differentiation is a stratified layer of corneocytes whose extracellular lipid bilayers provide a permeability barrier. It is generally accepted that the epidermis synthesizes most if not all of the lipids found in this tissue and that extra-epidermal tissues contribute very little to this lipid content. Moreover, the individual epidermal strata in which epidermal lipid biosynthesis occurs are not known. To address this question, we examined [3H]H2O incorporation into nonsaponifiable and saponifiable lipids in individual epidermal cell layers 3 hr after intraperitoneal injection into neonatal mice, and compared this to protein and DNA synthesis using intraperitoneal [3H]leucine and [3H]thymidine incorporation, respectively. Lipid biosynthesis was also assessed by [14C]acetate incorporation into lipid fractions in organ cultured skin and in epidermal subpopulations. The in vivo studies demonstrated that the biosynthetic activity of both saponifiable and nonsaponifiable lipids was comparable to, if not greater, in the stratum granulosum (SG) than in basal/spinous (SB + SS) layer, despite significantly lower levels of both protein and DNA synthesis in the SG. On a mass basis, the SG accounts for about four times the biosynthetic activity of the combined SB + SS layers. The lipid biosynthetic activity in vitro also was two- to fivefold higher in the SG, regardless of whether the epidermis was separated into individual cell layers before or after incubations with radiolabel. Moreover, this difference could not be ascribed to increased acetate pools or to elevated metabolism in the SG versus the SB + SS since the rates of CO2 production were much lower in the SG fraction. The increase in lipid biosynthesis in SG over SB + SS was greatest for phospholipids, followed by glycosphingolipids, and free sterols but was observed in almost all lipid classes. These studies show not only that mammalian epidermis is an active site of de novo lipid biosynthesis, but also that this activity remains high in the stratum granulosum, while other forms of metabolic activity are diminishing. These observations are consistent with the knowledge that lipids extruded from the stratum granulosum layer provide the hydrophobic permeability barrier, and further suggest that elevated synthetic activity in the stratum granulosum would allow rapid replenishment in the event that the barrier is damaged.
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