The ordered and distinct structural zones within the RPE basal labyrinth suggest that the structure regulates more than simply surface area. Although the relative contributions of paracellular (through the cell–cell junctions) and transcellular water transport remain a subject of debate, at least some water transport is transcellular and so must pass across the basal labyrinth. According to the osmotic coupling theory water transport across the epithelial cell basal membrane can be explained by salt being pumped across the membrane into a ‘space', creating an osmotic difference, and water thus follows by osmosis. Clearly the complex structure of the basal labyrinth generates a space with different geometries in the different structural zones. Diamond and Bossart
29 explicitly modeled how the space, visualized as a long, thin tube with solutes transported into the closed end, could generate a standing osmotic gradient, the shape of which would depend on the length of the ‘tube', its radius, the water permeability, and the rate and site of solute transport. We have shown that the radius and length of the paracellular space between basal infoldings (the ‘tube') varies from the cisternal to ribbon to stacked zones, becoming progressively narrower and longer (
Fig. 6). Furthermore, we have shown that the endoplasmic reticulum and mitochondria are restricted to the cisternal zone, which equates to the closed end of the tube in the Diamond and Bossart model, and so capacitive calcium flux (and the chloride transport that might result from it due to calcium-dependent chloride channels) may be restricted to this region. The short distance (<30 nm) between the outer mitochondrial membrane and the plasma membrane of the cisternal basal infoldings indicate the existence of membrane contact sites.
30 Interestingly, similar mitochondrial to plasma membrane contact sites have been described in yeast,
31 but have not been previously characterized by electron microscopy in mammalian cells. These would likely assist in anchoring the mitochondria into position against the plasma membrane, facilitating processes such as store-operate calcium entry (SOCE) from the paracellular space.
32 Why does the basal labyrinth need to be so complex, rather than a simple array of parallel ‘tubes'? One possibility may be to be able to rapidly change the geometry in order to respond to changes in isotonicity (
Fig. 6), which are necessary to maintain RPE cell volume. The variation that we observed in paracellular space between very thin (closed) and wider (open) even within the same specimen, could represent a response to subtle changes in osmolarity. Consistently, we saw major changes in basal labyrinth structure in whole-eye globes experimentally exposed to osmotic challenge (
Fig. 6). Loss of the ability to rapidly respond to osmotic changes with age and disease could lead to changes in RPE cell volume eventually leading to RPE cell death. An important area for future study will be to link the changes that we have observed with age and in response to osmotic challenge to functional changes in osmotic pressure and ion transport across the basal labyrinth.