A light scattering study on the ion permeabilities of dark-adapted bovine rod outer segment disk membranes.

The ion permeability properties of dark adapted bovine rod outer segment disk membranes were studied using light scattering to monitor osmotic responses of disks to various salts and ionophores. A preparation procedure is presented which provides very fresh rod outer segment material with mostly intact stacked disks, but with perforated plasma membrane. It is shown that in this preparation the disks (or rod sacs) are the only osmotically responding compartments and that these responses can be readily monitored by means of light-scattering techniques. The disk membrane is found under the conditions tested, to possess no measurable permeability to cations Na+, Ca2+, Mg2+ nor the the anions Cl-, Br-, NO3-, SO4(2-), H2PO4- and HPO4(2-). There is a considerable K+ permeability, which can be completely abolished by millimolar amounts of divalent cations. The proton permeability of the disk membrane is found to depend dramatically upon the preparation procedure and duration. The fresher the material used the lower is the proton permeability measured. In our freshest preparations, even after freeze-thawing in liquid nitrogen, the disks exhibit an H+ permeability which is so low that it cannot be measured with the techniques used in this study. Even in mitochondrial or chloroplast membmranes, in which proton gradients and therefore a low proton conductance play an essential role, such low proton permeabilities have not been found. This would suggest that proton gradients across the disk membrane could play an important role in the physiological function of the photoreceptor cell. In summary it can be said that the disk membrane, apparently more than any other natural membrane system studied so far, is capable of retaining ion gradients for extended periods of time.