Intercellular Ca(2+) waves induce temporally and spatially distinct intracellular Ca(2+) oscillations in glia.

Mechanically induced intercellular Ca(2+) waves propagated for approximately 300 microm in primary glial cultures. Following the wave propagation, 34% of the cells displayed Ca(2+) oscillations in a zone 60-120 microm from the stimulated cell. The initiation, frequency, and duration of these Ca(2+) oscillations were dependent on the cells' distance from the wave origin but were not dependent on the cell type nor on the magnitude of the Ca(2+) wave. When an individual cell propagated two sequential intercellular Ca(2+) waves originating from different sites, the characteristics of the Ca(2+) oscillations initiated by each wave were determined by the distance of the cell from the origin of each wave. Each Ca(2+) oscillation commonly occurred as an intracellular Ca(2+) wave that was initiated from a specific site within the cell. The position of the initiation site and the direction of the intracellular Ca(2+) wave were independent of the orientation of the initial intercellular Ca(2+) wave. Because initiation and frequency of Ca(2+) oscillations are dependent on the intracellular inositol trisphosphate concentration (IP(3)), we propose that the zone of cells displaying Ca(2+) oscillations is determined by an intercellular gradient of IP(3), established by the diffusion of IP(3) through gap junctions during the propagation of the intercellular Ca(2+) wave. Exposure to acetylcholine, a muscarinic agonist that initiates IP(3) production, shifted the zone of oscillating cells about 45 microm farther away from the origin of the mechanically induced wave. These findings indicate that a glial syncytium can resolve information provided by a local Ca(2+) wave into a distinct spatial and temporal pattern of Ca(2+) oscillations.