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. 2000 Oct;79(4):1800–1820. doi: 10.1016/S0006-3495(00)76431-9

Development and dissipation of Ca(2+) gradients in adrenal chromaffin cells.

F D Marengo 1, J R Monck 1
PMCID: PMC1301073  PMID: 11023887

Abstract

We used pulsed laser imaging to measure the development and dissipation of Ca(2+) gradients evoked by the activation of voltage-sensitive Ca(2+) channels in adrenal chromaffin cells. Ca(2+) gradients appeared rapidly (<5 ms) upon membrane depolarization and dissipated over several hundred milliseconds after membrane repolarization. Dissipation occurred with an initial fast phase, as the steep gradient near the membrane collapsed, and a slower phase as the remaining shallow gradient dispersed. Inhibition of active Ca(2+) uptake by the endoplasmic reticulum (thapsigargin) and mitochondria (carbonylcyanide p-trifluoro-methoxyphenylhydrazone/oligomycin) had no effect on the size of Ca(2+) changes or the rate of gradient dissipation, suggesting that passive endogenous Ca(2+) buffers are responsible for the slow Ca(2+) redistribution. We used a radial diffusion model incorporating Ca(2+) diffusion and binding to intracellular Ca(2+) buffers to simulate Ca(2+) gradients. We included a 3D optical sectioning model, simulating the effects of out-of-focus light, to allow comparison with the measured gradients. Introduction of a high-capacity immobile Ca(2+) buffer, with a buffer capacity on the order of 1000 and appropriate affinity and kinetics, approximated the size of the Ca(2+) increases and rate of dissipation of the measured gradients. Finally, simulations without exogenous buffer suggest that the Ca(2+) signal due to Ca(2+) channel activation is restricted by the endogenous buffer to a space less than 1 microm from the cell membrane.

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Selected References

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