Role of Ca2+ Feedback on Single Cell Inositol 1,4,5-Trisphosphate Oscillations Mediated by G-protein-coupled Receptors*

The dynamics of inositol 1,4,5-trisphosphate (Ins (1,4,5)P3) production during periods of G-protein-coupled receptor-mediated Ca2+ oscillations have been investigated using the pleckstrin homology (PH) domain of phospholipase C (PLC) δ1 tagged with enhanced green fluorescent protein (eGFP-PHPLCδ1). Activation of noradrenergic α1B and muscarinic M3 receptors recombinantly expressed in the same Chinese hamster ovary cell indicates that Ca2+ responses to these G-protein-coupled receptors are stimulus strength-dependent. Thus, activation of α1B receptors produced transient base-line Ca2+ oscillations, sinusoidal Ca2+ oscillations, and then a steady-state plateau level of Ca2+ as the level of agonist stimulation increased. Activation of M3 receptors, which have a higher coupling efficiency than α1B receptors, produced a sustained increase in intracellular Ca2+ even at low levels of agonist stimulation. Confocal imaging of eGFP-PHPLCδ1 visualized periodic increases in Ins(1,4,5)P3 production underlying the base-line Ca2+ oscillations. Ins(1,4,5)P3 oscillations were blocked by thapsigargin but not by protein kinase C down-regulation. The net effect of increasing intracellular Ca2+ was stimulatory to Ins(1,4,5)P3 production, and dual imaging experiments indicated that receptor-mediated Ins(1,4,5)P3 production was sensitive to changes in intracellular Ca2+ between basal and ∼200 nM. Together, these data suggest that α1B receptor-mediated Ins(1,4,5)P3 oscillations result from a positive feedback effect of Ca2+ onto phospholipase C. The mechanisms underlying α1B receptor-mediated Ca2+ responses are therefore different from those for the metabotropic glutamate receptor 5a, where Ins(1,4,5)P3 oscillations are the primary driving force for oscillatory Ca2+ responses (Nash, M. S., Young, K. W., Challiss, R. A. J., and Nahorski, S. R. (2001) Nature 413, 381–382). For α1B receptors the Ca2+-dependent Ins(1,4,5)P3 production may serve to augment the existing regenerative Ca2+-induced Ca2+-release process; however, the sensitivity to Ca2+ feedback is such that only transient base-line Ca2+ spikes may be capable of causing Ins(1,4,5)P3 oscillations.