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Cytosolic Ca2+ signals are often organized in complex temporal and spatial patterns, even under conditions of sustained stimulation. In this review we discuss the mechanisms and physiological significance of this behavior in nonexcitable cells, in which the primary mechanism of Ca2+ mobilization is through (1,4,5)IP3-dependent Ca2+ release from intracellular stores. Oscillations of cytosolic free Ca2+ ([Ca2+]i) are a common form of temporal organization; in the spatial domain, these [Ca2+]i oscillations may take the form of [Ca2+]i waves that propagate throughout the cell or they may be restricted to specific subcellular regions. These patterns of Ca2+ signaling result from the limited range of cytoplasmic Ca2+ diffusion and the feedback regulation of the pathways responsible for Ca2+ mobilization. In addition, the spatial organization of [Ca2+]i changes appears to depend on the strategic distribution of Ca2+ stores within the cell. One type of [Ca2+]i oscillation is baseline spiking, in which discrete [Ca2+]i spikes occur with a frequency, but not amplitude, that is determined by agonist dose. Most current evidence favors a model in which baseline [Ca2+]i spiking results from the complex interplay between [Ca2+]i and (1,4,5)IP3 in regulating the gating of (1,4,5)IP3-sensitive intracellular Ca2+ channels. Sinusoidal [Ca2+]i oscillations represent a mechanistically distinct type of temporal organization, in which agonist dose regulates the amplitude but has no effect on oscillation frequency. Sinusoidal [Ca2+]i oscillations can be explained by a negative feedback effect of protein kinase C on the generation of (1,4,5)IP3 at the level of phospholipase C or its activating G-protein. The physiological significance of [Ca2+]i oscillations and waves is becoming more established with the observation of this behavior in intact tissues and by the recognition of Ca2+-dependent processes that are adapted to respond to frequency-modulated oscillatory [Ca2+]i signals. In some cells, these [Ca2+]i signals are targeted to control processes in limited cytoplasmic domains, and in other systems [Ca2+]i waves can be propagated through gap junctions to coordinate the function of multicellular systems.

Calcium signaling results from a complex interplay between activation and inactivation of intracellular and extracellular calcium permeable channels. This complexity is obvious from the pattern of calcium signals observed with modest, physiological concentrations of calcium-mobilizing agonists, which typically present as sequential regenerative discharges of stored calcium, a process referred to as calcium oscillations. In this review, we discuss recent advances in understanding the underlying mechanism of calcium oscillations through the power of mathematical modeling. We also summarize recent findings on the role of calcium entry through store-operated channels in sustaining calcium oscillations and in the mechanism by which calcium oscillations couple to downstream effectors.

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