Glutamate-induced calcium signaling in astrocytes

Astrocytes respond to the excitatory neurotransmitter glutamate with dynamic spatio-temporal changes in intracellular calcium Ca²⁺]_i. Although they share a common wave-like appearance, the different Ca²⁺]_i changes--an initial spike, sustained elevation, oscillatory intracellular waves, and regenerative intercellular waves--are actually separate and distinct phenomena. These separate components of the astrocytic Ca²⁺ response appear to be generated by two different signal transduction pathways. The metabotropic response evokes an initial spatial Ca²⁺ spike that can propagate rapidly from cell to cell and appears to involve IP₃. The metabotropic response can also produce oscillatory intracellular waves of various amplitudes and frequencies that propagate within cells and are sustained only in the presence of external Ca²⁺. The ionotropic response, however, evokes a sustained elevation in Ca²⁺]_i associated with receptor-mediated Na⁺ and Ca²⁺ influx, depolarization, and voltage-dependent Ca²⁺ influx. In addition, the ionotropic response can lead to regenerative intercellular waves that propagate smoothly and nondecrementally from cell to cell, possibly involving Na⁺/Ca²⁺ exchange. All these astrocytic Ca²⁺]_i changes tend to appear wave-like, traveling from region to region as a transient rise in Ca²⁺]_i. Nevertheless, as our understanding of the cellular events that underlie these Ca²⁺]_i changes grows, it becomes increasingly clear that glutamate-induced Ca²⁺ signaling is a composite of separate and distinct phenomena, which may be distinguished not based on appearance alone, but rather on their underlying mechanisms. © 1994 Wiley-Liss, Inc.