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The Journal of Neurophysiology Vol. 81 No. 6 June 1999, pp. 2903-2913
Copyright ©1999 by the American Physiological Society
Department of Physiology and Pharmacology, State University of New York Health Science Center at Brooklyn, Brooklyn, New York 11203
Bianchi, Riccardo,
Steven R. Young, and
Robert K. S. Wong.
Group I mGluR Activation Causes Voltage-Dependent and
-Independent Ca2+ Rises in Hippocampal Pyramidal
Cells. J. Neurophysiol. 81: 2903-2913, 1999.
Group I mGluR activation causes voltage-dependent and -independent
Ca2+ rises in hippocampal pyramidal cells.
Application of the metabotropic glutamate receptor (mGluR) agonist
(1S,3R)-1-aminocyclopentane-1,3-dicarboxylic acid
(ACPD) or the selective group I mGluR agonist
(S)-3,5-dihydroxyphenylglycine (DHPG) depolarized both CA3
and CA1 pyramidal cells in guinea pig hippocampal slices. Simultaneous
recordings of voltage and intracellular Ca2+ levels
revealed that the depolarization was accompanied by a biphasic
elevation of intracellular Ca2+ concentration
([Ca2+]i): a transient calcium rise followed
by a delayed, sustained elevation. The transient
[Ca2+]i rise was independent of the membrane
potential and was blocked when caffeine was added to the perfusing
solution. The sustained [Ca2+]i rise appeared
when membrane depolarization reached threshold for voltage-gated
Ca2+ influx and was suppressed by membrane
hyperpolarization. The depolarization was associated with an increased
input resistance and persisted when either the transient or sustained
[Ca2+]i responses was blocked. mGluR-mediated
voltage and [Ca2+]i responses were blocked by
(+)-
-methyl-4-carboxyphenylglycine (MCPG) or
(S)-4-carboxy-3-hydroxyphenylglycine (4C3HPG). These data
suggest that in both CA3 and CA1 hippocampal cells, activation of group
I mGluRs produced a biphasic accumulation of
[Ca2+]i via two paths: a transient release
from intracellular stores, and subsequently, by influx through
voltage-gated Ca2+ channels. The concurrent mGluR-induced
membrane depolarization was not caused by the
[Ca2+]i rise.
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