Key result
Frog muscle cells exhibited a more marked peak in Ca2+ release and Ca2+ sparks compared to rat cells, indicating a greater role for calcium-induced calcium release in amphibians.
The study proposes a revised model of excitation-contraction coupling where isoform 3 channels in amphibians are activated by CICR, a mechanism that is minor or absent in mammals.
May suggest RyR3 enhances Ca2+ release peak in amphibian muscle; leaves open its role in mammalian cardiac EC coupling.
Here we compare excitation-contraction coupling in single muscle cells of frogs and rats. Because amphibians have isoform 3 (or 3) of the ryanodine receptor/Ca2+ release channel, in addition to 1 (alpha), which is also present in the mammal, any extra feature present in the frog may in principle be attributed to isoform 3. Ca2+ release under voltage clamp depolarization has a peak and a steady phase in both taxonomic classes, but the peak is more marked in the frog, where the ratio of amplitudes of the two phases is voltage-dependent. This dependence is a hallmark of CICR. Confocal imaging identified Ca2+ sparks in the frog, but not in the voltage-clamped rat cells. Because Ca2+ sparks involve CICR both observations indicate that the contribution of CICR is minor or null in the mammal. The "couplon" model well accounts for observations in the frog, but assumes a structure that we now know to be valid only for the rat. A revised model is proposed, whereby the isoform 3 channels, located parajunctionally, are activated by CICR and contribute its characteristic global and local features. Several issues regarding the roles of different channels remain open to further study.
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Rı́os et al. (2004) studied this question. Frog muscle cells (isoform 3 and 1) vs. Rat muscle cells (isoform 1) was evaluated on Ca2+ release under voltage clamp depolarization and Ca2+ sparks. Frog muscle cells exhibited a more marked peak in Ca2+ release and Ca2+ sparks compared to rat cells, indicating a greater role for calcium-induced calcium release in amphibians.
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