Takamatsu T, Wier W G
Department of Physiology, University of Maryland School of Medicine, Baltimore 21201.
FASEB J. 1990 Mar;4(5):1519-25. doi: 10.1096/fasebj.4.5.2307330.
A dual, digital, indo-1 fluorescence imaging system was used to obtain high-speed ratiometric images of [Ca2+]i waves in single voltage-clamped mammalian cardiac cells. The spatiotemporal origin of [Ca2+]i waves in depolarized cells was detected as the spontaneous appearance, over 100-300 ms, of domelike regions of elevated [Ca2+]i, approximately 20 microns in diameter and 300 nM at the center. Images of [Ca2+]i taken at 67-ms intervals during propagation of [Ca2+]i waves revealed that the [Ca2+]i wave front was 1) constant in shape, 2) spatially steep, typically rising from 500 to 1200 nM in about 10 microns, and 3) propagating at constant velocity, typically 100 microns/s at 22 degrees C. The observed spatial and temporal patterns of origin and propagation of [Ca2+]i waves are consistent with the hypothesis that [Ca2+]i waves arise from propagating Ca2(+)-induced release of Ca2+ mediated by diffusion of cytosolic Ca2+. The [Ca2+]i waves are smaller in peak magnitude and can occupy a larger fraction of the cell than thought previously on the basis of indirect observations.
使用双数字indo-1荧光成像系统获取单个电压钳制的哺乳动物心肌细胞中[Ca2+]i波的高速比率图像。去极化细胞中[Ca2+]i波的时空起源被检测为在100 - 300毫秒内自发出现的[Ca2+]i升高的穹顶状区域,直径约20微米,中心处为300 nM。在[Ca2+]i波传播期间以67毫秒间隔拍摄的[Ca2+]i图像显示,[Ca2+]i波前1)形状恒定,2)在空间上陡峭,通常在约10微米内从500 nM上升到1200 nM,3)以恒定速度传播,在22摄氏度时通常为100微米/秒。观察到的[Ca2+]i波起源和传播的时空模式与[Ca2+]i波由胞质Ca2+扩散介导的Ca2(+)-诱导的Ca2+释放传播产生的假设一致。[Ca2+]i波的峰值幅度较小,并且与之前基于间接观察所认为的相比,可以占据细胞的更大比例。