Mitochondrial Ca(2+) uptake depends on the spatial and temporal profile of cytosolic Ca(2+) signals.

Using confocal imaging of Rhod-2-loaded HeLa cells, we examined the ability of mitochondria to sequester Ca(2+) signals arising from different sources. Mitochondrial Ca(2+) (Ca(2+)mit) uptake was stimulated by inositol 1,4,5-trisphosphate (InsP(3))-evoked Ca(2+) release, capacitative Ca(2+) entry, and Ca(2+) leaking from the endoplasmic reticulum. For each Ca(2+) source, the relationship between cytosolic Ca(2+) (Ca(2+)cyt) concentration and Ca(2+)mit was complex. With Ca(2+)cyt < 300 nm, a slow and persistent Ca(2+)mit uptake was observed. If Ca(2+)cyt increased above approximately 400 nm, Ca(2+)mit uptake accelerated sharply. For equivalent Ca(2+)cyt increases, the rate of Ca(2+)mit rise was greater with InsP(3)-evoked Ca(2+) signals than any other source. Spatial variation of the Ca(2+)mit response was observed within individual cells. Both the fraction of responsive mitochondria and the amplitude of the Ca(2+)mit response were graded in direct proportion to stimulus concentration. Trains of repetitive Ca(2+) oscillations did not maintain elevated Ca(2+)mit levels. Only low frequency Ca(2+) transients (<1/15 min) evoked repetitive Ca(2+)mit signals. Our data indicate that there is a lag between Ca(2+)cyt and Ca(2+)mit increases but that mitochondria will accumulate calcium when it is elevated over basal levels regardless of its source. Furthermore, in addition to the characteristics of Ca(2+) signals, Ca(2+) uniporter desensitization and proximity of mitochondria to InsP(3) receptors modulate mitochondrial Ca(2+) responses.