A role for local calcium gradients upon hypoxic injury in human umbilical vein endothelial cells (HUVEC).

Upon hypoxic injury, bleb formation is an early event of cell damage observed in a variety of cell types. Although a rise in cytosolic free Ca2+ ([Ca2+]i) has been considered to be involved in this process, the exact relationship between these phenomena remains ill-defined. In order to examine the relationship between bleb formation, and [Ca2+]i or nuclear free Ca2+ ([Ca2+]n), we analyzed [Ca2+]i and [Ca2+]n in HUVEC during hypoxic injury using confocal laser scanning microscopy. [Ca2+]i and [Ca2+]n were measured using Fluo-3, and cell viability and mitochondrial membrane potential were assessed by the exclusion of propidium iodide (PI) and rhodamine 123, respectively. After the initiation of hypoxia, [Ca2+]i and [Ca2+]n rose gradually up to 15 min reaching peak values of 447 +/- 62 and 516 +/- 105 nM, respectively, which was accompanied by a decrease in rhodamine 123 fluorescence and an increase in PI-stained cells. Bleb formation was observed after [Ca2+]i and [Ca2+]n had reached their peak values and the number of blebs increased thereafter. Confocal z-sectioning images revealed a localized increase in [Ca2+]i at the bleb forming site and this localized elevation in [Ca2+]i was observed before bleb formation in the corresponding area. In conclusion, bleb formation induced by hypoxic stress appears to involve Ca(2+)-dependent reactions that are linked to a regional elevation of [Ca2+]i.