The above results imply that VEGF-induced signaling in RMECs does not rely upon TRPV1 and TRPV4 channel activation. In follow-up experiments, Ca
2+ signaling studies were done to investigate this more directly. Confocal Ca
2+ imaging revealed considerable heterogeneity in VEGF-induced Ca
2+ responses among individual RMECs (
Fig. 4Ai). Although VEGF-induced Ca
2+ responses in most cells were initiated as spreading intracellular Ca
2+ waves that propagated throughout the cell (
Supplementary Videos S1–
S3), the amplitude and temporal profile of the Ca
2+ signals varied widely among different RMECs over time, even within the same field of view (
Fig. 4Ai). Some cells displayed a single Ca
2+ transient, while others exhibited more complex oscillatory Ca
2+ signaling events. In addition, following VEGF exposure, Ca
2+ returned to basal levels in some cells, while in others a sustained increase in Ca
2+ was observed. Using confocal Ca
2+ imaging, we observed no effects of CapZ or HC06 on VEGF-induced Ca
2+ signals in RMECs (
Figs. 4Ai,
4ii;
Supplementary Videos S1–
S3). Given the considerable variability in RMEC Ca
2+ responses to VEGF at the single cell level combined with limitations on the number of cells that could be analyzed by confocal Ca
2+ imaging, we undertook FLIPR-based high throughput Ca
2+ imaging experiments to confirm our findings in RMEC cell populations. At the cell population level (average Ca
2+ level across all cells in a well), VEGF induced a biphasic Ca
2+ response in RMECs, comprising of an initial transient rise in Ca
2+, followed by a smaller sustained Ca
2+ elevation that remained above basal Ca
2+ levels for the duration of the experiment (∼10 minutes;
Fig. 4Bi). Again, CapZ and HC06 had no effect on VEGF-induced Ca
2+ signaling in these experiments (
Figs. 4Bi,
4Bii). Taken together, these Ca
2+ data are consistent with the view that VEGF does not trigger TRPV1 and TRPV4 channel activation in RMECs.