Background and Purpose
The TRPV4 ion channels are Ca
2+
permeable, non‐selective cation channels that mediate large, but highly localized, Ca
2+
signals in the endothelium. The mechanisms that permit highly localized Ca
2+
changes to evoke cell‐wide activity are incompletely understood. Here, we tested the hypothesis that TRPV4‐mediated Ca
2+
influx activates Ca
2+
release from internal Ca
2+
stores to generate widespread effects.
Experimental Approach
Ca
2+
signals in large numbers (~100) of endothelial cells in intact arteries were imaged and analysed separately.
Key Results
Responses to the TRPV4 channel agonist GSK1016790A were heterogeneous across the endothelium. In activated cells, Ca
2+
responses comprised localized Ca
2+
changes leading to slow, persistent, global increases in Ca
2+
followed by large propagating Ca
2+
waves that moved within and between cells. To examine the mechanisms underlying each component, we developed methods to separate slow persistent Ca
2+
rise from the propagating Ca
2+
waves in each cell. TRPV4‐mediated Ca
2+
entry was required for the slow persistent global rise and propagating Ca
2+
signals. The propagating waves were inhibited by depleting internal Ca
2+
stores, inhibiting PLC or blocking IP
3
receptors. Ca
2+
release from stores was tightly controlled by TRPV4‐mediated Ca
2+
influx and ceased when influx was terminated. Furthermore, Ca
2+
release from internal stores was essential for TRPV4‐mediated control of vascular tone.
Conclusions and Implications
Ca
2+
influx via TRPV4 channels is amplified by Ca
2+
‐induced Ca
2+
release acting at IP
3
receptors to generate propagating Ca
2+
waves and provide a large‐scale endothelial communication system. TRPV4‐mediated control of vascular tone requires Ca
2+
release from the internal store.