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Rapid ADP-evoked currents in human platelets recorded with the nystatin permeabilized patch technique
M P Mahaut-Smith1, S O Sage, T J Rink
1Physiological Laboratory, Cambridge, United Kingdom.
The Journal of Biological Chemistry
|February 15, 1992
Summary
Adenosine diphosphate (ADP) activates a novel ion channel in human platelets, facilitating rapid calcium influx. Thrombin appears to utilize a different, slower pathway for calcium entry.
Area of Science:
- Cellular physiology
- Ion channel biophysics
- Platelet function
Background:
- Human platelets play a crucial role in hemostasis and thrombosis.
- Agonist-induced calcium (Ca2+) influx is a key event in platelet activation.
- The specific ion channels responsible for early Ca2+ entry remain incompletely understood.
Purpose of the Study:
- To investigate the ion channels involved in agonist-evoked calcium influx in human platelets.
- To characterize the properties of an ADP-activated ion channel.
- To compare the mechanisms of calcium entry induced by ADP and thrombin.
Main Methods:
- Whole-cell patch-clamp recordings from single human platelets.
- Application of agonists (ADP, thrombin) using a "puffer" pipette.
- Ion substitution experiments to determine channel permeability.
- Fura-2 fluorescence measurements to monitor intracellular Ca2+ changes.
Main Results:
- Adenosine diphosphate (ADP) activated a transient inward current with rapid kinetics (tens of milliseconds).
- The ADP-evoked channel is permeable to Na+, K+, and Ba2+, but not Cl-, with a single channel conductance of 11-15 pS.
- Thrombin did not elicit detectable currents under identical conditions, suggesting a different Ca2+ entry mechanism.
Conclusions:
- A novel, rapidly activating ion channel permeable to cations mediates ADP-induced Ca2+ influx in human platelets.
- Early thrombin-evoked Ca2+ entry likely occurs through small conductance channels or an electroneutral pathway, distinct from the ADP-activated channel.
- The characterized ADP-evoked channel possesses the speed necessary to explain rapid Ca2+ influx observed in platelet activation studies.