Enhancement of calcium signalling dynamics and stability by delayed modulation of the plasma-membrane calcium-ATPase in human T cells

In addition to its homeostatic role of maintaining low resting levels of intracellular calcium ([Ca2+](i)), the plasma-membrane calcium-ATPase (PMCA) may actively contribute to the generation of complex Ca2+ signals. We have investigated the role of the PMCA in shaping Ca signals in Jurkat human leukaemic T cells using single-cell voltage-clamp and calcium-imaging techniques. Crosslinking the T-cell receptor with the monoclonal antibody OKT3 induces a biphasic elevation in [Ca2+](i) consisting of a rapid overshoot to a level > I muM, followed by a slow decay to a plateau of similar to0.5 mum. A similar overshoot was triggered by a constant level of Ca2+ influx through calcium-release-activated Ca2+ (CRAC) channels in thapsigargin-treated cells, due to a delayed increase in the rate of Ca2+ clearance by the PMCA. Following a rise in [Ca2+](i), PMCA activity increased in two phases: a rapid increase followed by a further calcium-dependent increase of up to approximately fivefold over 10-60 s, termed modulation. After the return of [Ca2+](i) to baseline levels, the PMCA recovered slowly from modulation (tau similar to 4 min), effectively retaining a 'memory' of the previous [Ca2+](i) elevation. Using a Michaelis-Menten model with appropriate corrections for cytoplasmic Ca2+ buffering, we found that modulation extended the dynamic range of PMCA activity by increasing both the maximal pump rate and Ca sensitivity (reduction of K-M). A simple flux model shows how pump modulation and its reversal produce the initial overshoot of the biphasic [Ca2+](i) response. The modulation of PNICA activity enhanced the stability of Ca2+ signalling by adjusting the efflux rate to match influx through CRAC channels, even at high [Ca2+](i) levels that saturate the transport sites and would otherwise render the cell defenceless against additional Ca2+ influx. At the same time, the delay in modulation enables small Ca2+ fluxes to transiently elevate [Ca2+](i), thus enhancing Ca2+ signalling dynamics.