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        Figure 2.33. Channel gating. A. WT single channel records from model simulation (left, green)
        and experiment (right, black) showing only single opening events in response to depolarization.
        B. ∆KPQ single channel records in the background mode (top 3 traces) and burst mode (bottom
        2 traces). Note second openings in background mode and fluctuation between closed and open
        states in burst mode, in absence of inactivation. Traces on left are simulated; traces on right are
        experimentally recorded. Adapted from Clancy and Rudy [125] with permission of Springer Nature.
        Experimental data from Chandra et. al. [126] with permission from the American Physiological
        Society.




               The reopening and bursting of ΔKPQ channels suggest that they generate a significant
        late I  current during an action potential plateau. This possibility and its effect on the action
              Na
        potential are examined in the simulations of Figure 2.34. The Markov models of Figure 2.32
        were introduced into the LRd ventricular cell model, which was then paced at various rates.

        In Figure 2.34, simulated action potentials (top) are shown with corresponding macroscopic I
                                                                                                               Na
        current (bottom) for: (I) wild-type paced at CL=400ms; (II) ΔKPQ mutant at CL=400ms; (III) ΔKPQ
        at a slower rate of CL=600ms. In (IV), ΔKPQ experimental data are included for comparison ,
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        showing close resemblance of the I  trace to that simulated in (II).
                                               Na


               During a wild-type action potential, I  has a large early spike that generates the action
                                                        Na
        potential upstroke. This early peak decays very quickly, reflecting the single opening of each
        individual ion channel. In contrast, secondary re-openings in background mode and bursting in

        the burst mode of ΔKPQ channels generate a late component of macroscopic I  current during
                                                                                               Na
        the action potential plateau. This late current is only 1% of the early peak I . However, despite its
                                                                                        Na
        small magnitude, it is sufficient to shift the delicate balance of currents in the inward direction,
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