Subcellular calcium dynamics in a whole-cell model of an atrial myocyte
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Edited by Michael J. Berridge, The Babraham Institute, Cambridge, United Kingdom, and approved December 22, 2011 (received for review September 30, 2011)

Abstract
In this study, we present an innovative mathematical modeling approach that allows detailed characterization of Ca2+ movement within the three-dimensional volume of an atrial myocyte. Essential aspects of the model are the geometrically realistic representation of Ca2+ release sites and physiological Ca2+ flux parameters, coupled with a computationally inexpensive framework. By translating nonlinear Ca2+ excitability into threshold dynamics, we avoid the computationally demanding time stepping of the partial differential equations that are often used to model Ca2+ transport. Our approach successfully reproduces key features of atrial myocyte Ca2+ signaling observed using confocal imaging. In particular, the model displays the centripetal Ca2+ waves that occur within atrial myocytes during excitation–contraction coupling, and the effect of positive inotropic stimulation on the spatial profile of the Ca2+ signals. Beyond this validation of the model, our simulation reveals unexpected observations about the spread of Ca2+ within an atrial myocyte. In particular, the model describes the movement of Ca2+ between ryanodine receptor clusters within a specific z disk of an atrial myocyte. Furthermore, we demonstrate that altering the strength of Ca2+ release, ryanodine receptor refractoriness, the magnitude of initiating stimulus, or the introduction of stochastic Ca2+ channel activity can cause the nucleation of proarrhythmic traveling Ca2+ waves. The model provides clinically relevant insights into the initiation and propagation of subcellular Ca2+ signals that are currently beyond the scope of imaging technology.
A human heart beats more than a billion times during the average lifespan, and is required to do so with great fidelity. The ventricular chambers of the heart are responsible for generating the force that propels blood to the lungs and body (1). Under sedentary conditions, the atrial chambers make only a minor contribution to blood pumping. However, during periods of increased hemodynamic demand, such as exercise, atrial contraction increases to enhance the amount of blood within the ventricles before they contract. This “atrial kick” is believed to account for up to 30% extra blood-pumping capacity. Deterioration of atrial myocytes with aging causes the loss of this blood-pumping reserve, thereby increasing frailty in the elderly. Atrial kick is also lost during atrial fibrillation (AF), the most common form of cardiac arrhythmia. The stagnation of blood within the atrial chambers during AF can cause thrombus formation, leading to thromboembolism. Approximately 15% of all strokes occur in people with AF. As shown in numerous reports, the genesis and maintenance of AF is causally linked to the dysregulation of Ca2+ signaling (2–4). Detailed characterization of Ca2+ movement within atrial myocytes is therefore necessary to understand changes involved in aging and conditions such as AF.
Elevation of the cytosolic Ca2+ concentration is the trigger for contraction of cardiac myocytes (1). Engagement of Ca2+ with troponin C (TnC) allows the actin and myosin filaments to interact and slide past each other, thereby causing cell shortening. The sequence of events that leads to a Ca2+ rise during excitation–contraction coupling (EC coupling) is well-known. Essentially, depolarization of cardiac myocytes activates voltage-operated Ca2+ channels (VOCs) that allow the entry of Ca2+ from the extracellular space. This Ca2+ influx signal is greatly amplified via a process known as Ca2+-induced Ca2+ release (CICR) by intracellular Ca2+ channels (ryanodine receptors; RyRs) expressed on the sarcoplasmic reticulum (SR). The SR membrane bearing RyRs comes within 10 nm of the sarcolemma, thereby forming compartments known as “dyadic junctions” in which CICR rapidly occurs. Mammalian ventricular myocytes have an extensive series of sarcolemmal invaginations (T tubules) that bring VOCs and RyRs into close proximity within dyadic junctions throughout the volume of the cells. Each dyadic junction produces an elementary Ca2+ signal known as a “Ca2+ spark” during EC coupling. The spatial overlap of many thousands of Ca2+ sparks gives rise to the homogeneous Ca2+ signals associated with ventricular EC coupling.
In contrast, the atrial myocytes of many mammalian species do not express extensive T-tubule networks. In this situation, the coupling of VOCs and RyRs occurs at dyadic junctions around the periphery of the cells. The consequence of this arrangement is that Ca2+ signals originate around the edge of atrial myocytes during EC coupling (2). We, and others, have shown that under resting conditions this peripheral Ca2+ signal does not propagate into the center of atrial cells, so that at the peak of the response substantial Ca2+ gradients can be observed from a cell's edge to its center (5–7). However, in addition to the junctional RyRs that are activated at the onset of EC coupling, atrial myocytes express clusters of RyRs in a regular three-dimensional lattice throughout their volume. It could be expected that these nonjunctional RyRs would sense the subsarcolemmal Ca2+ signal and convey it deeper into a cell via CICR. Indeed, to trigger substantial contraction, the Ca2+ wave must move toward the center of an atrial cell, because the extent of inward movement of the Ca2+ wave and atrial myocyte contraction are linearly related (8, 9). The nonjunctional RyRs therefore appear to act as an inotropic reserve that becomes active under conditions where greater atrial contraction is required. Little is known about the mechanisms that control the propagation of Ca2+ between RyRs within atrial myocytes.
In the present study, we characterized the movement of Ca2+ during EC coupling in an idealized atrial myocyte model. The model describes a three-dimensional lattice of discrete Ca2+ release sites that equate in position and function to those within a living atrial cell. Our method, which translates key properties of cellular Ca2+ transport into a framework of significantly low computational overhead, allows the activity of all of the discrete Ca2+ release sites to be simultaneously monitored, and for Ca2+ signals to be activated at any particular site(s). We provide an overview of the model in Materials and Methods, and refer the reader to SI Materials and Methods, for a detailed discussion of our modeling approach.
The model was validated by replicating known properties of atrial myocyte Ca2+ signaling, such as the centripetal diffusion of Ca2+ from the periphery of an atrial myocyte to the cell center. Moreover, the model allows us to explore factors critical to the fidelity of Ca2+ signaling that cannot be manipulated experimentally. Although our simulations used the geometry of an atrial myocyte without T tubules, our findings are also relevant to other myocytes that do not possess T tubules (e.g., neonatal myocytes). Furthermore, T tubules in mature ventricular myocytes are lost during aging or under disease conditions. In situations where T tubules are lost, EC coupling is initiated around the periphery of the cells and contraction will be dependent on saltatoric Ca2+ wave propagation as for the atrial myocytes described in this study. The arrhythmic calcium wave activity presented herein is relevant to non-tubulated and de-tubulated myocytes.
Results
The aim of this study was to produce a geometrically realistic model of an atrial myocyte. By incorporating the actual positioning of discrete Ca2+ release sites, we could explore their interaction and involvement in Ca2+ wave initiation and propagation. Based on empirical measurements of RyR distribution from numerous studies (2) (Fig. 1A), we modeled an atrial myocyte as a cylinder 100 μm in length and 12 μm in diameter, as depicted in Fig. 1B. Within the cylinder, Ca2+ release was constrained to 51 two-dimensional disks situated perpendicular to the long axis of the cylinder, and spaced 2 μm apart. These disks correspond to the z planes within atrial myocytes where the RyRs are expressed (8, 10, 11) (Fig. 1A). Within the z planes, the Ca2+ release sites were distributed as shown in Fig. 2A. The outermost ring of Ca2+ release sites represents the junctional RyRs that face the VOCs in dyadic junctions, whereas the inner Ca2+ release sites equate to nonjunctional RyRs. The radial distance between the rings of nonjunctional Ca2+ release sites is 1 μm (Fig. 2A). Between the junctional Ca2+ release sites and the first ring of nonjunctional Ca2+ release sites is a spacing of 2 μm, reflecting the gap of RyR expression observed in atrial myocytes (Fig. 1Aii). The spacing of Ca2+ release sites around each ring is 1 μm. This model allows us to investigate the movement of Ca2+ within one, two, or three dimensions, and to examine interactions between Ca2+ release sites within the same, or neighboring, z planes.
(A) Distribution of type 2 RyRs in an atrial myocyte immunostained with an anti-type 2 RyR antibody. (i) A portion of an atrial myocyte. The transverse striations of nonjunctional RyRs, and peripheral junctional RyRs are evident. “N” denotes the position of the nucleus. (ii) An enlarged section of the same cell. The gap in RyR distribution between the junctional RyRs and the nonjunctional RyRs is indicated by arrows. (iii) A cartoon representation of the arrangement of RyRs and cellular membranes relating to ii. The position of the RyR clusters was determined by thresholding the image in ii so that all positive pixels in the background were absent, and then identifying the remaining areas with positive fluorescence. (B) Cylindrical atrial myocyte geometry used in simulations showing a stack of z planes. The location of individual clusters within a disk is illustrated in Fig. 2A.
(A) Position of Ca2+ release sites within a single z plane as used in the simulations. See text for details concerning the colors. (B) Space–time plot of a one-dimensional saltatory propagating wave. Parameter values are τ = 1 s, D = 1 μm2⋅s−1, cth = 1 μM, and σ = 0.26 μM. The bars on the left indicate the time of successive release Ca2+ events.
Deterministic Release.
Movement of Ca2+ within the model relies on saltatory wave propagation involving discrete Ca2+ release sites. A one-dimensional representation of such a wave, obtained analytically, is shown in Fig. 2B (details will be published elsewhere). A centripetal Ca2+ wave travels from the periphery to the center of the cell. The propagation rate and amplitude of the Ca2+ wave in the full three-dimensional cell model both diminish as it moves inwardly. Essentially, Ca2+ diffusing between successive release sites has to overcome the continual inhibitory effect of sarcoendoplasmic reticulum Ca2+ ATPases (SERCAs), and as the Ca2+ signal diminishes it takes longer to initiate Ca2+ release at the next RyR cluster. It is already established that RyR activity is regulated by a range of factors including luminal Ca2+, phosphorylation, accessory proteins, and accessory factors. To simplify the model, we convolved the effect of these factors in two key parameters—release strength and release threshold. These parameters encompass possible changes in the total Ca2+ flux through a cluster of RyRs and RyR sensitivity irrespective of the molecular mechanism. Saltatory wave propagation critically depends on release strength and threshold. If the release strength is too small, or the threshold is too high, then Ca2+ waves cannot propagate.
We next examined the movement of Ca2+ within a single z plane. Ca2+ release was initiated by activating the six peripheral Ca2+ release sites colored black in Fig. 2A. The black curve in Fig. 3A illustrates the profile of the Ca2+ signal at those peripheral sites. The red, blue, and green curves depict the time courses of Ca2+ concentration at Ca2+ release sites deeper inside the cell (denoted by corresponding colors in Fig. 2A). Because we trigger release at the periphery, we observe an immediate response in that location. The next release site (red) opens with some latency, and the peak amplitude is damped in comparison with the outer release site. Moving further toward the interior of the cell, Ca2+ release begins even later, while peak values continue to decrease. The sharp rise and fall of the concentration profiles is a combined effect of the threshold dynamics of release in a 3D volume and the impact of SERCA pumps. Reducing the release strength leads to overall smaller Ca2+ profiles and slowing of saltatoric Ca2+ wave propagation, but the tendency of growing latencies and smaller maxima for inner release sites remains unchanged (compare Fig. 3 A and B). Note that a release strength of 45 μM⋅μm3⋅s−1 corresponds to ∼400 open RyRs when we assume a single channel current of 1 pA.
Time course of the Ca2+ concentration for σ = 90 μM⋅μm3⋅s−1 (A) and σ = 45 μM⋅μm3⋅s−1 (B) in the central z plane at θ = 0 and r = 5.9 μm (black), r = 4.9 μm (green), r = 3.9 μm (red), and r = 2.9 μm (blue) in the presence (solid lines) and absence (dotted lines) of a diffusive gap. Parameter values are as in Table S1 and dt = 0.002 s.
An aspect of atrial myocyte ultrastructure that we considered at this point was the effect of the gap in Ca2+ release sites between the junctional RyRs and the first ring of nonjunctional RyRs. As depicted in Fig. 2A, the spacing between rings of Ca2+ release sites is 1 μm inside the cell, with a 2 μm gap to the peripheral junctional ring of Ca2+ release sites. The 2 μm gap was adopted into the model because studies have shown such a discontinuity in the expression of RyR clusters (10, 12, 13). The physiological reason for this gap in atrial RyR distribution is not known. We observed that for minimal release strengths the gap prevented the inward propagation of the Ca2+ wave, such that only the peripheral Ca2+ release sites were active (Fig. S1).
The consequence of incorporating an additional ring of Ca2+ release sites (green release site in Fig. 2A) within the gap between the junctional and nonjunctional RyRs is depicted in Fig. 3. The essential effect of the additional Ca2+ release sites was to accelerate the centripetal propagation of the Ca2+ wave by reducing the distance over which Ca2+ had to diffuse before attaining a threshold concentration for CICR. These data suggest that the gap in RyR distribution imparts a natural barrier to hinder Ca2+ movement. This is likely to be a physiological mechanism for limiting atrial contraction under resting conditions.
The magnitude of atrial myocyte contraction is determined by the distance that the centripetal Ca2+ wave is able to spread (2, 8). This is due to the increasing recruitment of myofilaments as Ca2+ waves progress deeper into an atrial cell. The extent of propagation of the centripetal wave is modulated by application of positive inotropic hormones such as endothelin-1 or β-adrenergic agonists (8, 14).
To measure the effect of positive inotropic stimulation in our model, we determined the activity of Ca2+ release sites within the innermost rings (r = 0.9 μm) of all 51 z planes. For those release sites to be activated, Ca2+ has to travel in a saltatoric manner from the periphery of the cell, as described above. We varied the degree of cell stimulation by altering the fraction of peripheral Ca2+ release sites that were activated at the inception of a response (hereafter denoted “initial fraction”; the actual position of those sites was randomly assigned). The black curve in Fig. 4A depicts the increasingly successful recruitment of central Ca2+ release sites as the initial fraction was progressively enhanced. The data show that for strong stimulation, that is, for a large initial fraction, almost all release sites in the innermost rings become activated. On the other hand, a lesser initial fraction elicits a considerably damped response in the center.
Mean relative response and variance (error bars) of the central cylinder of release sites (r = 0.9 μm) as a function of initial fraction (A) and varying Ca2+ release strength σ (B). Parameter values are (A) σ = 3.5 (black), 3.4 (red), 3.3 (green), 3.2 (blue), 3.1 μM⋅μm3⋅s−1 (magenta). (B) The initial fraction is 0.8. All other parameter values are as in Table S1 and tref = 1 s.
An unexpected outcome was that the variance of central channel opening was not uniform. Generally, triggering either relatively few, or many, peripheral Ca2+ release sites gave consistent responses (small error bars on the curves in Fig. 4A), whereas activating an intermediate number of peripheral Ca2+ release sites gave more variable penetration into the cell (large error bars). The error bars indicate that not all triggered responses, even with the same number of initiating Ca2+ release sites, resulted in the same degree of centripetal Ca2+ wave propagation. The key point of this observation is that Ca2+ waves sometimes propagate into the cell center but at other times fail, even though they were triggered by the same number of peripheral release sites. This implies that the positions of the initiating sites are critical. Evidently, some configurations of initial calcium release sites fail to nucleate calcium waves. However, the same number of initiating sites, but in a different spatial configuration, can activate a centripetal calcium wave. Interestingly, we have previously observed that atrial myocytes use the same spatial distribution of initiating release sites with each beat [so-called eager sites (13)], thereby avoiding beat-to-beat variability in Ca2+ wave nucleation.
Varying the release strength alters the dependency of centripetal Ca2+ wave propagation on the initial fraction (colored curves in Fig. 4A). Essentially, for lesser release strengths, a greater initiating fraction of Ca2+ release sites is required to trigger centripetal Ca2+ wave propagation. The steep relationship between recruitment of the innermost Ca2+ release sites and strength of Ca2+ liberation with fixed initial fraction (0.5) is depicted in Fig. 4B. In addition to the positive inotropic effects of increased release strength and increased initial fraction, decreasing the threshold for Ca2+ release also promoted centripetal Ca2+ waves, and would therefore be positively inotropic (Fig. S2). A comparison of the effects of increasing release strength, increasing initial fraction, and decreasing threshold is depicted in Fig. S3. It is evident that altering any of the parameters could independently enhance centripetal Ca2+ wave propagation, but the effects of each parameter were not exactly alike. Increasing the initial fraction or decreasing the threshold for Ca2+ release promoted centripetal Ca2+ wave propagation and increased the global amplitude of pacing-evoked Ca2+ signals. However, the degree of Ca2+ signal enhancement was significantly greater if the Ca2+ release strength was increased. Essentially, increasing the release strength is the only parameter that actually adds more Ca2+ to the system. The other two parameters, initial fraction and threshold, can modulate the ease with which centripetal Ca2+ waves can be triggered and propagate, but do not impart any additional Ca2+ inside the cell. These analyses suggest that at least three different parameters control the success of Ca2+ wave movement within an atrial myocyte, but that release strength, the amount of Ca2+ released, is the most potent effector.
The three-dimensional atrial cell model also allows us to explore putative arrhythmic patterns of Ca2+ signaling that arise from localized Ca2+ release activity. In particular, we examined how Ca2+ liberated at one z plane influences Ca2+ release sites in neighboring z planes. Such a situation is depicted in Fig. 5A, which shows Ca2+ waves initiating at the central z plane within an atrial myocyte that subsequently propagate to the top and bottom of the cell. The figure shows three traveling Ca2+ waves of which only the first one was triggered, and the second and third arose autonomously. The reinitiation of such Ca2+ waves occurs if the Ca2+ concentration within the z plane that was first triggered is above the threshold for Ca2+ release when the RyRs emerge from being refractory. The reinitiation of Ca2+ waves reflects an interplay between the processes that serve to introduce Ca2+ into the cytoplasm (i.e., Ca2+ release strength), the processes that diminish the buildup of Ca2+ concentration (i.e., SERCA pumps and Ca2+ diffusion), and the refractory period of the Ca2+ release sites. Fig. 5B depicts the relationship between Ca2+ release strength and the maximal refractory period that will sustain Ca2+ wave reinitiation. Essentially, as the Ca2+ release strength increases, the time window in which Ca2+ wave reinitiation can occur also increases. Increasing the time constant of the SERCA pumps and hence weakening Ca2+ resequestration also extends the time window for Ca2+ wave reinitiation, because it takes longer for the Ca2+ concentration to fall below the threshold for any given release strength. In addition to increased release strength triggering arrhythmic Ca2+ waves, we observed that dramatically decreasing release strength also promoted autonomous Ca2+ signals. Below a critical Ca2+ release strength, RyR activity persists indefinitely once it is activated within a particular plane. This can be inferred from the faint bluish horizontal ribbon in Fig. 6A. The blue band represents a Ca2+ wave that never terminates because the release sites within that plane are never in a simultaneous refractory state. We call this type of activity “ping waves,” and within the model such waves are visualized as an elevated Ca2+ concentration within two counterrotating sectors of a single z plane (Movie S1). These perpetually rotating ping waves progressively feed Ca2+ to neighboring z planes, eventually evoking longitudinal Ca2+ waves. Essentially, a low Ca2+ release strength causes only a partial recruitment of Ca2+ release sites during EC coupling, thereby seeding ping wave activity. The period of a ping wave is much longer than the typical timescale for replenishing the SR after Ca2+ release, allowing the SR to return to its rest state before a new rotation of a ping wave is initiated. These observations are pertinent to conditions such as end-stage heart failure, where Ca2+ pumping into the SR is low and RyR expression is diminished (hence release strength is decreased) yet the propensity for arrhythmic Ca2+ release is high. The reduced Ca2+ release strength evident during heart failure would have the consequence of nonuniform RyR refractoriness, thereby leading to the likely triggering of ping waves.
(A) Traveling wave initiated in the central z plane for σ = 90 μM⋅μm3⋅s−1 and tref = 0.34 s. The Ca2+ wave was initiated by activating six adjacent peripheral release sites. (B) Maximal refractory period as a function of the release strength σ. Colors represent the proportion of open channels in a single z plane.
(A) Traveling wave initiated in the central z plane for σ = 7.85 μM⋅μm3⋅s−1 and tref = 0.34 s. The Ca2+ wave was initiated by activating six adjacent peripheral release sites. Colors represent the proportion of open channels in a single z plane. (B) Ping wave in the central z plane at t = 0.18 s (i), 0.33 s (ii), 0.60 s (iii), and 0.75 s (iv). The triangular shape of the concentration peaks is for illustration purposes only. Parameter values are as in Table S1.
Stochastic Release.
In the previous sections, the modeling assumed a uniform threshold for activation of Ca2+ release sites. However, ion channels are intrinsically stochastic (15), and within the heart the stochastic activity of RyRs is enhanced by factors such as phosphorylation, association with accessory proteins, and increased SR Ca2+ load. To model these effects, we make the threshold for Ca2+ release a random variable that fluctuates independently at each release site. Fig. 7 shows the number of open channels in every z plane as a function of time and illustrates how Ca2+ wave dynamics changes when threshold noise grows. At small noise levels (Fig. 7A), Ca2+ wave propagation resembles a deterministic motion, as in Fig. 5. Upon increasing the noise strength, waves emerge spontaneously (Fig. 7B). When two waves meet, they annihilate each other because they run into each other's refractory tail. Note that the spontaneously nucleated wave is weaker in the beginning compared with the induced wave, but eventually induces a longitudinal Ca2+ wave. Stronger noise leads to more spontaneous waves (Fig. 7C). If the noise strength grows beyond a critical value, almost all channels open immediately. This results in a global rise of activity without any traveling wave.
Traveling wave for σ = 60 μM⋅μm3⋅s−1 and β = 200 μM−1 (A), β = 100 μM−1 (B), β = 80 μM−1 (C), and β = 70 μM−1 (D). The first Ca2+ wave was initiated by activating six adjacent peripheral release sites. Parameter values are as in Table S1 and tref = 1.5 s. Colors represent the proportion of open channels in a single z plane.
As described above, refractoriness has a calming influence on Ca2+ release by preventing repetitive activation of release sites. A long refractory period ensures that Ca2+ declines below the threshold for Ca2+ release at the end of a response. However, the introduction of noise can negate the effect of refractory periods on the fidelity of Ca2+ signaling. In Fig. 7D, for example, several successive waves are evident in a simulation using a relatively long refractory period (1.5 s). In the deterministic model with no noise, only the first (triggered) Ca2+ wave would be evident. Essentially, introducing noisy thresholds allows some release sites to activate even when Ca2+ has recovered to diastolic levels.
Discussion
In the present study, we explored the characteristics of Ca2+ movement within an idealized atrial myocyte using a realistic geometrical representation of Ca2+ release sites and Ca2+ flux values. A key feature of the model is that we can initiate Ca2+ release from any of the sites within the three-dimensional lattice and subsequently examine the propagation of the Ca2+ signal to other parts. In this way, we could stimulate the peripheral Ca2+ release sites to generate a centripetal Ca2+ wave (Figs. 2 and 3) that mimics physiological pacing of atrial myocytes during EC coupling (6–8, 16), or activate Ca2+ release within the center of the cell to examine the movement of Ca2+ waves that would be arrhythmogenic (Figs. 5–7). The propagation of Ca2+ signals depends on the diffusion of Ca2+ between release sites. If the Ca2+ ions released by one site reach the threshold concentration at a neighboring site, then it will be activated and convey the Ca2+ signal further.
Atrial myocytes have an essential inotropic function in the heart. The extent of centripetal propagation of a Ca2+ wave determines the extent of atrial myocyte contraction. The further a Ca2+ wave progresses toward the center of the cell, the more myofilaments become activated (5). The junctional Ca2+ release sites are always the first to respond during EC coupling, but by themselves evoke little contraction because the Ca2+ signal occurs around the cell periphery. The nonjunctional RyRs therefore represent an inotropic reserve that is activated under conditions when strong contraction is required.
A structural feature of atrial myocytes that may credibly contribute to the peripheral restriction of Ca2+ waves is the 2 μm gap in RyR expression between the junctional and nonjunctional Ca2+ release sites (Fig. 1). This gap is a particular feature of atrial myocytes, and has been observed in several previous studies (10, 13). Our results indicate that the 2 μm discontinuity in RyR expression significantly hinders the movement of the centripetal Ca2+ wave (Fig. 3), because it introduces both a break in the regeneration of the Ca2+ wave and a space in which the Ca2+ signal can dissipate. Hypothetically introducing Ca2+ release sites within the gap has the effect of increasing both the velocity and amplitude of the centripetal Ca2+ wave (Fig. 3). These in silico results indicate that the gap in RyR expression is a structural feature to prevent inward movement of Ca2+, and thereby reduce atrial energy use when hemodynamic requirements are low.
When hemodynamic demand increases, the atrial chambers make a significant contribution to ventricular refilling. Adrenergic stimulation is a key physiological mechanism for enhancing atrial contraction (1) (Fig. S4). The effect of adrenergic stimulation is largely mediated by the activation of protein kinase A (PKA), which has numerous putative targets within a cardiac myocyte. Notably, PKA-dependent phosphorylation causes an increase in VOC activity, which will lead to additional recruitment of dyadic junctions during EC coupling (analogous to changing the initial fraction). Furthermore, phosphorylation of the endogenous SERCA inhibitor phospholamban causes a marked elevation of SR Ca2+ content that both sensitizes RyRs for CICR and increases the flux of Ca2+ through RyRs upon their activation (analogous to changing threshold and release strength, respectively) (1). It is difficult to experimentally separate the contributions of increased VOC activity, reduced threshold for CICR, and increased Ca2+ flux. Our simulations indicated that all three parameters have the potential to gradually modulate the inotropic status of an atrial myocyte by determining the ability of centripetal Ca2+ waves to propagate from the periphery to the cell center (Fig. 4 and Fig. S3). Furthermore, the effect of these parameters on Ca2+ wave propagation was codependent. For example, altering the fraction of activated peripheral Ca2+ release sites at the onset of a response produced a steeply graded response in terms of centripetal Ca2+ wave propagation. Activating only a few of the peripheral Ca2+ release sites was generally insufficient to trigger a centripetal Ca2+ wave. However, increasing the Ca2+ release flux compensated for the lack of peripheral Ca2+ release site activation, and promoted centripetal Ca2+ waves (Fig. 4). Similarly, decreasing the threshold for CICR, to mimic RyR sensitization by SR Ca2+, also supported centripetal Ca2+ waves. Our data indicate that multiple, interdependent processes determine the ability of centripetal Ca2+ waves to propagate, and thereby regulate contraction.
In addition to examining the factors underlying inotropy within atrial myocytes, we explored processes controlling the initiation and propagation of proarrhythmic Ca2+ waves. As described above, application of adrenergic agonists increases atrial myocyte inotropy, but also leads to the development of spontaneous Ca2+ signals (Fig. S5). A plausible explanation for such observations is stochastic activation of RyRs resulting from increased SR Ca2+ loading. We modeled this situation by changing the threshold at which cytosolic Ca2+ could activate Ca2+ release sites randomly in time. It is evident that increasing the spread of thresholds causes progressively more spontaneous Ca2+ wave generation (Fig. 7). In addition to RyRs, atrial myocytes express inositol 1,4,5-trisphosphate receptors (InsP3Rs). We and others (2, 5, 14) have demonstrated that specific activation of InsP3Rs provokes the generation of arrhythmic Ca2+ signals. Inclusion of InsP3Rs within the present model can be mimicked by changing RyR threshold. Essentially, the stochastic activation of InsP3Rs triggers further RyR activity and Ca2+ waves via CICR. However, even within a deterministic model, where all of the Ca2+ release sites have the same threshold for CICR, it is possible to trigger self-sustaining autonomous Ca2+ waves, such as the Ca2+ waves illustrated in Fig. 5. It is evident that several parameters are critical in determining whether autonomous Ca2+ waves persist. Essentially, Ca2+ waves are triggered when the cytosolic Ca2+ concentration is greater than the threshold for CICR. This implies that increased Ca2+ release flux or decreased SERCA activity makes autonomous Ca2+ signals more likely to occur. A further critical parameter determining the propensity for spontaneous Ca2+ wave initiation is the period in which RyRs remain refractory after the previous Ca2+ release event (17). Reducing the refractory period increases the likelihood that cytosolic Ca2+ will not recover sufficiently before RyRs are ready to respond again (Fig. 5B). Furthermore, mismatches in refractoriness between neighboring Ca2+ release sites can cause the nucleation of Ca2+ waves. This is the situation underlying the ping waves presented in Fig. 6, where two counterrotating Ca2+ waves perpetually travel around a z disk. The ping wave persists because RyRs within the z disk are never simultaneously refractory. These data therefore suggest that situations in which atrial myocyte Ca2+ signaling is enhanced (i.e., increased Ca2+ release flux or reduced threshold for CICR) can give rise to proarrhythmic Ca2+ signals. However, in addition, the activation of RyRs under conditions of relatively weak Ca2+ flux also leads to proarrhythmic Ca2+ release activity due to nonsynchronous activation of RyRs and their refractory states.
The formation of ping waves is a clear prediction of our modeling framework, a Ca2+ pattern that could not have been resolved with current experimental techniques. Our approach allows us to probe the way in which Ca2+ activity between different z planes interacts and hence to unravel the complex contributions to physiological and pathological Ca2+ signals, which emphasizes the useful power of a computational cell biology approach to Ca2+ signaling.
Materials and Methods
The dynamics of Ca2+ concentration, c(r, t), r ∈ ℝ3, t ∈ ℝ+, in the cylinder is governed by a generalization of the original fire-diffuse-fire model (18, 19):

Here, D and Δ denote the effective diffusion coefficient for Ca2+ and the Laplace operator in cylindrical coordinates, respectively. We model SERCA pumps as homogeneously distributed linear sinks of strength τ. The double sum corresponds to Ca2+ liberation from the SR through RyR channels. The Nrel release sites are located at discrete positions rn, , and η(t) holds all details about the release shape, which we here take as
. Ca2+ is released for a fixed time trel with a constant conductance σ, and Θ(x) represents the Heaviside step function, which equals 1 for x ≥ 0 and 0 otherwise. The time
in Eq. 1 corresponds to the instant when the nth release site conducts Ca2+ for the mth time. The computation of the release times
renders Eq. 1 highly nonlinear, because the mth liberation is obtained implicitly by demanding that the Ca2+ concentration reaches the threshold value cth at time
and that there is at least a refractory period of tref between successive release events. For a broader and more elaborate discussion of the model, we refer the reader to SI Materials and Methods.
Acknowledgments
R.T. was supported through a Leverhulme Trust Early Career Fellowship. M.D.B. and H.L.R. were supported by the Biotechnology and Biological Sciences Research Council and British Heart Foundation H.L.R. is a Royal Society University Research Fellow.
Footnotes
- ↵1To whom correspondence should be addressed. E-mail: ruediger.thul{at}nottingham.ac.uk.
Author contributions: R.T., S.C., H.L.R., and M.D.B. designed research; R.T., S.C., and M.D.B. performed research; R.T. and M.D.B. analyzed data; and R.T. and M.D.B. wrote the paper.
The authors declare no conflict of interest.
This article is a PNAS Direct Submission.
This article contains supporting information online at www.pnas.org/lookup/suppl/doi:10.1073/pnas.1115855109/-/DCSupplemental.
Freely available online through the PNAS open access option.
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