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Published as doi: 10.1096/fj.05-4561fje.
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(The FASEB Journal. 2006;20:973-975.)
© 2006 FASEB

Why Escherichia coli {alpha}-hemolysin induces calcium oscillations in mammalian cells–the pore is on its own

Andreas Koschinski*,1, Holger Repp*,1,2, Baris Ünver*, Florian Dreyer*, Dierk Brockmeier*, Angela Valeva{dagger}, Sucharit Bhakdi{dagger} and Iwan Walev{dagger},2


* Rudolf-Buchheim-Institute of Pharmacology, Justus-Liebig-University, Giessen, Germany; and

{dagger} Institute of Medical Microbiology and Hygiene, Johannes-Gutenberg-University, Mainz, Germany

2Correspondence: Frankfurter Str. 107, Rudolf-Buchheim-Institute of Pharmacology, Justus-Liebig-University, 35392 Giessen, Germany. Email: Holger.Repp{at}pharma.med.uni-giessen.de; and Obere Zahlbacher Str. 67, Institute of Medical Microbiology and Hygiene, Johannes-Gutenberg-University, 55101 Mainz, Germany. Email: walev{at}mail.uni-mainz.de

SPECIFIC AIMS

The hemolysin of Escherichia coli (HlyA) is prototypic of a large family of pore-forming toxins that are produced by many medically important gram-negative pathogens. It was reported that HlyA deregulates membrane Ca2+ channels, thus inducing periodic low-frequency Ca2+ oscillations that trigger transcriptional processes in mammalian cells. Our aim in this study was to delineate the mechanism underlying the Ca2+ oscillations that are induced by HlyA.

PRINCIPAL FINDINGS
1. HlyA induces nonperiodic Ca2+oscillations in renal cells
Within ~30 s after application of HlyA (5 ng/ml) to human kidney tubule epithelial (IHKE) cells, intracellular Ca2+ concentration ([Ca2+]i) increased and exhibited oscillations during further monitoring. It was previously reported that HlyA provoked periodic Ca2+ oscillations in primary rat proximal tubule (RPT) cells, with a constant periodicity of Ca2+ peaks of 12 min. However, we found no constant periodicities but instead found large variations of oscillation kinetics and peak-to-peak spans. Examples are shown in Fig. 1 A–D for Ca2+ tracings and in Fig. 1E for false-color images of [Ca2+]i. No Ca2+ oscillations were induced by the nonhemolytic HlyA mutant S177C/K564R/K690R, which is fully bindable to the plasma membrane but unable to form membrane pores (Fig. 1G ). Statistical analysis of time spans between directly neighboring Ca2+ peaks in Fig. 1A-D and 48 other Ca2+ tracings yielded a most frequent peak-to-peak span (not to be confused with peak periodicity) of 70 s, whereas spans above 10 min were very rare. Peak-to-peak span distribution was dependent on HlyA concentration, whereupon higher concentrations led to shorter time spans.


Figure 1
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Figure 1. Ca2+ oscillations induced by HlyA in IHKE cells loaded with the fluorescent Ca2+ indicator Fura-2/acetoxymethyl ester. A–D) Cells were exposed to HlyA (5 ng/ml) 3 min after start of recording. Traces represent examples of time courses of [Ca2+]i of 4 single cells. E) Single frames from an image series of [Ca2+]i. Frames 1–4 correspond to numbers 1–4 above trace in A. Traces in A and B were recorded from cells that are marked with A and B. F) Superposition of Ca2+ responses of 49 IHKE cells in the presence of nifedipine (100 µM). Application of HlyA (5 ng/ml) is indicated by arrow. Gap represents time when field of view was changed to an area that had not been UV irradiated before. G) Ca2+ tracing of a single IHKE cell on consecutive exposure to a nonhemolytic HlyA mutant (=nh HlyA, 25 ng/ml) and wild-type HlyA (2.5 ng/ml).

2. A periodicity of Ca2+ peaks is pretended by a power spectrum analysis
We subjected the Ca2+ data sets to a power spectrum analysis, which was previously used to identify HlyA-induced periodic Ca2+ oscillations of low frequency. Despite marked heterogeneity of the original Ca2+ tracings and rare occurrence of peak-to-peak spans above 10 min, this analysis yielded a periodicity of Ca2+ peaks with a dominant wavelength of 12.8 min, which was in remarkable agreement with the previously reported value of 12.0 min. Surprisingly, in Ca2+ tracings monitored in the absence of HlyA and devoid of Ca2+ elevations, a periodicity of ~12 min was again computed. Furthermore, analysis of a signal consisting only of white noise superimposed to a discretely drifting baseline yielded the same periodicity. In conclusion, power spectrum analysis appeared as an inadequate mathematical model for a proper interpretation of the Ca2+ data sets.

3. Nifedipine does not inhibit Ca2+ oscillations
When voltage-gated L-type Ca2+ channels in IHKE cells were blocked by nifedipine, HlyA still led to Ca2+ oscillations (Fig. 1F ). This contrasted with previous data of RPT cells where nifedipine abolished the Ca2+ response to HlyA. A striking phenomenon that we observed during the Ca2+ measurements can account for this difference. Nifedipine-treated cells that were in the microscopic field of view for several minutes during Ca2+ imaging, i.e., irradiated by ultraviolet (UV) light, did indeed not show Ca2+ oscillations after application of HlyA, whereas Ca2+ oscillations were observed in cells that had not "seen" UV light (Fig. 1F ). Thus, the previously reported suppressive effect of nifedipine on HlyA-induced Ca2+ oscillations was uncovered as experimental artifact. Additionally, HlyA still led to Ca2+ oscillations in HEK293 cells when a combination of blockers of voltage-gated and receptor-operated Ca2+ channels was present, including nifedipine (100 µM), Cd2+ (2 mM), and SK&F 96365 (25 µM).

4. Ca2+ oscillations and pore formation cease rapidly on removal of HlyA
The effect of HlyA on [Ca2+]i is essentially dependent on the presence of toxin in extracellular medium. Instantaneously after the start of a washout in HlyA-treated IHKE cells, [Ca2+]i decreased and reached initial concentration after ~3 min. Reapplication of HlyA again led to Ca2+ oscillations, which disappeared after the restart of washout. After the start of washout, disappearance of Ca2+ oscillations and HlyA pores followed the same time course. This synchronism was discovered by subjecting single IHKE cells exposed to HlyA to simultaneous measurement of [Ca2+]i and pore formation, using at the same time Ca2+ imaging and electrophysiological patch-clamp recording. A few seconds after the start of washout the number of open pores decreased and went to zero within ~4 min. A second HlyA application again led to pore formation. The short life span of HlyA pores was confirmed by propidium iodide influx measurements. Cells became permeable to dye during incubation with HlyA, but membranes returned to the impermeable state shortly after toxin removal.

5. Ca2+ elevations result from Ca2+ influx through HlyA pores
By simultaneous monitoring of pore formation and [Ca2+]i in IHKE cells exposed to HlyA, we detected an increase in [Ca2+]i directly after pore opening and a good temporal correlation between formation and closure of HlyA pores and Ca2+ elevations. We hypothesize that the decrease after an elevation reflects the restoration of cellular Ca2+ homeostasis by physiological Ca2+ redistribution after HlyA pore closure (Fig. 2 ).


Figure 2
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Figure 2. Schematic overview. Ca2+ oscillations induced by HlyA occur only in the presence of the toxin and are not blocked by nifedipine. After washout of HlyA, Ca2+ oscillations cease rapidly. Readdition of the toxin again leads to Ca2+ oscillations. We assume that the decrease after a Ca2+ elevation is managed by plasma membrane and sarco/endoplasmic reticulum Ca2+ pumps (illustrated by circles with blades).

CONCLUSIONS AND SIGNIFICANCE
The results of this study lead us to a new explanation for Ca2+ oscillations that occur in mammalian cells treated with HlyA. Contrary to a previous report, we showed that the ability of HlyA to induce Ca2+ oscillations does not rely on endogenous L-type Ca2+ channels. Furthermore, we found that the effect of HlyA on [Ca2+]i is not dependent on the activity of any voltage-gated or receptor-operated membrane Ca2+ channels. Instead, Ca2+ oscillations result from pulsed influxes of Ca2+ through short-lived HlyA pores, which are rapidly closed or removed from the membrane. The causal connection was directly seen in simultaneous patch-clamp measurements of pore formation and Ca2+ measurements, where Ca2+ elevations occurred as a consequence of opening of HlyA pores.

Pore formation by HlyA happens at random, which explains our observation that the Ca2+ peaks in individual cells occur in a stochastic sequence. This contrasts a previous claim on the existence of periodic low-frequency Ca2+ oscillations induced by HlyA. However, the mathematical model that this claim was based on turned out as inadequate for a proper interpretation of our measured Ca2+ data. Moreover, we found that the mean time span between two Ca2+ elevations was dependent on the concentration of HlyA, whereupon higher concentrations led to shorter time spans. This concentration dependence definitely rules out the idea that HlyA molecules may switch on in the target cell a periodic "Ca2+ oscillation run" with one defined frequency.

Washout experiments showed that pore formation, propidium iodide influx, and Ca2+ oscillations only occurred as long as HlyA molecules were present at the extracellular side. The observation that the Ca2+ oscillations ceased with the start of washout demonstrates further that the cell has no lasting memory on the encounter with HlyA regarding [Ca2+]i.

Whensoever Ca2+ oscillations are initiated by HlyA, the pore is on its own. Nonperiodic ("chaotic") Ca2+ oscillations resulting from the interplay of formation and disappearance of the pores along with cellular Ca2+ redistribution will obviously vary depending on toxin concentration and susceptibility and may provide the starting point of myriad reactions, but on a very individual basis, in cells attacked by pore-forming toxins such as HlyA.

FOOTNOTES

To read the full text of this article, go to http://www.fasebj.org/cgi/doi/10.1096/fj.05-4561fje

1 These authors contributed equally to this work.




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