Literature DB >> 28177616

Calcium Directly Regulates Phosphatidylinositol 4,5-Bisphosphate Headgroup Conformation and Recognition.

Eva Bilkova1,2, Roman Pleskot3,4, Sami Rissanen5, Simou Sun, Aleksander Czogalla1,6, Lukasz Cwiklik3,7, Tomasz Róg5,8, Ilpo Vattulainen5,8,9, Paul S Cremer, Pavel Jungwirth3,5, Ünal Coskun1,2.   

Abstract

The orchestrated recognition of phosphoinositides and concomitant intracellular release of Ca2+ is pivotal to almost every aspect of cellular processes, including membrane homeostasis, cell division and growth, vesicle trafficking, as well as secretion. Although Ca2+ is known to directly impact phosphoinositide clustering, little is known about the molecular basis for this or its significance in cellular signaling. Here, we study the direct interaction of Ca2+ with phosphatidylinositol 4,5-bisphosphate (PI(4,5)P2), the main lipid marker of the plasma membrane. Electrokinetic potential measurements of PI(4,5)P2 containing liposomes reveal that Ca2+ as well as Mg2+ reduce the zeta potential of liposomes to nearly background levels of pure phosphatidylcholine membranes. Strikingly, lipid recognition by the default PI(4,5)P2 lipid sensor, phospholipase C delta 1 pleckstrin homology domain (PLC δ1-PH), is completely inhibited in the presence of Ca2+, while Mg2+ has no effect with 100 nm liposomes and modest effect with giant unilamellar vesicles. Consistent with biochemical data, vibrational sum frequency spectroscopy and atomistic molecular dynamics simulations reveal how Ca2+ binding to the PI(4,5)P2 headgroup and carbonyl regions leads to confined lipid headgroup tilting and conformational rearrangements. We rationalize these findings by the ability of calcium to block a highly specific interaction between PLC δ1-PH and PI(4,5)P2, encoded within the conformational properties of the lipid itself. Our studies demonstrate the possibility that switchable phosphoinositide conformational states can serve as lipid recognition and controlled cell signaling mechanisms.

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Year:  2017        PMID: 28177616      PMCID: PMC5364432          DOI: 10.1021/jacs.6b11760

Source DB:  PubMed          Journal:  J Am Chem Soc        ISSN: 0002-7863            Impact factor:   15.419


Introduction

Cell signaling pathways are largely organized via a specific recruitment of signaling effector proteins to their target membranes and a confined release of calcium ions. The quintessential example of this is the action of phospholipase C (PLC) that binds and hydrolyzes phosphatidylinositol 4,5-bisphosphate (PI(4,5)P2) in the plasma membrane to diacylglycerol (DAG) and the water-soluble inositol 1,4,5-trisphosphate (IP3), the latter inducing the release of Ca2+ from the endoplasmic reticulum (ER) into the cytosol.[1] Another prominent example is synaptotagmin-1, the main Ca2+ sensor of neuronal exocytosis in the presynaptic axon terminal. Synaptotagmin-1 binding to PI(4,5)P2 directly amplifies protein cooperativity and thus sensitivity to Ca2+ by a factor of >40. This mutual interplay is a critical step in neurotransmitter release.[2] PI(4,5)P2 is enriched in the inner leaflet of the plasma membrane[3,4] and constitutes around 1% of the total anionic phospholipid content in cellular membranes.[5] In comparison with other phospholipids, it contains a rather bulky phosphorylated inositol headgroup with a negative charge ranging from −3 e to −5 e, depending on the pH and the presence of proteins or ions.[6] PI(4,5)P2 and other negatively charged lipids in the cytosolic leaflet are constantly exposed to divalent cations. In resting cells, the free cytosolic Ca2+ concentration is approximately 100 nM.[7,8] The cytosolic concentration of Ca2+ upon cell signaling has been reported to span a wide range from 0.5 μM to several hundred μM, with a half-life of 500 μs to 26 ms.[9−14] Ca2+ influx primarily originates from internal stores within the endoplasmic/sarcoplasmic reticulum or from specialized channels within the plasma membrane providing an essentially infinite supply of extracellular calcium.[9] In all cases, Ca2+ is delivered as brief transients, forming microdomains at the membrane site of influx,[10] and thus, local concentrations of Ca2+ can be expected to exceed cytosolic concentrations by orders of magnitude.[15] Meanwhile, unlike Ca2+, the levels of free, cytosolic Mg2+ are maintained within a fairly narrow concentration range of 0.25–1 mM.[16,17] Interestingly, calcium but not magnesium ions have been ascribed a strong propensity to promote the formation of PI(4,5)P2 clusters as demonstrated in several studies, primarily by using monolayer techniques.[18−22] While the overall effects of divalent cations, including calcium, on PI(4,5)P2 lateral organization have been intensely studied, the mechanism of Ca2+ and PI(4,5)P2 interactions at the molecular level remain unclear. Experiments with pure PI(4,5)P2 monolayers have suggested partial dehydration of both Ca2+ and PI(4,5)P2 upon interaction with each other,[23] triggering an electron density increase in the PI(4,5)P2 headgroup region as well as acyl chain region thickening.[24] Interactions between PI(4,5)P2 and Ca2+ have also been studied computationally. These studies, however, have typically focused on single PI(4,5)P2 molecules[25] or used simplified coarse-grained models[19] that lack sufficient details to deal with specific chemical features of phosphatidylinositides. Herein, we combine protein–lipid binding assays and spectroscopic experiments with atomistic molecular dynamics (MD) simulations employing refined state-of-the art force fields to unravel the functional and structural consequences of the interplay between Ca2+ and PI(4,5)P2. Our data indicate a hitherto undiscovered role and mechanism for Ca2+ in cellular signaling, namely the direct organization of the phosphoinositide headgroup conformation and the selective recognition thereof by the pleckstrin homology (PH) domain of PLC δ1, the canonical PI(4,5)P2 sensor.

Results and Discussion

Protein–Lipid Binding Assays

To determine the equilibrium dissociation constants (KD) for divalent cation/PI(4,5)P2 interaction, we employed a simple fluorescent assay using a supported lipid bilayer platform[26−28] containing 5 mol % of PI(4,5)P2 (for details, see the Supporting Information). Significantly, the KD values differed by less than a factor of 2, with a KD of 0.6 ± 0.2 mM for Ca2+ compared to 1.2 ± 0.2 mM for Mg2+ (Figure S1). We therefore decided to use a cation concentration of 1 mM for all follow-up experiments, matching the free Mg2+ concentration in the cytosol. In order to systematically study the effects of Ca2+ on PI(4,5)P2, we produced 100 nm diameter large unilamellar vesicles (LUVs), facilitating the control of membrane lipid composition and properties. For quality control and physicochemical characterization, all preparations were first subjected to thin layer chromatography (TLC), dynamic light scattering (DLS), and zeta potential measurements (Figure S2). Having the opposite charge of PI(4,5)P2, it is not surprising that Ca2+ and Mg2+ equally reduce the zeta potential of POPC liposomes containing 5 mol % of PI(4,5)P2, the former being described previously.[29] In fact, the presence of either cation attenuates the electrokinetic potential of the membrane down to the level of POPC alone (Figure S2c). Because of its extraordinary stereospecificity, the PLC δ1-PH domain is widely used as the canonical reporter for cellular PI(4,5)P2 levels at the plasma membrane as well as with in vitro assays.[30−34] We therefore used recombinant PLC δ1-PH domain to follow PI(4,5)P2 binding to synthetic liposomes. Size-exclusion chromatography and DLS confirmed that the purified PLC δ1-PH domain (Figure S3a,b) was monomeric in solution, even in the presence of Ca2+ and Mg2+ (Figure S3c,d). Next, we performed liposome flotation assays to follow PLC δ1-PH binding efficiency to POPC/PI(4,5)P2 vesicles. Interestingly, preincubation with 1 mM Ca2+ but not 1 mM Mg2+ fully inhibited liposome binding (Figure a,b). Moreover, PLC δ1-PH did not bind to pure POPC liposomes, highlighting its specificity to PI(4,5)P2.
Figure 1

(a) Setup of the LUV flotation assay. (b) PLC δ1-PH binding to LUVs with POPC/PI(4,5P)2 (95/5 mol %). Error bars are standard deviations of three independent experiments. (c) GUVs after ECFP-PLC δ1-PH addition (green) and Dil as membrane marker (red). The scale bar corresponds to 10 μm. (d) The distribution of median ECFP-PLC δ1-PH intensity per pixel of individual GUVs and different sizes of control (blue) and after preincubation with 1 mM Mg2+ (green) or Ca2+ (red) (data from two additional independent experiments are provided in Figure S5). Each dot represents a single GUV. The number of analyzed GUVs is indicated in the respective color. The median intensity values with mean and standard deviation are depicted in the inset. The Mann–Whitney test was used as significance test (p value <0.0001 for all cases).

(a) Setup of the LUV flotation assay. (b) PLC δ1-PH binding to LUVs with POPC/PI(4,5P)2 (95/5 mol %). Error bars are standard deviations of three independent experiments. (c) GUVs after ECFP-PLC δ1-PH addition (green) and Dil as membrane marker (red). The scale bar corresponds to 10 μm. (d) The distribution of median ECFP-PLC δ1-PH intensity per pixel of individual GUVs and different sizes of control (blue) and after preincubation with 1 mM Mg2+ (green) or Ca2+ (red) (data from two additional independent experiments are provided in Figure S5). Each dot represents a single GUV. The number of analyzed GUVs is indicated in the respective color. The median intensity values with mean and standard deviation are depicted in the inset. The Mann–Whitney test was used as significance test (p value <0.0001 for all cases). Circular dichroism (CD) spectroscopy excluded a direct effect for cations on the secondary structure of the protein (Figure S3e,f). As such, although Ca2+ and Mg2+ bind to PI(4,5)P2 with comparable KD values and reduce electrokinetic membrane properties in an equal manner, only Ca2+ was capable of inhibiting PLC δ1-PH binding. This indicates that PI(4,5)P2 recognition by proteins cannot be solely based on electrostatic interactions. Because a concentration of 1 mM Ca2+ corresponds to twice its KD for PI(4,5P)2 interaction, we performed additional flotation assays with lower Ca2+ concentrations. Here, a significant reduction in protein binding could be observed already at a concentration of 0.6 mM Ca2+ (Figure S4). In this context, recent data by Milovanovic and colleagues show that Ca2+ but not Mg2+ promotes syntaxin-1/PI(4,5)P2 domain formation by an underlying mechanism in which Ca2+ clusters PI(4,5)P2 and syntaxin-1 independently from each other. Moreover, Ca2+ acts as a charge bridge that merges multiple syntaxin-1/PI(4,5)P2 clusters into larger domains. Also here, Ca2+ was found to be effective at a concentration of 0.5 mM while even 1 mM Mg2+ had no effect.[35] Ca2+ binding to membranes has been recently reported to increase with high curvature.[36] We therefore additionally followed the binding of monomeric ECFP-PLC δ1-PH fusion protein to giant unilamellar vesicles (GUVs) (Figure c). Despite limited control over membrane lipid composition at the individual GUV level,[37] GUVs provide the most appropriate synthetic approach for flat and freestanding bilayer systems. In this system, the presence of 1 mM Ca2+ drastically reduced ECFP-PLC δ1-PH binding (Figure d and Figure S5), demonstrating the robustness of the observed effect, irrespective of membrane curvature. Magnesium, however, also reduced ECFP-PLC δ1-PH domain binding, halfway toward the Ca2+ effect. To understand this result, it is important to note that liposome flotation experiments with proteins are nonequilibrium assays because much of the protein stays in the bottom of the tube. At the same time, cation concentrations remain constant, leading to an additional stoichiometric shift. By contrast, protein binding in the GUV experiment is at equilibrium and binding events are quantified at the individual GUV level.

Vibrational Sum Frequency Spectroscopy

To analyze the molecular basis for the cation specificity, vibrational sum frequency spectroscopy (VSFS) was employed to study the effects of Ca2+ and Mg2+ on pure PI(4,5)P2 monolayers at the air/water interface. The spectra were recorded over frequency ranges corresponding to the headgroup and acyl-chain portions of the lipid molecules and included the adjacent interfacial water structure. We present VSFS spectra from the inositol ring and phosphate regions of PI(4,5)P2 in the absence and presence of 1 mM Ca2+ and Mg2+ (Figure a, detailed peak assignments in Figure S6 and Table S1). In the absence of cations in the subphase, both the inositol ring vibrations and the phosphate stretches were rather weak (black data points). This is because of a relatively disordered arrangement of the PI(4,5)P2 headgroups adopted in a pure buffer with a wide range of tilt angles relative to the surface normal. With 1 mM Ca2+, however, the inositol ring signal (961 cm−1 and 1012 cm–1 peaks from the CC and C–O coupled vibrations, respectively)[38] increased substantially (red data points). In fact, the resonances showed 2.7- and 3.6-fold increases, respectively, in oscillator strength (Table S1). These changes reflect both reorientation of the inositol rings and a narrowing of their orientational distribution upon cation binding. Significantly, the changes were not nearly as strong upon the addition of 1 mM Mg2+ (blue data points). In that case, the oscillator strength of the inositol ring vibrations was increased by only a factor of 1.5 and 2.1, respectively. Such results indicated that Ca2+ rigidified the configuration of the PI(4,5)P2 headgroups much more effectively than Mg2+.
Figure 2

VSFS spectra of (a) the inositol ring and phosphate regions and (b) the carbonyl C=O symmetric stretch region of PI(4,5)P2 on a buffer subphase (black spectra) containing 1 mM MgCl2 (blue spectra) or 1 mM CaCl2 (red spectrum) at a surface pressure of 17 mN/m. The open circles represent VSFS data points, and the solid lines are fits to the data. All spectra were taken with the ssp polarization combination. Spectra of the same data offset along the y-axis are provided in Figure S7. Details of monolayer preparation and images are provided in Figure S14.

VSFS spectra of (a) the inositol ring and phosphate regions and (b) the carbonyl C=O symmetric stretch region of PI(4,5)P2 on a buffer subphase (black spectra) containing 1 mM MgCl2 (blue spectra) or 1 mM CaCl2 (red spectrum) at a surface pressure of 17 mN/m. The open circles represent VSFS data points, and the solid lines are fits to the data. All spectra were taken with the ssp polarization combination. Spectra of the same data offset along the y-axis are provided in Figure S7. Details of monolayer preparation and images are provided in Figure S14. In addition to the inositol ring modes, the phosphate peaks (e.g., symPO32– at 982 cm–1, symPO2– at 1086 cm–1, asyPO32– at 1115 cm–1, asyPO2– at 1154 cm–1, detailed assignments in Figure S6 and Table S1) also showed a substantial intensity increase upon the introduction of Ca2+ to the subphase. This indicates a strong net orientation and/or ordering of the headgroup phosphates upon Ca2+ binding. It should be noted that Ca2+ binding may help to deprotonate the second monoesterified phosphate,[25] which would prompt additional changes in the spectra beyond those related to ordering and tilt angle. Moreover, upon the addition of Ca2+, the symmetric PO32– stretch exhibited a relatively large 20 cm–1 blue shift, while the asymmetric PO32– and PO2– stretches shifted by 6 cm–1 and 8 cm–1, respectively (Table S1). The shifts of both PO32– peaks are consistent with phosphate dehydration upon cation binding and/or a symmetry change of the C3 point group.[39,40] The shift of the asymmetric PO2– peak also suggests headgroup phosphate dehydration upon Ca2+ binding.[40−42] The spectral change brought about by 1 mM Mg2+ in the phosphate region was much less pronounced overall compared to that with 1 mM Ca2+. The difference in the interactions of Ca2+ and Mg2+ with phosphate could be explained at least in part by different dehydration penalties for these two cations. It has been suggested that Ca2+ binding to phosphate groups is favored because Ca2+ is more easily dehydrated than Mg2+.[23] This difference in the hydration shell chemistry may, in turn, act to disfavor the bridging of the inositol rings of PI(4,5)P2, which would weaken the ordering effect of Mg2+. In addition to phosphate and inositol resonances, VSFS spectra were also obtained in the carbonyl C=O symmetric stretch (1730 cm–1)[43] region before and after addition of 1 mM CaCl2 or MgCl2 (Figure b). Again, Ca2+ showed a more prominent effect on the PI(4,5)P2 than Mg2+. In fact, a 1.6-fold increase in the oscillator strength of this peak was observed upon binding of Ca2+, while only a 1.3-fold increase was found for Mg2+ (Table S2). This oscillator strength increase should correspond to a backbone ordering effect, thus helping to reinforce a more rigid configuration of the headgroup inositol rings. Ordering of the lipid acyl chains was also observed (Figure S8 and Table S3).[44] Taken together, the changes in the VSFS spectra provide strong experimental evidence for distinct conformational changes within the lipid headgroup region in the presence of Ca2+, but less with Mg2+. Such results should be important for the PLC δ1-PH domain selectivity of PI(4,5)P2 found above with liposomes and GUVs.

Atomistic Molecular Dynamics Simulations

With the aim of obtaining mechanistic insights into the effects of Ca2+ and Mg2+ on PI(4,5)P2 molecules at a molecular level, we employed atomistic MD simulations. In order to reduce methodological bias, we used two all-atom force fields (OPLS-AA and CHARMM36) as well as the united-atom force field from Berger (Table S4).[45−47] Importantly, to further account for electronic polarization effects of charged groups in a mean field manner, for Ca2+ interacting with PI(4,5)P2 phosphates we also employed the recently developed electronic continuum correction with rescaling (ECCR) method.[48] This, to a large extent, dampens the unrealistically high ion pairing found when employing nonpolarizable force fields.[48] It is particularly useful in the present case where strong electronic polarization can be expected in the vicinity of multiple-charged moieties. We generated multiple sets of 1 μs long trajectories for different initial PI(4,5)P2 distributions prior to and after the addition of Ca2+ or Mg2+. For all simulations, consistently with all force fields used, we find that Ca2+ interacts with PI(4,5)P2 and has a pronounced effect on the lipid headgroup orientation (Figure and Figures S9 and S13). Moreover, control simulations with Mg2+ showed that the effects induced by magnesium are much weaker than those induced by calcium for all simulations (Figure c,d and SI), in full agreement with experiments.
Figure 3

Snapshots from MD simulations of the lipid bilayer taken at 1 μs (a) without and (b) with Ca2+. (c) Tilt angle distribution of the PI(4,5)P2 headgroup and (d) density profiles of lipid headgroups without (blue) and with Mg2+ (green) or Ca2+ (red). Numbers in (c) represent mean tilt angles for each system. Here, only the results of the Berger force field simulations are presented. Additional force field simulations with similar outcomes can be found in the Supporting Information.

Snapshots from MD simulations of the lipid bilayer taken at 1 μs (a) without and (b) with Ca2+. (c) Tilt angle distribution of the PI(4,5)P2 headgroup and (d) density profiles of lipid headgroups without (blue) and with Mg2+ (green) or Ca2+ (red). Numbers in (c) represent mean tilt angles for each system. Here, only the results of the Berger force field simulations are presented. Additional force field simulations with similar outcomes can be found in the Supporting Information. The addition of Ca2+ or Mg2+ immediately leads to a significant reduction of the area per lipid (Figure S10 and Table S5). This macroscopic effect is in agreement with lateral condensation of the PI(4,5)P2-containing monolayers by Ca2+ [20,22−24] and our VSFS analysis of the CH stretches (Figure S8). At the microscopic level, we found that each PI(4,5)P2 molecule binds on average 1.6–3.1 Ca2+ molecules, depending on the force field that is employed (Table S5). This is consistent with the water peak spectral changes, which show that each lipid molecule binds more than two Ca2+ ions (Figure S8). Ca2+ binds mostly to the phosphate groups at positions 4 and 5, but it also penetrates deeper into the lipid bilayer to interact with the carbonyl groups (Figure S11). Ca2+ binding to the lipid carbonyl group is consistent with the VSFS data in the carbonyl stretch region, as documented herein (Figure b) and elsewhere.[49−53] In agreement with previously published computational and experimental results,[24,50] we observed that Ca2+ increases the order parameters of the PI(4,5)P2 acyl chains (Figure S12). The acyl chain ordering is also fully in line with the effects observed in the VSFS spectra (Figure S8). The most prominent feature observed by simulations is a pronounced headgroup reorientation, primarily caused by the ability of Ca2+ to bridge two PI(4,5)P2 headgroups (Figure a,b). This result was found regardless of which force field was used. To quantitatively analyze the headgroup reorientation, we monitored the tilt angle between the C1–C4 atoms of the PI(4,5)P2 inositol ring and the bilayer normal. The average tilt angle in the control simulation without Ca2+ was in the range of 35–41°, depending on the employed force field. This result is in agreement with previously published MD studies.[54−56] In the presence of Ca2+ ions, however, the average tilt angle significantly increased for all of the force fields up to 65° (Figure c and Figures S9 and S13). Simulations thus consistently showed bending of the PI(4,5)P2 headgroup toward the plane of the bilayer and away from bulk water (Table S5). Moreover, consistent with a narrowing of the inositol ring’s distribution as indicated by VSFS results above (Figure a), Ca2+ slowed PI(4,5)P2 headgroup rotational diffusion as revealed by the rotational correlation function (Figure S9e). The Ca2+ effect was also manifested in the density profiles (Figure d), where the location of the PI(4,5)P2 headgroups shifted in the presence of calcium toward the bilayer center. Moreover, Ca2+ significantly decreased the solvent accessible surface area of PI(4,5)P2, which correlated with a reduced average number of hydrogen bonds between the PI(4,5)P2 headgroups and water molecules (Table S5). These data also match the experimentally observed partial dehydration of PI(4,5)P2 in the presence of Ca2+ as measured here by VSFS and elsewhere.[23] The charge state of PI(4,5)P2 in lipid membranes is highly sensitive to the cellular pH and the presence of proteins and ions.[6,57] By using not only the default parametrization (CHARMM36 and OPLS-AA) but also the ECCR corrected charges for the ions and PI(4,5)P2 phosphate groups (Berger, OPLS-AA), we were able to assess the potential effects of the lipid charge state. Namely, the charge used for PI(4,5)P2 varied from −3.75 to −5, depending on the particular force field (for more details, see the SI). Reassuringly, we found semiquantitatively the same effect of Ca2+ on the PI(4,5)P2 tilt angle with Ca2+ in all the systems which were tested. This indicates that under the conditions of these investigations the protonation state of PI(4,5)P2 was not particularly critical for the observed effects.

Conclusion

By means of protein–lipid binding assays and spectroscopic experiments, together with atomistic MD simulations, we have unraveled and characterized in molecular detail the pronounced effect of Ca2+ on PI(4,5)P2 headgroup presentation. First, we confirmed the previously observed increase of the PI(4,5)P2 acyl chain order and PI(4,5)P2 cluster formation,[18−21] as evidenced here by VSFG spectroscopy and MD simulations. Second, we characterized at the molecular level the interactions of Ca2+ with PI(4,5)P2 headgroup phosphates, as well as the more deeply seated carbonyl groups. We observed the hitherto unrecognized consequences of Ca2+ binding for PI(4,5)P2 at the molecular level. Namely, we observed a dramatic change in the PI(4,5)P2 headgroup tilt angle. By means of liposome flotation and GUV binding assays, we show that Ca2+ has a strong propensity to render the PI(4,5)P2 headgroup invisible to the PLC-δ1 PH domain. Our data lead to the plausible conjecture that the calcium-induced switching of phosphoinositide conformational states may serve as a potential cellular mechanism for lipid recognition and thus play a decisive role in cell signaling and membrane trafficking. A systematic correlation of kinetics and curvature sensitivities at the nanoscale in vitro(58) will be key to understanding the general applicability of our data to other proteins and to different endomembranes.
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