|Home | About | Journals | Submit | Contact Us | Français|
Progress in the biology of myo-inositol hexakisphosphate (InsP6) has been delayed by the lack of a quantitative description of its multiple interactions with divalent cations. Our recent initial description of these [J. Torres, S. Dominguez, M.F. Cerda, G. Obal, A. Mederos, R.F. Irvine, A. Diaz, C. Kremer, J. Inorg. Biochem. 99 (2005) 828–840] predicted that under cytosolic/nuclear conditions, protein-free soluble InsP6 occurs as Mg5(H2L), a neutral complex that exists thanks to a significant, but undefined, window of solubility displayed by solid Mg5(H2L) · 22H2O (L is fully deprotonated InsP6). Here we complete the description of the InsP6–Mg2+–Ca2+ system, defining the solubilities of the Mg2+ and Ca2+ (Ca5(H2L) · 16H2O) solids in terms of Ks0 = [M2+]5[H2L10−], with pKs0 = 32.93 for M = Mg and pKs0 = 39.3 for M = Ca. The concentration of soluble Mg5(H2L) at 37 °C and I = 0.15 M NaClO4 is limited to 49 μM, yet InsP6 in mammalian cells may reach 100 μM. Any cytosolic/nuclear InsP6 in excess of 49 μM must be protein- or membrane-bound, or as solid Mg5(H2L) · 22H2O, and any extracellular InsP6 (e.g. in plasma) is surely protein-bound.
myo-Inositol hexakisphosphate (InsP 6, derived from inositol hexaphosphoric acid C6H18O24P6, abbreviated in this work as H12L) is an ubiquitous and abundant metabolite in eukaryotic cells (reviewed in [1–3]). It is the precursor of at least two inositol pyrophosphates; these less abundant, fast-turnover metabolites, have been assigned a variety of functions including the regulation of membrane trafficking, telomere length, and membrane–protein interactions involved in chemotaxis (reviewed in ). However, the functions of InsP 6 itself are still poorly understood. In mammalian cells, it is a necessary cofactor for the repair of double-stranded breaks in DNA, through the binding of the Ku component of DNA-PK, and is necessary for RNA editing events, through its binding of some of the adenosine deaminase enzymes [5–8]. In yeasts, the compound is necessary for mRNA export from the nucleus, through as yet undefined protein targets [9–11]. In addition, InsP 6 may contribute to localise PDK-1 to the cytosol, by competing for the enzyme’s PH domain with plasma membrane phosphoinositides . InsP 6 concentrations in animal and yeast cells are not thought to undergo acute fluctuations under normal physiological conditions: the three functions mentioned above are apparently fulfilled by basal concentrations of InsP 6. In plant cells, InsP 6 levels can have significant signalling roles by regulating K+ and Ca2+ fluxes [13,14]. In addition, a major function of InsP 6 in plants is to give rise to deposits for the storage of phosphorus and metal cations, as further discussed below.
In addition to the apparently unconnected set of roles mentioned above, InsP 6 has been assigned a bewildering number of other biological functions as well as pharmacological actions. This has been critically reviewed by Shears who pointed out that a number of the proposals in the literature may arise from experimental artefacts . Indeed, it is easy to run into artefacts when carrying out biological experiments with InsP 6. This stems from: (i) the compound being abundant, and so including high concentrations of it in experiments is initially justified, and (ii) its chemistry of interaction with divalent cations being complicated, non-intuitive, and so far poorly described. This chemistry encompasses solution complexation and precipitation reactions. Complexation can deplete solutions of divalent cations, while precipitation (easily unnoticed when working with small volumes) can not only deplete divalent cations, but also acidify the solutions and interfere with assays per se.
Equally seriously, the lack of understanding of InsP 6 chemistry means that the physical and chemical forms of the compound in cells are still partially obscure. This problem is compounded by the questions about the cellular distribution of InsP 6. Most InsP 6 in mammalian cells is thought to be cytosolic and/or nuclear . In addition, in plants [16–18], and in a particular (invertebrate) animal system [19,20], the compound occurs in vesicular/vacuolar and/or extracellular compartments, there appearing as “phytate deposits”, i.e. InsP 6 salts with monovalent, and mostly divalent, cations. Speculations on the status of InsP 6 in mammalian cells encompass the possible existence of vesicular pools as well as of insoluble deposits in cytosol (see for example [15,21]). In addition, dietary InsP 6 has been shown to be absorbed in the intestine, circulate in plasma, and to be excreted in urine (reviewed in ).
The chemistry of InsP 6 in solution in the presence of divalent cations has been addressed in several works (see in particular [23,24]). However, this chemistry was only comprehensively described, and its biological consequences directly inferred, in our recent study . A major feature of this chemistry is that InsP 6 forms high-affinity complexes of 1:1 stoichiometry with divalent (and trivalent) cations; this is the dominant behaviour when InsP 6 is in molar excess with respect to cation(s). A further, biologically significant, feature of the solution chemistry is that InsP 6 also forms, in the presence of molar excess of Mg2+, the neutral soluble species Mg5(H2L) (where L denotes fully deprotonated InsP 6). Under cytosolic or nuclear conditions, all soluble InsP 6 not bound to proteins or other organic components is predicted to be found in this form (InsP 6 binds at least certain proteins bearing very basic sites in Mg2+-free form ). Although we verified experimentally that relevant concentrations of Mg5(H2L) could exist under cytosolic/nuclear conditions, the species is only sparingly soluble; in fact, isolation of the corresponding solid, Mg5(H2L) · 22H2O, was straightforward . The significant (though small) solubility of Mg5(H2L) is a peculiarity, not displayed by other divalent cations, Ca2+ included: the dominant aspect of InsP 6 chemistry under molar excess of the divalent (or trivalent) cations is the formation of solids.
The limited solubility of its presumed cytosolic form Mg5(H2L), plus the proven formation of solids by InsP 6 in certain biological contexts (and the possibility of this taking place in others), call for a quantitative description of the solubility behaviour of this metabolite. The experimental problems (described above) arising from not being able to predict this behaviour also call for such a study, and this in turn requires the stoichiometries of the solids to be known. Stoichiometries reported for the divalent metal solids of InsP 6 range from 4:1 to 6:1 (metal:InsP 6 ratios); the 5:1 ratio, as we found for the Mg2+ solid , is the one reported most often [23,24,26–29]. The precipitation equilibria are tied to the complexation and protonation equilibria in solution, so the quantitative description of these  is also needed to describe the solubility behaviour. In the present work, we have determined the stoichiometry of the Ca2+ salt of InsP 6; together with the data in our previous work, this allowed us to translate analytical measurements of total Ca and Mg at equilibrium with the solid phytates into solubility product constants for the two salts. Therefore a full description of the InsP 6–Ca2+–Mg2+ system has resulted. The data put an upper limit to the concentration of InsP 6 that can exist in cytosol or nucleus of mammalian cells in protein-free, soluble form, a limit that is within the range of available estimates of the total InsP 6 concentration in cells. Our data also indicate that protein-free extracellular InsP 6 cannot exist in solution. In addition, we have been able to summarise the complex and non-intuitive solubility behaviour of InsP 6 in a series of plots that indicate clearly whether total, partial or nil solubility is to be expected across a wide range of conditions.
All common laboratory chemicals were reagent grade, purchased from commercial sources and used without further purification. CaCl2 · 2H2O, and MgCl2 · 6H2O, were used as metal sources. Phytate solutions for the synthesis of the complexes were prepared by dilution of a phytic acid solution in water (40 wt.%; Aldrich). Solutions were used immediately after preparation. Ultrapure water obtained from a Millipore-MilliQ plus system was used throughout this work.
Infrared spectroscopy was carried out on a Bomen FT-IR spectrophotometer, with samples present as KBr (1%) pellets. Thermal analysis was performed on a Shimadzu DTA-50, TGA-50 instrument with a TA 50I interface, using a platinum cell and nitrogen atmosphere. Experimental conditions were 1 °C min−1 temperature ramp rate and 50 mL min−1 nitrogen flow rate.
Elemental analysis (C, H) was performed on a Carlo Erba EA 1108 instrument. Na and K were determined by atomic absorption spectroscopy on a Perkin–Elmer 5000 instrument. Ca content was determined gravimetrically as CaC2O4 as follows: calcium phytate was dissolved in 2 M HCl and 100% excess of H2C2O4 · 2H2O was added and the pH of the solution was raised with NH4OH (7.4 M) up to 1.5–3.0. Calcium oxalate then precipitated, and was washed with water (2 × 5 mL), centrifugued, and dried at 70 °C for 12 h.
The magnesium compound was prepared as previously reported . Preparation of [Ca5(H2L)] · 16H2O followed a similar procedure. An aqueous solution of InsP 6 (0.01 M) was prepared and its pH adjusted to 10–11 by addition of LiOH (1 M). To this solution (30 mL; 0.3 mmol), CaCl2 · 2H2O (0.22 g; 1.5 mmol) dissolved in the minimum amount of water was added. A white solid immediately appeared, which was separated by centrifugation, thoroughly washed with water (3 × 10 mL), and dried with ethanol (2 × 10 mL). Yield was 37% (126 mg). Elemental analysis calcd (%) for Ca5C6H40O40P6 (1138.59): C 6.3, H 3.5, Ca 17.6; found C 6.4, H 3.3, Ca 17.7. Thermal analysis agreed with the proposed formula: 25.3% weight loss corresponding to the elimination of water, compared with a calculated value of 25.6%. IR (KBr pellets) ν = 3447 (ν O–H), 1114 (ν P–O), 545 (ρ w, H2O) cm−1.
Solubility measurements were carried out at constant ionic strength I = 0.15 M NaClO4, and 37.0 °C. Approximately 50 mg of the compound (Mg or Ca phytate) was suspended in 0.15 M aqueous NaClO4 (Mg, 20.0 mL; Ca, 15.0 mL). Known amounts of HCl were added, so as to reach equilibrium points corresponding to measurable amounts of metal in solution (Table 1 ). Each mixture was kept in a glass jacketed cell under continuous stirring until measured pH was constant (ca. one week). After the equilibrium was reached, excess solid was filtered out (Macherey–Nagel MN 640 m paper), and the metal concentration was determined in the supernatant. Mg was determined volumetrically according to standard techniques . Ca was determined as described in Section 2.2. With these M2+ concentration values, and assuming a 5:1:2 stoichiometry (M2+:InsP 6:H+), total amounts of InsP 6 were calculated. Then total concentrations of M2+, InsP 6 and H+ were used as inputs in the HySS software  to determine the equilibrium concentrations of (free) M2+ and H2L10−, which define the K s0. In this calculation, the complete set of equilibria involved  was taken into account. At least four independent determinations were performed for each metal.
As mentioned, previous works dealing with the interaction of M2+ ions with InsP 6 under metal excess report the formation of very insoluble compounds having M2+:InsP 6 ratios of 4:1, 5:1 or 6:1 [23–29]. The solids contain large amounts of crystallization water, which hampers their full characterization. An additional feature reported is the presence of mixed salts containing two cations (for example Ca and Na, Ca and Zn, etc.) [31–34] or two anions (Cl− and InsP 6) .
We previously prepared and characterized by several techniques the salt [Mg5(H2L)] · 22H2O . In our hands, the calcium analogue formed under straightforward conditions fitted perfectly this same (5:1) stoichiometric ratio. The solid incorporated 16 water molecules, thus responding to the formula [Ca5(H2L)] · 16H2O. The presence of a large amount of crystallized solvent was qualitatively evident from the strong and broad absorption in the IR spectrum at 3447 cm−1. Quantification of water content by thermogravimetric analysis showed that the sixteen water molecules were lost across a wide temperature range, namely between 50 and 210 °C.
To assess whether the Mg2+ and Ca2+ solids can change their compositions in the presence of Na+ or K+, we performed the syntheses as described in Section 2 but in media containing either 0.15 M NaClO4 or 0.15 M KCl. The solids so obtained agreed perfectly with the expected formula . Na or K determinations by atomic absorption demonstrated that only residual amounts (i.e. less than 0.1% molar ratio with respect to M2+) of the alkaline cations were present, probably as occluded chloride salts not eliminated during the washing procedure. Thus the formation of mixed cation compounds with fixed M2+/Na or M2+/K stoichiometries can be ruled out under these experimental conditions.
Mg and Ca phytates are only sparingly soluble in water. Given their stoichiometries, the solubilities of these solids will be governed by solubility product constants with the form: K s0 = [M2+]5[H2L10−]; the constant K s0 depends only on the temperature. It is easy to appreciate that precipitation of Mg or Ca phytate depends strongly on the concentration of free Ca2+ or Mg2+ in the system. Moreover, it further depends on the concentration of di-protonated phytate, H2L10−. This is very much a minority species for soluble InsP 6 under most conditions, the dominant species being the less highly charged ones, in which the anion is associated with more protons, and/or monovalent and/or divalent cations . This notwithstanding, with other conditions fixed, the concentration of H2L10− (a highly deprotonated species) can be expected to increase as pH is increased. This rationalises the straightforward observation that phytates are more soluble under acidic than under basic conditions. A closely related point is that the precipitation of phytates will tend to acidify the solutions in which it takes place. For example, the dominant InsP 6 species in solution in the absence of divalent cations and at neutral pH have three and four protons . Addition of sufficient calcium or magnesium removes, through precipitation, H2L10− from solution. This species is in turn replenished at the expense of the more highly protonated forms of soluble InsP 6, with the release of protons into solution.
Determination of the K s0 values obviously requires measuring sets of values for the concentrations of H2L10− and of free metal at equilibrium with the solids. These can in turn be calculated from the straightforward analytical data by means of an appropriate software such as HySS  fed with the complete set of equilibrium constants for the protonation and complexation equilibria . We thus equilibrated the solid phytates with unbuffered, M2+-free, dilute acid at 37.0 °C and under physiological ionic strength. Then total Ca or Mg in solution were determined, and the amounts of InsP 6 that went into solution calculated as 1/5 the former figures. From the total concentration of InsP 6, M2+, and total exchangeable protons present in the solution, the HySS software calculated concentrations of H2L10− and of free metal, yielding in turn estimations for pK s0 (i.e. −log K s0). The results shown in Table 1 can be summarised in the solubility products:
which are valid at I = 0.15 M NaClO4 and 37.0 °C.
The higher pK s0 value for Ca reflects the lower solubility of Ca phytate in comparison to its Mg analogue. With these values in hand, it was possible to calculate the solubility of both compounds in water at different pH values (under physiological ionic strength and in the absence of added Ca2+ or Mg2+), as shown in Table 2 .
The pK s0 values for the solid phytates, together with the protonation and Ca and Mg complexation constants in solution previously reported by us  allow a complete description of the behaviour of InsP 6 in the presence of Ca2+ and/or Mg2+. Since this is a system comprising 22 equilibrium equations, it can only be handled by specialised software such as HySS .
Fig. 1 summarises the behaviour of InsP 6 in the presence of Ca2+. It can be seen that at pH 7.5 Ca2+ causes InsP 6 to fall out of solution even at very low concentrations of the polyphosphate. At a fixed total calcium concentration, as the total InsP 6 concentration is raised, the abundance of the solid phytate increases, reaching a maximum near to the stoichiometric (5:1) calcium:InsP 6 ratio. As InsP 6 concentration is increased beyond this point, the solid (Fig. 1a) is gradually replaced by the soluble 1:1 complexes (Fig. 1b). This is the “paradoxical” solubility behaviour of InsP 6, whereby for some concentration ranges, adding InsP 6 to a partially insoluble system causes it to become fully soluble. This behaviour can be rationalised on the basis of the excess InsP 6 acting, through the formation of the soluble 1:1 complexes, as a calcium sequestering agent. Thus in this context the addition of excess InsP 6 is analogous to the addition of EDTA (ethylenediaminetetraacetate), the system’s solubility being therefore caused by the absence of free Ca2+. The broad features of the InsP 6-calcium system do not vary to a great extent with pH, except for strongly acidic conditions, i.e. pH 3 and below. For these acidic conditions, the range of dominance of solid phytate shrinks, with a concomitant increase in the dominance range of the 1:1 complexes (Fig. 1c and d). This is the consequence of the linked equilibria established by soluble InsP 6 being shifted away from H2L10− towards the more highly protonated species as well as the 1:1 complexes that these can form with Ca2+.
The behaviour in the presence of Mg2+ is slightly more complex. This is due to the 5:1 species having a significant window of solubility, a feature that is undetectable in the case of Ca2+ . Thus under Mg:InsP 6 excess, the dominant species in solution is the neutral 5:1 complex. However, beyond a certain concentration, this species precipitates, as [Mg5(H2L)] · 22H2O. Hence, to summarise the behaviour of the InsP 6–Mg2+ system, three major forms need to be considered: the solid, the soluble 5:1 species, and the soluble 1:1 complexes (Fig. 2 ). With respect to the solid and the soluble 1:1 complexes, the overall behaviour is similar to that described previously for Ca2+ (Fig. 2a and c). However, the lower pK s0 of the system is reflected in a significant region of full solubility even under conditions of metal excess (compare Fig. 2a, inset with Fig. 1a, inset); in this window, virtually all of the InsP 6 is present as the soluble neutral 5:1 species (Fig. 2b). Interestingly, the concentration of this soluble 5:1 complex has an upper limit at 49 μM, as figure that is fixed, irrespective of total InsP 6 concentration, size of the Mg2+ excess, or pH. Mathematically, this is the consequence of the fact that multiplying the expression for the equilibrium constant for the formation of the soluble 5:1 complex 
by the expression for the solubility product constant
In other words, the concentration of soluble pentamagnesium species at equilibrium with solid magnesium phytate is a constant at a given temperature. Under conditions of Mg2+ excess, increasing total InsP 6 beyond 49 μM always means that the concentration of the soluble pentamagnesium complex also breaks the 49 μM barrier, and hence solid magnesium phytate starts to accumulate (Fig. 2a and b). The overall behaviour of the Mg2+–InsP 6 system is fairly invariant for pH values above 6. However, at acidic pH values the ranges of formation of the soluble and solid 5:1 species shrink. This behaviour is similar to that of the Ca2+ system but more pronounced, being very marked already at pH 4.5 (Fig. 2d–f).
The behaviour of the system with both Ca2+ and Mg2+ present is broadly similar to the single-metal ones just described, as long as the concentrations of the two cations are considered together. As previously described, molar excesses of cation over InsP 6 are accompanied by precipitation, while molar excesses of InsP 6 result in soluble 1:1 complexes. Within the range of formation of the solids, the more insoluble calcium phytate dominates over its magnesium counterpart. Notwithstanding, as long as the Ca2+:InsP 6 ratio is less than 5, and Mg2+ is abundant, magnesium phytate does precipitate together with calcium phytate (Fig. 3 a). For InsP 6 concentrations below 49 μM and similar concentrations of Ca2+, the presence of excess Mg2+ actually confers solubility to the system, as InsP 6 is drawn towards the soluble pentamagnesium complex (Fig. 3b).
The chemical data presented above make it possible to predict the speciation of InsP 6 under biological conditions. The most relevant of these conditions are those of cytosol and nucleus, in which most or all of the InsP 6 in typical animal cells is probably present . In our previous paper , to simulate cytosolic/nuclear conditions we had set the prediction conditions at pH 7.4  and 0.5 mM free Mg2+ ; Ca2+ signals were taken into account by including total Ca2+ concentrations of up to 10 μM (reviewed in ). Those calculations indicated that all InsP 6 not bound to protein and/or membranes existed as the pentamagnesium complex . At the time we did not have the solubility product constants, and so we stated that the validity of our predictions was restricted to the solubility range of magnesium phytate. When predictions including the precipitation equilibria are run for the set of conditions detailed above and InsP 6 concentrations between 1 and 100 μM, the following results are obtained: (i) there is no association with Ca2+, whether in solution or in the solid phase; (ii) up to a total concentration of 49 μM, InsP 6 is present exclusively as the soluble pentamagnesium complex; (iii) any InsP 6 in excess of 49 μM, is present as solid magnesium phytate. Therefore our previous predictions are confirmed, but a complication arises as a result of the limited solubility of Mg5(H2L).
Estimations of total InsP 6 concentrations in mammalian cells are mostly in the 10–60 μM range, with data from some cell lines going up to 105 μM [39–45]. As these estimations do not take cell compartmentalisation into account, actual concentrations are probably higher. It is conceivable that InsP 6 in cells is at equilibrium with its solid magnesium salt – note that massive amounts of solid magnesium InsP 6 exist in a peculiar biological system, namely within specialised cells of the dispersal larva of the mesozoan Dicyema typus . However, we envisage as the more likely possibility that the InsP 6 pool available for the formation of Mg5(H2L) is kept below 49 μM in typical eukaryotic cells. From this standpoint, any InsP 6 in excess of this figure would be bound to cellular components such as proteins and/or cell membranes . Polyamines are unlikely to contribute substantially to the InsP 6-binding capacity of the cell. This reasoning is based on the facts that: (i) once association with nucleic acids and nucleotides is taken into account, the remaining pools of spermidine and spermine are relatively small , and (ii) InsP 6 affinity constants reported for polyamines are not large enough for effective competition with the more abundant Mg2+, except in the case of the tri-protonated forms of polyamines, which represent only a minor proportion at physiological pH .
In summary, our data suggest that InsP 6 in the cytosol and nucleus of mammalian cells is close to the saturation of its solubility. Therefore the manipulation of cells so as to increase their InsP 6 concentrations to a significant extent (e.g. [50–52]) probably causes the intracellular precipitation of magnesium phytate. It is worth commenting at this point that although, as mentioned, InsP 6 has a second range of solubility at concentrations in molar excess with respect to total Mg2+ plus Ca2+, these conditions are non-physiological, as they entail the complete absence of free divalent cations.
The case of slime molds deserves a special mention is this context. The overall concentration of InsP 6 in Dictyostelium discoideum amoebae has been estimated at 0.7 mM ; no information on the intracellular distribution of the compound is available. Our data predict that whatever its localisation, most of this InsP 6 must be present in a physicochemical form other than the soluble pentamagnesium species. It seems likely that InsP 6 in D. discoideum may form deposits in so-called “mass-dense granules” or “polyphosphate bodies”; these are acidic organelles rich in P, Mg and Ca, which are now known to be intimately related to the contractile vacuoles [54–57]. Phosphorus in these granules has been ascribed to inorganic pyrophosphate and polyphosphates [54,55]; however, the presence of InsP 6 in them, suggested by Schlatterer et al. , has not yet been assessed. Electron-dense granules ascribed to polyphosphate deposits have been also described, though in lesser abundance, in the cytosol, nucleus and mitochondria of D. discoideum . As the overall Ca2+:InsP 6 molar ratio in D. discoideum amoebae is less than 1 , phytate deposits can be expected to be formed mostly by magnesium phytate, irrespective of their localisation. If indeed localised in the acidic “mass-dense granule” vacuoles, the InsP 6 solid(s) would be at equilibrium with significant concentrations of the soluble compound. This would both make the InsP 6 pool a metabolically active one, and allow the compartment’s osmolarity to be regulated through the pH-dependent solubilisation/precipitation of InsP 6.
The pK s0 of calcium phytate is very high. Therefore the set of equilibria described in this work and the previous one  allow no soluble InsP 6 under conditions that include physiological pH and extracellular concentrations of free Ca2+ and Mg2+. Being present at concentrations similar to those of Ca2+, Mg2+ has no impact on the system, so InsP 6 is predicted to be entirely in the form of solid calcium phytate. This is basically the case of the only known system that displays extracellular accumulation of InsP 6, namely the larva of the cestode parasite Echinococcus granulosus [19,20]. However, a soluble extracellular InsP 6 pool has also been suggested to exist in mammals: although widely varying according to diet, InsP 6 levels in human or rat plasma have been reported to reach around 0.5 μM [58,59]. Our data predict that this extracellular pool will be associated with carrier proteins. A further important consequence of our results is that experiments in which exogenous InsP 6 is added to cells in culture (see for example [60–62], out of an extensive literature) have to be examined with caution. The two obvious possibilities are: i) cells are being fed particulate calcium phytate, with concomitant lowering of the Ca2+ concentration, and possibly also pH, of the medium (when using sub-millimolar InsP 6 concentrations), and ii) the medium is being depleted of free Ca2+ and Mg2+ through complexation in solution (when millimolar InsP 6 doses are used). A third possibility (only likely to apply for InsP 6 concentrations in the μM range) is that the medium may contain proteins with sufficient InsP 6-binding capacity as to keep it soluble.
Phytate has long been recognised to interfere with the absorption of Zn, Fe, and Ca in the gut (reviewed in ). Our data provide a rationale for explaining the effect on Ca, and possibly on the remaining metals mentioned. The bulk of the phytate counterions in cereals is accounted for by Mg and K [17,18]. Under highly acidic digestion conditions in the stomach (pH 1–2), these InsP 6 salts are expected to dissolve. Corn grain for example contains approximately 4 mol of Mg per mol of InsP 6 (Max Tate, University of Adelaide, personal communication, based on data in ); therefore almost any Ca or additional Mg in the meal would put the system under conditions of divalent metal excess with respect to InsP 6. In consequence, under duodenal conditions (pH 6–7), InsP 6 is predicted to (re-)precipitate. Our data predict that this precipitation will take virtually all Ca2+ present (plus enough Mg2+ as to complete the 5:1 M2+:InsP 6 ratio). In other words, the acidification-neutralisation cycle in vertebrate digestion allows cations that form relatively more soluble solids with phytate to be replaced by those that form less soluble solids. Thus it may be precipitation, and not complexation in solution, that is the most likely reason for Ca malabsorption by phytate. Although pK s0 values for the corresponding solids are not yet available, the same mechanism probably applies to malabsorption of Fe and Zn.
The data in this paper provide a few simple “rules of thumb” to keep experiments involving InsP 6 within reasonably physiological conditions. When mimicking cytosolic/nuclear conditions, total Mg2+ should be set at a concentration exceeding (by at least 0.5 mM) five times the concentration of InsP 6; obviously, additional Mg2+ must be included when in the presence of further Mg2+ complexating agents such as ATP. In addition, total InsP 6 concentrations must be kept below 49 μM, unless working with particulate phytate is desired and/or a substantial InsP 6-binding capacity (in proteins or membranes) is expected. In order to imitate extracellular or vesicular system conditions, a millimolar-range excess of Ca over five times the molar amount of InsP 6 present must be included. Moreover, it must be borne in mind that InsP 6 will be present in solid form (generally as a very fine precipitate), except for the fraction of it that may be bound by proteins.
Many experiments and procedures require conditions other than those mentioned above. These include the preparation of stock solutions, the extraction of InsP 6 from biological samples, experiments mimicking intestinal conditions, and assays of phytase activity. As mentioned, the multiple equilibrium constants involved can only be put to practice with the help of specialised software, and even so, with some technical difficulties. We have thus put together a series of plots that summarise the solubility behaviour of InsP 6 in the presence of Ca2+ and Mg2+ (Fig. 4 ). In these plots, the frontiers between solubility and precipitation are given in terms of total concentrations of InsP 6 and metal. Overall, for each given condition, the area of dominance of solid phytate in the plots is wedged within the region of full solubility, which encompasses both low and high InsP 6 concentrations. However, for Ca2+ at neutral and alkaline pH, the low-[InsP 6] solubility region does not exist, reflecting that as long as enough metal is present, even very low concentrations of phytate are insoluble. For Mg2+ at neutral and alkaline pH, the low-[InsP 6] solubility region corresponds to the dominance of Mg5(H2L), and it has therefore a straight-line limit at [InsP 6] = 49 μM.
The plots in Fig. 4 are given in terms of total metal ion. For neutral and alkaline pH, free cation can be calculated as total cation minus five times total InsP 6; when [M2+]total is less than 5 × [InsP 6]total, free divalent cations are absent. It is important to bear in mind that in some situations it is the concentration of free metal ion that is fixed. For example, when InsP 6 is parenterally administered, extracellular fluids can be expected to equilibrate with respect to (free) Ca2+: thus once InsP 6 precipitates, the local total “concentration” of Ca2+ will be equal to the overall physiological [Ca2+]free plus the five times the local InsP 6 “concentration”. Similarly, when dialysis of InsP 6 against Ca2+- or Mg2+-containing media is attempted, free metal equilibrates between the two compartments, and InsP 6 precipitation takes place.
Conditions including both Ca2+ and Mg2+ are difficult to summarise. However, a simple rule is that within dominance ranges of calcium phytate (Fig. 4d–g), the additional inclusion of Mg2+ will not alter the system, except under the very special set of conditions depicted in Fig. 3b. Another rule of thumb is that, at the same total divalent cation concentration, Ca2+–Mg2+ systems will be less soluble than the corresponding Mg2+-only systems.
Our data are derived from constants measured in the presence of 0.15 M NaClO4. Including K+ instead of Na+ does not change the systems significantly ( and our unpublished results). However, changes in ionic strength are expected to alter the systems, with higher ionic strength generally enhancing solubility and viceversa.
This work was supported by a PDT (Ministry of Education, Uruguay) grant to C.K. R.F.I. is supported by the Royal Society and the Wellcome Trust.