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. 2024 Sep 30;27(11):111077. doi: 10.1016/j.isci.2024.111077

Modeling calcium and magnesium balance: Regulation by calciotropic hormones and adaptations under varying dietary intake

Pritha Dutta 1,5,, Anita T Layton 1,2,3,4
PMCID: PMC11530821  PMID: 39493879

Summary

Magnesium (Mg2+) is crucial for several cellular and physiological processes and is tightly regulated due to health risks associated with imbalances. Mg2+, calcium (Ca2+), parathyroid hormone, and vitamin D3 are tightly coupled, ensuring proper bone metabolism and intestinal and renal absorption of Mg2+ and Ca2+. While several Ca2+ homeostasis models exist, no computational model has been developed to study Mg2+ homeostasis. We developed a computational model of Mg2+ homeostasis in male rats, integrating it with an existing Ca2+ homeostasis model, to understand the interconnected physiological processes regulating their homeostasis. We then analyzed adaptations in these interconnected processes under (1) dietary Mg2+ deficiency, (2) low/high dietary Ca2+ with Mg2+ deficiency, and (3) vitamin D3 deficiency. Model simulations predicted severe hypomagnesemia and mild hypocalcemia with significant dietary Mg2+ deficiency. Low dietary Ca2+ improved, while high dietary Ca2+ worsened Mg2+ deficiency. Finally, vitamin D3 deficiency caused severe hypocalcemia, with minimal impact on Mg2+ homeostasis.

Subject areas: Physiology, Bioinformatics, Computational bioinformatics

Graphical abstract

graphic file with name fx1.jpg

Highlights

  • We have developed a computational model of Mg2+ and Ca2+ homeostasis in a male rat

  • Severe dietary Mg2+ deficiency caused severe hypomagnesemia and mild hypocalcemia

  • Dietary Ca2+ deficiency in the presence of Mg2+ deficiency improved plasma Mg2+ level

  • Vitamin D3 deficiency significantly impacted Ca2+ homeostasis but not Mg2+ homeostasis


Physiology; Bioinformatics; Computational bioinformatics

Introduction

Magnesium (Mg2+) is the fourth most abundant cation in the body. Mg2+ is the cofactor for several enzymes and hence plays an important role in most major cellular processes such as energy metabolism, DNA transcription, and protein synthesis. In addition, Mg2+ is required for muscle contraction, neuromuscular stability, and bone formation. Thus, any disturbance in Mg2+ homeostasis can disrupt several essential cellular and physiological processes.

Extracellular Mg2+ is tightly regulated, with plasma [Mg2+] maintained relatively constant between 1.6 and 2.3 mg/dL1 under normal physiological conditions in humans. Mg2+ homeostasis is maintained by three organs: the intestine, responsible for Mg2+ uptake from diet; bones, responsible for Mg2+ storage; and the kidneys, responsible for Mg2+ excretion. Almost all of the body’s Mg2+ (approximately 99%) is either stored in bone or within cells and less than 1% is present in the blood.1 The normal daily Mg2+ intake of humans averages around 300 mg, about half of which is absorbed by the intestine.2 About 70% of the circulating Mg2+ is non-protein-bound and is thus filtered by the glomerulus, accounting for 2,400 mg in humans.

A complex interconnection exists between parathyroid hormone (PTH), calcitriol (1,25(OH)2D3), Mg2+, and calcium (Ca2+). Mg2+ is an important regulator of PTH secretion and vitamin D3 metabolism. Although Mg2+ has only ∼60% of the effect of Ca2+ on PTH secretion, it is still an important regulator of PTH secretion. In fact, acute elevations and reductions in plasma [Mg2+] inhibit PTH secretion irrespective of plasma Ca2+ levels. Mg2+ also plays an important role in the activation of vitamin D3 which occurs in two steps: (1) in the liver, cholecalciferol is hydroxylated to 25(OH)D, and (2) in the kidneys, 25(OH)D is converted to 1,25(OH)2D3. The activity of the enzymes involved in both these processes is dependent on Mg2+. Thus, dysregulation of Mg2+ homeostasis can significantly impact PTH secretion and vitamin D3 metabolism which in turn can disrupt bone and Ca2+ homeostasis.

Maintaining Mg2+ and Ca2+ balance relies on the highly coupled regulation of various processes, including intestinal absorption, renal filtration and reabsorption, and bone remodeling. Given the multitude of interconnected physiological processes involved in the homeostasis of these two divalent cations, mathematical modeling proves valuable in comprehending the system’s complexities. In this study, we developed the first Mg2+ homeostasis model for male rats and integrated it with a previously developed calcium homeostasis model for male rats.3,4 Figure 1 provides a schematic representation of the fundamental fluxes and hormones involved in Mg2+ and Ca2+ homeostasis. We then used this model to understand how these different interconnected processes adapt in the presence of different disorders (dietary Mg2+ deficiency, low/high dietary Ca2+ in the presence of Mg2+ deficiency, and vitamin D3 deficiency) to maintain Mg2+ and Ca2+ homeostasis.

Figure 1.

Figure 1

Schematics of the Mg2+ homeostasis model

The model consists of five compartments: plasma, intestine, kidney, parathyroid gland, and bone. Arrows with triangular arrowheads indicate activation, while those with circular arrowheads indicate inhibition. All arrows are color coded. Green arrow, Ca2+; red arrow, Mg2+, blue arrow, parathyroid hormone (PTH); mauve arrow, 1,25(OH)2D3.

Results

Baseline results

The predicted baseline steady state concentrations of PTH, 1,25(OH)2D3, Mg2+, and Ca2+, and the steady state Mg2+ and Ca2+ fluxes are given in Table 1. The predicted baseline [PTH]p, [1,25(OH)2D3]p, [Mg2+]p, and [Ca2+]p fall within the physiological ranges reported in the literature.

Table 1.

Baseline steady state concentrations and fluxes

Steady-state value Range Source
[PTH]p, pM 6.28 1.5–13 Table 4 of ref.3 (mathematical model of Ca2+ homeostasis in rats),5,6 (experimental studies on Sprague-Dawley rats)
[1,25(OH)2D3]p, pM 154 80–250 Table 4 of ref.3,7,8 (experimental studies on Sherman rats and Sprague-Dawley rats)
[Mg2+]p, mM 0.65 0.45–0.85 9,10,11 (experimental studies on Sprague-Dawley rats and Wistar rats)
[Ca2+]p, mM 1.25 1.1–1.3 Table 4 of ref.3,5,12 (experimental studies on Sprague-Dawley rats and Wistar Hannover rats)
Intestinal Ca2+ absorption, μmol/min 0.59 0.55–1.22 Table 4 of ref.3
Intestinal Mg2+ absorption, μmol/min 0.032 0.027–0.05 13 (experimental study on Wistar rats)
Urinary Ca2+ excretion, μmol/min 0.045 0.015–0.054 Table 4 of ref.3
Urinary Mg2+ excretion, μmol/min 0.024 0.01–0.038 13 (experimental study on Wistar rats)
Bone Ca2+ accretion, μmol/min 1.08
Bone Mg2+ accretion, μmol/min 0.02
Bone Ca2+ resorption, μmol/min 0.53
Bone Mg2+ resorption, μmol/min 0.014
Ca2+ flux from fast bone pool to plasma, μmol/min 0.45
Mg2+ flux from fast bone pool to plasma, μmol/min 0.16
Ca2+ flux from plasma to fast bone pool, μmol/min 1.53
Mg2+ flux from plasma to fast bone pool, μmol/min 0.18

Sensitivity analysis

Local sensitivity analysis

We performed a local sensitivity analysis by varying each model parameter listed in Table 2 by ±5% and computing the corresponding steady state. The resulting percent changes in [PTH]p, [1,25(OH)2D3]p, [Mg2+]p, and [Ca2+]p are shown in Figure 4.

Table 2.

Description and values of model parameters

Parameter Symbol Value Reference
Plasma volume Vp 10 mL Granjon et al. 3

PTH

Maximal rate constant of PTH secretion from the parathyroid gland βexoPTHg 1.034 min−1 estimated (refer to section: STAR Methods:Method details:Parathyroid gland and parathyroid hormone
and Figure 2)
Factor controlling the maximal PTH secretion at a given plasma Ca2+ concentration γCa 0.15 mM estimated (refer to section: STAR Methods:Method details:Parathyroid gland and parathyroid hormone and Figure 2)
Factor controlling the maximal PTH secretion at a given plasma Ca2+ concentration γp 2 estimated (refer to section: STAR Methods:Method details:Parathyroid gland and parathyroid hormone and Figure 2)
Factor controlling the slope of the PTH secretion curve Cm 3.8 mM estimated (refer to section: STAR Methods:Method details:Parathyroid gland and parathyroid hormone and Figure 2)
IC50 value of Mg2+ for inhibition of PTH secretion KlowMg 0.25 mM Quitterer et al. 14
Basal rate of PTH production in the parathyroid gland kprodPTHg 2.53 pmol/min estimated
Inhibition of PTH synthesis by 1,25(OH)2D3 γprod1,25(OH)2D3 0.003 p.m.−1 Stadt et al.4
Rate of degradation of PTH in parathyroid gland kdegPTHg 0.035 min−1 Granjon et al. 3
Degradation rate constant of plasma PTH kdegPTHp 0.081 min−1 estimated

Vitamin D3

Inactive vitamin D3 [25(OH)D]p 25 nM Granjon et al. 3
Minimum production rate constant of 1,25(OH)2D3 kconvmin 4.4 x 10−6 min−1 Granjon et al. 3
Maximal increase in 1,25(OH)2D3 production rate δconvmax 6 x 10−5 min−1 Granjon et al. 3
Stimulation of 1,25(OH)2D3 production by PTH KconvPTH 3 p.m. Granjon et al. 3
PTH sensitivity coefficient nconv 6 Granjon et al. 3
Inhibition of 1,25(OH)2D3 production by Ca2+ γconvCa 0.3 mM−1 Granjon et al. 3
Inhibition of 1,25(OH)2D3 production by itself γconv1,25(OH)2D3 1.8 x 10−2 p.m.−1 Granjon et al. 3
Factor controlling the maximal increase in 1,25(OH)2D3 production by Mg2+ δMgact 6.6 estimated (refer to section: STAR Methods:Method details:Plasma 1,25(OH)2D3 and Figure 3)
Michaelis-Menten constant KMgact1 1.1 mM estimated (refer to section: STAR Methods:Method details:Plasma 1,25(OH)2D3 and Figure 3)
Michaelis-Menten constant KMgact2 1.2 mM estimated (refer to section: STAR Methods:Method details:Plasma 1,25(OH)2D3 and Figure 3)
Inhibition of 1,25(OH)2D3 degradation by PTH γinactPTH 0.52 p.m.−1 Granjon et al. 3
Michaelis-Menten constant KD3 1.7 mM estimated
Degradation rate constant of 1,25(OH)2D3 kdeg1,25(OH)2D3 0.008 min−1 estimated

Kidneys

Minimal fractional reabsorption of Mg2+ in proximal tubule λMgPT0 0.185 Quamme et al.15
Stimulation of Mg2+ reabsorption in proximal tubule by PTH δMgPTmax 0.015 estimated
Sensitivity of Mg2+ reabsorption in proximal tubule to PTH PTHref 12 p.m. Granjon et al. 3
Hill coefficient nPT 5 Granjon et al. 3
Minimal fractional reabsorption of Mg2+ in thick ascending limb λMgTAL0 0.66 Quamme et al.15
Stimulation of Mg2+ reabsorption in thick ascending limb by CaSR δMgCaSRmax 0.028 estimated
Stimulation of Mg2+ reabsorption in thick ascending limb by PTH δMgPTHmax 0.012 estimated
Sensitivity of Mg2+ reabsorption in thick ascending limb to Ca2+ Caref 1.25 mM Brown et al. 16
Sensitivity of Mg2+ reabsorption in thick ascending limb to Mg2+ Mgref 2.5 mM Brown et al. 16
Hill coefficient nTAL 4 Granjon et al. 3
Sensitivity of Mg2+ reabsorption in thick ascending limb to PTH KTALPTH 4 p.m. Stadt et al.4
Minimal fractional reabsorption of Mg2+ in distal convoluted tubule λMgDCT0 0.08 Quamme et al.15
Stimulation of Mg2+ reabsorption in distal convoluted tubule by PTH and 1,25(OH)2D3 δMgDCTmax 0.02 estimated
Sensitivity of Mg2+ reabsorption in distal convoluted tubule to PTH KDCTPTH 7.25 p.m. Stadt et al. 4
Sensitivity of Mg2+ reabsorption in distal convoluted tubule to 1,25(OH)2D3 KDCT1,25(OH)2D3 160 p.m. Stadt et al. 4
Glomerular filtration rate (GFR) ΦGFR 1.25 mL/min Sadick et al. 17

Intestine

Dietary Mg2+ intake IMg 0.04 μmol/min Coudray et al. 13
Maximal rate of active absorption of Mg2+ Vactive 0.764 μmol/min Hardwick et al.18
Stimulation of active Mg2+ absorption by dietary Mg2+ intake Kactive 0.17 μmol/min Hardwick et al.18
Stimulation of Mg2+ absorption by 1,25(OH)2D3 Kabs1,25(OH)2D3 100 p.m. Granjon et al. 3

Bones

Rate of Mg2+ uptake from plasma by fast bone pool kpfMg 0.074 min−1 estimated
Rate of Mg2+ release from fast bone pool to plasma kfpMg 0.2 x 10−3 min−1 estimated
Rate of accretion into the slow bone pool γacMg 3.98 x 10−4 min−1 estimated
Minimal resorption rate τresmin 0.142 x 10−3 mmol/min Granjon et al. 3
Maximal resorption rate δresmax 0.7 x 10−3 mmol/min Granjon et al. 3
Stimulation of bone resorption by PTH KresPTHp 2.45 p.m. Granjon et al. 3
Stimulation of bone resorption by 1,25(OH)2D3 Kres1,25(OH)2D3 160 p.m. Granjon et al. 3

Plasma

Fraction of magnesium bound to proteins κbMg 0.3 Jahnen-Dechent et al. 19
Figure 4.

Figure 4

Local sensitivity analysis

Local sensitivity analysis conducted by (A) increasing individual parameters by 5% and (B) decreasing individual parameters by 5%. The resulting percent change in model steady state concentrations from baseline is presented here. White indicates the resulting change was less than 1%.

A 5% change in minimal thick ascending limb fractional reabsorption λMgTAL0 causes a significant change in [PTH]p, [1,25(OH)2D3]p, [Mg2+]p, and [Ca2+]p. Let us analyze the results when λMgTAL0 is increased by 5% (Figure 4A). As intestinal Mg2+ absorption is mostly dependent on dietary Mg2+ intake and only a small fraction (12%) is regulated by 1,25(OH)2D3 (Equation 19), the kidneys play a major role in determining and maintaining [Mg2+]p. The thick ascending limb is the major Mg2+ reabsorption segment in the kidney; hence, a 5% increase in λMgTAL0 increases [Mg2+]p by 6.7% to 0.69 mM from the baseline value of 0.65 mM (Figure 4). The higher [Mg2+]p increases the synthesis of 1,25(OH)2D3, which in turn increases the intestinal absorption of Ca2+ as 45% of it is regulated by 1,25(OH)2D3.3 Thus, [Ca2+]p increases to 1.28 mM from the baseline value of 1.25 mM. [PTH]p decreases by 5.2% because (1) the increased [1,25(OH)2D3]p inhibits PTH synthesis in the parathyroid gland and (2) the increased [Mg2+]p and [Ca2+]p inhibits PTH secretion.

It is interesting to note that the fractional reabsorption of Ca2+ along the proximal tubule, which is the major segment of renal Ca2+ reabsorption (represented by the parameter λCaPT0), does not significantly alter [PTH]p, [1,25(OH)2D3]p, [Mg2+]p, and [Ca2+]p (Figure 4). This somewhat unintuitive result is mainly due to the negative feedback loop between [Ca2+]p and 1,25(OH)2D3 synthesis and PTH secretion. The increased renal Ca2+ reabsorption increases [Ca2+]p. This in turn inhibits PTH secretion. The increased [Ca2+]p and decreased [PTH]p inhibit 1,25(OH)2D3 synthesis, which in turn inhibits intestinal Ca2+ absorption. Thus, the negative feedback loop between [Ca2+]p and [1,25(OH)2D3]p attenuates the effect on [Ca2+]p when renal Ca2+ reabsorption is varied. By contrast, the feedback loop between [Mg2+]p and [1,25(OH)2D3]p is reinforcing which contributes to significantly alter [Mg2+]p in the face of increased/decreased renal Mg2+ reabsorption.

Global sensitivity analysis

We conducted global sensitivity analysis by applying the variance-based Sobol method.20 This method decomposes the output variance into contributions from individual parameters and their interactions, thus identifying parameters that have the most significant effect on the output. Sobol indices are of different orders that reflect the number of parameters interacting with each other. Therefore, the 1st-order Sobol indices measure the effect of individual parameters, 2nd-order Sobol indices measure the effect of the interaction between two parameters and so on. The total Sobol index measures the influence of a parameter, including interactions with other parameters.

We performed the Sobol sensitivity analysis with 10,000 samples. Each parameter listed in Table 2 was varied in the range of ±20%. Figure 5 shows the Sobol indices of parameters that have significant influence on [PTH]p, [1,25(OH)2D3]p, [Mg2+]p, and [Ca2+]p. The figure shows the 1st-order Sobol indices (blue bars) and the other order Sobol indices indicating interactions (red bars). The other order index was calculated as total Sobol index ˗ 1st-order Sobol index. The figure shows only those parameters which had total Sobol indices greater than 0.05. For all the parameters, we observe that the 1st-order Sobol indices predominate over the Sobol indices due to interactions. Thus, these parameters individually make significant contributions to the model outputs. Plasma volume (Vp) has the highest influence on [PTH]p, minimal fractional reabsorption of Mg2+ in thick ascending limb (λMgTAL0) has the most impact on [1,25(OH)2D3]p and [Mg2+]p, and rate of Ca2+ uptake from plasma by fast bone pool (kpfCa) has the highest impact on [Ca2+]p.

Figure 5.

Figure 5

Global sensitivity analysis

Sobol indices of parameters that have significant impact on (A) [PTH]p, (B) [1,25(OH)2D3]p, (C) [Mg2+]p, and (D) [Ca2+]p. Parameters were varied in the range of ±20% and Sobol indices were calculated on steady state concentrations.

Parameters with total Sobol indices greater than 0.05 are shown. Blue bars indicate the 1st-order Sobol indices and red bars indicate the other order indices representing interaction with other parameters. The other order indices were calculated as total Sobol indices ˗ 1st-order Sobol indices.

Effect of deficiency of dietary Mg2+

A large portion of the population in all continents consumes less than two-thirds of the recommended dietary allowances for Mg2+.21 In the United States, the standard diet contains only about 50% of the recommended daily Mg2+.22 Insufficient dietary Mg2+ intake may lower plasma Mg2+ level which can have severe consequences. For instance, vitamin D metabolizing enzymes, 1α-hydroxylase and 24-hydroxylase, are Mg2+-dependent and hence Mg2+ deficiency can significantly lower plasma 1,25(OH)2D3 levels.23,24 In addition, Mg2+ deficiency also impairs PTH response. To evaluate its effect on Ca2+ and Mg2+ homeostasis, we conducted simulations in which dietary Mg2+ intake (IMg) was reduced by 50%, 75%, and 90% for 6 months according to the experiments conducted by Rude et al.9,25,26 The predicted fractional changes in plasma concentrations of PTH, 1,25(OH)2D3, Mg2+, and Ca2+ and Mg2+ and Ca2+ fluxes after 6 months of restricted IMg are shown in Figure 6.

Figure 6.

Figure 6

Dietary Mg2+ deficiency

Predicted fractional changes in plasma concentrations and fluxes at 50%, 75%, and 90% dietary Mg2+ intake (IMg) restrictions from baseline (denoted by the gray line at 0) for 6 months (A) Predicted (bars) and experimental (black diamonds) fractional changes in plasma concentrations of PTH, 1,25(OH)2D3, Ca2+, Mg2+, bone Ca2+ content, and bone Mg2+ content.

(B) Predicted fractional changes in Mg2+ and Ca2+ fluxes into plasma.

(C) Predicted fractional changes in Mg2+ and Ca2+ fluxes out of plasma.

Figure 6A shows the predicted and experimental9,25,26 fractional changes in [PTH]p, [1,25(OH)2D3]p, [Mg2+]p, [Ca2+]p, bone Ca2+ content, and bone Mg2+ content at different IMg restrictions. Bone Ca2+ and Mg2+ contents were measured from bone ash in the experimental studies.9,25,26 The predicted fractional changes in [PTH]p, [1,25(OH)2D3]p, [Mg2+]p, and bone Mg2+ content are almost in line with the experimentally reported changes. However, while the experimental study reported [Mg2+]p to decrease by 6% at 50% IMg restriction, the model predicted a decrease of 17%. The model might have underestimated the adaptive increase in intestinal Mg2+ absorption at moderate Mg2+ deficiency in rats, since the intestinal absorption parameters were obtained from a study conducted on humans. Nevertheless, the predicted [Mg2+]p at 50% IMg restriction (0.54 mM) is within the normal range (0.45–0.85 mM). In addition, the predicted change in [Ca2+]p content differs significantly from the experimental values. The experimental studies9,25,26 reported [Ca2+]p to decrease by 5% at 50% IMg restriction, and increase by 5% and 9% at 75% and 90% IMg restrictions, respectively. By contrast, our model predicted [Ca2+]p to decrease by 10%, 20%, and 23% after 6 months of 50%, 75%, and 90% IMg restrictions, respectively. Severe dietary Mg2+ deficiency causes hypocalcemia in most species (including humans27,28) with the exception of rats and mice, where hypercalcemia develops.29 The exact reasons for this are not clearly understood but could be due to the reduction in osteoblastic and osteocytic activity in the presence of hypomagnesemia, which significantly lowers the rate of bone formation.29,30,31 Further investigation is required to understand why severe dietary Mg2+ deficiency results in hypercalcemia in rodents and hypocalcemia in other species.

At 50% IMg restriction, [Mg2+]p was predicted to decrease to 0.54 mM from the baseline concentration of 0.65 mM, and [Ca2+]p decreased to 1.12 mM from the baseline concentration of 1.25 mM, thus triggering increased PTH secretion (Figure 6A). By contrast, at 75% and 90% IMg restrictions, [Mg2+]p was predicted to decrease to 0.31 and 0.17 mM, respectively, which are significantly below 0.4 mM. These very low plasma Mg2+ concentrations inhibit PTH secretion (based on Equation 5). Similar observations were reported in dietary Mg2+ restriction experiments conducted on humans.32 Intestinal Mg2+ absorption was predicted to decrease proportionally with the IMg restrictions (Figure 6B). Since 45% of intestinal Ca2+ absorption is regulated by [1,25(OH)2D3]p, it was predicted to decrease by 13%, 21%, and 22%, respectively (Figure 6B). Urinary Ca2+ and Mg2+ excretions decreased proportionally with decrease in [Ca2+]p and [Mg2+]p (Figure 6C).

Dietary Mg2+ reduction causes significant bone loss.9,25,26,33 Bone loss is characterized by a decrease in bone mineral density (i.e., decrease in Ca2+, Mg2+, and other mineral content in the bone). Our model predicted bone Mg2+ content to decrease by 9%, 17%, and 39%, respectively, following 6 months of 50%, 75%, and 90% IMg restrictions (Figure 6A), which are in line with the experimental values.9,25,26 Several experimental and clinical studies have shown that Mg2+ deficiency promotes osteoporosis (summarized in34). Due to this bone loss, the exchange of Mg2+ between the bone and plasma drops significantly (Figures 6B and 6C). The model predicted almost no change in bone Ca2+, in line with the experimental results.(Figure 6A).

Taken together, model results reveal the mechanisms by which sufficiently large deficiency in dietary Mg2+ causes dysregulation in Ca2+ and Mg2+ homeostasis.

Effect of low/high dietary Ca2+ in the presence of low dietary Mg2+

Since, as noted previously, a large portion of the population consumes Mg2+ lower than the recommended level, we investigated the effect that low dietary Ca2+ or Ca2+ supplementation has on Ca2+ and Mg2+ homeostasis in the presence of 60% dietary Mg2+ (IMg) restriction. To simulate low and high dietary Ca2+, we decreased and increased ICa by 50%, respectively. Figure 7 shows the predicted fractional changes in steady state plasma concentrations of PTH, 1,25(OH)2D3, Mg2+, and Ca2+ and the steady state Mg2+ and Ca2+ fluxes from the steady state values at 60% IMg restriction (shown by the gray line at 0) for each set of simulations.

Figure 7.

Figure 7

Dietary Ca2+ deficiency or supplementation in the presence of dietary Mg2+ deficiency

Predicted fractional change in steady state plasma concentrations and fluxes at (i) 60% dietary Mg2+ (IMg) restriction combined with 50% dietary Ca2+ (ICa) restriction and (ii) 60% IMg restriction combined with 50% ICa increase from the steady state values at 60% IMg restriction (shown by the gray line at 0).

(A–C) (A) Fractional change in steady state plasma concentrations of PTH, 1,25(OH)2D3, Ca2+, and Mg2+. (B) Fractional change in steady state Mg2+ and Ca2+ fluxes into plasma. (C) Fractional change in steady state Mg2+ and Ca2+ fluxes out of plasma.

At 60% IMg restriction and baseline ICa, [Mg2+]p decreased by 31% to 0.45 mM from the baseline concentration of 0.65 mM and [Ca2+]p decreased by 13% to 1.08 mM from the baseline concentration of 1.25 mM. Restricting ICa by 50% further lowered [Ca2+]p to 0.88 mM, resulting in hypocalcemia (Figure 7A). This enhanced PTH secretion (Equation 2). The decreased [Ca2+]p and increased [PTH]p enhanced 1,25(OH)2D3 synthesis (Equation 7). The increased [PTH]p and [1,25(OH)2D3]p increased resorption of Mg2+ from the slow bone pool by 13% (Equation 22). In addition, the increased [1,25(OH)2D3]p enhanced intestinal absorption of Mg2+ raising [Mg2+]p to 0.49 mM (Figure 7A). Thus, lowering dietary Ca2+ intake during dietary Mg2+ deficiency improved plasma Mg2+ concentration and ameliorated hypomagnesemia.35

The opposite changes were observed when ICa was increased by 50%. [Ca2+]p increased to 1.21 mM which inhibited PTH secretion and 1,25(OH)2D3 synthesis (Figure 7A). This in turn inhibited resorption of Mg2+ from the slow bone pool and intestinal Mg2+ absorption. Consequently, [Mg2+]p decreased further from 0.45 mM to 0.41 mM (Figure 7A). Thus, higher dietary Ca2+ intake combined with dietary Mg2+ deficiency exacerbated hypomagnesemia.36,37,38,39

To understand these changes in the cellular level, note that when ICa is decreased, [Ca2+]p decreases, which stimulates the calcium-sensing receptors (CaSR) on the parathyroid glands and PTH secretion increases. Now Ca2+ is an inhibitor and PTH is an activator of 1α-hydroxylase, the enzyme responsible for converting 25(OH)D to 1,25(OH)2D3. Thus, the decreased plasma Ca2+ and increased plasma PTH increase the synthesis of 1,25(OH)2D3. The increased PTH and 1,25(OH)2D3 increase production of release receptor activator of nuclear factor kappa-B ligand (RANKL) and osteoprotegerin (OPG), leading to increased osteoclast formation and activity and hence increased bone resorption. Along the renal thick ascending limb, increased PTH decreases claudin 14 and activated CaSR increases claudin 14 expression; these two opposing responses slightly increase claudin 16/19 expression and hence paracellular transport of Mg2+. Along the renal distal convoluted tubule, PTH increases Mg2+ uptake through receptor-mediated cAMP release and activation of protein kinase A and 1,25(OH)2D3 increases Mg2+ uptake through calbindin-D. All these responses combine to increase plasma Mg2+ concentration. The opposite responses occur when ICa is increased. Taken together, reduced dietary Ca2+ intake in the presence of Mg2+ deficiency helped to improve plasma Mg2+ concentration, whereas, increased dietary Ca2+ intake caused further decline in plasma Mg2+ concentration.

Effect of change of inactive vitamin D3 (25(OH)D)

Low plasma level of 25(OH)D, the substrate for 1,25(OH)2D3 (Figure 8), is commonly observed in chronic liver disease and chronic kidney disease, with the degree of 25(OH)D deficiency increasing with the severity and progression of disease.40,41,42,43,44 Since 1,25(OH)2D3 plays an important role in Mg2+ and Ca2+ homeostasis, we studied the effect of different levels of 25(OH)D deficiency on Mg2+ and Ca2+ homeostasis. To accomplish that, we progressively decreased the parameter [25(OH)D]p up to 100%. The predicted normalized steady state plasma concentrations of PTH, 1,25(OH)2D3, Mg2+, and Ca2+ and the normalized steady state Mg2+ and Ca2+ fluxes are shown in Figure 9.

Figure 8.

Figure 8

Schematic of the regulation of different forms of vitamin D3 by Mg2+, Ca2+, PTH, and 1,25(OH)2D3

Arrows denote activation and closed circles denote inhibition.

Figure 9.

Figure 9

Inactive vitamin D3 (25(OH)D) deficiency

Predicted normalized steady state plasma concentrations and fluxes at decreased [25(OH)D]p

(A–C) All y axis values are normalized to the baseline values. (A) Normalized steady state plasma concentrations of PTH, 1,25(OH)2D3, Ca2+, and Mg2+. (B) Normalized steady state Mg2+ and Ca2+ fluxes into plasma. (C) Normalized steady state Mg2+ and Ca2+ fluxes out of plasma.

As [25(OH)D]p was decreased, 1,25(OH)2D3 synthesis in the kidneys decreased, resulting in lower [1,25(OH)2D3]p (Equation 7), which became zero when [25(OH)D]p = 0 (Figure 9A). Now, [1,25(OH)2D3]p directly and indirectly regulates the following: (1) PTH synthesis, (2) intestinal absorption of Ca2+ and Mg2+, (3) renal Ca2+ and Mg2+ reabsorption, and (4) bone resorption. Let us first assess the impact on intestinal absorption of Mg2+ and Ca2+. [1,25(OH)2D3]p regulates 45% of intestinal Ca2+ absorption3 but only 12% of intestinal Mg2+ absorption (Equation 19). Hence, the decrease in intestinal Ca2+ absorption45 was significantly higher compared to Mg2+ (Figure 9B). Consequently, [Ca2+]p decreased by 14% to 1.08 mM (below the normal range of 1.1–1.3 mM) at 50% inhibition of [25(OH)D]p, and further by 54% to 0.58 mM, which was significantly below the normal range (Figure 9A), at full inhibition. Several experimental and clinical studies have reported hypocalcemia in the presence of low serum 25(OH)D concentration.45,46,47 By contrast, [Mg2+]p did not change significantly until [25(OH)D]p was inhibited by over 60%, at which point [Mg2+]p was about 2.4% lower than baseline (Figure 9A). At full inhibition, [Mg2+]p dropped by 11% to 0.58 mM, within the normal range (normal range is 0.45–0.85 mM) (Figure 9A). The lower [Ca2+]p and [Mg2+]p enhanced PTH secretion to maintain levels of these two divalent cations (Equation 2). In addition, the inhibitory effect of [1,25(OH)2D3]p on PTH synthesis in the parathyroid gland (Equation 1) was attenuated, which further increased PTH secretion. Thus, [PTH]p increased by 29% and 193%, respectively, at 50% and 100% inhibitions (Figure 9A).48 Now, the higher [PTH]p increased Ca2+ and Mg2+ reabsorption along the thick ascending limb and distal convoluted tubule. In addition, the fall in [Ca2+]p and [Mg2+]p also decreased the Ca2+ and Mg2+ loads filtered by the kidneys. These two factors contributed to reducing urinary excretion of Ca2+ and Mg2+ to preserve plasma levels of these cations. Ca2+ and Mg2+ excretions decreased by 13% and 8% respectively, following a 50% inhibition of [25(OH)D]p, and by 26% and 13% respectively, when [25(OH)D]p was fully inhibited (Figure 9C).

Following the significant decrease in [Ca2+]p, the exchange of Ca2+ between bone and plasma decreased significantly (Figures 9B and 9C). The decrease in Mg2+ exchange was comparatively lower (Figures 9B and 9C). Ca2+ content in the fast bone pool was predicted to decrease by 13% and 47% respectively, whereas the Mg2+ content decreased by 1.2% and 8.5%, respectively, at 50% and 100% [25(OH)D]p inhibition (Figure 9A). Now in the slow bone pool, Ca2+ content decreased by 4.9% and 24% respectively (Figure 9A). By contrast, our model predicted the Mg2+ content in the slow bone pool to remain almost unchanged (Figure 9A).

These results indicated that 1,25(OH)2D3 plays a major role in maintaining Ca2+ homeostasis as its deficiency can cause severe hypocalcemia.49 Mg2+ homeostasis on the other hand is not severely impacted by deficiency of 1,25(OH)2D3.49

Recall that the model predicted that a decrease in plasma Ca2+ in response to dietary Ca2+ restriction would increase plasma Mg2+ level (section: Effect of low/high dietary Ca2+ in the presence of low dietary Mg2+). However, a decrease in plasma Ca2+ level in response to 25(OH)D inhibition resulted in a decrease in plasma Mg2+ level (section: Effect of change of inactive vitamin D3 (25(OH)D)). Why does a decrease in plasma Ca2+ level cause opposite changes in plasma Mg2+ level in these two scenarios? Figure 10 summarizes the responses in these two scenarios which help answer this question. The difference lies in the change in plasma 1,25(OH)2D3. During dietary Ca2+ restriction, plasma 1,25(OH)2D3 increases which together with the increased plasma PTH increase Mg2+ reabsorption along the distal convoluted tubule and bone resorption. By contrast, during 25(OH)D inhibition, plasma 1,25(OH)2D3 decreases significantly, which inhibits Mg2+ reabsorption along the distal convoluted tubule and bone resorption. Thus, plasma Mg2+ increases during dietary Ca2+ restriction and decreases during 25(OH)D inhibition.

Figure 10.

Figure 10

Summary of changes in response to dietary Ca2+ restriction and 25(OH)D inhibition

Downward red arrows indicate decrease and upward green arrows indicate increase. Arrows with the green plus sign (+) indicate activation and arrows with the red minus sign (−) indicate inhibition. TAL, thick ascending limb; DCT, distal convoluted tubule.

Discussion

Mg2+ balance is primarily maintained by the absorption of Mg2+ in the intestine and kidney. Typically, approximately 30–50% of ingested Mg2+ is absorbed by the intestine. The refining and processing of food in modern society has resulted in a substantial loss of the naturally occurring Mg2+. For example, the refining and processing of wheat to flour, rice to polished rice, and corn to starch depletes Mg2+ by >80%.50 Thus, the consumption of modern processed food may partially explain why a significant segment of the population has an Mg2+ intake that falls below the recommended dietary amounts. The intestine absorbs a fraction of Mg2+ that is inversely proportional to intake.18 This may have an unfortunate clinical consequence of prolonging the time for the treatment of Mg2+ deficiency with oral supplements to be effective. In the kidneys, the proximal tubule accounts for 15–25% of Mg2+ reabsorption, the thick ascending limb for 60–70%, and the distal convoluted tubule for ∼10%.51 Intestinal and renal Mg2+ transport occurs through both paracellular and transcellular pathways. Approximately 90% of Mg2+ absorption in the intestine and kidneys occurs passively through the paracellular pathway. Active reabsorption of Mg2+ occurs transcellularly. Although it accounts for only a small fraction of the total intestinal and kidney absorption, active Mg2+ transport is regulated and therefore fine tunes intestinal and renal Mg2+ excretion.

Hypomagnesemia is not uncommon, especially among hospitalized patients (up to 12%).52 Hypomagnesemia can be caused by decreased intake and absorption, or increased losses and redistribution. We considered the physiological implications of low Mg2+ intake (model predictions summarized in Figure 11). Model simulations indicated that severe Mg2+ deficiency leads to hypocalcemia and bone loss (Figure 6). Indeed, Mg2+ deficiency has been implicated as a risk factor for osteoporosis. Epidemiological studies53,54,55 have demonstrated a positive correlation between dietary Mg2+ intake and bone density and/or an increased rate of bone loss with low dietary Mg2+ intake. In mouse studies,29 Mg2+ depletion has also been reported to induce impaired bone growth, decreased osteoblast number, increased osteoclast number, and loss of trabecular bone with stimulation of cytokine activity in bone.

Figure 11.

Figure 11

Summarized predicted changes in plasma concentrations of Mg2+, Ca2+, PTH, and 1,25(OH)2D3 in the presence of (i) dietary Mg2+ deficiency, (ii) low/high dietary Ca2+ in the presence of dietary Mg2+ deficiency, and (iii) 25(OH)D deficiency

Arrow lengths are representative of the extent of change. Downward red arrows indicate decrease and upward green arrows indicate increase.

Besides a low Mg2+ diet, low Mg2+ input can also be caused by decreased absorption. Gastrointestinal diseases that reduce the transit time of intestinal fluid or interfere with absorption can also cause hypomagnesemia. Examples of such gastrointestinal diseases include severe diarrhea, steatorrhea, malabsorption syndromes, and short-bowel syndrome. The capacity of the intestine to absorb dietary Mg2+ also declines with aging.56 As such, aging is a major risk factor for Mg2+ deficiency.

The causes of renal Mg2+ loss can be further divided into those due to increased flow, for example in case of polyuria, and those due to decreased tubular reabsorption. The causes of decreased tubular reabsorption of Mg2+ can, in turn, be classified according to the location in the nephron at which Mg2+ transport is perturbed. Because the thick ascending limb and the distal convoluted tubule are the major sites of renal Mg2+ reabsorption, most causes affect these regions of the kidney. For instance, Type 1 Bartter’s syndrome and Gitelman’s syndrome, which inhibit Na+ transporters along the thick ascending limb and distal convoluted tubule, respectively, cause increased Mg2+ excretion.57,58

The body’s handling of Ca2+ and Mg2+ is coupled in the kidneys and via their regulation by PTH and vitamin D. Approximately half of the world’s population has inadequate access to dietary Ca2+.59 Inadequate Ca2+ intake is linked not only to poor bone health but to other negative health outcomes, including pregnancy complications, cancers, and cardiovascular disease. As such, Ca2+ supplementation is often recommended to vulnerable subpopulations such as pregnant women. We conducted model simulations to investigate the combined physiological implications of low Mg2+ intake combined with either low or high Ca2+ diet (model predictions summarized in Figure 11). Model predictions indicated that reduced dietary Ca2+ intake may improve serum Mg2+ levels; although plasma Ca2+, which is suppressed in Mg2+ deficiency, would be even lower as expected (Figure 7). In contrast, increased dietary Ca2+ intake raises serum Ca2+ levels, which inhibits PTH secretion and 1,25(OH)2D3 synthesis, suppressing the resorption of Mg2+ from the slow bone pool, intestinal Mg2+ absorption, and renal reabsorption. Thus, higher dietary Ca2+ intake may exacerbate hypomagnesemia (Figure 7).

Mg2+ and Ca2+ homeostasis is altered in chronic kidney disease, even though the kidneys undergo adaptations such that hypermagnesemia and hypocalcemia are not observed until advanced chronic kidney disease. Mg2+ deficiency can be associated with abnormal vitamin D function. Indeed, chronic kidney disease is one of the main conditions associated with low 25(OH)D serum levels, with the vast majority of patients with chronic kidney disease exhibiting vitamin D insufficiency (>80% of cases60,61). The known causes and risk factors for vitamin D insufficiency include age,62 female sex,60 proteinuria,62 diabetes,63 and impaired 25(OH)D tubular reabsorption.64

Our simulations results (summarized in Figure 11) suggested that deficiency of 1,25(OH)2D3 has a critical role in maintaining Ca2+ homeostasis as its deficiency can cause severe hypocalcemia.49 In contrast, deficiency of 1,25(OH)2D3 was not predicted to severely impact Mg2+ homeostasis, even though low 1,25(OH)2D3 levels may reduce intestinal Mg2+ absorption in patients with chronic kidney disease. Interestingly, patients with advanced chronic kidney disease (estimated glomerular filtration rate (eGFR) <30 mL/min) were observed to develop hypermagnesemia not hypomagnesemia. That is due to the drastically reduced filtered Mg2+ and thus Mg2+ excretion, despite an increase in fractional excretion of Mg2+. While our simulations of 1,25(OH)2D3 deficiency was motivated by the impacts of chronic kidney disease on Ca2+ and Mg2+ homeostasis, they did not represent impairment in kidney function and thus predicted a drop in plasma Mg2+ in advanced chronic kidney disease rather than hypermagnesemia (Figure 9).

In summary, we have developed a computational model of Mg2+ and Ca2+ homeostasis and their regulation by the calciotropic hormones, PTH and 1,25(OH)2D3, in a male rat. The model was used to understand the underlying mechanisms involved in regulating Mg2+ and Ca2+ balance during dietary Mg2+ deficiency, low/high dietary Ca2+ with Mg2+ deficiency, and vitamin D3 deficiency.

Limitations of the study

Substantial efforts have been invested in understanding the sex differences in Ca2+ regulation and balance.4,65,66,67,68 In contrast, much less is known about the sex differences in Mg2+ homeostasis, with no sex differences reported in serum Mg2+ levels.69,70 That said, urinary Mg2+ excretion appears to be higher in men,71 an observation that may stem, at least in part, from differences in kidney structure and function between the two sexes. In rodent studies, Veiras et al. characterized major differences in transport capacities across tubular nephron segments in male and female rat kidneys.72 Specifically, in the proximal tubule, female rats exhibit heightened NHE3 phosphorylation and relocation to the base of microvilli, where activity is reduced compared to male rats. Consequently, the proximal tubule of female rats reabsorbs a notably smaller portion of filtered Na+ in comparison to male rats. Because proximal tubular Mg2+ transport is linked to Na+ transport, a modeling study73 predicted that the proximal tubule of female rats also reabsorbs a smaller fraction of filtered Mg2+ compared to males. The present model is based primarily on a male rat. A worthwhile extension is to develop sex-specific models for whole-body Ca2+ and Mg2+ regulation, in health and diseases (e.g., chronic kidney disease). In addition, age is also an important factor in Mg2+ homeostasis. Aging is often associated with Mg2+ deficiency which can result from reduced intestinal absorption, increased urinary excretion due to reduction in kidney function, or inadequate dietary Mg2+ intake.56 Developing age-specific models will help us better understand the mechanisms involved in Mg2+ dyshomeostasis in old age. Another limitation of this model is the data used to estimate the parameters; for instance, parameters representing fractional intestinal absorption of Mg2+ were obtained from studies conducted on humans. Also, the model describes transport and regulation mechanisms at the cellular level in the kidneys and intestine by means of simplified relationships, such as first-order kinetics and Michaelis-Menten equations. We have developed detailed epithelial cell-based models of Ca2+ and Mg2+ transport in a rat kidney65,73; these could be integrated in the present mathematical model in the future. In addition, Mg2+ plays an important role in bone remodeling. Mg2+ increases osteoblast proliferation and its deficiency causes increased osteoclast formation and release of inflammatory cytokines leading to significant bone loss.74,75 Developing a detailed model of bone remodeling by considering the impact of Mg2+ on bone resorption and formation may shed light into why severe dietary Mg2+ deficiency results in hypercalcemia in rodents and hypocalcemia in other species.

Resource availability

Lead contact

Further information and requests for resources should be directed to the lead contact, Pritha Dutta (p7dutta@uwaterloo.ca).

Materials availability

This study did not generate new unique reagents or other new materials.

Data and code availability

The code generated in this study can be accessed at https://github.com/Pritha17/Magnesium_calcium_homeostasis.76

Acknowledgments

This work was supported by the Canada 150 Research Chair program, National Sciences and Engineering Research Council of Canada (NSERC) Discovery Grant (RGPIN-2019-03916), and Canadian Institutes of Health Research (CIHR) Project grant (TNC-174963) to A.T.L.

Author contributions

Conceptualization, P.D. and A.T.L.; methodology, P.D. and A.T.L.; software, validation, formal analysis, and investigation, P.D.; resources, A.T.L.; data curation, P.D.; writing – original draft, P.D. and A.T.L; writing – review and editing, P.D. and A.T.L.; visualization, P.D.; supervision, P.D. and A.T.L.; funding acquisition, A.T.L.

Declaration of interests

The authors declare no competing interests.

STAR★Methods

Key resources table

REAGENT or RESOURCE SOURCE IDENTIFIER
Software and algorithms

Computer code This study https://github.com/Pritha17/Magnesium_calcium_homeostasis (https://doi.org/10.5281/zenodo.13787641)

Method details

The Mg2+ homeostasis model consists of five compartments: plasma, intestine, kidney, parathyroid gland, and bone. The model equations in each compartment are described in the following sections. Model parameters are listed in Table 2. For model equations and parameters related to Ca2+ homeostasis refer to Refs.3,4

Parathyroid gland and parathyroid hormone

PTH secretion and plasma Ca2+ and Mg2+ levels are regulated by a feedback loop. As plasma Ca2+ and Mg2+ levels drop, it signals the parathyroid glands to secrete more PTH. PTH stimulates Ca2+ and Mg2+ reabsorption in the kidney, Ca2+ and Mg2+ absorption in the intestine, and bone resorption. All these actions increase plasma Ca2+ and Mg2+ concentrations. The increased levels of these two cations then serve as a negative feedback signal to the parathyroid glands to decrease PTH secretion.

Parathyroid cells sense extracellular Ca2+ and Mg2+ concentrations through the calcium-sensing receptors (CaSR) on their cell surface.77 Ca2+ is the main agonist of CaSR and small changes in plasma Ca2+ concentration can induce rapid secretion of PTH.78 At equimolar concentrations, Mg2+ is 1/2 to 2/3 as potent as Ca2+ in activating CaSR.79,80 Mg2+ has different impacts on PTH secretion depending on the plasma Ca2+ concentration. The combined effect of Ca2+ and Mg2+ on PTH secretion, as reported in an in vitro study,81 is represented by model equations as described below.

Change in PTH concentration in the parathyroid gland (PTHg) is given by

d[PTHg]dt=kprodPTHg1+γprod1,25(OH)2D3[1,25(OH)2D3]p(kdegPTHg+F([Ca2+]p,[Mg2+]p))[PTHg] (Equation 1)

where kprodPTHg denotes the basal rate of PTH production in the parathyroid gland, γprod1,25(OH)2D3 denotes the inhibition of PTH synthesis by [1,25(OH)2D3]p, and kdegPTHg denotes the rate constant for PTHg degradation. The first term on the right-hand-side of Equation 1 denotes the inhibition of PTHg synthesis by [1,25(OH)2D3]p and is adopted from ref.3 This term is based on the findings of Silver et al.82 who found an exponentially decreasing relationship between the mRNA expression of the PTH precursor in parathyroid glands and the injected quantity of 1,25(OH)2D3. F([Ca2+]p,[Mg2+]p) models the exocytosis of PTHg regulated by plasma Ca2+ and Mg2+ and is defined as

F([Ca2+]p,[Mg2+]p)=h([Mg2+]p)×F1([Ca2+]p,[Mg2+]p)+(1h([Mg2+]p))×F2([Mg2+]p) (Equation 2)

where h([Mg2+]p) controls the weightage given to each function and depends on the plasma Mg2+ concentration. The function h([Mg2+]p) is defined as

h([Mg2+]p)=([Mg2+]p[Mg2+]thresPTH)501+([Mg2+]p[Mg2+]thresPTH)50 (Equation 3)

where [Mg2+]thresPTH = 0.4 mM. The function F1([Ca2+]p,[Mg2+]p) is defined as

F1([Ca2+]p,[Mg2+]p)=(γCa[Ca2+]p)γp(βexoPTHg11+(Cm[Mg2+]p)2). (Equation 4)

The above equation is formulated based on observations reported in ref.81:

  • 1.

    Very high (>=5 mM) [Mg2+]p inhibits PTH secretion at all [Ca2+]p.

  • 2.

    At low or moderately low [Ca2+]p (0.8-1 mM), [Mg2+]p (0.5-2 mM) stimulates PTH secretion.

  • 3.

    At normal [Ca2+]p (1.2-1.25 mM), [Mg2+]p (0.5-2 mM) does not have significant effect on PTH secretion; however, if [Mg2+]p is very high (=5 mM), it inhibits PTH secretion.

  • 4.

    At high [Ca2+]p (=1.5 mM), [Mg2+]p inhibits PTH secretion.

The parameter, βexoPTHg, denotes the maximal rate of PTH secretion from the parathyroid gland. (γCa[Ca2+]p)γp controls the maximum effect of [Mg2+]p on PTH secretion at a specific [Ca2+]p, such that the lower the plasma Ca2+ concentration, the higher the maximum effect of [Mg2+]p on PTH secretion. Cm controls the slope of the curve. The lower the Ca2+ concentration, the steeper the slope, a relation that reflects a significant effect of [Mg2+]p on PTH secretion. The parameters βexoPTHg, γCa, γp, and Cm were estimated by fitting to experimental data reported in ref.81 and the comparison between model results and experimental data is given in Figure 2. All parameter descriptions and values are listed in Table 2.

Figure 2.

Figure 2

Comparison between experimental and simulated changes in PTH secretion at different plasma Ca2+ and Mg2+ concentrations

The lsqcurvefit function of MATLAB, which is a non-linear least-square solver, was used to fit our model simulations to experimental values.

The last term in Equation 2, F2([Mg2+]p), is defined as

F2([Mg2+]p)=11+KlowMg[Mg2+]p. (Equation 5)

Equation 5 captures the following observation from ref.83: very low plasma [Mg2+]p (<0.4 mM) inhibits PTH secretion at all [Ca2+]p.

The rate of change in plasma PTH concentration (PTHp) is given by

d[PTHp]dt=F([Ca2+]p,[Mg2+]p)VgVp[PTHg]kdegPTHp[PTHp] (Equation 6)

where kdegPTHp denotes the rate of degradation of PTHp. Vg and Vp denote the volumes of the parathyroid gland and plasma, respectively. The ratio VgVp takes into account the dilution of PTH in plasma.

Plasma 1,25(OH)2D3

Dietary vitamin D3 is first converted to 25-hydroxy vitamin D3 (25(OH)D) by 25-hydroxylase in the liver.84 25(OH)D is then carried to the kidney, where it is either converted to the active form of vitamin D3, 1,25-dihydroxy vitamin D3 (1,25(OH)2D3), by 1α-hydroxylase or the inactive form, 24,25-dihydroxy vitamin D3 (24,25(OH)2D3), by 24-hydroxylase.84 Some of the 1,25(OH)2D3 is converted to the inactive form, 1,24,25(OH)2D3, by 24-hydroxylase.84 The conversion from the inactive 25(OH)D to the active 1,25(OH)2D3 is regulated by Mg2+, Ca2+, PTH, and 1,25(OH)2D3 (Figure 8).

The plasma concentration of active 1,25(OH)2D3 is given by

d[1,25(OH)2D3]pdt=[kconvmin+δconvmax×fPTHact×fCaSRact×f1,25(OH)2D3act×fMgact][25(OH)D]p(kdeg1,25(OH)2D3×(fPTHinact+fMginact))[1,25(OH)2D3]p (Equation 7)

where kconvmin denotes the minimum production rate constant of 1,25(OH)2D3, δconvmax denotes the maximum increase in 1,25(OH)2D3 production rate, and kdeg1,25(OH)2D3 denotes the degradation rate constant of 1,25(OH)2D3. PTH promotes the production of 1,25(OH)2D3 which is represented by fPTHact=([PTH]p)nconv(KconvPTH)nconv+([PTH]p)nconv. CaSR in the proximal tubule of the kidney inhibits production of 1,25(OH)2D3, which is represented by fCaSRact=11+γconvCa[Ca2+]p. 1,25(OH)2D3 has a self-inhibitory effect on its own production, which is represented by f1,25(OH)2D3act=11+γconv1,25(OH)2D3[1,25(OH)2D3]p. The regulation of 1,25(OH)2D3 production by Mg2+ is represented by the following equation23:

fMgact=hm×fMgact1+(1hm)×fMgact2 (Equation 8)

where hm controls the weightage given to each function and depends on the plasma Mg2+ concentration and is defined as hm=11+([Mg2+]p[Mg2+]thres1,25(OH)2D3)50. The parameter [Mg2+]thres1,25(OH)2D3 = 2.4 mM. The terms fMgact1 and fMgact2 are defined as

fMgact1=δMgact×([Mg2+]p)4(KMgact1)4+([Mg2+]p)4 (Equation 9)
fMgact2=δMgact×(KMgact2)4(KMgact2)4+([Mg2+]p)4 (Equation 10)

The parameters δMgact, KMgact1, and KMgact2 were estimated by fitting to experimental data reported in ref.23 The comparison between model results and experimental data is given in Figure 3.

Figure 3.

Figure 3

Comparison between experimental and simulated changes in [1,25(OH)2D3]p at different plasma Mg2+ concentrations

The lsqcurvefit function of MATLAB was used to fit our model simulations to experimental values.

The degradation of 1,25(OH)2D3 is mediated by 24-hydroxylase. PTH has a negative effect on this enzyme, whereas Mg2+ has a positive effect (Figure 10). The effect of PTH is represented by fPTHinact=11+γinactPTH[PTH]p and the effect of Mg2+ is represented by fMginact=([Mg2+]p)4(KD3)4+([Mg2+]p)4. Model parameters are given in Table 2.

Proximal tubule of the kidney

About 15-20% of the filtered Mg2+ is reabsorbed paracellularly along the proximal tubule. PTH indirectly inhibits Mg2+ reabsorption in the proximal tubule by inhibiting the activity of NHE3. Since Na+ reabsorption is accompanied by water reabsorption, less water is reabsorbed which reduces the lumen-to-interstitium Mg2+ concentration gradient; this results in decreased paracellular reabsorption of Mg2+. We model the fractional reabsorption of Mg2+ in the proximal tubule as:

λMgPT=λMgPT0+δMgPTmax1+([PTH]pPTHref)nPT. (Equation 11)

λMgPT0, which denotes the minimal fractional reabsorption of Mg2+ in the proximal tubule, is assumed to be 0.185 and δMgPTmax, which denotes the maximal stimulation of Mg2+ reabsorption in the proximal tubule by PTH, is assumed to be 0.015. These parameters yield a maximum value of λMgPT of 0.20.

Thick ascending limb of the kidney

Along the cortical thick ascending limb, about 60-70% of the filtered Mg2+ is reabsorbed, again via the paracellular pathway. In this segment Mg2+ reabsorption is upregulated by PTH and downregulated by CaSR through claudin 14 85. Claudin 14 inhibits claudins 16 and 19, which regulate paracellular permeability of Ca2+ and Mg2+ along the thick ascending limb. Activation of PTH1R (PTH receptor on the basolateral membrane) decreases claudin 14 expression, whereas activation of CaSR increases claudin 14 expression.85 The fractional reabsorption of Mg2+ along the thick ascending limb is modelled as

λMgTAL=λMgTAL0+δTAL,CASR([Ca2+]p,[Mg2+]p)+δTAL,PTH(PTH) (Equation 12)

where

δTAL,CASR([Ca2+]p,[Mg2+]p)=δMgCaSRmax(1+([Ca2+]pCaref)nTAL)(1+0.6([Mg2+]pMgref)nTAL) (Equation 13)

and

δTAL,PTH(PTH)=δMgPTHmax[PTH]p[PTH]p+KTALPTH. (Equation 14)

λMgTAL0 denotes the minimal fractional reabsorption of Mg2+ in this segment and is set to be 0.66.; δMgCaSRmax, which denotes the maximal stimulation of Mg2+ reabsorption by CaSR, is taken to be 0.028; and δMgPTHmax, which denotes the maximal stimulation of Mg2+ reabsorption by PTH, is set to be 0.012. Together these parameters yield a maximum value of λMgTAL of 0.7.

Distal convoluted tubule of the kidney

Mg2+ is reabsorbed transcellularly along the distal convoluted tubule mediated by TRPM6/7 on the apical membrane and Na-Mg exchanger (solute carrier family 41 member 1 (SLC41A1) and/or cyclin M2 (CNNM2)) on the basolateral membrane, with a fractional reabsorption rate of 5-10%. In this segment, Mg2+ reabsorption is upregulated by PTH and 1,25(OH)2D3. PTH regulates Mg2+ uptake through receptor-mediated cAMP release and activation of protein kinase A and 1,25(OH)2D3 regulates Mg2+ uptake through calbindin-D.86 We assume that the contribution of PTH is greater than that of 1,25(OH)2D3.3

λMgDCT=λMgDCT0+δDCT(PTH,D3) (Equation 15)

where

δDCT(PTH,D3)=δMgDCTmax(0.8×[PTH]p[PTH]p+KDCTPTH+0.2×[1,25(OH)2D3]p[1,25(OH)2D3]p+KDCT1,25(OH)2D3) (Equation 16)

λMgDCT0, which denotes the minimal fractional reabsorption of Mg2+ in this segment, is assumed to be 0.08 and δMgDCTmax, which denotes the maximal stimulation of Mg2+ reabsorption by PTH and 1,25(OH)2D3, as 0.02. Thus, the maximum value of λMgDCT is 0.10.

Finally, the total renal reabsorption of Mg2+ is defined as

λMgreab=λMgPT+λMgTAL+λMgDCT. (Equation 17)

The urinary excretion of Mg2+ is defined as

λMgurine=ΦGFR×[Mg2+]p×(1λMgreab) (Equation 18)

where ΦGFR denotes the glomerular filtration rate (GFR).

Model parameters are given in Table 2. The fractional reabsorption of Ca2+ along the proximal tubule, thick ascending limb, and distal convoluted tubule is modeled similar to ref.3

Intestine

Up to 70% of dietary Mg2+ is absorbed in the colon. Intestinal Mg2+ absorption has a biphasic, non-linear relationship with luminal Mg2+ concentration. Studies suggest that there are at least two intestinal transport systems for Mg2+: one dependent on 1,25(OH)2D3 and the other independent of 1,25(OH)2D3.18,87

Mg2+ absorption by the intestine consists of a non-saturable paracellular component and a saturable transcellular component.18,87 Paracellular Mg2+ absorption is responsible for 11% of intestinal Mg2+ uptake.18 Thus, the equation for fractional absorption of Mg2+ along the intestine is formulated as follows. The intestine can absorb at most 70% of the ingested Mg2+. We assume that 12% of the ingested Mg2+ is absorbed through 1,25(OH)2D3 regulation, 11% is absorbed paracellularly, and the rest (47%) is absorbed transcellularly. Thus, fractional absorption of Mg2+ along the intestine is given by

λMgintestine=IMg(0.11+0.47×VactiveKactive+IMg+0.12×f1,25(OH)2D3intestine) (Equation 19)

where f1,25(OH)2D3intestine=([1,25(OH)2D3]p)2([1,25(OH)2D3]p)2+(Kabs1,25(OH)2D3)2 represents the stimulation of Mg2+ by 1,25(OH)2D3. IMg denotes dietary Mg2+ intake, Vactive denotes the maximal rate of active absorption of Mg2+, Kactive denotes the stimulation of active Mg2+ absorption by dietary Mg2+ intake, and Kabs1,25(OH)2D3 denotes the stimulation of Mg2+ absorption by 1,25(OH)2D3.

Bones

Of the total body magnesium, about 50–60% is found in the bones where it accounts for about 1% of bone ash.19,88 One third of the bone Mg2+ is surface limited and easily exchangeable with plasma (referred to as the fast bone pool) for maintaining a normal extracellular Mg2+ concentration.19,88 The remainder is complexed with the crystalline structure of bone mineral within the hydroxyapatite lattice (referred to as the slow bone pool), which may be released during bone resorption.

The change in the amount of Mg2+ in the readily exchangeable fast bone pool (NMgf) is defined as

dNMgfdt=kpfMg[Mg2+]pVpkfpMgNMgfτacNMgf (Equation 20)

where kpfMg denotes the rate of Mg2+ uptake from the plasma by the fast bone pool, kfpMg denotes the rate of Mg2+ release from the fast bone pool to the plasma, and τac denotes the rate of accretion into the slow bone pool.

The amount of Mg2+ in the slow bone pool (NMgs) varies with time as

dNMgsdt=γacMgNMgfτres(PTH,1,25(OH)2D3). (Equation 21)

Bone resorption rate (τres(PTH,1,25(OH)2D3)) is given by3

τres(PTH,1,25(OH)2D3)=τresmin+δresmax(0.2×fPTHres+0.8×f1,25(OH)2D3res) (Equation 22)

where fPTHres=([PTH]p)2(KresPTHp)2+([PTH]p)2 represents the effect of PTH on bone resorption, and f1,25(OH)2D3res=([1,25(OH)2D3]p)2(Kres1,25(OH)2D3)2+([1,25(OH)2D3]p)2 represents the effect of 1,25(OH)2D3 on bone resorption. PTH indirectly stimulates osteoclasts (bone cells responsible for resorption) by binding to receptors on osteoblasts (bone-forming cells), which then release receptor activator of nuclear factor kappa-B ligand (RANKL) and osteoprotegerin (OPG) that stimulate osteoclast formation and activity.89 In addition, 1,25(OH)2D3 enhances bone resorption by promoting the differentiation of osteoclast precursors into mature osteoclasts by increasing the expression of RANKL.90

Plasma magnesium

The rate of change of plasma Mg2+ concentration is modeled by

d[Mg2+]pdt=(1κbMg)Vp(λMgintestine+τres(PTH,1,25(OH)2D3)+kfpMgNMgfkpfMg[Mg2+]pλMgurine) (Equation 23)

where κbMg denotes the fraction of magnesium bound to proteins. All model parameters and descriptions are given in Table 2.

Quantification and statistical analysis

The model was implemented in MATLAB. The lsqcurvefit function of MATLAB, which is a non-linear least-square solver, was used to fit our model simulations to experimental values and this is mentioned in the legends of Figures 2 and 3.

Published: September 30, 2024

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Associated Data

This section collects any data citations, data availability statements, or supplementary materials included in this article.

Data Availability Statement

The code generated in this study can be accessed at https://github.com/Pritha17/Magnesium_calcium_homeostasis.76


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