22
CALCIFICATION OF TEETH I. COMPOSITION IN RELATION TO BLOOD AND DIET* BY ALBERT E. SOBEL AND ALBERT HANOK (From the Department of Biochemistry and the Pediatric Research Laboratory, The Jewish Hospital of Brooklyn, New York) (Received for publication, July 27, 1948) These investigations were undertaken to test the hypothesis, of the au- thors, that there is a relationship between the inorganic composition of teeth and the fluid from which the tooth salts precipitate and that the composition of this jluid in turn is related to the blood serum. If this hypothesis is valid, it should be possible to vary the composition of teeth (during the period of active lime salt deposition), since the composition of blood serum can be regulated by the diet (l-6). The mineral phase is regarded as essentially the same in teeth and bone (7, 8). The variations in the composition of bone are well known (9) and were shown to be related to that of blood (5, 6). Hitherto no such rela- tionships have been shown for teeth. In fact, some recent investigations, indicate that t,he inorganic composition of enamel is constant (10). There is, however, evidence that teeth are tissues in equilibrium with body fluids, Barnum and Armstrong (11) fed P32 to cats and found that it was present in both enamel and dentin after an interval. They then postulated that dentin phosphate may be in equilibrium with blood phosphate and that enamel phosphate may be in equilibrium with dentin phosphate. Green- berg (12) administered Ca* to rachitic rats and found that in the absence of vitamin D the uptake of the isotope in the femurs was greater than in the molars but less than in the incisors. In the presence of vitamin D, the uptake was greatest in the femur, less in the incisors, and least in the molars. Vitamin D had a minor influence on teeth but a major influence on bone. Armstrong and Barnum (13) fed Ca46 and P32 to albino rats and measured the amounts found in the teeth. They found that the turnover of the isotopes in the incisor dentin was two-thirds and in the incisor enamel about one-third of that in the femur. The molar dentin was about one- sixth that of the femur and the molar enamel was from 1.5 to 3 per cent of the femur. These studies with isotopes indicate that the continually growing incisors may undergo changes almost as rapidly as bone and thus were considered suitable for our experiments. It is worth pointing out that the hypothesis * Presented in part before the Division of Biological Chemistry at the 112th meet- ing of the American Chemical Society, New York, September G-19,1947. 1103 by guest on October 5, 2020 http://www.jbc.org/ Downloaded from by guest on October 5, 2020 http://www.jbc.org/ Downloaded from by guest on October 5, 2020 http://www.jbc.org/ Downloaded from

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Page 1: CALCIFICATION OF TEETHCALCIFICATION OF TEETH I. COMPOSITION IN RELATION TO BLOOD AND DIET* BY ALBERT E. SOBEL AND ALBERT HANOK (From the Department of Biochemistry and the Pediatric

CALCIFICATION OF TEETH

I. COMPOSITION IN RELATION TO BLOOD AND DIET*

BY ALBERT E. SOBEL AND ALBERT HANOK

(From the Department of Biochemistry and the Pediatric Research Laboratory, The Jewish Hospital of Brooklyn, New York)

(Received for publication, July 27, 1948)

These investigations were undertaken to test the hypothesis, of the au- thors, that there is a relationship between the inorganic composition of teeth and the fluid from which the tooth salts precipitate and that the composition of this jluid in turn is related to the blood serum. If this hypothesis is valid, it should be possible to vary the composition of teeth (during the period of active lime salt deposition), since the composition of blood serum can be regulated by the diet (l-6).

The mineral phase is regarded as essentially the same in teeth and bone (7, 8). The variations in the composition of bone are well known (9) and were shown to be related to that of blood (5, 6). Hitherto no such rela- tionships have been shown for teeth. In fact, some recent investigations, indicate that t,he inorganic composition of enamel is constant (10). There is, however, evidence that teeth are tissues in equilibrium with body fluids, Barnum and Armstrong (11) fed P32 to cats and found that it was present in both enamel and dentin after an interval. They then postulated that dentin phosphate may be in equilibrium with blood phosphate and that enamel phosphate may be in equilibrium with dentin phosphate. Green- berg (12) administered Ca* to rachitic rats and found that in the absence of vitamin D the uptake of the isotope in the femurs was greater than in the molars but less than in the incisors. In the presence of vitamin D, the uptake was greatest in the femur, less in the incisors, and least in the molars. Vitamin D had a minor influence on teeth but a major influence on bone. Armstrong and Barnum (13) fed Ca46 and P32 to albino rats and measured the amounts found in the teeth. They found that the turnover of the isotopes in the incisor dentin was two-thirds and in the incisor enamel about one-third of that in the femur. The molar dentin was about one- sixth that of the femur and the molar enamel was from 1.5 to 3 per cent of the femur.

These studies with isotopes indicate that the continually growing incisors may undergo changes almost as rapidly as bone and thus were considered suitable for our experiments. It is worth pointing out that the hypothesis

* Presented in part before the Division of Biological Chemistry at the 112th meet- ing of the American Chemical Society, New York, September G-19,1947.

1103

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Page 2: CALCIFICATION OF TEETHCALCIFICATION OF TEETH I. COMPOSITION IN RELATION TO BLOOD AND DIET* BY ALBERT E. SOBEL AND ALBERT HANOK (From the Department of Biochemistry and the Pediatric

1104 CALCIFICATION OF TEETH. I

proposed in the first paragraph applies to teeth only during the period when active calcification takes place. In human teeth active calcification is almost complete before eruption.

The knowledge of the factors that influence the composition of teeth is of theoretical and practical importance, since further studies may reveal some relation between caries and structural, mechanical, and other properties (such as resistance to acids and bacteria) and composition.

In the experiments reported here, evidence is given that there is a rela- tionship between the POd:COs ratios of enamel, dentin, and blood serum, which in turn is regulated by the diet.

EXPERIMENTAL

The three diets used are shown in Table I. The basal diet contained traces of calcium (0.029 per cent) and suboptimal amounts of phosphorus (0.118 per cent).l To this basal diet 3.0 per cent CaC03 was added to pro- duce a high calcium-low phosphorus diet (Diet B) ; 3.0 per cent of anhy- drous NazHPOe was added to give a low calcium-high phosphorus diet (Diet C) ; and 0.4 per cent CaC03 was added to give the low calcium-low phosphorus diet (Diet D). The calcium and phosphorus contents of the diets were determined by replicate analysis. Each diet contained the same amount of either calcium or phosphorus as one of the others.

Young rats, 23 days old, were used. The animals were raised in our lab- oratory from a Wistar strain stock colony, fed on the standard stock diet of Bills et al. (14). Litters were chosen having at least eight animals per litter. Two animals of each litter were sacrificed on the 1st day of the ex- periment to furnish data on the initial composition of the blood and teeth of the litter. These animals were termed the reference group. It was necessary, owing to the small size of the young animals, to pool the blood and teet.h of both animals for analysis. The remaining six animals in each litter were divided into three pairs and each pair placed on one of the three experimental diets. In addition to these diets, one animal of each pair received daily 100 I.U. of vitamin D in 0.1 ml. of corn oil administered orally by means of a pipette. The six groups thus established were caged sep- arately, in a darkened room, to prevent mixing of the diets and to prevent the access of those animals not receiving vitamin D to this factor.

Eleven litters of rats were used. The mean initial weights of the rats were almost identical (see Table II). A reasonable basis for comparing the results of the various groups was established because of the similarity

1 In these experiments a basal diet, low in phosphate, was desired to obtain greater freedom in changing the Ca:P ratio. This was accomplished by selecting deger- minated yellow corn-meal which is low in phosphorus (Hoger Cereal Company, New York).

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A. E. SOBEL AND A. HANOK 1105

of heredity, the distribution of litters among the various groups, and the: close agreement of the initial weights.

The first group consisting of six litters, and referred to as the short term experiment, was kept on the experimental diets for 30 days, at the end of which time the rats were sacrificed by cutting the jugular vein and the carotid artery. The blood was collected under oil and centrifuged imme- diately upon clotting. The upper incisors were immediately removed, cleaned from adhering tissues, and prepared for analysis. The second group of animals, consisting of five litters (referred to as the long term ex- periment), was treated exactly the same as the animals on the short term

TABLE I Composition of Experimental Diets

Diet

B. High calcium-low phos- phorus

C. Low calcium-high phos- phorus

D. Low calcium-low phos- phorus

Basal

Constituents

Basal diet Calcium carbonate Basal diet NazHP04 Basal diet Calcium carbonate Yellow corn-meal Wheat gluten Brewers’ yeast Sodium chloride

-

-

T ports

97

3 97

3 99.6 0.4

75 19 5 1

Ca

per cent

1.20

0.028

0.189

0.029

-

-

P

per cent

-

_ - n

0.121 7.67

0.759 0.029

0.124 1.18

0.118 0.191

experiment except that they were kept on the experimental diets for 45 days.

Analytical Procedures

The serum, under oil, was analyzed for CO2 on 0.1 ml. by the manometric method of Van Slyke and Neil1 (15), for calcium in duplicate on 0.1 ml. portions by the method of Sobel and Sobel (16), and for inorganic phos-- phate in duplicate on 0.1 ml. portions by the micro modification of the Fiske-Subbarow method (17, 18), with the micro cups of the Klett-Sum- merson photoelectric calorimeter with a 660 rnp filter. Standards were run for COz, calcium, and inorganic phosphate for each set of sera. Standards for CO2 consisted of a sodium carbonate solution, 1 ml. of which is equiva- lent to 100 volumes per cent of COZ. The standard for calcium consisted of a calcium carbonate solution, 0.1 ml. of which is equivalent to 10.00 y of calcium. The standard for inorganic phosphate consisted of a solu- tion of KHzPO+ 5 ml. of which are equivalent to 40.0 y of P. The pre- cision of the methods is shown in Table III.

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1106 CALCIFICATION OF TEETH. I

The upper incisors were split into fragments and extracted for three over- night periods with two portions of acid- and aldehyde-free ethyl alcohol and one portion of ethyl ether. The fragments were then dried overnight

Experimental period, 30 days

Experimental period, 45 days

TABLE II

Growth data

Dietary group

Reference group B C D B + vitamin D (J + “ “ D + ‘I “

B-C (6 - D c - ‘C

B + vitamin D - C + vitamin D “ I‘ ‘I _ ,, + “ “

c+ “ 6‘ _ “ + I‘ ‘I

B - (B + vitamin D) c-(c+ “ “1 D-CD+ “ “1 Reference group B C D B + vitamin D c + “ “ Df “ “ B-C (1 - D c - “

B + vitamin D - C + vitamin D “+ “ “ - D + “ “ c- (6 “ _ (6 + ‘L “

B - (B + vitamin D) c-cc+ “ ‘6) D-(D+ “ “1

- Initial weight

+93mo.1

-t-31.1 +31.2 $30.0 +30.6 +30.3 +29.7

-0.1 +1.1 +1.2 +0.3 +0.9 +0.6 +0.5 +0.9 +0.3

+35.6 f36.8 f36.6 +35.8 f36.1 +36.1 f36.8

+0.2 +1.0 +0.8

0.0 -0.7 -0.7 +0.7 +0.5 -1.0

Final weight

P.

+55.0 +44.5 1-64.9 +43.6 f48.5 +73.5 +11.5

-9.9 -20.4

-4.9 -29.9 -25.0 +11.4

-4.0 -8.6

+51.9 +45.9 +82.1 +43.4 +64.5 +88.4

+6.0 -30.2 -36.2 -21.1 -45.0 -23.9

+8.5 -18.6

-6.3

-

- Gain

m.

+23.9 +13.3 f34.9 f13.0 f18.2 +43.8 +10.6 -11.0 -21.6

-5.2 -30.8 -25.6 +10.9

-4.9 -8.9

+15.1 +9.3

+46.3 +7.3

+28.4 +51.6

+5.8 -31.2 -37.0 -21.1 -44.3 -23.2 +7.8

-19.1 -5.3

at 105”, weighed, and the enamel and dentin separated by the method of Manly and Hodge (19), which was modified to the extent that the tube used for carbonate analysis (20) was employed instead of the centrifuge tube recommended by Manly and Hodge. This was done to obviate the neces-

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A. E. SOBEL AND A. HANOK 1107

sity of transferring small amounts of enamel and dentin obtained from the teeth, with the consequent mechanical loss of material. The separated enamel and dentin were dried overnight at 105”, after two acetone washings, and placed in a desiccator till cool and then weighed. These weights were used to calculate the percentages of the inorganic constituents of the enamel and dentin.

The enamel was analyzed for carbonate, calcium, phosphate, and total base as previously described (18), except that the Coleman spectropho- tometer was used instead of the visual calorimeter for phosphate. For the carbonate analysis, the gasometric reagents were prepared in 25 per cent sodium chloride for added sensitivity (21). Standard solutions were run for calcium, phosphate, total base, and for carbonate solid mixtures. The

TABLE III Precision of ihe Determinations of Standard Solutions Employed As Controls for

Enamel, Dentin, and Blood Serum Analysis

Mean values (approximately 50 determinations plus-minus average deviations).

Ca’ cat Colt co30 PO4 Total base1

Y Y uol. per celat wt. per Cell Y tn.ep.

10.03 f 0.12 199.0 f 1.7 100.0 zt 1.3 2.00 f 0.02 39.0 f 0.5;0.101 f 0.001

* 10.00 y of Ca present in 0.1 ml. used for analysis. t 200 y of Ca present in 1.0 ml. of solution used for analysis (bone method). $ 100.0 volumes per cent of CO2 present; 0.1 ml. used for analysis. $2.00 per cent as CO3 in a mixture of solid NaCl and Na&Os (bone method). 11 40.0 y of phosphate P present (bone and blood methods). q 0.100 milliequivalent of Ca present in 1.00 ml.

latter consisted of a dry sodium chloride-sodium carbonate mixture con- taining 2.00 per cent COS. The precision of these determinations is given in Table III.

Cazcuzations (6, 20) Carbonate

Mg. CO3 in sampIe = Pcoz X factor for Cot Pco, = p1 - p2 - c

c = pi - pi for blank analysis

Calcium

Mg. Ca in sample = titer X normality of acid X 20 X total volume

volume of aliquot used

Klett-Summerson calorimeter: Phosphate

Mg. P in aliquot = reading of unknown

X concentration of standard reading of standard

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1108 CALCIFICATION OF TEETH. I

For the Coleman spectrophotometer (used for tooth analysis) a calibration curve was employed.

Mg. P in sample = mg. P in aliquot X total volume of solution volume of aliquot used

Total Base

Milliequivalents total base = titer X normality of acid X total volume of solution

volume of aliquot used

mM Ca = (mg. Ca in enamel or dentin)/40.08 “ PO4 = (mg. inorganic P in enamel or dentin)/31.02 “ CO3 = (mg. CQ in enamel or dentin)/60.01 “ 7, Ca, P04, COS, or total base = (mM Ca, P04, COQ or total base X lOO)/mg. weight of dry, fat-free enamel or dentin

Ca:P04 ratio = mM Ca:mM PO4 mM residual Ca = mM total Ca minus mM CO3

total base Milliequivalents residual p2 = milliequivalents total base minus mM CO1

2 Residual Ca:P04 = mM residual Ca:mM PO4

‘< total base: 2PO4 = milliequivalents residual total base: 2 mM PO4 Po4: 2co~ = rnhf P04: 2 mM Cot

The POe:2C03 = n in the usual way of representing the inorganic com- position of bone and teeth [Ca3(PO&],[CaCO&.o (7, 8) when the molar ratio of residual Ca: PO1 is 1.50. This holds true also when the residual Ca : PO1 molar ratio is more than 1.50 if we take the CaC03 as unity. The formula in this case would be [Ca3(P0&],[CaC0&.o[CaX],. When the residual Ca:POd molar ratio is less than 1.50, we have the type of formula represented by [Cas(PO&],[CaC0&.o[CaHP04]x and n is then overstated.

The mean results of the enamel and dentin analysis were evaluated by the statistical methods of Fisher (22) as applied to small samples. P represents the probability that the difference between two means is due to chance. When P has a value less than 0.05, the difference between two means is statistically significant.

Weight Changes

The weight, changes, including the initial and final weights are given in Table II. Both in the absence and in the presence of vitamin D, Diet D gave the best, growth. This is in harmony with the fact that dietary cal- cium to phosphorus ratios between 1.0 and 2.0 are optimum for best growth (l-3). The absence of vitamin D gave better growth in Group C than in Group D, and in the presence of vitamin D, the reverse was the case. In previous experiments (5) better growth was obtained in Group B than in Group C, since the phosphate level was 0.32 per cent instead of the present 0.12 per cent.

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A. E. SOBEL AND A. HANOK 1109

The influence of vitamin D was greatest in Group C. In Group B, there was a reduction which again may be explained on the basis of the relatively high calcium-low phosphorus ratio. On such diets vitamin D diverts the available phosphorus from the soft tissues to the bone. In Group D, in which growth was greatest, the addition of vitamin D had no significant effect. In the absence of vitamin D the rickets produced in Group B were severe and in Group C mild.

TABLE IV

Composition of Serum in Relation to Diet (Mean Values)

Experimental period, 30 days

I.

Experimental period, 45 days

I -

Dietary group

B C D B + vitamin D c + “ “ D + “ “ Reference B C D B + vitamin D c + “ “ D + “ “ Reference

- n

Ca

“s‘;;; ,Gd,Qf

11.7 2.1 5.6 7.5 9.4 4.7

13.3 3.4 8.8 8.4

11.1 6.0 11.2 9.5 12.3 1.8 5.1 4.9

10.0 2.6 15.0 3.4

8.9 5.2 11.2 4.6 10.9 7.7

P

1

co2

ml. per cent

60.6 53.7 58.0 62.6 57.6 56.0 47.6 54.1 57.7 50.6 57.6 56.2 55.6 53.9

‘a x P Ca:P04

molar ratio

23.1 4.32 41.8 0.58 44.1 1.55 44.9 3.03 74.2 0.81 65.8 1.43

105.8 0.92 22.2 5.30 25.0 0.81 26.0 2.98 51.0 3.42 46.4 1.33

OF

-

‘On: Dietary CO8 Ca:P

molar molar ratio ratio

0.025~ 7.67 0.101~ 0.029 0.057 1.18 0.0391 7.67 0.108’ 0.076!

0.029 1.18

0.148i 0.024~ 0.062;

7.67 0.029

0.037' 0.043:

1.18 7.67

0.067; 0.060~

0.029 1.18

0.1041

Composition of Blood, Enamel, and Dentin

Blood Serum and Diet-The results obtained from the analysis of the blood sera are presented in Table IV. There is a direct relationship in the order of magnitude of serum Ca:POd and dietary Ca:P ratios. There is an inverse relationship in the order of magnitude of serum POa:COa and dietary Ca:P ratios. Vitamin D raised the Ca X P product in all cases, the per cent rise being more in that member of the calcium-phosphorus pair which was low compared to the normal, but did not completely over- come the influence of the diet. For this reason the differences between the maxima and minima in the Ca : PO4 and the PO4 : CO, ratios are less, though still in the same order as in the absence of vitamin D. These relationships confirm, even more definitely, the results of previous investigators (l-6).

Deposition of Inorganic Components As Indicated by Percentages Present- It is evident from Table V that the density of calcium, carbonate, and total base is decisively higher in the enamel than in the dentin in all cases.

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1110 CALCIFICATION OF TEETH. I

The density of phosphorus is higher in all but two cases. This confirms previous work indicating higher density in enamel (19, 23-26). Dietary calcium, phosphorus, and vitamin D were not decisive in influencing the density of either enamel or dentin, though in the long term experiment the carbonate was highest in Group B and lowest in Group C.

Enavzel, Dentin, and Blood Serum-The composition of enamel and den- tin in relation to blood serum and diet is given in Table VI and the statis- tical evaluation of the data in Table VII. One is impressed by the fact that the differences that existed in composition were magnified in the long term experiment. The Pod: CO, ratios in dentin and enamel arrange them-

TABLE V

Composition of Enamel and Dentin (Mean Values)

The results for total base are given in milliequivalents per cent X 100; for Ca, PO1, and CO, in rnM per cent X 100.

Experimental period, 30 days

Experimental period, 45 daye

Dietary group

B C D B + vitamin D

c + “ “ D + “ “ Reference B C D B + vitamin D c + “ “ D + “ “ Reference

Enamel Dentin

~--_____ -__- 200.0 96.6 50.6 5.31 124.3 61.2-43.6 5.05 199.5 94.3 55.6 5.20 111.3 54.1 39.3 3.67 224.2108.9 56.0 5.02 118.7 58.5 45.1 4.27 149.0 71.5 40.8 6.57 116.8 57.3 41.5 4.56 166.3 80.3 46.4 4.37 117.5 58.2 44.9 3.83 186.0 87.3 51.7 5.64 119.2 59.0 44.1 4.12 219.0102.2 47.8 5.99 125.3 59.6 45.2 3.61 181.4 90.1 45.2 6.17 133.8 64.2 44.1 4.15 196.2 96.1 51.5 3.47 124.6 61.5 44.2 2.48 188.6 93.5 46.4 4.00’ 143.0 68.1 50.4 3.63 188.5 93.2 50.5 6.35, 130.8 63.4 46.6 4.46 198.3 98.5 55.1 4.01 132.3 65.4 48.1 3.02 191.6 94.7 47.9 4.32 135.4 67.2 47.2 3.39 169.4 84.5 49.8 7.78; 124.61 59.9 44.3 3.62

selves in the same order as the serum POa:COs ratios for the three groups not receiving vitamin A. The same holds true for the three groups re- ceiving vitamin D. When all six groups of the short term experiment are arranged in the order of magnitude of serum Pod: CO3 ratios, the POa: CO3 ratios in both dentin and enamel follow the same order. In the long term experiment the dentin and enamel P04:C0, and serum POa:COs ratios do not show the same pattern as in the short term experiment when all six groups are arranged in order of magnitude. This may be indirect evidence that vitamin D has an influence. Statistically, the most signifi- cant differences are between the two extreme groups; namely, Group B (high calcium-low phosphorus) a.nd Group C (low calcium-high phosphorus).

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A. E. SOBEL AND A. HANOK 1111

The Pod: CO3 ratios of the enamel in all cases are lower than of the cor- responding dentin. The difference was most marked in the high calcium- low phosphorus group (Diet B) and least in the low calcium-high phos- phorus group (Diet C). In fact the differences in the absence of vitamin D for this group were not statistically significant, though all other differences were statistically significant for corresponding enamels and dentins. In this connection one can point out that the differences in composition be- tween enamel and dentin of humans and dogs (26) and rats (27) may be due to the particular diet given rather than to species differentiation.

TABLE VI Composition of Enamel and Dentin in Relation to Blood Serum and Diet (Mean Values)

The results represent molar ratios.

Experimental period, 30 days

Experimental period, 45 days

- I

Dietary WXIP

B C D B + vitamin D Cf “ “

Df “ “ Reference B C D B + vitamin D c + “ ‘I

D + “ “ Reference

lietary a:POc -

2 a

v --

7.67 4.32 0.029 0.58 1.18 1.55 7.67 3.03 0.029 0.81 1.18 1.43

0.92 7.67 5.30 0.029 0.81 1.18 2.98 7.67 3.42 0.029 1.33 1.18 1.89

1.10

--

g - . . & w

& 2

v --

2.51 1.92 10.10 1.68 5.86 1.95 3.94 1.75

10.80 1.74 7.75 1.70

14.80 2.20 2.41 1.99 6.15 1.85 3.72 2.01 4.27 1.86 6.70 1.77 5.991 1.98

10.40/ 1.68

2.08 1.41 4.60 1.38 2.65 1.31 2.43 1.38 3.68 1.29 3.00 1.36 3.25 1.31 3.71 1.51 7.72 1.41 5.92 1.36 3.62 1.39 6.94 1.36 5.67 1.41 3.34 1.39

-

Dentin

-

4.40 5.43 5.15 4.60 5.98 5.41 6.56 5.47 9.31 6.87 5.55 7.97 7.27 4.88

* x 100.

Not until we understand the influence of diet in a given species can we dis- cuss the differences between enamel and dentin as characteristic of different species.

Though Ca:P04 ratios of serum undergo wide variations, in the enamel and dentin the ratios undergo no corresponding variations. Statistically there were significant differences in the two extreme groups; namely, the high calcium-low phosphorus and the low calcium-high phosphorus group (Diets B and C). In the short term experiment these differences were so only in the enamel, while in the long term experiment they were true for both enamel and dentin. In our earlier studies on bone (6), significant

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1112 CALCIFICATION OF TEETH. I

differences were obtained only between the two extreme diets (Diets A and B) in the absence of vitamin D.

The Ca:POJ ratio in the enamel is significantly higher, in all cases, than the ratio for the corresponding dentin. This would imply that if we as- sume t,he apatite formula, ICa3(P0&],[CaX], X, in addition to carbonate, must have some other radical in the enamel, possibly citrate, which was reported (28), or fluoride, and in the dentin it must be some phosphate, probably HP04- (6, 29).

The ratios of residual total base to 2PO4 and residual Ca:POe are given

TABLE VII

Statistical Evaluation of Ratios Presented in Table VI (P Values) All P values are less than the numbers shown,

Experimental period, 30 days

B vs. C “ “ D c “ <‘

B + vitamin D vs. C + vita- min D

5 B + vitamin D OS. D + vita- min D

6 C + vitamin D vs. D + vita- min D

7 8 9

10 11 12 13 14 15 16 17 18 19 20 21 22 I

B ~.a. B + vitamin D

c “ c + “ “ D “ D + “ “ Reference vs. B

“ “ c <‘ (& D “ “ B + vitamin D i‘ “ c + “ “ “ “ D + (‘ “

B C D B + vitamin D

c + “ “ D + “ “ Reference

- T

0.0. 0.0 0.0: 0.0:

0.01 0.0: 0.01, 0.9 0.01’ 0.2 0.61 0.6

0.0: 0.01 0.7

0.0: 0.1 0.9

O.O! 0.05’ 0.2 0.0: 0.6 0.7 0.6 0.1 0.1 0.0: 0.01 0.5 0.1 0.01 0.2 0.0: 0.01 0.6 0.0: 0.011 0.2 0.2 0.01; 0.3 0.0: 0.01 0.2

0.4 0.0: 0.01 0.2 0.02 0.6 0.02 0.01

0.6 0.0:

0.2 0.5 0.05 0.2 0.3 0.6 0.02 0.01 0.1 0.2 1.00 0.1 0.05 0.01 0.7 0.5 0.4 0.2

0.01 0.3 0.01 0.01 0.01 0.01 0.01

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A. E. SOBEL AND A. HANOK

TABLE VII-Concluded

1113

Serum Enamel Dentin e ylele~.

Line NO. Dietary group

Experimental period, 45 days

1’ 2’ 3’ 4’

5’

6’

7’ 8’ 9’

10’ 11’ 12’ 13’ 14’ 15’ 16’ 17’ 18’ 19’ 20’ 21’ 22’

i

B vs. C “ “ D (J“ (( B + vitamin D vs. C + vita-

min D B + vitamin D vs. D + vita-

min D C + vitamin D vs. D + vita-

minD B vs. B + vitamin D c “ c + “ “ D “ D + “ “ Reference vs. B

‘I “ c ‘I “ D ‘I “ B + vitamin D “ (‘ c + “ “ ‘I “ D + “ “

B C D B + vitamin D c + “ “ D + “ “ Reference

0.05 0.01 0.9

0.01 0.0: 0.01 0.01 0.05’ 0.8 0.01 0.6

0.1 0.3 0.2 0.01 0.8

0.01 0.6 0.01 0.05 0.4

0.2 0.2 0.2 0.01 1.00 0.8 0.1 0.1 0.7 0.01 0.01 0.02 0.01 0.01 0.2 0.01 0.01 0.01 0.01 0.01 0.1 0.01 0.01 0.3

0.8 0.1 0.4 0.7 0.6 0.5 0.2 0.02 0.01 0.4 0.01 0.6 0.3 1.0 0.01 0.2 0.01 0.8 0.01 0.01 0.01

0.0 0.0: 0.0: 0.0:

0.1

0.3

0.9 0.2 0.1 0.3 0.01 0.0: 0.01

0.01

0.0:

0.01 0.01 0.01 0.01 0.01 0.01 0.01

0.01 0.2 0.05 0.05 0.02 0.05 0.01

in Table VIII. It is evident that the ratios are still above 1.50 for enamel and below 1.50 for dentin. Thus the differences cannot be accounted for on the basis of the high carbonate content of the enamel.

Another point worth mentioning is that the difference between total base and calcium is not as great as that in bone (6).

Some differences in the two reference groups, shown in Table VI, need to be pointed out. The Ca:P04 ratio of the enamel and of the dentin is much higher in the first reference group than in the second. The rats in the two reference groups were raised about 10 months apart and differences in them may be accounted for by the fact that the stock diet used (14) is made up of dried milk, crude casein, yellow corn, alfalfa, cottonseed

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1114 CALCIFICATION OF TEETH. I

meal, brewers’ yeast, and salt. Each one of the components, except the salt, can undergo wide variations in composition from batch to batch and thus may cause changes in the fluids that feed the embryo (of which prac- tically nothing is known at the present time) and in the composition of the mother’s milk, which is known to undergo change (30).

TABLE VIII

Comparison of Residual Total Base to PO4 and Residual Ca to PO1 of Enamel and Dentin (Mean Values)

Experimental period, 30 days

B .._._,................ 95.7 91.31.971.921.891.80 57.156.11.431.411.311.29 C. ._....,..____...,._._ 94.6 89.11.791.681.701.60 52.050.51.421.381.321.28 D . . . . .._._....._____._. 107.1103.92.001.951.921.86 55.154.21.321.311.221.20 B + vitamin D. . . 67.9 64.91.821.751.661.59 53.852.71.411.381.301.27 c+ “ “ 78.7 75.91.791.741.701.63 55.054.41.311.291.231.21 D+ “ “ ,.._..._. 87.4 81.71.821.701.691.58 55.554.91.351.341.261.25 Reference..............103.5 96.22.292.202.172.01 59.156.01.391.311.311.24

B ......................

C ...................... D ...................... B + vitamin D ......... c+ “ “. ........ D+ “ “ ......... Reference. .............

T.B. = total base.

Experimental period, 45 days

84.5 83.92.001.991.871.86 62.760.01.521.511.421.36 94.6 92.61.901.851.841.80 59.859.01.411.411.351.33 90.0 89.52.032.011.941.93 67.964.51.421.361.351.28 87.9 86.61.871.861.741.72 60.958.91.401.391.311.26 95.2 94.51.801.771.731.71 63.262.41.381.361.311.30 91.5 90.42.001.981.911.89 64.363.81.441.411.361.35 76.9 76.71.701.681.541.54 58.756.61.401.391.331.28

DISCUSSION

It is evident from these experiments that there is a relationship between the PO1:CO1 ratio of blood serum and that of enamel and dentin; this is illustrated in Table IX. For enamel and dentin the Pod: COS ratio in those groups without vitamin D follows that for serum. The same holds true for those groups given vitamin D. These three groups are arranged in a descending order of diet’ary Ca:P ratios. Thus the relationship of diet, blood, and teeth is evident. This relationship, in the 30 day experiment,

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A. E. SOBEL AND A. HANOK 1115

between blood and teeth is complete. In the 45 day experiment, however, we must segregate the vitamin D-fed groups from the non-vitamin D groups. Vitamin D may manifest an influence that is evident, only in the older animals. The effect of vitamin D is not as great on the tooth Pod: CO3 ratios as one might expect from the changes in the serum POc:COS ratios. In this connection it is worth mentioning that the density of neither enamel nor dentin was influenced by vitamin D. The rate of turnover of isotopic calcium and phosphorus in the teeth is not markedly influenced by vitamin D (12, 13). This points to an import,ant difference between tooth and bone; namely, that in bone vitamin D exerts a marked influence on the POd:COa ratio, density of calcification, and rate of turnover of cal- cium and phosphorus (5, 6, 12, 13). However, it was possible to demon-

TABLE IX

Relation of Enamel, Dentin POI: 2COs, and Blood Serum POC: CO2 (il4ean Values)

Group Vitamin D..

Experimental period, 45 days

Serum X 1000.. 104 24.1 37.2 42.7 59.9 Enamel X 100. . 334 371 592 362 567

Dentin X 100. 488 547 687 555 727

-

108 368 598

67.0 694 797

strate histological changes in teeth due to lack of vitamin D on a high calcium-low phosphorus diet analogous to that found in bone (31-37).

P04:COa ratios in enamel are in all cases lower than in dentin. The difference was most marked in the high calcium-low phosphorus group (Diet B) and least in the low calcium-high phosphorus group (Diet C). Logan reported (26) that human enamel has a lower carbonate content than human dentin, whereas the carbonate contents of dog enamel and dentin were nearly equal. Bremer (38) found more carbonate in dog dentin than in dog enamel. He also found differences in regions of the enamel and dentin of a single human tooth. Armstrong and Brekhus (24) reported higher Pod: COa ratios in the enamel than in the dentin of human teeth. In view of the above findings with rats, one can point out that the diferences in composition between enamel and dentin may be due to a par- ticular diet rather than to species diferentiation. That more than one type

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1116 CALCIFICATION OF TEETH. I

of composition of dentin exists in a given species is indicated by the find- ings of Bale et al. (39). They found that on heating dentin to 900” some samples gave the apatite pattern, while others had the p-Ca3(P0& lattice. Not until we understand the influence of diet in a given species can we dis- cuss the differences between enamel and dentin as characteristic of various species.

The variations in P04:2C03 ratios in the different groups, which is a measure of n in the apatite formula, [Ca,(PO&],[CaCO,], in these teeth, is far greater than those hitherto encountered in bone. In enamel this is from 2.08 to 7.72 and in the dentin from 4.40 to 9.31. In bone the widest spread hitherto found has been 1.86 to 3.33 (6, 9, 40). The question arises as to whether with longer experimental periods (over 45 days) the spread of n would not be even greater.

The Ca:P04 ratios2 of the enamel are distinctly higher than those of the corresponding dentin in all dietary groups (see Tables VI to VIII). Such differences were not found in the reported analyses of human teeth, most of which are given in Armstrong’s review (41), nor in dog teeth (26). The ratios of residual total base to 2P04 (Table VIII) are all higher than 1.50 for enamel and less than 1.50 for dentin. Our x-ray diffraction studies3 indicate that apatite is the main lattice in both the enamel and dentin of such teeth. This would imply that in enamel for the apatite formula, [Ca3(P04)&[CaX], X must have some other radical in addition to car- bonate, which may be hydroxyl or possibly citrate (28) or fluoride. For dentin, X is some phosphate, probably HPOh (6, 29). We hope that x- ray diffraction studies, which are in progress, may throw further light on this subject.

While Ca : PO1 ratios in serum undergo wide variation, no such wide vari- ations are found for Ca:PO1 or residual Ca: POa in enamel and dentin. On the whole, the ratios in Group B were higher than those in Group C. In this connection one may note that the variations in Ca:POa ratios in bone are relatively slight and were significant only between Groups B and C in the absence of vitamin D (6). It may be concluded that the POC: CO3 ratios in bone and teeth are characterized by large variations, whereas the Ca:P04 ratios are characterized by slight variations.

2 It must be emphasized that all through these analyses a ground-up bone sample was periodically analyzed with approximately the same amounts of solid and by the same methods as in the case of enamel and dentin. In each instance we obtained the same residual Ca:POd ratio, which was between 1.51 and 1.52. The theoretical residual Ca:POc ratio is 1.50 for [Caa(PO&[CaCOs]. Thus the changes in Ca:POa and residual Ca:POa ratios must be taken as valid.

3 Sobel, A. E., Hanok, A., Kirshner, H., and Fankuchen, I., unpublished experi- ments.

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A. E. SOBEL AND A. HANOK 1117

In Table X, data from Experiments 112 and 117 of Logan and Taylor were recalculated (42). It may be noted that for a 33 per cent increase in the POh:COa ratio of the initial liquid composition the ratio of the solid increased 41 per cent. For a 33 per cent increase in the Ca:P04 ratio of the initial liquid, the ratio in the solid increased 3 per cent, and the residual Ca:POd ratio underwent no change at all. These studies are fragmentary and by no means conclusive; nevertheless they may be taken as clues explaining the relative constancy of Ca:POd ratios in teeth and bone and the wide variations in the POd:COs ratios. A systematic in- vestigation of the inorganic precipitates formed in the presence of various amounts of Ca, PO+ and COS ions is needed to understand fully the rela- tionships found between the composition of teeth and bone and blood serum.

TABLE X POIWOS and Ca:P04 Ratios of Liquid and Solid (Calculated from Data of Logan and

Taylor (~9))

I PO,: 2co. I Ca: PO4

Experiment No., Logan and Taylor (42) . 112 117 112 ,~ molar ratio molar ratio molar ratio

Liquid initially.. . . . . 2.39 1.79 1.00 I‘ at end of 20 days. . . . 1.00 0.17 0.0035

Ppt. at end of 20 days. . . . . . 4.71 3.35 1.54 1.44*

* Residual Ca:POd ratio.

117

molar ratio

1.33 0.0094 1.59 1.44*

The relationships established in these studies were found in the continu- ously growing incisors of rats. The question naturally arises as to whether molars and incisors of species which do not have continuous growth would behave in a similar fashion. The full answer cannot be given at present owing to lack of sufficient evidence. Experiments with isot*opes indicate a turnover in even fully erupted molars (11-13). It is our contention that during the period of most active calcification of molars (or of incisors that do not grow continuously) the same laws must essentially hold true. As permanent teeth become more completely calcified, equilibrium with the body fluids slows up to such an extent that only minor changes can be ob- served. It is our hope that by controlling the diet of a species that has secondary dentition during the period of active calcification of the second- ary teeth we will be able to put the above contention to experimental test.

An exact quantitative relationship between the composition of blood and teeth cannot be expressed at present, since this would involve a knowledge

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1118 CALCIFICATION OF TEETH. I

of the activities of the tooth-forming ions at the site of deposition. It would also require knowledge of the exact relationship between composition of the solid and the ionic activities of the ions that form the solid. Such knowledge is not yet available. These experiments, however, do indicate that the composition of serum is one of the controlling factors. Another factor is one which affects diffusion to the site of deposition. Vitamin D and age may play a part in the permeability of the membrane interposed between blood serum and growing teeth. Various “local factors” may also be instrumental in changing the composition of the fluid. Enzymatic fac- tors have been shown t.o play a part in calcification of bone (4345). Ex- periments on calcification of bone in vitro have shown that a minimal Ca X P product is required for deposition (46). This minimal Ca X P product was lowest in embryonic rabbit bone (47). In rachitic animals, a higher product was necessary for new calcification, and the more pro- longed the rachitic period the higher the product required (48). In rickets due to beryllium and strontium the required product is much higher (49, 50). The experiments with rickets due to strontium indicate a reversible injury to a “local factor,” enzymatic in nature and other than phosphatase. The more recent experiments of Gutman et al. (45) indicate that the enzyme system for “phosphorylative glycolosis” is important in the calcification of bone cartilage. From this discussion, it is evident that the “local factors” must be considered in t,he deposition of lime salts. “Local factors” in themselves operate within the limits prescribed by physicochemical laws, because in each case a minimal Ca X P product is required. The composi- tion of bone is a reflection of the composition of serum (6), and the same holds true for teeth, as shown in these experiments. As yet the validity of a minimal Ca X P product for a given tooth has not been experimentally proved, but in view of the changes in composition, which indicate a phys- icochemical mechanism, it is likely that the “local factors” in teeth require a minimal Ca X P product. That “local factors” do have an influence is indicated by the difference in composition between enamel and dentin. There should be no differences if only humoral factors are effective.

It is possible that in addition to the Ca and P content other components of the diet will have an effect on the composition of the tooth. This may happen either by affecting the concentration or the diffusion of Ca, POI, and CO, across the body membranes or else by altering the nature of the “local factors.” There is some evidence that dietary nutrients must play a part in the calcification of teeth and probably have a r81e in affecting composition. The importance of vitamins A and C for the proper develop- ment of the organic matrix and that of vitamin D for proper calcification have been repeatedly emphasized. The subject has been reviewed by Armstrong (51). Pincus has shown that an essential amino acid, tyrosine,

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A. E. SOBEL AND A. HANOK 1119

is present in appreciable amounts in enamel protein (52). The diets which were used in these experiments are essentially modified rickets-producing diets and are not complete because, by adding vitamin D and sufficient optimal amounts of Ca and P, the rate of growth is still not that of the stock diet. It has been pointed out that rickets-producing diets have inade- quate amounts of lysine (53). It is quite possible that on a different diet, for example one rich in all the essential amino acids, the composition of the teeth would have been different, since both the humoral and local factors might have been influenced. It is our contention, however, that a relation- ship between the POl:COa ratios of serum and enamel and dentin would still exist, though possibly shifted to a higher or lower level. These studies serve to introduce the concept of the variability of the composition of the inorganic portion of teeth in relation to blood serum and diet, and will be continued. All of the factors that influence the composition of teeth merit serious attention.

The factors that influence the composition of enamel and dentin are likely to be of fundamental importance in understanding the problem of dental caries. Reports by Logan and Taylor (54) and by Dallemagne et al. (55, 56), indicate that the carbonate content of bone salt can be preferen- tially dissolved by dilute hydrochloric or citric acids. “Hence, bone salts are a simple physical complex of phosphate and carbonate. If we were dealing with carbonate-apatite, the two constituents.. . could not possibly be separated by using the same chemical methods” (56). From the fact that the acid-extracted bone residue before heating gave the apatite pat- tern and after ignition at 900” gave the @-Ca3(PO& pattern, they concluded that the main structure is Q-Ca3(PO&.2Hz0 admixed with CaC03. When the two are heated together at 900”, apatite is obtained (56). The theo- retical conclusions may be questioned, since treatment with acids (which remove the carbonate) may have also caused production of CaHP04. It has already been established that hydroxyapatite when ignited in the presence of CaHP04 is converted to p-Ca3(PO& (29). Regardless of the full validity of the theoretical conclusions, the important fact remains that the carbonate portions of bone salts can be dissolved under conditions that leave the phosphate practically intact. Ij this holds true for teeth, it would indicate that teeth high in carbonate are more soluble in dilute acids than teeth low in carbonate, and are therefore more susceptible to at least one type of caries.

Dallemagne et al. (56, 57) report, on the basis of optical methods only, that the mineral fract,ion of dentin and cementum from teeth is the same as that of bone. Enamel prisms consist of real carbonatoapatite. The interprismatic substance consists of organic matter impregnated mostly with a-Caa(P0&.2H20. Dallemagne and Melon showed that the inter-

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1120 CALCIFICATION OF TEETH. I

prismatic substance (presumably cr-Cas(P0&.2Hz0) may be preferentially dissolved by salicylic acid (58). They did not exclude the possibility that t,he 01-&(P0& is, in turn, admixed with CaCO$ to varying proportions. Thus one may envision a portion of the carbonate as the Achilles heel of the tooth, while that portion that goes int,o the carbonatoapatite is the resist,ant portion of the tooth. Further investigations are required to de- termine to what degree the diet influences the proportions of carbonato- apatite and adsorbed CaCOs in the tooth.

We hope that other investigations in progress will help to show the re- lationship of the present studies to caries.

SUMMARY

1. Experimental evidence is given for part of the hypothesis of the authors that there is a relationship between the composition of teeth and the fluid from which the tooth salts precipitate and that the composition of this Jluid in turn is related to the blood serum. It was possible to show relationship between blood serum and the composition of the upper incisor of the white rat.

2. Pod: CO3 ratios of enamel and dentin are related to Pod: CO3 ratios in serum.

3. POd:COs ratios of dentin are in all cases higher than those of cor- responding enamels. The differences are not statistically significant when the PO4:COs ratios are highest.

4. In the formula [Ca,(PO&],[CaCO,J, n ranges from 2.08 to 7.72 for enamel and 4.40 to 9.31 for dentin in the various experimental groups. This is a far greater variation than has hitherto been observed in bone under comparable conditions.

5. The Ca:POe ratios of enamel and dentin have undergone relatively small changes, whereas changes in the ratios for serum are relatively large.

6. The Ca: PO4 ratios of enamel are in all groups significantly higher than those for the corresponding dentins.

7. Ratios for the residual total base to PO4 and the residual Ca to PO4 indicate that in the formula [Ca3(PO&],[CaX] for enamel X must have some other anion in addition to carbonate. In the dentin, X, in addition to carbonate, must have some phosphate, probably HPOh.

8. It has been shown that the composition of the diet is reflected in the blood serum and that the composition of teeth (just as that of bone) is related t,o that of serum.

9. The density of minerals in neither enamel nor dentin is influenced by vitamin D. This is in contrast to the observations in bone, in which the density is significantly increased under the influence of vitamin D.

10. The implications of these findings for the understanding of the mech-

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A. E. SOBEL AND A. HANOK 1121

anism of calcification of teeth and the relation of composition to caries are discussed.

BIBLIOGRAPHY

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1122 CALCIFICATION OF TEETH. I

39. Bale, W. F., LeFevre, M. L., and Hodge, H. C., Naturwissenschaften, 24,636 (1936).

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Albert E. Sobel and Albert HanokBLOOD AND DIET

COMPOSITION IN RELATION TO CALCIFICATION OF TEETH: I.

1948, 176:1103-1122.J. Biol. Chem. 

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CORRECTION

In the article on page 1103, Vol. 176, No. 3, December, 1948, substitute the follow- ing Tables V and VIII.

TABLE V Composition of Enamel and Dentin (Mean Values)

The results for total base are given in milliequivalents per cent X 100; for Ca, POa, and COn in rn~ per cent x 100.

Enamel Dentin

CC% Dietary group -

Total ,-.a base POa coa Total

base PO4 cos

4.96 3.62 4.38 4.51 3.75 4.08

E 2.38

E 3.02 3.24 4.54

I- Experimental period, 30 days

: D B + vitamin D c + :: 1: DS Reference B c u B + vitamin D c”t :I :: Df Reference

12.12 6.05

10.56 8.40

!f 7:38 6.10

2 6.95 3.97 4.22 7.45

124.3 111.3 118.7 116.8

::;4 125:3 133.8 124.6 143.0 130.8 132.3 135.4 124.6

61.2 54.1 58.5 57.3

2: 59:6 66.6 61.5 68.1 64.4 65.4 67.2 61.2

43.6

E

% 44:1

ii:; 44.2

Ei:64 48.1 47.2 44.3

TABLE VIII Conzparison ofResidw1 Total Base (T.B.) to PO* end Residual Ca to POa of Enamel and Dentin (Mean Values)

Enamel I

Dentin

Dietary group -2

- Experimental period, 30 days

k% 101.5 66.1 76.9 84.4

102.1

lizA Pe” cent < 100 I/’ E:i I 54.1 52.8 54.4 54.9 56.1

WM Per molar molar molar molar m&q.

cent ratio ratio mtio ratio Per cent K 100 x 100 ,

84.5

2:oo E

1.92 1.67

ii:; 1.68 :z

:% I:81 1.59 1.76 ii:; 55.0 63.1 1.62 1.54 53.9 74.0

f %

1:81 1174 1.66 1.60 55.0

78.7 1.70 1.63 1.52 55.5 97.8 2.29 2.20 2.14 2.03 59.2

1.43 I I 1.41 1.31 1.28 1.42 I 1.38 1.32 1.28 1.32

~ 1.31 1.22 1.20

1.41 1.38 1.30 1.27 1.31 1.29 1.23 1.21 1.35 1.34 1.26 1.24 1.39 , 1.31 1.31 1.24

Experimental period, 45 days

1 84.6 84.0 I 2.00 ’ 1.99 1.90 1.85 2.03 2.01 1.87 1.86 1.80 1.77 2.00 , 1.98

Reference 1.70 / 1.68