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Scientific American Supplement, No. 275, April 9, 1881 by Various
page 20 of 159 (12%)

PHOSPHATE OF CALCIUM.--Mr. Payen was the first to make the observation
that the greatest amount of phosphate of chalk is found in the teguments
adjoining the farinaceous or floury mass. This observation is important
from two points of view; in the first place, it shows us that this mineral
aliment, necessary to the life of animals, is rejected from ordinary bread;
and in the next place, it brings a new proof that phosphate of chalk is
found, and ought to be found, in everyplace where there are membranes
susceptible of exercising vital functions among animals as well as
vegetables.

Phosphate of chalk is not in reality (as I wished to prove in another work)
a plastic matter suitable for forming bones, for the bones of infants are
three times more solid than those of old men, which contain three times
as much of it. The quantity of phosphate of chalk necessary to the
constitution of animals is in proportion to the temperature of those
animals, and often in the inverse ratio of the weight of their bones, for
vegetables, although they have no bones, require phosphate of chalk. This
is because this salt is the natural stimulant of living membranes, and the
bony tissue is only a depot of phosphate of chalk, analogous to the adipose
tissue, the fat of which is absorbed when the alimentation coming from the
exterior becomes insufficient. Now, as we know all the parts constituting
the berry of wheat, it will be easy to explain the phenomena of
panification, and to conclude from the present moment that it is not
indifferent to reject from the bread this embryous membrane where the
agents of digestion are found, viz., the phosphoric bodies and the
phosphate of chalk.

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