Scientific American Supplement, No. 458, October 11, 1884Various
Science
Scientific American Supplement, No. 458, October 11, 1884
Various
Science -- Periodicals
Several observations made recently in Rome tend to demonstrate that the
schizomycete of malaria does not always assume the complete bacillary form
described by Klebs and myself; but this morphological question possesses
no further interest for the hygienist. For him the essential thing is to
know that he has to deal with a living ferment which can flourish in soils
of very varied composition, and without the presence of which neither
marshes nor stagnant pools of water are capable of producing malaria.
We must not think, however, that all earth containing this ferment is
capable of poisoning the superjacent atmosphere. Popular experience,
certain modern scientific investigation, and the facts which one can often
verify when the soil, which was malarious in ancient times and which has
since ceased to be so, is turned up to a great depth, all agree in proving
that the ground remains inoffensive as long as it is not placed in certain
conditions indispensable for the multiplication of this specific ferment.
Up to this point the organism lives, so to speak, in an inert state, and
may remain so during centuries without losing any of its deleterious
power. There is nothing in this fact that ought to surprise us, since we
know that the life and the power of evolution belonging to the seeds of
plants of a much higher order than these vegetable organisms constituting
ferments, may remain latent for centuries, and may then revive at once
when these grains are placed in the conditions suitable for their
germination.
Among the conditions favorable to the multiplication of the malarial
ferment contained in the soil, and to its dispersion through the
superjacent atmosphere, there are three which are absolutely essential,
and the concurrence of which is indispensable for the production of bad
air (malaria). First, a temperature which does not fall below 20°C.
(67.5°F.); next, a very moderate degree of permanent humidity of the soil;
and finally, the direct action of the oxygen of the air upon the strata of
earth which contain the ferment. If a single one of these three conditions
be wanting, the development of malaria becomes impossible. This is a point
of prime importance in the natural history of malaria, and it gives us the
key to most of the methods of sanitary improvement attempted by man.
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