The modes of origin of lowest organisms: including a discussion of the experiments of M. PasteurBastian, H. Charlton
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The modes of origin of lowest organisms: including a discussion of the experiments of M. Pasteur
Bastian, H. Charlton
Life -- Origin; Spontaneous generation
Other evidence which is so much vaunted by M. Pasteur and his
supporters, as to the possibility of inducing fertility in previously
sterile flasks, by the addition of a portion of asbestos containing
the solid particles filtered from the atmosphere,[80] is also equally
valueless for confirming the proposition that fermentation is only
capable of being initiated by living ferments. The same asbestos which
_may_ contain living spores or organisms (“germs”), does undoubtedly
contain many decomposable particles and fragments of organic
matter.[81] The previously barren solution may therefore be rendered
fertile by the mere addition of those portions of unstable organic
matter, whose molecular mobility has not been impaired by the agency
of heat, and which are therefore capable of initiating fermentations.
This view is strengthened, as M. Pouchet has pointed out, by the fact
that in these cases, instead of meeting some of the _various_ kinds
of organisms which are supposed to have representatives in the air,
and whose spores or ova may be supposed to have been sown, it is often
merely _Bacteria_ which are encountered,--differing in no respect from
those that may present themselves in a somewhat similar infusion, which
has undergone change in a closed flask without any such hypothetical
sowing of living spores or germs. It is more especially important to
bear in mind this consideration, when portions of organic matter can
always be easily demonstrated amongst such atmospheric dust; whilst
living _Bacteria_, or other organisms, such as are first produced as a
result of the supposed sowing of spores, either cannot be demonstrated,
or would seem, from other evidence, to be at least very sparingly
distributed.[82]
[80] Loc. cit., p. 40.
[81] Speaking of experiments in closed flasks, in which the air has
been either calcined or filtered, Gerhardt (‘Chimie Organique,’ t.
IV. p. 545) says:--“Si dans les premières expériences l’air calciné
ou tamisé s’est montré beaucoup moins actif que l’air non soumis à ce
traitement, c’est que la chaleur rouge ou le tamisage enlève à l’air
non seulement les germes des infusoires et des moisissures, mais
encore les débris des matières en décomposition qui y sont suspendues,
c’est-à-dire les ferments dont l’activité viendrait s’ajouter à celle
de l’oxygène de l’air.”
[82] On what other supposition can one explain the results of
experiments LVII.-LXV., and of others alluded to on p. 100?
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