Louis Pasteur: His Life and LaboursVallery-Radot, René
Science
Louis Pasteur: His Life and Labours
Vallery-Radot, René
Pasteur, Louis, 1822-1895; Scientists -- France -- Biography
Before replying to this argument, which Liebig and M. Bouillaud
believed to be irrefutable, Pasteur, wishing to mark all the phases
of the phenomena, expounded in a short preamble the part played by
atmospheric oxygen in the destruction of animal and vegetable matters
after death. It is easy to understand, indeed, that fermentation and
putrefaction only represent the first phase of the return to the
atmosphere and to the soil of all that has lived. Fermentations and
putrefactions give rise to substances which are still very complex,
although they represent the products of decomposition of fermentable
matters. When sugar ferments, a large proportion of it becomes gas;
but alongside of the carbonic acid gas which is formed, and which
is, indeed, a partial return of the sugar to the atmosphere, new
substances, such as alcohol, succinic acid, glycerine, and materials
of yeast, are produced. When the flesh of animals putrifies, certain
products of decomposition, also very complex, are formed with the
vapour of water and the other gases of putrefaction. Where, then, does
nature find the agents of destruction of these secondary products?
The great fact of the destruction of animal and vegetable matters
is accomplished by slow combustion, through the appropriation of
atmospheric oxygen. Here, again, one must banish from science the
preconceived views which assumed that the oxygen seized directly on the
organic matter after death, and that this matter was consumed by purely
chemical processes. It is life that presides over this work of death.
If fermentation and putrefaction are principally the work of
microscopic anaérobies, living without free oxygen, the slow combustion
is found very largely, if not exclusively, to depend upon a class of
infinitely small aérobies. It is these last which have the property
of consuming the oxygen of the air. It is these lower organisms which
are the powerful agents in the return to the atmosphere of all which
has lived. Mildew, mould, bacteria, which we have already noticed,
monads, two thousand of which would go to make up a millimeter,
all these microscopic organisms are charged with the great work of
re-establishing the equilibrium of life by giving back to it all that
it has formed.
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