Page 125 - Ethel D. Hume - Bešam ili Paster: Izgubljeno poglavlje u istoriji biologije
P. 125

BfiCHAMP OR PASTEUR?
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       first built up, but from which they are afterwards freed
       by that disruption we call death. The two Professors of
       Montpellier, working together, began to trace and follow
       life in its marvellous processes.
          At the risk of being wearisome by repetition, we must
        remind ourselves of the order in which Bechamp achieved
       his early discoveries.  First, he demonstrated that the
        atmosphere  is  filled  with  minute  living  organisms,
        capable of causing fermentation in any suitable medium
        which they chance to light upon, and that the chemical
        change in the medium is effected by a ferment engendered
        by them, which ferment may well be compared to the
        gastric juice of the stomach. Secondly, he found in ordin-
        ary chalk, and afterwards in limestone, minute organisms
        capable of producing fermentative changes, and showed
        these to bear relation to the infinitesimal granulations he
        had observed in the cells and tissues of plants and animals.
        He proved these granulations, which he named micro-
        zymas, to have independent individuality and  life, and
        claimed that they are the antecedents of cells, the up-
        builders ofbodily forms, the real anatomical, incorruptible
        elements.  Thirdly, he set forth that the organisms in the
        air, the so-called atmospheric germs, are simply either
        microzymas, or their evolutionary forms set free by dis-
        ruption from their former vegetable or animal habitat,
        and that the "little bodies" in the limestone and chalk are
        the survivors of the living forms of past ages. Fourthly, he
        claimed that, at this present time, microzymas constantly
        develop into the low type of living organisms that go by
        the name of bacteria.
          We have already superficially studied the rigid experi-
        ments that established Bechamp's views on the fermenta-
        tive role of air-borne organisms and of those found in
        chalk; let us now follow a very few of the innumerable
        experiments he carried out in the establishment of his
        other conclusions. His work was so incessant, his observa-
        tions so prolific, that only their fringe can be touched and
        no attempt can be made to trace the exact chronological
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