Catholic Churchmen in Science [First Series]: Sketches of the Lives of Catholic Ecclesiastics Who Were Among the Great Founders in ScienceWalsh, James J. (James Joseph)
Religion
Catholic Churchmen in Science [First Series]: Sketches of the Lives of Catholic Ecclesiastics Who Were Among the Great Founders in Science
Walsh, James J. (James Joseph)
Catholics; Religion and science; Scientists -- Biography
In the course of his observations in Italy, Stensen had seen many
mussel shells, which had been gathered from various layers of the
earth's surface. With regard to the shells themselves, he said that
there could be no doubt that they had come as the excretion of the
mantle of the mussel, and that the differences that could be noted in
them were in accordance with the varying forms of these animals. He
pointed out, however, that some of the mussel shells found in {158}
strata of rock were really mussel shells in every respect as regards
the material of which they were composed as well as their interior
structure and their external form, so that there could be no possible
question of their origin. On the other hand, a certain number of the
so-called mussel shells were not composed of the ordinary materials of
which such shells are usually made up; but had indeed only the
external form of genuine shells. Stensen considered, however, that
even these must be regarded as originating in real mussel shells, the
original substance having been later on replaced by other material. He
explained this replacement process in very much the same way that we
now suggest the explanation of various processes of petrification.
There is no doubt that in this he went far beyond his contemporaries,
and pointed out very clearly what was to be the teaching of
generations long after his own.
The same principles he applied to mussel shells, Stensen considered
must have their application also to all other portions of animal
bodies, teeth, bones, whole skeletons, and even more perishable animal
materials that might be found buried in the earth's strata. His
treatment of the question of the remains of plants was quite as
satisfactory as that of the animals. He distinguished between the
impressions of plants, the petrification of plants, the carbonization
of plants, and then dwelt somewhat on the tendency of certain minerals
to form dendrites, that is, branching {159} processes which look not
unlike plants. He pointed out how easy it is to be deceived by these
appearances, and stated very clearly the distinction between real
plants and such simulated ones.
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