The Geological History of PlantsDawson, John William, Sir
Science
The Geological History of Plants
Dawson, John William, Sir
Paleobotany
In the "Bulletin of the Chicago Academy of Science," January, 1884, Dr.
Johnson and Mr. Thomas, in their paper on the "Microscopic Organisms
of the Boulder Clay of Chicago and Vicinity," notice _Sporangites
Huronensis_ as among these organisms, and have discovered them also in
large numbers in the precipitate from Chicago city water-supply. They
refer them to the decomposition of the Erian shales, of which boulders
filled with these organisms are of frequent occurrence in the Chicago
clays. The Sporangites and their accompaniments in the boulder clay are
noticed in a paper by Dr. G. M. Dawson, in the "Bulletin of the Chicago
Academy," June, 1885.
Prof. Clarke has also described, in the "American Journal of Science"
for April, 1885, the forms already alluded to, and which he finds to
consist of macrospores enclosed in sporocarps. He compares these with my
_Sporangites Huronensis_ and _Protosalvinia bilobata_, but I think it is
likely that one of them at least is a distinct species.
I may add that in the "Geological Magazine" for 1875, Mr. Newton, F.
G. S., of the Geological Survey of England, published a description
of the Tasmanite and Australian white coal, in which he shows that the
organisms in these deposits are similar to my _Sporangites Huronensis_,
and to the macrospores previously described by Prof. Huxley, from the
Better-bed coal. Mr. Newton does not seem to have been aware of my
previous description of _Sporangites_, and proposes the name _Tasmanites
punctatus_ for the Australian form.
Here we have the remarkable fact that the waste macrospores, or larger
spores of a species of Cryptogamous plant, occur dispersed in countless
millions of tons through the shales of the Erian in Canada and the United
States.
No certain clue seemed to be afforded by all these observations as to
the precise affinities of these widely distributed bodies; but this was
furnished shortly after from an unexpected quarter. In March, 1883, Mr.
Orville Derby, of the Geological Survey of Brazil, sent me specimens
found in the Erian of that country, which seemed to throw a new light on
the whole subject. These I described and pointed out their connection
with _Sporangites_ at the meeting of the American Association at
Minneapolis, in 1883, and subsequently published my notes respecting them
in its proceedings, and in the "Canadian Record of Science."
Public-domain text, read in full here on John Shaqi.
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