The Geological History of PlantsDawson, John William, Sir
Science
The Geological History of Plants
Dawson, John William, Sir
Paleobotany
Found in the same formations with the last species, though, in so far as
the specimens indicate, not precisely in the same beds. Collected by Mr.
Derby.
4. _Protosalvinia Clarkei_, Dawson, _P. bilobata_, Clarke, "American
Journal of Science."--Macrospores two-thirds to one millimetre in
diameter. One, two, or three contained in each sporocarp, which is
cellular. The macrospores have very thick walls with radiating tortuous
tubes. Unless this structure is a result of mineral crystallisation,
these macrospores must have had very thick walls and must have resembled
in structure the thickened cells of stone fruits and of the core of the
pear, or the tests of the Silurian and Erian seeds known as _Pachytheca_,
though on a smaller scale.
It is to be observed that bodies similar to these occur in the Boghead
earthy bitumen, and have been described by Credner.
I have found similar bodies in the so-called "Stellar coal" of the coal
district of Pictou, Nova Scotia, some layers of which are filled with
them. They occur in groups or patches, which seem to be enclosed in a
smooth and thin membrane or sporocarp. It is quite likely that these
bodies are generically distinct from _Protosalvinia_.
5. _Protosalvinia punctata_, Newton, "Geological Magazine," New Series,
December 2d, vol. ii.--Mr. Newton has named the discs found in the
white coal and Tasmanite, _Tasmanites_, the species being _Tasmanites
punctatus_, but as my name _Sporangites_ had priority, I do not think it
necessary to adopt this term, though there can be little doubt that these
organisms are of similar character. The same remark may be made with
reference to the bodies described by Huxley and Newton as occurring in
the Better-bed coal.
In Witham's "Internal Structure of Fossil Vegetables," 1833, Plate XI,
are figures of Lancashire cannel which shows _Sporangites_ of the type of
those in the Erian shales. Quekett, in his "Report on the Torbane Hill
Mineral," 1854, has very well figured similar structures from the Methel
coal and the Lesmahagow cannel coal. These are the earliest publications
on the subject known to me; and Quekett, though not understanding the
nature of the bodies he observed, holds that they are a usual ingredient
in cannel coals.
II.--The Nature and Affinities of Ptilophyton.
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