The Geological History of PlantsDawson, John William, Sir
Science
The Geological History of Plants
Dawson, John William, Sir
Paleobotany
[DM] Great allowance has to be made for the variability of leaves of the
same species. The modern hazel (_C. rostrata_) is a case in point. Its
leaves, from different parts of the same plant, are so dissimilar in form
and size that they might readily be regarded as of different species.
In the matter of names of fossil leaves, I sympathise very strongly
with Dr. Nathorst, of Stockholm, in his objection to the use of modern
generic names for mere leaves, and would be quite content to adopt some
non-committal termination, as that of "_phyllum_" or "_ites_" suggested
by him. I feel, however, that almost as much is taken for granted if a
plant is called Corylophyllum or _Corylites_, as if called _Corylus_. In
either case a judgment is expressed as to its affinities, which if wrong
under the one term is wrong under the other; and after so much has been
done by so many eminent botanists, it seems inexpedient to change the
whole nomenclature for so small and questionable an advantage. I wish
it, however, to be distinctly understood that plants catalogued on the
evidence of leaves alone are for the most part referred to certain genera
on grounds necessarily imperfect, and their names are therefore subject
to correction, as new facts may be obtained.
The more noteworthy modern genera included in the Dakota flora, as
catalogued by Lesquereux, are the following: _Liquidambar_, the
sweet-gum, is represented both in America and Europe, the leaves
resembling those of the modern species, but with entire edges, which
seems to be a common peculiarity of Cretaceous foliage.[DN] _Populus_
(poplar), as already stated, appears very early in Greenland, and
continues with increasing number of species throughout the Cretaceous and
Tertiary. _Salix_ (willow) appears only a little later and continues. Of
the family _Cupuliferæ_ we have _Fagus_ (beech), _Quercus_ (oak), and
_Castanea_ (chestnut), which appear together in the Dakota group and
its equivalents. Fruits of some of the species are known, and also wood
showing structure. _Betula_ (birch) is represented by a few species,
and specimens of its peculiar bark are also common. _Alnus_ (alder)
appears in one species at least. The genus Plat anus (Fig. 71), that of
the plane-trees, represented at present by one European and one American
species, has several species in the Cretaceous, though the plane-trees
seem to culminate in the early part of the succeeding Eocene, where
there are several species with immense leaves. The large leaves,
known as _Credneria_, found in the Cenomanian of Europe, and those
called _Protophyllum_ (Fig. 72) in America, appear to be nearer to the
plane-trees than to any others, though representing an extinct type. The
laurels are represented in this age, and the American genus Sassafras,
which has now only one species, has not one merely but several species in
the Cretaceous. _Diospyros_, the persimmon-tree, was also a Cretaceous
genus.
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