The Geological History of PlantsDawson, John William, Sir
Science
The Geological History of Plants
Dawson, John William, Sir
Paleobotany
"But when we have reached the branch representing the generic form we
have made but little progress in the phylogenesis of _Salix_. With
_Populus_ this genus forms a small order, Salicineæ, The two genera are
closely allied, yet separated by well-marked characters; it is not,
however, difficult to conceive of both having sprung from a generalised
form. But there is no record of such a form. The two genera appear
together among the earliest known dicotyledons, the willows being
represented by six and the poplars by nine species. The ordinal form, if
it ever existed, must necessarily be much older than the period of the
Upper Cretaceous rocks, that is, than the period to which the earliest
known dicotyledons belong.
"The Salicineæ are related to five other natural orders, in all of which
the apetalous flowers are arranged in catkins. These different though
allied orders must be led up by small modifications to a generalised
amentiferous type, and thereafter the various groups of apetalous
plants by innumerable eliminations of differentiating characters until
the primitive form of the apetalous plant is reached. Beyond this the
uncurbed imagination will have more active work in bridging over the gap
between Angiosperms and Gymnosperms, in finding the intermediate forms
that led up to the vascular cryptogams, and on through the cellular
plants to the primordial germ. Every step in this phylogenetic tree
must be imagined. The earliest dicotyledon takes us not a step farther
back in the phylogenetic history of _Salix_ than that supplied by
existing vegetation. All beyond the testimony of our living willows is
pure imagination, unsupported by a single fact. So that here, also, the
evidence is against evolution, and there is none in favour of it."
It is easy to see that similar difficulties beset every attempt to trace
the development of plants on the principle of slow and gradual evolution,
and we are driven back on the theory of periods of rapid origin, as we
have already seen suggested by Saporta in the case of the Cretaceous
dicotyledons. Such abrupt and plentiful introduction of species over
large areas at the same time, by whatever cause effected--and we are
at present quite ignorant of any secondary causes--becomes in effect
something not unlike the old and familiar idea of creation. Science
must indeed always be baffled by questions of ultimate origin, and,
however far it may be able to trace the chain of secondary causation
and development, must at length find itself in the presence of the
great Creative Mind, who is "before all things and in whom all things
consist."
APPENDIX.
I.--COMPARATIVE VIEW OF THE SUCCESSIVE PALÆOZOIC
FLORAS OF NORTHEASTERN AMERICA AND
GREAT BRITAIN.
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