The Testimony of the Rocks: or, Geology in Its Bearings on the Two Theologies, Natural and Revealed
John Stuart Mill · en
The earlier flora of this Tertiary division presents an aspect widely
different from that of any of the previous ones. The ferns and their
allies sink into their existing proportions; nor do the coniferæ,
previously so abundant, occupy any longer a prominent place. On the
other hand, the dicotyledonous herbs and trees, previously so
inconspicuous in creation, are largely developed. Trees of those
Amentiferous orders to which the oak, the hazel, the beech, and the
plane belong, were perhaps not less abundant in the Eocene woods than in
those of the present time: they were mingled with trees of the Laurel,
the Leguminous, and the Anonaceous or custard apple families, with many
others; and deep forests, in the latitude of London (in which the
intertropical forms must now be protected, as in the Crystal Palace,
with coverings of glass, and warmed by artificial heat), abounded in
graceful palms. Mr. Bowerbank found in the London clay of the island of
Sheppey alone the fruits of no fewer than thirteen different species of
this picturesque family, which lends so peculiar a feature to the
landscapes in which it occurs; and ascertained that the undergrowth
beneath was composed, in large proportion, of creeping plants of the
gourd and melon order. From the middle or Miocene flora of the Tertiary
division,--of which we seem to possess in Britain only the small but
interesting fragment detected by his Grace the Duke of Argyll among the
trap-beds of Mull,--most of the more exotic forms seem to have been
excluded. The palms, however, still survive in no fewer than thirty-one
different species, and we find in great abundance, in the place of the
other exotics, remains of the plane and buckthorn families,--part of a
group of plants that in their general aspect, as shown in the Tertiary
deposits of the Continent, not a little resembled the vegetation of the
United States at the present day. The nearer we approach to existing
times, the more familiar in form and outline do the herbs and trees
become. We detect, as has been shown, at least one existing _order_ in
the ferns of the Coal Measures; we detect at least existing _genera_
among the Coniferæ, Equisetaceæ, and Cycadaceæ of the Oolite; the
acacias, gourds, and laurels of the Eocene flora, and the planes,
willows, and buckthorns of the Miocene, though we fail to identify their
species with aught that now lives, still more strongly remind us of the
recent productions of our forests or conservatories; and, on entering,
in our downward course, the Pleistocene period, we at length find
ourselves among familiar _species_. On old terrestrial surfaces, that
date before the times of the glacial period, and underlie the boulder
clay, the remains of forests of oak, birch, hazel, and fir have been
detected,--all of the familiar species indigenous to the country, and
which still flourish in our native woods. And it was held by the late
Professor Edward Forbes, that the most ancient of his five existing