The story of the universe. Volume 2 (of 4) : $b The earth : land and sea
History
The story of the universe. Volume 2 (of 4) : $b The earth : land and sea
Astronomy; Earth (Planet); Natural history
2. _Angiosperms_, which produce true fruits inclosing the seeds. In
this group there are two well-marked subdivisions differing in the
structure of the seed and stem. They are the _Endogens_, or inside
growers, with seeds having one seed-leaf only, as the grasses and
the palms; and the _Exogens_, having outside-growing woody stems and
seeds with two seed-leaves. Most of the ordinary forest trees of
temperate climates belong to this group.
On referring to the geological table, it will be seen that there is
a certain rough correspondence between the order of rank of plants
and the order of their appearance in time. The oldest plants that we
certainly know are Algæ, and with these there are plants apparently
with the structures of Thallophytes but the habit of trees, and
which, for want of a better name, I may call _Protogens_. Plants
akin to the Rhizocarps also appear very early. Next in order we
find forests in which gigantic Ferns and Lycopods and Mare’s-tails
predominate, and are associated with pines. Succeeding these we have
a reign of Gymnosperms, and in the later formations we find the
higher Phænogams dominant.
THE SILURIAN BEACH
--LOUIS AGASSIZ
The crust of our earth is a great cemetery where the rocks are
tombstones on which the buried dead have written their own epitaphs.
They tell us not only who they were and when and where they have
lived, but much also of the circumstances under which they lived.
We ascertain the prevalence of certain physical conditions at
special epochs by the presence of animals and plants whose existence
and maintenance requires such a state of things, more than by any
positive knowledge respecting it. Where we find the remains of
quadrupeds corresponding to our ruminating animals, we infer not
only land, but grassy meadows and an extensive vegetation; where we
find none but marine animals, we know the ocean must have covered
the earth; the remains of large reptiles, representing, though in
gigantic size, the half aquatic, half terrestrial reptiles of our
own period, indicate to us the existence of spreading marshes still
soaked by retreating waters; while the traces of such animals as live
now in sand and shoal waters, or in mud, speak to us of shelving
sandy beaches and mud flats. The eye of the Trilobite tells us that
the sun shone on the old beach where he lived; for there is nothing
in nature without a purpose, and when so complicated an organ was
made to receive the light there must have been light to enter it.
The immense vegetable deposits in the Carboniferous period announce
the introduction of an extensive terrestrial vegetation; and the
impressions left by the wood and leaves show that these first forests
must have grown in a damp soil and a moist atmosphere. In short, all
the remains of animals and plants hidden in the rocks have something
to tell of the climatic conditions and the general circumstances
under which they lived, and the study of fossils is to a naturalist
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