A Short History of the WorldWells, H. G. (Herbert George)
History
A Short History of the World
Wells, H. G. (Herbert George)
World history
But it is during periods of change that life undergoes its most rapid
modifications, and under hardship that it learns its hardest lessons.
As conditions revert towards warmth and moisture again we find a new
series of animal and plant forms established, We find in the record
the remains of vertebrated animals that laid eggs which, instead of
hatching out tadpoles which needed to live for a time in water, carried
on their development before hatching to a stage so nearly like the
adult form that the young could live in air from the first moment of
independent existence. Gills had been cut out altogether, and the gill
slits only appeared as an embryonic phase.
These new creatures without a tadpole stage were the Reptiles.
Concurrently there had been a development of seed-bearing trees, which
could spread their seed, independently of swamp or lakes. There were
now palmlike cycads and many tropical conifers, though as yet there
were no flowering plants and no grasses. There was a great number of
ferns. And there was now also an increased variety of insects. There
were beetles, though bees and butterflies had yet to come. But all the
fundamental forms of a new real land fauna and flora had been laid down
during these vast ages of severity. This new land life needed only the
opportunity of favourable conditions to flourish and prevail.
A FOSSIL ICHTHYOSAURUS, A MESOZOIC FISH-LIZARD
A FOSSIL ICHTHYOSAURUS, A MESOZOIC FISH-LIZARD
Found in the Lower Lias in Somersetshire
_Nat. Hist. Mus._
Age by age and with abundant fluctuations that mitigation came. The
still incalculable movements of the earth’s crust, the changes in its
orbit, the increase and diminution of the mutual inclination of orbit
and pole, worked together to produce a great spell of widely diffused
warm conditions. The period lasted altogether, it is now supposed,
upwards of two hundred million years. It is called the Mesozoic
period, to distinguish it from the altogether vaster Palæozoic and
Azoic periods (together fourteen hundred millions) that preceded it,
and from the Cainozoic or new life period that intervened between its
close and the present time, and it is also called the Age of Reptiles
because of the astonishing predominance and variety of this form of
life. It came to an end some eighty million years ago.
Public-domain text, read in full here on John Shaqi.
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