Life Past & Present
The earth teems with
life. Mountains, prairies, deserts, beaches, lakes,
rivers and sees—every part of lend, sea end air is
inhabited by living things. The number of different
species of living things is enormous. More then
350,000 species of plants end 1,120,000 species of
animals are known.
How did these many
species originate? Has life always been the same es
it is now? Men have asked these questions for
thousands of years. To answer them we must turn to
fossils and to a knowledge of living organisms end
their structure. Only an understanding of living
animals can put life in the fragments of bones and
shells millions of years old.
The elephant is the
largest living land animal in the world today. But
the study of fossils shows not only that elephants
area recent group in the long history of living
things but also that early elephants looked more
like hogs. As geologists trace elephant fossils from
older to younger rocks they piece together the
history of elephant evolution. Fossil bones and
teeth reveal the structure of early elephants, but
by studying these fossils in the light of the
anatomy of living elephants, complete
reconstructions of extinct elephants can be made
with reasonable accuracy. Some unusual occurrences
ot mastodon fossils with crude flint weapons prove
that these elephants were hunted by our ancestors.

All forms of life have
evolved from early beginnings, some three billion
years ago. From relatively few primitive forms, the
major groups of plants and animals developed. Living
things became more complicated and adapted to many
different ways of living. The number of different
species gradually increased until they reached the
tremendous diversity of today. The study of fossils
(paleontology) traces the various paths by which
animals and plants evolved to their present forms.
Some, like elephants and horses, have changed
greatly through the ages. Others, like the horseshoe
crab and cockroach, have not changed in hundreds of
millions of years. Still other fossils show lines of
development that came to a dead end. Giant Sloths,
once plentiful, are known only as fossils.
The
Glyptodont, a 9foot armored mammal from the late
Cenozoic, is a fossil that shows spectacular and
obvious adaptation. This relation of modern day
armadillos was protected against carnivores and
other enemies by a thick, solid, domed armor, which
reached almost 5 feet in length in some forms. The
head and tail were also armored, and in some
species, the tail terminated in a spiked, mace-like
club. Yet despite, or because of, these unusual
adaptions glyptodonts became extinct.
Most plants and
animals exist only because they are successfully
adapted to their environments. Each distinct
environment such as a desert, pond or mountain top
supports a more or less distinct population of
animals and plants. Those which, over long periods
of time, have become fitted to cope with local
conditions have survived. All the rest have become
extinct. Many living things are uniquely adapted to
particular environments. The streamlined shape of a
fish and the structure and function of its fins and
tail are adaptations to life in the water. The
fleshy stems of a cactus are adaptations that
conserve water in the desert. Such adaptations
succeeded, but the fossil record is strewn with the
remains of those that failed. The slogan of life may
well be—adapt or perish.
Survival
in animals depends on adaptations as varied and as
intricate as the animals themselves. Virtually every
structure at a plant or animal may be regarded as
adaptive. Many animals have protective coloring and
a few forms, such as the bottom-living flounder are
able to change their color to conform to their
background. Such an intricate adaptation in rarely
discernible in fossils. However, if the adaptation
affects bone or shell, it may show op clearly in the
fossil record.
Development of modern
animal life is difficult to trace because the fossil
record is incomplete. Enough is known to suggest the
general pattern of evolution and to reconstruct in
some detail history of groups in those areas where
fossils occur abundantly. The chart below shows some
of the relationships among major groups of
vertebrates:
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