Geology: The Science of the Earth's Crust — John Stuart Mill — John Shaqi
Geology: The Science of the Earth's Crust
John Stuart Mill · en
When did animal life begin on the earth, and what were the first forms
like? We can only partially answer the first question by saying that
animals have existed for tens of millions of years, certainly as early
at least as Proterozoic time. Up to the present time we are utterly
in the dark as to what the earliest animal forms looked like, but we
have positive knowledge that the oldest forms found as fossils in the
rocks represent creatures which were far more primitive and lower in
organization than many animals of to-day, and that since those oldest
known forms lived, the animal kingdom has undergone various profound
alterations. In view of the above statements, and also the fact that
the oldest known plant forms were extremely simple or single-celled,
it is more than likely that the first animal life of the earth was
single-celled. In harmony with this view is the fact that fossil
single-celled animals are found in the very oldest (Proterozoic) rocks
which contain any definitely determinable fossil animals.
Do the most ancient known rocks show that animal life existed during
Archeozoic time? In the preceding chapter we pointed out the fact that
the carbon (in the form of graphite), so commonly present in those most
ancient known strata, proves the existence of life of some kind during
Archeozoic time. But because nothing like definitely determinable
fossil forms have thus far been discovered in those rocks, we cannot be
sure whether the carbon represents plant or animal life or both, though
certainly plants of very low order at least must have existed. Because
of the intense alteration (metamorphism) of those very old strata,
all definite forms have long since been obliterated as such. We may,
however, in the light of the vast evolution which took place through
succeeding geological time, be very sure that any animals which may
have existed during Archeozoic time were in general much simpler forms
than those of even early Paleozoic time.