Geology: The Science of the Earth's CrustMiller, William J. (William John)
Philosophy
Geology: The Science of the Earth's Crust
Miller, William J. (William John)
Geology
The early and middle Proterozoic strata throw no more light upon the
early history of animal life than do the Archeozoic strata. The upper
or later Proterozoic rocks, however, contain the oldest recognizable
animal fossils. Very recently fossil remains of single-celled,
shell-bearing Protozoans have been found in northern France, while
the upper Proterozoic strata of the Rocky Mountains in Montana, and
the Grand Canyon of Arizona have yielded worm tracks, a Molluscoid
(brachiopod) and fragments of lower forms of Arthropods. This record,
although very meager, clearly proves that animal life was so well
advanced by late Proterozoic time, that next to the highest subkingdom
was actually represented (see above classification), and that there
must have been a long line of simpler and simpler ancestors, probably
extending far back into the Archeozoic era. When we stop to consider
that Archeozoic and Proterozoic time was fully as long as all
succeeding geological time, it is not so surprising that fairly highly
developed animals (except Vertebrates) had been evolved before the
close of the Proterozoic era.
In regard to abundance of fossil animals the oldest (Cambrian)
Paleozoic strata stand out in marked contrast to the Proterozoic. Many
hundreds of species of animal fossils have been described from Cambrian
strata, and a great many others yet remain to be discovered. Cambrian
fossils are remarkably numerous, varied in species, and complex
in organization (Plate 13). All subkingdoms of animals except the
Vertebrates were represented, though usually only by the simpler types
in each subkingdom. It is quite generally agreed that no less than 50
per cent of animal evolution had taken place before the beginning of
the Cambrian period. The reader should, however, clearly bear in mind
that tremendous advances in evolution have taken place since early
Cambrian time when not only all forms from lower scale Arthropods to
the highest mammals (including man) have evolved, but also when many
thousands of species of lower subkingdom animals developed.
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