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
--------------------+---------------------+--------------------------
ANIMALS |SYSTEMS OF FORMATIONS| PLANTS
--------------------+---------------------+--------------------------
| Kainozoic |
| Modern |
Age of Man and | Pleistocene | Angiosperms and
Mammalia | Pliocene | Palms dominant
| Miocene |
| Eocene |
--------------------+---------------------+--------------------------
| Mesozoic |
| Cretaceous | Cycads and Pines
Age of Reptiles | Jurassic | dominant
| Triassic |
--------------------+---------------------+--------------------------
| Palæozoic |
| Permian |
| Carboniferous |
Age of Amphibians | Erian | Acrogens and Gymnosperms
and Fishes | Silurian | dominant
Age of Invertebrates| Ordovician |
| Cambrian |
| Huronian (Upper) |
--------------------+---------------------+--------------------------
| Eozoic |
| Huronian (Lower) |
Age of Protozoa | Upper Laurentian | Protogens and Algæ
| Middle Laurentian |
| Lower Laurentian |
--------------------+---------------------+--------------------------
It will be observed, since only the latest of the systems of
formations in this table belongs to the period of human history, that
the whole lapse of time embraced in the table must be enormous. If
we suppose the modern period to have continued for say ten thousand
years, and each of the others to have been equal to it, we shall
require two hundred thousand years for the whole. There is, however,
reason to believe, from the great thickness of the formations and the
slowness of the deposition of many of them in the older systems, that
they must have required vastly greater time. Taking these criteria
into account, it has been estimated that the time-ratios for the
first three great ages may be as one for the Kainozoic to three for
the Mesozoic and twelve for the Palæozoic, with as much for the
Eozoic as for the Palæozoic. This is Dana’s estimate. Another, by
Hull and Houghton, gives the following ratios: Azoic, 34.3 per cent;
Palæozoic, 42.5 per cent; Mesozoic and Kainozoic, 23.3 per cent. It
is further held that the modern period is much shorter than the other
periods of the Kainozoic, so that our geological table may have to be
measured by millions of years instead of thousands.
Public-domain text, read in full here on John Shaqi.
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