The History of Creation, Vol. 2 (of 2): Or the Development of the Earth and its Inhabitants by the Action of Natural CausesHaeckel, Ernst
Science
The History of Creation, Vol. 2 (of 2): Or the Development of the Earth and its Inhabitants by the Action of Natural Causes
Haeckel, Ernst
Evolution; Heredity; Human beings -- Origin
The whole population of the tertiary epoch approaches much nearer, on
the whole as well as in detail, to that of the present time than is the
case in the preceding epochs. From this time the class of _Mammals_
greatly predominates over all other vertebrate animals. In like manner,
in the vegetable kingdom, the group—so rich in forms—of the
_Angiosperms_, or _plants with covered seeds_, predominates, and its
_leafy forests_ constitute the characteristic feature of the tertiary
epoch. The group of the Angiosperms consists of the two classes of
single-seed-lobed plants, or _Monocotyledons_, and the double-seed-lobed
plants, or _Dicotyledons_. The Angiosperms of both classes had, it is
true, made their appearance in the Cretaceous period, and mammals had
already occurred in the Jurassic period, and even in the Triassic
period; but both groups, the mammals and the plants with enclosed seeds,
did not attain their peculiar development and supremacy until the
tertiary epoch, so that it may justly be called after them.
The fifth and last main division of the organic history of the earth is
the _quaternary epoch, or era of Civilization_, which in comparison with
the length of the four other epochs almost vanishes into nothing, though
with a comical conceit we usually call its record the “history of the
world.” As the period is characterized by the development of _Man_ and
his _Culture_, which has influenced the organic world more powerfully
and with greater transforming effect than have all previous conditions,
it may also be called the era of Man, the anthropolithic or anthropozoic
period. It might also be called the era of Cultivated Forests, or
Gardens, because even at the lowest stage of human civilization man’s
influence is already perceptible in the utilization of forests and their
products, and therefore also in the physiognomy of the landscape. The
commencement of this era, which extends down to the present time, is
geologically bounded by the end of the pliocene stratification.
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