The Chain of Life in Geological Time: A Sketch of the Origin and Succession of Animals and PlantsDawson, John William, Sir
Science
The Chain of Life in Geological Time: A Sketch of the Origin and Succession of Animals and Plants
Dawson, John William, Sir
Paleobotany; Paleontology
A very noteworthy and specially American group of mammals is that of the
_Edentates_, the Sloths and Ant-eaters, a group which _à priori_ we
should have supposed would have been one of the earliest in time. They
appear, however, first in the Miocene, without even any suggested
ancestry, and are represented from the first by large species, though
they attain their grandest stature in the _Megatherium_ and _Mylodon_ of
the Post-Pliocene (Figs. 178, 179), which were sloths of so gigantic
size that they must have pulled down trees to feed on their leaves,
unless, indeed, there were trees equally colossal for them to climb. But
before the modern time, like the American horses, the larger herbivorous
forms suddenly disappear, and are now represented only by a few
diminutive South American species, which can scarcely, by any stretch of
imagination, be supposed to be descendants of their gigantic
predecessors. The history of these animals, like those of the great
Tertiary marsupials of Australia and the many Miocene elephants of
India, affords a remarkable illustration of the persistence of similar
groups of creatures in successive ages in the same region, along with
diminution in magnitude and number of species toward the modern times.
[Illustration: FIG. 180.—Tooth of Eocene Whale (_Zeuglodon cetioides_).
One-half natural size.]
The Whale-tribe (Cetaceans) at once in the earliest Eocene takes the
place of the great Sea-lizards of the Cretaceous; and the oldest of the
whales are in their dentition more perfect than any of their successors,
since their teeth are each implanted by two roots, and have serrated
crowns, like those of the Seals. The great Eocene whales of the Southern
Atlantic (_Zeuglodon_) (Fig. 180), which have these characters, attained
the length of seventy feet, and are undoubtedly the first of the whales
in rank as well as in time. This is perhaps one of the most difficult
facts to be explained on the theory of evolution. Allied to the whales
is the small and peculiar group of the Sea-cows or Dugongs
(_Sirenians_). These creatures, highly specialised and very distinct
from all others, appear in the Early Tertiary in forms very similar to
those which now exist, and probably in much more numerous species, and
they pursue the even tenor of their way down to modern times without
perceptible elevation or degradation. “We have questioned,” says Gaudry,
when speaking of the Tertiary Cetaceans, “these strange and gigantic
sovereigns of the Tertiary oceans as to their progenitors—they leave us
without reply.” Their silence is the more significant as one can
scarcely suppose these animals to have been nurtured in any limited or
secluded space in the early stages of their development. The true Seals,
which are more elevated than the Whales, and very different in type,
appear much later, and without any probable ancestry.
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