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
The Rodents, or gnawing animals, appear in the Early Eocene on both
continents in familiar forms allied to our Squirrels and Rats.
Porcupines and Beavers are added in the Miocene. This group seems thus
to have continued much as it was; and it is still perhaps represented by
as many species as at any previous time. Many of the ancient forms were,
however, much larger than any modern species, and some of these larger
forms[82] present singular points of approach to very distinct types,
as, for example, to that of the Bears; but these large and composite
species are long since extinct. The insectivorous mammals have much the
same history with the Rodents. Such highly specialised and abnormal
forms as the Bats might be supposed to be modern. But, strange to say,
they appear with fully developed wings both in Europe and America in the
Eocene (Fig. 183). Gaudry thinks that it is “natural to suppose” that
there must have been species existing previously with shorter fingers
and rudimentary wings; but there are no facts to support this
supposition, which is the more questionable since the supposed
rudimentary wings would be useless, and perhaps harmful to their
possessors. Besides, if from the Eocene to the present the Bats have
remained the same, how long would it take to develop an animal with
ordinary feet, like those of a shrew, into a bat?
The Early Eocene was not altogether a time of peace in the animal world.
The old carnivorous Saurians were dead and buried, but their place was
taken by carnivorous mammals, allied to our modern Tigers, Hyænas,
Foxes, and Weasels. The Carnivora, however, were subordinate in the
Eocene, and, as already remarked, some of them appear to be intermediate
between marsupial and placental forms—a fact which evolutionists have
noticed with much satisfaction. They appear to attain to their
culmination in the Miocene, when their powers seem to be proportionate
to those of the great and well-armed quadrupeds they had to deal with.
To this age belongs the introduction of the terrible “Cymetar-toothed
Tiger” (_Machairodus_, Fig. 184). Its huge tusk-like canines and
powerful limbs seem to fit it more than any other of the cat family for
destructive efficiency. Yet ordinary cat-like animals were contemporary
with it, and have survived it, since _Machairodus_ disappears in the
Post-Pliocene, though in previous periods it had been very widely
distributed on both continents. It is a curious fact, perhaps of more
significance in various ways than we yet understand, that the Dog-bear
(_Arctocyon_), of the oldest French Eocene, believed to be the oldest
placental mammal known, though technically placed among the Carnivora,
has a kind of dentition indicating that, like the modern Bears, it was
really omnivorous; and its skull shows some peculiarities tending to
those of the Marsupials.
[Illustration: FIG. 184.—Skull of a Cymetar-toothed Tiger (_Machairodus
cultridens_). Pliocene, France. Reduced.]
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