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or some few 1859 1860 1861 1866 1869
OMIT 1872

species 1859 1860
groups of species 1861 1866 1869
groups or species 1872

but 1859 1860
and consequently that the transitional forms would often long remain confined to some one region; but 1861 1866 1869 1872

had 1859 1860
adaptation had once 1861 1866 1869 1872

be able to 1859 1860 1861 1866
OMIT 1869 1872

4 blocks not present in 1859 1860; present in 1861 1866 1869 1872
Professor Pictet, in his excellent Review of this work, in commenting on early transitional forms, and taking birds as an illustration, cannot see how the successive modifications of the anterior limbs of a supposed prototype could possibly have been of any advantage. But look at the penguins of the Southern Ocean; have not these birds their front limbs in this precise intermediate state of "neither true arms nor true wings"? Yet these birds hold their place victoriously in the battle for life; for they exist in infinite numbers and of many kinds. I do not sup- pose that we here see the real transitional grade through which the wings of birds have passed; but what special difficulty is there in believing that it might profit the modified descendants of the penguin, first to become enabled to flap along the surface of the sea like the logger-headed duck, and ultimately to rise from its surface and glide through the air?

1 blocks not present in 1859 1860; present in 1861 1866 1869 1872
Even in so short an interval as that between the first and second editions of Pictet's great work on Palæontology, published in 1844-46 and in 1853-57, the conclusions on the first appearance and disappearance of several groups of animals have been considerably modified; and a third edition would require still further changes.

the great class of mammals was 1859 1860
the whole class of mammals was 1861 1866
mammals were 1869 1872

belongs 1859 1872
for its thickness, belongs 1860 1861 1866 1869

series. 1859 1860 1861 1869 1872
series. Cuvier used to urge that no monkey occurred in any tertiary stratum; but now extinct species have been discovered in India, South America, and in Europe, as far back as the miocene stage. 1866

probably
probably
elapsed between our consecutive formations,— longer perhaps in
most
many
some
cases than the time required for the accumulation of each formation. These intervals will have given time for the multiplication of species from some one or some few
parent-form:
parent-forms;
and in the succeeding
formation,
formation
such species will appear as if suddenly created.
I may here recall a remark formerly made,
namely,
namely
that it might require a long succession of ages to adapt an organism to some new and peculiar line of life, for
instance,
instance
to fly through the air; but
that,
that
when this had been effected, and a few species had thus acquired a great advantage over other organisms, a comparatively short time would be necessary to produce many divergent forms, which would be able to spread rapidly and widely throughout the world.
I will now give a few examples to illustrate
the foregoing
these
remarks,
remarks;
and to show how liable we are to error in supposing that whole groups of species have suddenly been produced. I may recall the well-known fact that in geological treatises, published not many years ago, the great class of mammals was always spoken of as having abruptly come in at the commencement of the tertiary series. And now one of the richest known accumulations of fossil
mammals,
mammals
belongs to the middle of the secondary series; and
one
one
true
mammals
mammal
have
has
been discovered in the new red sandstone at nearly the commencement of this great series. Cuvier used to urge that no monkey occurred in any tertiary stratum; but now extinct species have been discovered in India, South America, and in
Europe,
Europe
even
even
as far back as the
miocene
eocene
stage. The most striking case, however, is that of the Whale family; as these animals have huge bones, are marine, and range over the world, the fact of not a single bone of a whale having been discovered in