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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

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

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

kinds of birds, 1860 1861 1866 1869
different bird-like animals, 1872

beds. Notwithstanding that the number of joints shown in the fossil impressions correspond with the number in the several toes of living birds feet, some authors doubt whether the animals which left the impressions were really birds. 1860
beds. 1861 1866 1869 1872

an early tertiary 1860 1861
the eocene 1866 1869

(as may be seen in Lyells Manual), 1860
OMIT 1861 1866 1869

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,
for its thickness, 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. Had it not been for the rare accident of the preservation of footsteps in the new red sandstone of the United States, who would have ventured to suppose
that
that,
besides reptiles,
besides reptiles,
no less than at least thirty kinds of birds, some of gigantic size, existed during that period? Not a fragment of bone has been discovered in these beds. Notwithstanding that the number of joints shown in the fossil impressions correspond with the number in the several toes of living birds feet, some authors doubt whether the animals which left the impressions were really birds. Until quite recently these authors might have maintained, and some have maintained, that the whole class of birds came suddenly into existence during an early tertiary period; but now we know, on the authority of Professor
Owen,
Owen
(as may be seen in Lyells Manual), that a bird certainly lived during the deposition of the upper
green-sand.
greensand;
greensand.
I may give another instance,
which,
which
from having passed under my own
eyes,
eyes
has much struck me. In a memoir on Fossil Sessile Cirripedes, I
have
have
stated that, from the