See page in:
1859
1860
1861
1866
1869
1872

Compare with:
1859
1860
1861
1866
1872

F 14 , 1861 1866 1869 1872
F 14 , 1859
F 14 1860

(F 14 ) 1866 1869 1872
(F 14 ) 1859
(F 14 1860
( F 14 ) 1861

several million generations; it may also represent 1869
hundred million generations, and likewise 1859 1860 1861 1866
more generations; it may also represent 1872

Thus it is, as I believe, that two or more genera are produced by
descent,
descent
with modification, from two or more species of the same genus. And the two or more parent-species are supposed to
be
have
descended from some one species of an earlier genus. In our diagram, this is indicated by the broken lines, beneath the capital letters, converging in sub-branches downwards towards a single point; this point
represents
representing
a
single
single
species, the supposed
single parent
progenitor
of our several
new
new
sub-genera and genera.
It is worth while to reflect for a moment on the character of the new species F 14 ,
, which
which
is supposed not to have diverged much in character, but to have retained the form of (F), either unaltered or altered only in a slight degree. In this case, its affinities to the other fourteen new species will be of a curious and circuitous nature.
Being
Having
descended from a form which stood between the
two
two
parent-species
parent species
(A) and (I), now supposed to be extinct and unknown, it will be in some degree intermediate in character between the two groups descended from these
two species.
species.
But as these two groups have gone on diverging in character from the type of their parents, the new species (F 14 )
) will
will
not be directly intermediate between them, but rather between types of the two groups; and every naturalist will be able to
call
bring some
such
cases
case
before his mind.
In the diagram, each horizontal line has hitherto been supposed to represent a thousand generations, but each may represent a million or several million generations; it may also represent a section of the successive strata of the
earth's
earths
crust including extinct remains. We shall, when we come to our chapter on Geology, have