have attempted to show that the geological record is extremely imperfect; that only a small portion of the globe has been geologically explored with care; that only certain classes of organic beings have been largely preserved in a fossil state; that the number both of specimens and of species, preserved in our museums, is absolutely as nothing compared with the
incalculable incalculable 1859 1860 1861 1866 | incalculable 1869 1872 |
number of generations which must have passed away even during a single formation; that, owing to subsidence being
almost necessary almost necessary 1861 1866 1869 1872 | necessary 1859 1860 |
for the accumulation of
....... 1861 1866 1869 1872 | fossiliferous 1859 1860 |
deposits
rich in fossils and thick rich in fossils and thick 1861 1866 |
thick 1859 1860 |
rich in fossil species of very many kinds and thick 1869 |
rich in fossil species of many kinds, and thick 1872 |
enough to
resist resist 1859 1860 1861 1866 1869 | outlast 1872 |
future degradation,
enormous enormous 1859 1860 1861 1866 | great 1869 1872 |
intervals of time
have have 1859 1860 1861 1866 | must have 1869 1872 |
elapsed between
most of our most of our 1861 1866 1869 1872 |
the 1859 1860 |
successive formations; that there has probably been more extinction during the periods of subsidence, and more variation during the periods of elevation, and during the latter the record will have been least perfectly kept; that each single formation has not been continuously deposited; that the duration of each formation is,
perhaps, perhaps, 1859 1860 1861 | probably, 1866 1869 1872 |
short compared with the average duration of specific forms; that migration has played an important part in the first appearance of new forms in any one area and formation; that widely ranging species are those which have varied
most, most, 1859 1860 1861 | most 1866 1869 1872 |
and and 1859 1860 1861 | frequently, and 1866 1869 1872 |
have oftenest given rise to new species;
and and 1859 1860 1861 | and 1866 1869 1872 |
that varieties have at first
often often 1859 1860 1861 | often 1866 1869 1872 |
been
local. local. 1859 1860 1861 |
local; and lastly, although each species must have passed through numerous transitional stages, it is probable that the periods, during which each underwent modification, though many and long as measured by years, have been short in comparison with the periods during which each remained in an unchanged condition. 1866 1869 1872 |
....... 1861 1866 1869 1872 | All 1859 1860 |
These These 1861 1866 1869 1872 | these 1859 1860 |
causes causes 1859 1860 1861 | causes, 1866 1869 1872 |
taken conjointly,
must have made the geological record extremely imperfect, and must have made the geological record extremely imperfect, and 1861 |
must have tended to make the geological record extremely imperfect, and 1859 1860 |
OMIT 1866 1869 1872 |
will to a large extent explain
why— though why— though 1861 1866 1869 1872 | why 1859 1860 |
we do
find find 1861 1866 |
not find 1859 1860 |
find many links— we do not find 1869 1872 |
many links between the members of the same group— we do not find interminable many links between the members of the same group— we do not find interminable 1861 |
interminable 1859 1860 1869 1872 |
many links between the species of the same group— we do not find interminable 1866 |
varieties, connecting together all
....... 1861 1866 1869 1872 | the 1859 1860 |
extinct and existing forms
....... 1861 1866 1869 1872 | of life 1859 1860 |
by the finest graduated steps. ↑1 blocks not present in 1859 1860 1861; present in 1866 1869 1872 | It should also be constantly borne in mind that any linking varieties
between two or more
forms, which might be found, would be ranked, unless the whole chain could be perfectly restored, as so many
new and distinct species; for it is not pretended that we have any sure criterion by which species and varieties can be discriminated.
|
|