The Cambridge natural history, Vol. 10 (of 10)Beddard, Frank E. (Frank Evers)
Science
The Cambridge natural history, Vol. 10 (of 10)
Beddard, Frank E. (Frank Evers)
Animals; Mammals
During certain periods of the Tertiary epoch it is true that there was more
similarity between Europe and North America than there is at present. It
would have been quite necessary to unite both into a Holarctic area, such
as is now insisted upon by many; but the reasons for this union would then
have been stronger. The fact is, however, that the closer resemblances were
due to the larger number of families of animals which existed then than
now; these have decayed away from both continents, and allowed the
unlikenesses between the mammalian fauna of both to become evident. But the
likenesses which still survive have led many to associate the two regions
closely together.
So far as the history of a genus or family or larger division {84} can be
traced, it results as a conclusion that from a given area of origin the
group in question migrated in all directions where possible to a varying
degree; it then died out in intervening tracts, or was left only in a
certain part of its former and more extensive area of range.
ZOOLOGICAL REGIONS.--Seeing that each species of animal has its own
definite range, it is clear that the earth's surface can be apportioned
into divisions which are characterised by their animal inhabitants. We
shall divide the earth into realms, which are the largest divisions; then
into regions; and finally into subregions. It must be borne in mind that
the various groups of the animal kingdom are of different ages,
geologically speaking, and have therefore had less or more time, as the
case may be, to settle down into their present distribution, and that
different animals differ greatly in their rate of multiplication, their
power of migration, and their susceptibility to the effectiveness of
various natural and other barriers to distribution. It is not, therefore,
possible to divide the world into realms and regions which shall express
the facts of distribution of the entire animal kingdom. Such divisions,
which are common in text-books of zoology having but a small section
devoted to zoogeography, are at best mere approximations and averages; no
good is gained by taking such a comprehensive view of the matter, as the
essential object of subdividing the earth's surface is thereby lost sight
of. The zoogeographical division of the earth which will be adopted here is
that originally recommended by Dr. Blanford, and now accepted by a number
of authorities. There are three "realms," to which a fourth may perhaps be
added--though on negative grounds, and merely for the purpose of
emphasising the parts of the world to which mammals have not gained access.
The realms are again divisible into regions, at least in the case of one of
them, and the regions may be again separated into more or less distinct
subregions or provinces. The three primary divisions or realms which
contain mammals are the Notogaean, including Australia and certain islands
to the north of it; the Neogaean, or the South American continent and
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