The History of the European FaunaScharff, R. F. (Robert Francis)
History
The History of the European Fauna
Scharff, R. F. (Robert Francis)
Animals -- Europe; Zoogeography
On the whole, the number of mollusca which we might point to as having
migrated to Europe is not large, the great majority being indigenous to
our continent. However, some of the other groups of invertebrates differ
very materially in that respect from the mollusca. I cannot leave the
consideration of the mollusca without referring to the fact that there
appears to be a very important centre of distribution in South-eastern
Europe. It is from this centre that many species have spread north and
south, east and west. Take, for example, the genus _Clausilia_, a small
land-shell shaped like a pointed round tower, and abundant on old walls
and tree trunks. In England we have four species of _Clausilia_, in
Ireland only two. In the greater part of Spain only our common _Cl.
bidentata_ occurs. As we go east the number of species rapidly
increases. A maximum is reached in South-eastern Europe, where hundreds
of different kinds are found. Towards Northern Europe a similar decrease
of species takes place. So far the history of the _Clausiliæ_ seems
perfectly simple. An active centre of origin appears to exist in
South-eastern Europe, from which the species radiate out in all
directions. But when we come to look more closely into the
extra-European distribution of the genus, and especially when we
examine its past history, we find that its origin is extremely complex,
and dates back to a much more remote period than would have been
imagined, had we merely taken into account its present range in our own
continent. Professor Boettger, who is the highest authority on
_Clausilia_, tells us that the genus is known from the earliest deposits
of the Tertiary Era. About 700 species are now known, and these have
been sub-divided by Professor Boettger and others into a number of
sub-genera. Some of these are extinct, but the great majority are still
living. The sub-genus _Phædusa_ occurs in the eocene and oligocene of
Southern Europe, but it is extinct as far as our continent is concerned.
Close upon a hundred species, however, still inhabit India, the Malayan
Islands, China, Ceylon, and Japan. Then again, the sub-genus
_Laminifera_ occurs in the oligocene and miocene of Central Europe, and
survives in a single species, _Cl. Pauli_, in South-western France. The
groups _Garnieria_ of China, _Macroptychia_ of East Africa, _Boettgeria_
of Madeira, and _Nenia_ of South America, have no fossil
representatives. We have here some very remarkable cases of
discontinuous distribution which testify to the antiquity of the genus,
and this is certainly confirmed by the fossil evidence. However, it is
hardly likely that the headquarters, as it were, of _Clausilia_ have
always been in South-eastern Europe. Most of that part of the Continent
has been submerged since eocene times more than once. The peculiar
distribution of the genus might be explained, I think, if we supposed
the original home of _Clausilia_ to have been in Southern Asia, that
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