Evolution (Biology); Glacial epoch; Human beings -- Origin; Human evolution
There is also another geographical fact equally in favour of the
antiquity of the mounds, namely, that they are wanting on those parts of
the coast which border the Western Ocean, or exactly where the waves are
now slowly eating away the land. There is every reason to presume that
originally there were stations along the coast of the North Sea as well
as that of the Baltic, but by the gradual undermining of the cliffs they
have all been swept away.
Another striking proof, perhaps the most conclusive of all, that the
"kitchen-middens" are very old, is derived from the character of their
embedded shells. These consist entirely of living species; but, in the
first place, the common eatable oyster is among them, attaining its
full size, whereas the same Ostrea edulis cannot live at present in the
brackish waters of the Baltic except near its entrance, where, whenever
a north-westerly gale prevails, a current setting in from the ocean
pours in a great body of salt water. Yet it seems that during the whole
time of the accumulation of the "kitchen-middens" the oyster flourished
in places from which it is now excluded. In like manner the eatable
cockle, mussel, and periwinkle (Cardium edule, Mytilus edulis, and
Littorina littorea), which are met with in great numbers in the
"middens," are of the ordinary dimensions which they acquire in the
ocean, whereas the same species now living in the adjoining parts of
the Baltic only attain a third of their natural size, being stunted and
dwarfed in their growth by the quantity of fresh water poured by rivers
into that inland sea.*
(* See "Principles of Geology" chapter 30.)
Hence we may confidently infer that in the days of the aboriginal
hunters and fishers, the ocean had freer access than now to the Baltic,
communicating probably through the peninsula of Jutland, Jutland having
been at no remote period an archipelago. Even in the course of the
nineteenth century, the salt waters have made one irruption into the
Baltic by the Lymfiord, although they have been now again excluded. It
is also affirmed that other channels were open in historical times which
are now silted up.*
(* See Morlot "Bulletin de la Societe Vaudoise des Sci.
Nat." tome 6.)
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