The Ocean World: Being a Description of the Sea and Its Living Inhabitants.Figuier, Louis
Science
The Ocean World: Being a Description of the Sea and Its Living Inhabitants.
Figuier, Louis
Marine animals; Ocean
"When the animal is engaged in increasing the dimensions of its abode,
the margin of the mantle is protruded and firmly adherent all round to
the circumference of the valve with which it corresponds. Thus
circumstanced, it secretes calcareous matter and deposits it upon the
extreme edge of the shell, when the secretion hardens and becomes
converted into a layer of solid testaceous substance. At intervals this
process is repeated, and every newly-formed layer enlarges the diameter
of the valve. The concentric strata thus deposited remain
distinguishable externally, and thus the lines of growth marking the
progressive increase of size may easily be traced."
"While the margin of the mantle is thus the sole agent in enlarging the
circumference of the shell," the professor continues farther on, "its
growth in thickness is accomplished by a secretion of a kind of
calcareous varnish derived from the external surface of the mantle
generally, which, being deposited layer by layer over the whole interior
of the previously existing shell, progressively adds to its weight and
solidity. There is, however, a remarkable difference in character
between the material secreted by the marginal fringe and that furnished
by the general surface of the mantle membrane. The former we have found
more or less covered by glands appointed for the purpose, situated in
the circumference of the mantle; but as these glands do not exist
elsewhere, no colouring matter is ever mixed with the layers that
increase the thickness of the shell, so that the latter always remain of
a delicate whitish hue, and form the well known iridescent material
usually distinguished by the name of nacre or mother-of-pearl."
(_General Outline_, p. 385.)
The process by which shells attain their beautiful markings is thus
described by Mr. Jones:--"The external surface is exclusively deposited
by the margin of the mantle, which contains in its substance certain
coloured spots, which are found to be of a glandular character, and to
owe their peculiar character to a pigment they secrete, which is mixed
with the calcareous matter; coloured lines are therefore found on the
exterior of the shell wherever these glandular organs exist. Where the
deposition of colour is kept up throughout the process of enlargement,
the lines are unbroken and perfect; but where the coloured matter is
furnished only at intervals, spots and patches of irregular form and
increasing in size with the enlargement of the mantle are the
consequence."
Public-domain text, read in full here on John Shaqi.
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