The Cambridge natural history, Vol. 01 (of 10)Hickson, Sydney J. (Sydney John)
Science
The Cambridge natural history, Vol. 01 (of 10)
Hickson, Sydney J. (Sydney John)
Animals
The shell-substance, if calcareous, has one of the two types, porcellanous
or vitreous, that we have already mentioned, but _Polytrema_, a form of
very irregular shape, though freely perforated, is of a lovely pink colour.
In the calcareous shells sandy particles may be intercalated, forming a
transition to the Arenacea. In these the cement has an organic base
associated with calcareous or ferruginous matter; in some, however, the
cement is a phosphate of iron. The porcellanous shells are often deep brown
by transmitted light.
{63}[Illustration: FIG. 13.—Shells of _Foraminifera_. In 3, 4, and 5, _a_
shows the surface view, and _b_ a section; 8_a_ is a diagram of a coiled
cell without supplemental skeleton; 8_b_ of a similar form with
supplemental skeleton (_s.sk_); and 10 of a form with overlapping whorls;
in 11_a_ half the shell is shown in horizontal section; _b_ is a vertical
section; _a_, aperture of the shell; 1-15, successive chambers, 1 being
always the oldest or initial chamber. (From Parker and Haswell, after other
authors.)]
Despite the apparent uniformity of the protoplasmic body in this group, the
shell is infinitely varied in form. As Carpenter writes, in reference to
the Arenacea, "There is nothing more wonderful in nature than the building
up of these elaborate and symmetrical structures by mere jelly-specks,
presenting no traces {64}whatever of that definite organisation which we
are accustomed to regard as necessary to the manifestations of conscious
life.... The tests (shells) they construct when highly magnified bear
comparison with the most skilful masonry of man. From the same sandy bottom
one species picks up the coarsest quartz grains, unites them together with
a ferruginous cement, and thus constructs a flask-shaped test, having a
short neck and a single large orifice; another picks up the finer grains
and puts them together with the same cement into perfectly spherical tests
of the most extraordinary finish, perforated with numerous small pores
disposed at pretty regular intervals. Another species selects the minutest
sand grains and the terminal portions of sponge-spicules, and works them up
together—apparently with no cement at all, but by the mere laying of the
spicules—into perfect white spheres like homoeopathic globules, each
showing a single-fissured orifice. And another, which makes a straight,
many-chambered test, the conical mouth of each chamber projecting into the
cavity of the next, while forming the walls of its chambers of ordinary
sand grains rather loosely held together, shapes the conical mouths of the
chambers by firmly cementing together the quartz grains which border it."
The structure of the shell is indeed variable. The pylome may be single or
represented by a row of holes (_Peneroplis_, _Orbitolites_), or, again,
there may be several pylomes (_Calcituba_); and, again, there are in
addition numerous scattered pores for the protrusion of pseudopodia
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