The Story of a Boulder; or, Gleanings from the Note-book of a Field GeologistGeikie, Archibald
Science
The Story of a Boulder; or, Gleanings from the Note-book of a Field Geologist
Geikie, Archibald
Geology; Petrology
Each bryozoon consists externally of a single horny or calcareous cell,
sometimes furnished with a valve-like lid that folds down when the
animal withdraws itself. When danger is past, and the creature begins
again to emerge, the upper parts, which were drawn in like the inverted
finger of a glove, are pushed out until a series of tentacles, covered
with minute hair-like bodies, called cilia, are expanded. The vibratile
motion of these cilia causes a constant current in the direction of
the mouth, which lies in the centre of the hollow whence the tentacles
spring; animalcules are in this way brought in rapid succession within
reach of the mouth, and form a never-failing source of nourishment.
The interior is greatly more complex than that of the _polypi_. The
stomach is connected above with a cavity like the gizzard of a bird,
furnished with pointed sides, which serve to triturate the food before
it passes into the stomach. There is also a distinct intestine. The
muscular action for the expansion and retraction of the animal is
highly developed, and the generative system is a greatly more complex
one than that of the polyps already referred to. In short, however
closely they might be thought to resemble the corals in outward form,
their internal structure undoubtedly links them with a much higher type
of organization, and justifies the naturalist in subjoining them as a
sub-order to the mollusca.
The cells are grouped at short intervals along a horny or calcareous
substance, that sometimes encrusts sea-weed, or spreads out as a flat
leaf-like membrane, or rises into cup-shaped or dendritic forms. A
series of cells constituting a separate and independent colony, is
termed a polypidom. The cells are further connected together by an
external jelly-like integument, in which they are sunk, and which
serves to secrete the calcareous particles from the sea.
It is interesting to know that creatures so minute and yet so complexly
organized, existed abundantly in the seas of the Carboniferous period.
No less than fifty-four species are enumerated as having been obtained
from the carboniferous strata of the British Islands, and scarcely a
year passes without one or two new species being added to the list.
The most frequent belong to the genus _Fenestella_, or little window,
a name indicative of the reticulated grouping of the branches like the
wooden framework of a window. Each of these branches, or interstices,
as they are called, was more or less straight, being connected with
that on either side by a row of transverse bars, just as the central
mullion of an abbey window is connected with the flanking ones by means
of cross-bars of stone. Not unfrequently some of the branches subdivide
into two, as we saw to be the case among the cup-corals.
[Illustration: Fig. 18.--_a_, Fenestella oculata (M'Coy), nat. size;
_b_, magnified portion of the same.]
Public-domain text, read in full here on John Shaqi.
Reviews
Reviews
No reviews yet
Be the first to share your thoughts on this work.
Elsewhere in the archive
Join the Discussion
Join the discussion
Sign in to leave a comment or review.
Sign InorCreate an account