The Crayfish: An Introduction to the Study of Zoology.Huxley, Thomas Henry
Science
The Crayfish: An Introduction to the Study of Zoology.
Huxley, Thomas Henry
Crayfish; Zoology
Where the cuticular layer of the integument is uncalcified, for
example, between the sterna of the abdominal somites, it presents an
external, thin, dense, wrinkled lamina, the _epiostracum_, followed
by a soft substance, which, on vertical section, presents numerous
alternately more transparent and more opaque bands, which run
parallel with one another and with the free surfaces of the slice
(fig. 56, D). These bands are very close-set, often not more than
1‐5000th of an inch apart near the outer and the inner surfaces, but
in the middle of the section they are more distant.
If a thin vertical slice of the soft cuticle is gently {193} pulled
with needles in the direction of its depth, it stretches to eight or
ten times its previous diameter, the clear intervals between the dark
bands becoming proportionally enlarged, especially in the middle of
the slice, while the dark bands themselves become apparently thinner,
and more sharply defined. The dark bands may then be readily drawn
to a distance of as much as 1‐300th of an inch from one another; but
if the slice is stretched further, it splits along, or close to, one
of the dark lines. The whole of the cuticular layer is stained by
such colouring matters as hæmatoxylin; and, as the dark bands become
more deeply coloured than the intermediate transparent substance, the
transverse stratification is made very manifest by this treatment.
Examined with a high magnifying power, the transparent substance is
seen to be traversed by close-set, faint, vertical lines, while the
dark bands are shown to be produced by the cut edges of delicate
laminæ, having a finely striated appearance, as if they were composed
of delicate parallel wavy fibrillæ.
In the calcified parts of the exoskeleton a thin, tough, wrinkled
epiostracum (fig. 56, B, _a_), and, subjacent to this, a number of
alternately lighter and darker strata are similarly discernible:
though all but the innermost laminæ are hardened by a deposit of
calcareous salts, which are generally evenly diffused, but sometimes
take the shape of rounded masses with irregular contours.
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