The Structure and Life-history of the Cockroach (Periplaneta orientalis): An Introduction to the Study of InsectsMiall, L. C. (Louis Compton)
Science
The Structure and Life-history of the Cockroach (Periplaneta orientalis): An Introduction to the Study of Insects
Miall, L. C. (Louis Compton)
Cockroaches
A third distinction between palæozoic and modern Cockroaches is found
in the veinlets of the anal area. These, unlike the branches of the
other veins, do not part from the main anal vein at various points
along its course, but form a series of semi-independent veinlets, and
in palæozoic Cockroaches take the same general course as the main anal
vein, or “anal furrow” (the curved, deeply sunken vein that marks
off the anal area from the rest of the front wing, both in ancient
and modern Cockroaches), and terminate at sub-equidistant intervals
upon the inner margin; while in modern Cockroaches these veins either
run sub-parallel to the inner margin and terminate on the descending
portion of the anal furrow, or they form a fusiform bundle and
terminate in proximity to one another and to the tip of the anal furrow.
These differences, which were mentioned by Germar and Goldenberg,
and their universality pointed out in my memoir on Palæozoic
Cockroaches,[197] seem to warrant our separating the older forms from
the modern as a family group, under the name of _Palæoblattariæ_; this
family has been thus characterised:--
[197] Memoirs Bost. Soc. Nat. Hist., III., 23 seq. (1880).
Fore wings diaphanous, generally reticulated, and nearly symmetrical on
either side of a median line. Externomedian vein completely developed,
forking in the outer half of the wing, its branches generally occupying
the apical margin; internomedian area broad at base (beyond the anal
area), rapidly tapering apically, and filled with oblique mostly
parallel veins, having nearly the same direction as the anal veinlets,
which, like them, strike the inner margin.
About eighty palæozoic species have been published up to the present
time, and have been grouped in two sub-families and thirteen genera.
Besides these, Brongniart has not yet given any hint of how many have
been found at Commentry, a French locality which may be expected to
increase the number largely, and about twenty undescribed species are
known to me from the American Carboniferous rocks.
[Illustration: Fig. 120.--_Etoblattina mazona_ Scudd. × 3. (The outline
of natural size.) Carboniferous, Illinois.]
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