The Life of CrustaceaCalman, W. T. (William Thomas)
Science
The Life of Crustacea
Calman, W. T. (William Thomas)
Crustacea
Of the Decapoda the geological history is tolerably full, and it is
possible to trace in its broad outlines the course of evolution of the
various suborders. Here again it is likely that the beginnings of the
group are to be sought for in the Carboniferous epoch, and some of the
obscure shrimp-like forms of that age show hints of an affinity with the
Decapods. In the Triassic epoch, however, and more abundantly in the
succeeding Jurassic, a number of types are found which seem to include
primitive representatives of several of the existing groups of Natantia
and Reptantia. It is noteworthy that among them are some forms (_Æger_,
etc.) resembling the existing Stenopidea, a tribe which in some respects
is intermediate between these two suborders. In the Stenopidea the first
three pairs of legs bear pincer-claws, as in the Lobster, but the third
pair is much the largest; and _Æger_ agrees with them in this unusual
character, though there is little else, in what is known of its
structure, to help to determine its affinities.
The tribe Penæidea, which occupies in many respects a primitive place
among the Natantia, is abundantly represented in the Jurassic epoch,
especially in the lithographic stone (Upper Jurassic) of Solenhofen, and
by somewhat doubtful specimens from the earlier Trias. All these agree
in having the first three pairs of legs with pincer-claws, and not
differing greatly in size. Some of the Jurassic and later fossils are of
so modern a type that they have been referred to the existing genus
_Penæus_.
The Upper Jurassic rocks also preserve the earliest undoubted specimens
of true Prawns of the tribe Caridea, and some of these show swimming
branches (exopodites) on the thoracic legs, so that they were probably
related to the primitive family Acanthephyridæ, of which the existing
members are found in the deep sea. It is possible, however, that Caridea
were already in existence far earlier, for some of the obscure
Carboniferous forms seem to have the broadened side-plates of the second
abdominal somite, which, so far as we know, are exclusively
characteristic of that tribe.
Public-domain text, read in full here on John Shaqi.
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