The Cambridge natural history, Vol. 04 (of 10)Warburton, Cecil
Science
The Cambridge natural history, Vol. 04 (of 10)
Warburton, Cecil
Animals
Trilobites seem to have been exclusively marine, since they are found
only in association with the remains of marine animals. Their range in
depth was evidently considerable, for they occur in many different kinds
of sediment, and were apparently able to live regardless of the nature
of the sea-floor—whether muddy, sandy, calcareous, or rocky. In some
cases they occur in deposits containing reef-building corals and other
shallow water animals; in others they are associated with organisms
which lived at greater depths. The group appears to have had a
world-wide distribution, for the remains of Trilobites are found in the
Palaeozoic rocks of all countries. Their range in size is considerable;
for whilst a large proportion of the species are about two or three
inches in length, some, like _Agnostus_, are only a quarter of an inch
long, others are from ten to twenty inches long, the largest forms
including species of _Paradoxides_, _Asaphus_, _Megalaspis_, _Lichas_,
and _Homalonotus_.
The feature in a Trilobite which first attracts attention is the marked
division of the dorso-ventrally flattened body into a median or axial
part, and a lateral or pleural part on each side. It was this character
that led Walch, in 1771, to give the name by which the group is now
known. The axial part of the body contained the alimentary canal, as is
shown by the position of the mouth and anus, as well as by casts in mud
of the canal which are found in some specimens. The trilobation of the
body is quite distinct in the majority of Trilobites, but in a few
genera belonging to the Asaphidae and Calymenidae (Fig. 136) it becomes
more or less completely obsolete.
[Illustration:
FIG. 136.—_Homalonotus delphinocephalus_, Green, × 1. Silurian. (After
Zittel.)
]
In most cases the only part of the Trilobite which is preserved is the
exoskeleton which covered the dorsal surface of the body. That skeleton
consists largely of calcareous material, and shows in sections a finely
perforated structure. Generally it is arched above, but in some cases is
only slightly convex; in outline it is more or less oval. Three regions
can always be distinguished in the body of a Trilobite—the head, the
thorax, and the abdomen or pygidium.
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