The Chain of Life in Geological Time: A Sketch of the Origin and Succession of Animals and PlantsDawson, John William, Sir
Science
The Chain of Life in Geological Time: A Sketch of the Origin and Succession of Animals and Plants
Dawson, John William, Sir
Paleobotany; Paleontology
The most curious history in this group is that of the feather-stars. In
the Early Cambrian they are represented by a few species known to us
only in fragments, and these belong to a humble group (Cystideans)
resembling the larval or immature condition of the higher Crinoids. Fig.
49 shows one of these animals of somewhat later age. They have few or
rudimentary arms and short stalks, and want the beautiful radial
symmetry of the typical star-fishes. In the Silurian these creatures are
reinforced by a vast number of beautiful and perfect feather-stars
(Figs. 50, 51). These continue to increase in number and beauty, and
apparently culminate in the Mesozoic, where gigantic forms exist, some
of them probably having more complicated skeletons, in so far as number
of distinct parts is concerned, than any other animals. Buckland has
calculated that in a crinoid similar to that in Fig. 52 there are no
less than 150,000 little bones, and 300,000 contractile bundles of
fibres to move them. In the modern seas the feather-stars have somewhat
dwindled both in numbers and complexity, and are mostly confined to the
depths of the ocean. On the other hand, the various types of ordinary
star-fishes and sea-urchins have increased in number and importance. We
thus find in this group a certain advance and improvement from the
Cystideans of the Early Palæozoic to the sea-urchins and their allies.
This advance is not, however, along one line for the Cystideans
continue unimproved to the end. The Crinoids culminate in the Mesozoic,
and are not known to give origin to anything higher. The star-fishes and
sea-urchins commence independently, before the culmination of the
Crinoids, and, though greatly increased in number and variety, still
adhere very closely to their original types.
[Illustration: FIG. 49.—_Pleurocystites squamosus_. Siluro-Cambrian.
After Billings.]
[Illustration: FIG. 50.—_Heterocrinus simplex_ (Meek). One of the least
complex crinoids of that period. Siluro-Cambrian.]
[Illustration: FIG. 51.—Body of _Glyptocrinus_. Siluro-Cambrian.]
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