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ubes of _Halysites agglomerata_, of the natural size; d, Vertical section of two tubes of the same, showing the tabulae, enlarged. Niagara Limestone (Wenlock), Canada. (Original.)] [Illustration: Fig. 60.--Upper Silurian Star-fishes. 1, _Palasterina primoeva_, Lower Ludlow; 2, _Paloeaster Ruthveni_, Lower Ludlow; 3, _Paloeocoma Colvini_, Lower Ludlow. (After Salter.)] [Illustration: Fig. 61.--A, _Protaster Sedgwickii_, showing the disc and bases of the arms; B, Portion of an arm, greatly enlarged. Lower Ludlow. (After Salter.)] Amongst the _Echinodermata_, all those orders which have hard parts capable of ready preservation are more or less largely represented. We have no trace of the Holothurians or Sea-cucumbers; but this is not surprising, as the record of the past is throughout almost silent as to the former existence of these soft-bodied creatures, the scattered plates and spicules in their skin offering a very uncertain chance of preservation in the fossil condition. The Sea-urchins (_Echinoids_) are said to be represented by examples of the old genus _Paloechinus_. The Star-fishes (_Asteroids_) and the Brittle-stars (_Ophiuroids_) are, comparatively speaking, largely represented; the former by species of _Palasterina_ (fig. 60), _Paloeaster_ (fig. 60), _Paloeocoma_ (fig. 60), _Petraster, Glyptaster_, and _Lepidaster_--and the latter by species of _Protaster_ (fig. 61), _Paloeodiscus, Acroura_, and _Eucladia_. The singular _Cystideans_, or "Globe Crinoids," with their globular or ovate, tesselated bodies (fig. 46, A, C, D,), are also not uncommon in the Upper Silurian; and if they do not become finally extinct here, they certainly survive the close of this period by but a very brief time. By far the most important, however, of the Upper Silurian Echinodenns, are the Sea-lilies or _Crinoids_. The limestones of this period are often largely composed of the fragmentary columns and detached plates of these creatures, and some of them (such as the Wenlock Limestone of Dudley) have yielded perhaps the most exquisitely-preserved examples of this group with which we are as yet acquainted. However varied in their forms, these beautiful organisms consist of a globular, ovate, or pear-shaped body (the "calyx"), supported upon a longer or shorter jointed stem (or "column"). The body is covered externally with an armour of closely-fitting calcareous plates (fig. 62), and its upper surface is protected by similar but sm
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