96 
sent collector and dealer in fossils, to whose zeal and integrity in collecting and 
preserving all Crinoidal remains which fell under his observation, I am much 
indebted for acquiring a series of highly illustrative specimens. 
Description. 
The Corumn (Pu. 1. fig. 1. Px. vi. fig. 1. to 22.) of this animal, is near 
the pelvis formed of very thin joints, alternately a little longer and thicker, with 
a still larger one intervening every second or third joint. This regularity is in- 
terrupted further down by the intervention of four or five small joints, all ap- 
pearing muscular, and as if they had not yet acquired solidity by the secretion 
of calcareous matter, which I consider as a proof of the formation and interpos- 
ing of new joints during the life of theanimal between those already existing. 
Stull lower down the column the joints become of a more uniform thickness 
and size, and vary but very little. In an early stage of growth they are ex- 
ternally much contracted near the margin of adhesion, thence somewhat moni- 
liform, which form is continued when they increase in size, though less conspi- 
cuously showing itself, sometimes only in a slight central elevation. The arti- 
culating surface of the joints (PL. v1. fig. 1.3. 5.) is very regularly striated or 
grooved in radii, from the middle, producing externally a most regular and 
beautiful suture of mutual insertion, (PL. vi. fig. 15.) Near the centre they 
are excavated on both sides, forming a muscular edge, which surrounds the ali- 
mentary canal. In sections we may sometimes see the alimentary canal of a 
considerable size (PL. vi. fig. 14. and 16.) and not unfrequently observe it at 
regular intervals more or less alternately contracted and dilated, yet always 
leaving a large passage open. It is from the increased size of the alimentary canal 
in columns of larger diameter, that I apprehend the epidermis or periosteum, 
whose usual office was to secrete the calcareous matter forming the joints, had 
also the power of absorbing and removing it ; for, without this, the passage for 
the alimentary canal could not be enlarged, unless we indeed could admit that 
the induration of the calcareous matter forming the joints did not take place till 
the animal was full grown, which, however, is quite contrary to the operations 
of nature in the other Crinoidea. 
The Cotumn (PL. vi. fig. 17. to 22.) sometimes exhibits a swelling out of 
several joints, which renders it barrel-shaped, and a lateral concave depression 
with a central perforation as noticed in Poteriocrinites crassus, page 69. 
