92 PALEONTOLOGY OF NEW-YORK. 
129, 1. TENTACULITES? FLEXUOSA (n. sp.). 
Pu. XXIX. Figs. 6 a, b,c, d. 
Tubes single or aggregate, adhering, more or less curved at the tip or along the whole 
length ; surface marked by strong annulations, which are crossed by fine longitudinal strie; 
annulations somewhat irregular ; interior distinctly septate ; septa with the concave sides 
upwards. 
The mode of growth and the interior structure here developed give us more information 
regarding the habits of this hitherto doubtful fossil, than we have before possessed. If the 
species in question be a true Tenracutites, of which perhaps we may have some doubt, 
it appears to have been developed like many of the Corals, viz. a simple tube affixed at 
the base, occupied by an animal which secretes calcareous matter, building up the walls 
of the cell, and extending across it transverse septa as the tube became elongated. The 
structure of the tube, however, allies it more nearly with Crinoideans than with Corals ; 
and it is probable that it was inhabited by a simply constructed animal of the same order. 
The specimen fig. 1 a first attracted my attention by its curved tip, showing that it must 
have been attached to some other body. A further careful search among a large number of 
specimens from Lowville enabled me to discover the attached group, which shows that an 
exudation of calcareous matter attaches them firmly to the shell, while a group of the cells 
of Chetetes lycoperdon have commenced their growth on the same. 
I have referred this, with some hesitation, to the Genus Tentacuites, both on account 
of its general form and mode of adhering to other bodies, as well as from its internal 
structure, which, however, has not heretofore been shown in the true Tenracuuires. All 
the other species known in our strata are straight, rigid, and gradually tapering to a point, 
always separate, and never known as adhering to other bodies. 
Fig. 6 a. A single specimen of this species, with a portion of the same magnified, showing the transverse 
septa. 
Fig. 6 b. A group of the same species, adhering by their smaller extremities to the dorsal valve of Orthis 
testudinaria. At c, there is the base of several cells of the Chatetes lycoperdon, adhering to 
the same shell. 
Fig. 6 d. A single tube, magnified, showing more distinctly the striz upon the surface, and, also, in some 
degree, the irregularity of the annulations. 
Position and locality. 'This fossil is only known to me as occurring in the thinbedded 
portions of the Trenton limestone, from sixty to one hundred feet above its base. Lowville, 
Lewis county. 
