TRENTON LIMESTONE. 7a 
108. 6. STREPTOPLASMA PARVULA (n. sp.). 
PE XXYV. Figs, 4 a, b, ¢. 
Turbinate, curved, somewhat gradually expanding above ; cup deep, occupying about 
one half the length of the specimen ; lamelle few (about 30), strong; surface smooth ; 
edge of the cup not recurved. 
This species is much smaller than either of the preceding, and, presenting a nearly 
smooth surface, differs externally from the young specimens of S. corniculum. The lamelle 
are also fewer than in that species, and are comparatively thinner and weaker than in S. 
crassa. In many instances the margin is broken off to the depth of the cup, showing the 
lamelle in the centre as high as on the outer margin, but this is always due to accident. 
It is much more numerous than either of the preceding species, and is rarely associated 
with them in the rock. 
Fig. 4 a. The lower part of a specimen of ordinary size, with the margin of the cup broken off, showing 
the lamelle within. 
Fig. 4 6. Transverse section of the same, showing the simple radiating lamelle. 
Fig. 4c. A group of the same. Three of the specimens lie upon the surface of the stone, with their 
bases nearly in contact. 
Position and locality. In the thin shaly layers just above the Birdseye limestone, at 
Middleville, Herkimer county. (State Collection.) 
109. 1. PORITES? VETUSTA (x. sp.). 
Pu, XXV. Figs. 5 a, b. 
A sub-hemispheric coral, composed of irregular concentric lamine ; cells vertical to the 
lamine ; openings upon the surface, nearly circular, with internal vertical lamella which 
reach half way to the centre. 
To some extent, this specimen presents the character of PoriTEs, in a great degree of 
perfection. The surface of the specimen being weathered, the radiating lamelle are often 
obliterated. The centre of the cells are also destitute ( perhaps from weathering ) of the ~ 
fine elevated points characteristic of some recent species of the PorirEs. 
This is the only species known to me in the lower term of our system, which presents, 
in any degree of perfection, the characters of the recent PoriTEs. 
Fig. 5 a. Surface of the specimen, a part only showing the cells. 
Fig. 5 b. A portion magnified. The figure on the right hand is one of the cells more distinctly enlarged. 
Position and locality. In the lower part of the Trenton limestone, near its junction with 
the Black-river limestone. Watertown, Jefferson county. 
