CLINTON GROUP. 
39 
GRAPTOLITES. 
I have detected two species of Graptolites in this group : One of them was known and 
published in the Report of the Fourth Geological District, 1843 ; the other is new. Thus far 
all our examinations have not sufficed to bring out a single species of Graptolithus from any 
more recent period than the Clinton group. This genus must therefore be ranked among those 
families which, though living in great profusion in early geological periods, never prolong their 
existence into the modern periods even of the palaeozoic era. In all our more recent formations 
of Silurian and Devonian age, we have nothing which represents the Graptolite : we bid a fare? 
well to the genus. 
416. 15. GRAPTOLITHUS CLINTONENSIS. 
Pl. a. XVII. Fig. la-i. 
Graptolithus clintonensis. Geol. Rep. 4th Dist. N. York, 1843, p. 74; fig. 12, p. 72. 
Stipe slender, simple, linear, straight or curving, serrated on one side, the opposite side (or 
back) marked by a fine longitudinal groove; serrae long, deeply cut into the stipe, with the 
points recurved ; surface slightly granulated 1 
This species is readily distinguished from any in the lower strata, by its long recurved teeth, 
which are very peculiar. When the points of these are imperfect, its distinctive characters rest 
on the depth to which they are cut into the stipe, and their close arrangement, which likewise 
distinguishes this one from those in the lower rocks. In specimens where the back of the stipe 
is shown, it presents a longitudinal groove; and at the base of the teeth it becomes much 
thicker, and again diminishes towards the points. 
Fig. 1 a. A lamina of slate, with fragments of this species upon the surface. Where imbedded 
in the soft greeh shale, the depth of the sefratures and the pointed extremities are 
not so clearly preserved. 
Fig. 1 b. A fragment of a stipe, showing the depth of the serratures and the curved extremities. 
Fig. 1 c. A similar fragment, showing the opposite side. 
Fig. 1 d. A small fragment which is less flattened, the axis more solid, and the teeth appearing 
shorter. 
Fig. 1 e & \ f. Enlargements from the previous figure. 
Fig. 1 g. A small fragment of the same species, showing some small nodes at the base of the 
teeth. 
Fig. 1 h. A portion of 1 g enlarged. 
Fig. 1 i. The back of the stipe enlarged, showing a slight groove. 
Position and locality. This species is very abundant in the upper green shale of the group 
at Sodus, Wayne county; also in the eastern part of Williamson, and in the banks of the 
Genesee river at Rochester. ( state Collection.) 
