Mohawk Valley Fossils
Isotelus
The figure below shows the distribution of samples containing the trilobite Isotelus. Learn more about Isotelus
Isotelus is a common trilobite in some parts of the MRV strata.
Figure modified from Sloan, North American Ordovician
Trilobites.
More images of Isotelus can be found here and here.
- Isotelus DeKay, 1824 [*I. gigas ]
-
Cephalon and pygidium mostly with poorly defined
flattened border. Frontal area moderately long, cephalic
axis ill-defined, almost obsolete in several species,
slightly expanding in front of medium-size eyes situated
somewhat behind transverse mid-line of cranidium; no
posterior border furrow; genal angles rounded, pointed,
or with short genal spines. Hypostoma almost
parallel-sided, posterior margin with broad, deep notch;
anterior lobe short. Thoracic axis considerably broader
than pleurae. Pygidial axis broad, poorly defined, almost
obsolete in several species; pleural fields smooth or
very faintly ribbed.
M. Ord. - U. Ord., North America, Siberia, Northern Europe, Greenland
- Family Asaphidae Burmeister, 1843
-
Librigenae separated anteriorly by a median suture;
glabella well defined to obsolete, considerably longer
than frontal area; lateral glabellar furrows mostly weak
or absent; most genera with distinct glabellar tubercle;
eyes generally somewhat distant from axial furrows;
faint, almost obsolete eye ridges known only in 2 genera.
Doublure commonly broad; posterior margin of hypostoma
varying from pointed to deeply notched. Thorax of 8
segments; pleural furrows generally diagonal, if present.
Panderian organs developed as notches or separate
openings, but absent in some (Ogygiocaridinae,
Symphysurininae). External margin of pygidium varying
from rounded to pointed, in some genera with terminal
spine; paired pygidial spines present only in single
genus of uncertain affinities. Dorsal surface of carapace
with small pits, terrace lines, or both; no tuberculate
or granulose ornamentation. Family tends toward loss of
apparent segmentation of cephalon and pygidium,
obsolescence of axial furrows, and deep notching of
posterior margin of hypostoma.
U. Cam. - U. Ord.
Order Ptychopariida Swinnerton, 1915
NOTE: The classification of trilobites has undergone several revisions since the 1959 publication of Volume O of the Treatise. The classification presented here only represents a starting point for the search for further information.
Treatise on Invertebrate Paleontology, O339