|
|
Oklahoma
is remarkable in terms of its representation of formations
spanning much of geological history. The Paleozoic is also
well-represented, and some of the most spectacular trilobites
that originate from within the boundaries of the United
States come from Lower Devonian formations in Coal County,
Oklahoma, located near the tip of the white arrow on the
map (click the map to enlarge). This map to the left correlates
location and age of the
Oklohoma geology. The nearest townto the Haragan and Bois
d' Arc formations is Clarita, which amounts to little more
than a few humble residences and a post office. Three commercial
quarries operate and supply a steady, if sometimes minimal
supply of 19 different trilobite species. Two primary formations
are the Haragan and Bois d' Arc, with soft limestone that
yields with proper equipment and skilled operator beautiful
honey-colored trilobites of a shade and quality resembling
those from the Saint
Petersburg region of Russia, except in greatly less
quantity.
Interestingly,
the Devonian trilobites of Oklahoma have look-a-likes found
in the Atlas Mountains of Morocco. While on distantly continents
and separated by thousands of miles today, such was not the
case during Devonian-time. During the Devonian, present-day
Morocco was part of the Eastern continental shelf of Gondwana,
and present-day Oklahoma was part of the Southern continental
shelf of Euramerica. These locations were adjacent and at
essentially equal latitudes and therefore probably had nearly
identical environments. Thus, each of the comparable species
undoubtedly shares a close common ancestry and are classified
in the same trilobite genera. The Table below lists the species
found in Devonian of Oklahoma, as well as information on classification
and relative frequency that the species are found.
Mr.
Robert Carroll has operated one of the commercial quarries
in the area for nearly two decades. Actually, he works several
quarries that have exposures of both the Haragan and Bois
d' Arc Formations. I have hunted in these quarries, and the
process is markedly different from hunting the Great Basin
in the Western U.S. While surface hunting is possible for
trilobites weathering out of matrix, if your goal is an exquisite
specimen, you'll have to do a lock of rock splitting. The
trilobites are discovered by their very thin cross sections,
which requires breaking the rock through the exposkeleton
to expose; hence, the trilobite will already be in two or
more pieces prior to beginning the laborious preparation process.
Expert eyes like Bob's are usually required to ID the species
and to estimate whether it is possible that the matrix may
contain a complete specimen. Most are not complete. If it
can not be determined that it is incomplete, the next step
is to take it back to the prep lab and rough it out with a
pneumatic chisel. The complete specimen is the exception,
which is than finished using air abrasive tools. The trilobites
that come from Bob's lab are exquisite
in every respect, each represent many tedious hours of preparation.
The good news is that the limestone matrix melts away under
AlO2 grit at 100 psi pressure, yielding a life-like, three
dimensional specimen that is a darker brown than the matrix.
The picture below shows Bob setting by his circa 1953 White
air abrasion machine. As old as it is, it is meticulously
maintained. Bob's preparation is a source a professional pride,
and examples of his work can, for example, be found in Riccardo
Levi-Setti's book, Trilobites.
The
Table below lists the 19 species found to occur in the Devonian,
Haragan and Bois d' Arc Formations, and I thank Bob Carroll
for providing this information; links are also provided where
you will find pictures for many of the species. Some of these
are exceedingly rare and no complete specimens have been found.
Cysphaspis carrolli, a diminuative Aulocopleurid, is named
for Bob Carroll. Bob is also credited for the discovery of
a rare petite lichid which is still undescribed, and which
Bob has affectionately named Bug X. As previously mentioned,
Morroco and Oklahoma were proximal during Devonian time, such
that some trilobite genera are common to both Coal County
and the Morocan Atlas Mountains. The Oklohoma species tend
to be smaller and, I believe, more elegant. A perfect example
is the highly sought Odontopleurid, Dicranurus. The Morrocan
species is named Monstrosus, and the Oklahoma species Elegantus
- it appears that the names pretty much tell it all.
| Devonian
trilobites of Oklahoma |
| Family |
Name |
Classification |
Occurence |
Possible
Moroccan Counterpart |
| Aulocopleurid |
Cysphaspis
carrolli |
Order:
Proetida;
Suborder: Proetina;
Superfamily: Aulacopleuroidea; Family Aulacopleuridae
|
Scarce |
na |
| Harpidella
sp. |
Rare |
na |
| Otarion
axitiosum |
Haragan,
fragments only |
Otarion
sp. |
| Brachymetopid |
Cordania
falcata |
Order:
Proetida;
Suborder: Proetina;
Superfamily: Aulacopleuroidea; Family Brachymetopidae
|
Haragan,
Scarce |
na |
| Cordania
wessmani |
Bois
d' Arc, Rare |
na |
| Dalmanatid |
Huntonia
oklahomae |
Order:
Phacopida; Suborder Phacopina;
Superfamily: Dalmanitoidea; Family: Dalmanitidae
|
Haragan,
Scarce |
Odontochile
sp. |
| Huntonia
huntonensis |
Bois
d' Arc, Scarce |
na |
| Huntonia
lingulifer |
Haragan,
Rare |
na |
| Odontochile
syncrama |
. |
Extremely
rare |
na |
| |
Bug
X - Lichid sp. |
. |
Haragan
& Bois d' Arc, Extremely rare |
na |
| Echinolichas
coccymelum |
. |
Haragan
& Bois d' Arc, fragments only |
na |
| Echinolichas
bigsbyi |
. |
Haragan
& Bois d' Arc, fragments only |
na |
| Odontopleurid |
Kettneraspis
williamsi |
Order:
Lichida; Suborder: Lichina; Superfamily: Odontopleurida;
Family: Odontopleuridae
|
Haragan,
Fairly common |
Leonaspis
sp. |
| Ceratonurus |
. |
Haragan,
Rare |
Ceratonurus
sp |
| Dicranurus
elegantus |
Order:
Lichida; Suborder: Lichina; Superfamily: Odontopleurida;
Family: Selenopeltidae
|
Haragan,
Rare |
Dicranurus
monstosus |
| Phacopid |
Paciphacops
campbelli |
Order:
Phacopida; Suborder: Phacopina; Superfamily: Phacopoidea;
Family: Phacopidae;
|
Haragan
& Bois d' Arc, Common |
na |
| Reedops
deckeri |
Haragan,
Fairly common |
Reedops
maurulus |
| Viaphacops
sp. |
Bois
d' Arc, Scarce |
Phacops
sp. |
| Thysanopeltid |
Scutelid
sp. |
. |
Haragan,
Extremely rare |
Scutellum
sp. |
|
|