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A Hot Day for Virginia Trilobites
by Marc Behrendt
Previously published
1-2006 Fossil News Magazine
All summer I’d
put off going on local collecting trips, primarily because the Ohio
temperatures were in the high 90’s nearly every miserable day. My Nevada
trip plans fell through as several events dissolved any opportunities to
return to last year’s exciting sites. Finally as summer was ending, I still
had not gone out once! A call to my trusted partner Ron Rea quickly set up
what we’d hoped would make up for lost time - a 4 day trip in the eastern
US. Another set of phone calls gave us access to a private dig site in
Virginia. On the way home we’d examine the myriad of roadcuts that border
the roads from Virginia all the way into Tennessee.
Ron bravely
drove his truck on this journey. Our history of flat tires and vehicle
trouble is one that is hard to forget. Forecasted temperatures were for
upper 90’s both in Ohio and Virginia. Humidity was so high that we could
barely see the forested green Appalachian Mountains. Arriving in Roanoke,
Virginia after a 6 hour drive, we secured 2 motel rooms and traveled to the
landowner’s home to finalize our permission and plans. Mrs. C has lived on
this property her whole life and truly cherishes her personal trilobite
exposure. As always, she loves to talk about the site and the things she’s
found.
The next morning Ron drove the truck through the front
gate and along the path as I walked ahead, opening and closing gates. After
passing through the gauntlet of gates and reluctant groups of bovine we
arrived at the shale outcrop, a small exposure in the middle of a cow
pasture (complete with cows.) Dense fog hovered just above the ground
creating a surreal view of the valley.
We are
collecting in the lower Middle Ordovician Liberty Hall Shale, the upper
portion of the Edinburg Formation. Fossils are uncommon except in widely
scattered pockets. This particular exposure is a lagerstaaten of remarkable
preservation. The site is only about 10 X 10 meters; however the density
and quality of specimens yield a large number of complete trilobites
including Ampyxina powelli, and rarely Edmundsonia typa, Dionide holdoni, and
Porterfieldia caecigenus. Fragments of Robergia and the cheiurid
Calliops have been found. Also found are huge numbers of graptolites
and less commonly brachiopods, tiny gastropods, cephalopods, and trace
fossils. Many other species of trilobites have been recorded from the
Liberty Hall Shale, however this particular site does not have the species
diversity that is known from other localities.
The shale lies
at roughly a 45 degree angle. Since cows are actively wandering around as
we work, extreme caution had to be maintained to insure no hole was big
enough to harm the animals should they stumble in. So unlike a typical dig
where we would clean off a nice exposure and work a bench deep into the
ground, here we kept the holes small and simple. Fractures and partings run
throughout the shale, so it was just a matter of exposing the shale and
pulling out the chunk. Then we split it as completely as possible.
The rock
alternates from nicely laminated shale to nodular mudstone to a nasty storm
hash layer. The Ampyxina seem to predominate in the clean shale
while the Dionide are associated with the mudstone. Graptolites
appear at every level and layer. At the edge of the exposure in finely
laminated shale rare Porterfieldia, a Triathrus-like
trilobite, were found mixed in with a plethora of graptolites, but
associated with no other trilobites.
Ron and I
immediately began finding Ampyxina. They are small, most measuring 10
mm or less. A complete juvenile possesses a long “nose” spine; the adults
do not have the anterior spine. A typical specimen has very thin shell,
presenting itself as a positive/negative cast. The trick was to find a
complete one with good, thick shell that was not fragmented between the
positive and negative. The lace-collar trilobites – the Dionide and
Edmundsonia - tended to have sturdier shells and split out much
nicer. Some of the Dionide were tiny, however I found a couple that
measured 25 mm. The Edmundsonia often possessed long genal spines.
By 9 am the sun burned through the fog and quickly heated the countryside.
Thistle was in full bloom and hundreds of butterflies flew from flower to
flower, keeping the meadow in constant motion. Looking out, I could see
the long parallel mountains on my right and left, the lush emerald valley of
farms and woodlands extended in between. After a couple hours of kneeling
and bending over the shale, a stroll through the meadow offered a pleasant
break for both the mind and body. By the end of the day I took over 100
digital pictures of butterflies and flowers, trying to capture that
indescribable feeling of peace within the meadow.
The intense sunshine through the haze created increasingly uncomfortable
conditions. The thermometer on the truck read 98 degrees. We set up a
canopy to afford us a little bit of shade. The cows migrated to a nearby
stand of pine trees. And suddenly we had several large insects loudly
buzzing just past our ears. At first I thought they were cicada killers, a
large type of hornet. After 5 minutes of cringing and trying to avoid these
creatures, I spotted one that crash-landed in the pasture. I crept up to it
and to my amazement, it was a huge, metallic green beetle! It was digging
into the soil and quickly buried itself.
I
have collected this site previously, and the one bug I really wanted to find
that I have had absolutely no success was a complete Porterfieldia.
Up to this moment, I’d yet to find even a fragment. Literature indicates I
should find Porterfieldia as well as some other unusual species.
Early in the
afternoon 3 children came through the pasture to visit us and to see what we
had found. They knew all about the trilobites at this spot, and after
introductions they began to pick around on the surface. The youngest of the
children was a girl about 4 years old, the others being about 7 and 12. One
at a time the two oldest children brought fossils they found, usually
graptolites or fragments of weathered Ampyxina. Ron and I enjoyed
the kids and their enthusiasm, though we wearied looking at their fossils
over and over and over again. Then for the first time the youngest came to
me and said “Look at my fossil.”
I reached for
it and after my eyes rejoined my head, I said “How would you like to trade
this fossil for a really nice pretty one,” and I offered her a very nice
Ampyxina. Ron spoke up from the shaded canopy, “Young lady, I’m not sure
what you gave him, but you better ask him for two trilobites in trade!”
Yep, that little girl laid into my hand a negative to a complete
Porterfieldia! I asked her to think very carefully to remember where
she found this fossil. She walked around thinking it was here, then there,
then another place, and finally she settled on a spot on the fringe of the
shale exposure.
Not wasting
time, I moved over to that area and began to poke around, immediately
finding 2 partials! After working through the top, weathered shale, I found
a solid chunk of shale and pulled it out. It was solid and did not want to
split, in spite of the obvious multiple laminations. Using a tiny chisel, I
split the chunk. The negative showed 2 complete Porterfieldia! I
picked up the positive and wanted to cry – the chisel went through both
bugs.
I worked the
shale from this spot for more than an hour with nothing to show but several
partial Porterfieldia and thousands of graptolites. Finally I split
out the right piece of black shale and out popped a perfect, white
Porterfieldia! By the time the little girl left to go home, she had all
sorts of fossil rewards to add to her collection!
By 6 pm, Ron
and I both had filled all the flats we brought on the trip to store
specimens. We filled 5 gallon buckets with shale chunks that would split
further after weathering. The heat and humidity was overwhelming. We
wanted to return the next day, however we had to think about how much room
was remaining in the truck, as well as whether we wanted to deal with the
weather, which was predicted to be the same or even more oppressive.
Under a reluctant but agreeable consensus, we decided to quit and head home
the next morning. We made sure the shallow holes we created were completely
filled in. The cows came out from the trees as we policed the area as if
checking our work. Then we eased our way back down the path to the main
road.
Mrs. C was anxious to hear how we did. She spoke again of many of her
excellent finds, most having been recently donated to a local university. I
can think of no finer landowner who heartily appreciates and understands the
significance of the exposed rock on their property. We thanked her again
for her wonderful hospitality and then headed for our motel. The air
conditioners barely worked, but we were so hot that any coolness seemed like
Heaven.
On
our journey home we drove the backroads looking for roadcuts, however the
State of Virginia made a concerted effort to plant crown vetch to hide those
unsightly rock exposures. Perhaps during the winter months the roadcuts can
be collected, but not during summer. We finally gave up and drove home on
the interstate. The temperature hovered around 100 all the way home. But
there is nothing like a terrific rare find to make a long hot trip home
tolerable.
References:
Cooper, Bryon N., Trilobites from the
Lower Champlainian Formations of the Appalachian Valley 1953, Geological
Society of America memoir 55, 69 pages, 19 plates.
Moore, Raymond C., Treatise on Invertebrate Paleontology – Part O,
1959, Geological Society of America, 560 pages.

Collecting the layers The exposure in a
cow pasture

Up close view of the shale exposure

Double Ampyxina powelli
Porterfieldis caecigenus

Dionide holdoni
Unidentified graptolites

Unidentified trilobite
Calliops sp.

Pipevine swallowtail feeding on
thistle in cow pasture

Trilobite collecting can be very
relaxing -
if approached correctly....
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