By Cindy Smith
The Pioche Formation of eastern Nevada is world famous for its amazing preservation of trilobites. Very old trilobites, from the Lower Cambrian (542 – 521 million years old), almost the oldest on record.
Stones ‘n Bones members got together to study and then identify seven species of Olenellus trilobites collected from the very boundary of their extinction event 521 million years ago. Due to a devastating change in the temperature and oxygenation of the ocean surface waters, the Olenellus sub-group died out, though other trilobites were able to adapt and survive.
Diana Biggs and Mary Chamberlain identifying Olenellus trilobites
Olenellids are considered a primitive trilobite with a thin exoskeleton, crescent-shaped eye ridges, and a variety of other anatomical features that provide diagnostic information, allowing us to identify them down to the species level. But it’s not easy because the preservation varies, as these features have been distorted by millions of years of pressure and movement. And because we don’t (yet) possess the uncanny ability that experienced paleontologists have developed to detect the nuanced details contained in the trilobite cephalon.
Though some of our trilobite specimens were complete, most were fragments, and we focused only on the cephalon (the head). To determine the species, we noted the shape and length of the glabella (the raised lobe on the cephalon), the length and robustness of the eye ridge, the length and location of the genal spine, and the distance from the anterior tip of the glabella to the anterior margin of the trilobite. This is the simplified version of identification. There are many more structures and measurements that go into the scientific distinction that leads to species identification.
An excellent website with good charts on trilobite anatomy is: https://amazingzoology.com/anatomy-of-trilobites/
We also studied hypostomes, the hard mouth part found on the underside of the trilobite. These diagnostic structures vary enormously in shape due, apparently, to the type of feeding behavior and prey devoured by the trilobite. Like our patella (kneecap), which is attached to our limb bones by tendons and ligaments, the hypostome is also unattached to the trilobite itself and can sometimes be found separately on pieces of slate.
Some of our trilobites were collected from Ruin Wash, a lagerstätte (area of extremely good preservation and extraordinary fossils). These fossils were collected on a 2018 WIPS (Western Interior Paleontological Society) field trip led by Joe Dabelko and John Foster (author of “Cambrian Ocean World”). Other sites included Oak Springs, Klondike Pass, and Comet Shale Mine, all in either the Lower or Middle Cambrian Period.
As I watched our group tackle the identification process, I was again struck by the joy of learning. In such busy lives that we all lead, we make the time to come together to share not only an appreciation for the intricacy of trilobite anatomy, but even more so to marvel at the meticulous research done by many before us who share our passion for an understanding of once-living creatures.