
from the August 4, 2008 Newsletter,
issued from near Natchez, Mississippi: Since the topmost gravel around Natchez was deposited during the Pleistocene only about 700,000 years ago, or 0.7 million years, Karen's trilobite, which couldn't have been fossilized less than 250 million years old, wasn't fossilized in place here. The pebble carrying the trilobite inside was transported to here as part of an enormous amount of gravel deposited here by meltwater from the retreating glacier in the north. To get a name for Karen's trilobite I went to the nifty Fossil Forum at http://www.thefossilforum.com. This public forum for fossil fanciers includes a section on "Fossil ID." I registered for free, uploaded the picture linked to above, and before the day was over two experts had told me what they thought. Solius in the central US wrote, "The pygidium looks like it could be a proetid, but it appears to have glabellar, and occipital lobes like a Ceraurus... It is a nice one, and probably fairly rare." The genus Ceraurus occurred mostly during the Orodovician age (±488.3 to ±443.7 mya) and is most commonly found in strata outcropping in the lower Great Lakes region. That fact meshes nicely with what's said on my "Gravel Below the Loess" page at http://www.backyardnature.net/loess/citronel.htm:
Beautiful how it all comes together... |