An article I wrote for the April 2014 WCGMC News
The Rochester shale comprises the upper 85’-90’ of the Middle Silurian Clinton Group in upstate New York and southern Ontario. The upper two-thirds of the unit contain numerous grey limestone beds, which can be sufficiently resistant to form outcrops, but which are poor in fossil content. The lower 20’ of the Rochester shale is notoriously susceptible to erosion such that outcrop exposure is rare. Unfortunately, it is this rapidly weathering unit at the base that contains the abundant fossil assemblage (specifically trilobites) for which the formation is famous. The best visible exposure of the full Rochester shale section is in the gorge walls of High Falls on the Genesee River. However, this section is agonizingly unapproachable for fossil collection, particularly so the lower 10-20’ of section best known for fossil diversity and abundance.
Over 200 invertebrate fossil species have been identified from the Rochester shale including corals, brachiopods, bivalves, gastropods, cephalopods and crinoids. But, it is the spectacularly preserved trilobites that have attracted collectors to the Rochester shale since James Hall first detailed their occurrence in the 1840’s. The diverse fauna combined with the fine grained shale beds and thin limestone units indicate that the Rochester shale was deposited in warm, well oxygenated marine waters of intermediate depth. But where does one find outcrop to search for fossils?
How about the Erie Canal? From May until November, the Rochester shale is submerged along the banks of the Erie Canal while the canal serves as a commercial and tourist waterway. From December until February snow and ice typically cover any rock cropping out along its winding shorelines through Rochester after the New York State Canal Corporation drops the water level for the winter. That pretty much leaves March for fossil enthusiasts to brace the late winter weather to seek trilobite and brachiopod treasures in the exposures afforded by the man-made waterway.
And that is just what several members of the WCGMC did on March 22nd. With temperatures just a touch above freezing and cold NW winds blowing along the canal, Gary Thomas, Scott Jones, Jerry Donahue and Fred Haynes put on their woolies and tramped along the north side of the Canal to the Rochester shale outcrops just east of Long Pond Road. The search for Dalmanites and Trimerus trilobites was partly successful: both were found, but only as parts! Complete trilobites are, of course, rare due to the fact that trilobites are anthrapods and molt their exoskeletons. Thus, most parts are actually molts. Gary located a nice Trimerus pygidium and partial thorax, but no cephalon (head), similar to the one pictured in the photo collage on the next page. A few Dalmanites pygidiums were found also, but again the heads were not preserved. One such specimen I found is pictured below.
Several nice brachiopods were found, including a number of complete Strophemenids which are likely Coolina subplana. The Strophemenid Order of brachiopods are flat, exhibit very straight hinge lines and show strong radiating placations (ridges). They exhibit a bit of a silvery sheen (see photo on page 1). It is disappointing that this location disappears below canal level when the collecting conditions are a bit more tolerable.
Brett, C.E., et. al.,1994, Ordovician and Silurian Strata in the Genesee Valley Area Sequences, Cycles and Facies, in NYSGA Field Trip Guidebook for 66th Ann. Mtg., p. 381-442.
Grasso, T.X., and Liebe, R.M., 1994, Geology of the Erie Canal: Rochester Gorge and Eastern Monroe County, NY, in NYSGA Field Trip Guidebook for 66th Ann. Mtg., p. 129-220.
NYSGA, 1956, Guidebook for Field Trips in Western NY, 28th Annual NYSGA meeting (held in Rochester, NY, May 1956)
Want to read more: visit (http://research.amnh.org/paleontology/trilobite-website/featured-trilobite-locality/description-rochester-shale-locality) for an interesting discussion about a privately owned exposure of Rochester shale in Middleport, NY called Caleb’s Quarry where the Middle Silurian suite of trilobites and other invertebrates have been found.