Cambrian Fossils in the Bright Angel Shale

of Northern Arizona

Trilobite Pygidiums Fossils Section

SH Locality near Ashfork, Az.

  The primary trilobite at the SH Locality is Zacanthoides Walapai. Pygidiums here are internal or external molds in a green glauconitic shale.
Updated 7/23/17

The most common fossil found in the green shales at our SH locality are trilobite pygidiums for the Zacanthoides Walapai species. They are joined by assorted cranidiums, thorax and rib segments, and hordes of hyolithids, and a very rare coralomorph. Generally low diversity such as this site suggests has been attributed to a stressed enviorment, with perhaps low food sources, agressive wave action, or an influx of fresh water from the nearby deltas. This was a shallow sea outbound from the deposits known as the Tapeats Sandstone which marked shore, delta and beach deposits. Combined with the deeper water Muav Limestone, this trio of formations is known as the Tonto Group. All three can be found outside the Grand Canyon to the south in small limited areas such as here, yeilding an opportunity to explore the paleo fauna without hiking miles and thousands of feet into the Grand Canyon.


Collecting at the SH Locality!
The greenish shales are in thin beds, with a reddish
surface weathering.
Key Pygidum Diagram:
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Component Key to pygidium features for Zacanthoides Walapai.  
Most pygidiums are 1/4 - 1/2 inches in size, and the state of
preservation varies.
Pygdium Images - Web cam close ups:
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Microscope Images - 10x:
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