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.
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