Image from the Biodiversity Heritage Library.
Contributed by Yale Peabody Museum of Natural History.
| www.biodiversitylibrary.org
Transcription
start 3066 end
brier fauna. These shales maybe 10 feet thick
followed by mac shales interbedded with red shales.
for fully 60 foot more before the Potterville
comes in. Therefore the brieferina is here in the
low Mancul Chert. It abounds in genuine
Chester fossils as Lemnula cutguadata, Spirifera
leidgi, Productus chesterensis etc.
In the brieferina zone are also red beds
abounding in bivalves of many species and Ostr-
acodidea. Therefore these red-beds are marine
but those below and above identical in color have
no fossils. It seems to me that much if not
all of the Mancul Chert is here marine. It
is a cycle of deposition like the marine ones
of the Pennsylvanian beginning with marine deposits
and ending in a filled sea and continental deposits.
At the eastern end of this cut about one
mile west of Briclion may be seen a fine example
of marked unconformity of the Lower Potte-
sville on the Mancul Chert. The sketch of it
is on the next page and a photo (Film 1-12).