Is member of Woodbine Formation following Norton (1965). Is tentatively assigned a late middle or early late Cenomanian (Late Cretaceous) age based on probable occurrence of ammonite EUCALYCOCERAS TEMPLETONENSE from J. P. Conlin collection from Dallas Co, TX in Ouachita tectonic belt province. Taxon ranges through the latest middle Cenomanian PLEISIACANTHOCERAS WYOMINGENSE zone and the earliest late Cenomanian DUNVEGANOCERAS PONDI zone.
Source: GNU records (USGS DDS-6; Denver GNULEX).
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