Where: Sublette County, Wyoming (43.3° N, 109.8° W)
• Paleocoordinates: 34.0° N, 114.6° W (Wright 2013)
• local area-level geographic resolution
When: Middle Cedaria trilobite zone, DuNoir Formation, Dresbachian (497.0 - 486.9 Ma)
• The Open Door Formation underlies the Ordovician Bighorn dolomite Formation. 95.5 feet below top of DuNoir limestone. Was "Cedaria (Middle Cedaria subzone)".
• bed-level stratigraphic resolution
Environment/lithology: shallow subtidal; lithified, green limestone
Size class: macrofossils
Collection methods: Collected from 1938 to 1941 by the Texas Christian University Geology Department
Primary reference: C. Lochman and C. H. Hu. 1960. Upper Cambrian faunas from the northwest Wind River Mountains, Wyoming. Part 1. Journal of Paleontology 34(5):793-834 [M. Patzkowsky/P. Borkow/J. Alroy]more details
Purpose of describing collection: taxonomic analysis
PaleoDB collection 9055: authorized by Mark Patzkowsky, entered by Phil Borkow on 19.09.2000
Creative Commons license: CC0 (CC0)
Taxonomic list
unclassified | |
Paterinata | |
Lingulata | |
Trilobita | |
"Holcacephalus tenerus" = Hardyoides tenerus
"Holcacephalus tenerus" = Hardyoides tenerus Walcott 1916 trilobite | |
Crinoidea | |
|