Where: Yukon, Canada (64.7° N, 132.0° W: paleocoordinates 1.7° N, 64.8° W)
• coordinate based on political unit
• outcrop-level geographic resolution
When: Rabbitkettle Formation, Menevian (504.5 - 499.5 Ma)
• The formation at section """"N"""" of Pratt (1992) is over 400m thick, but only the lower 200 m are of interest. No sedimentological differences can be discerned through the upper Marjuman - lower Steptoean interval.
• formation-level stratigraphic resolution
Environment/lithology: deep subtidal ramp; lithified, argillaceous, calcareous sandstone and lithified siltstone
Size class: macrofossils
Collection methods: surface (in situ),
• The collection contains fossils from the upper Marjuman. The stage boundary between the Marjuman and Steptoean seperates two biomeres and is one of the global mass extinction events.
Primary reference: B. R. Pratt. 1998. Probable predation on Upper Cambrian trilobites and its relevance for the extinction of soft-bodied Burgess Shale-type animals. Lethaia 31:73-88 [M. Patzkowsky/P. Borkow]more details
Purpose of describing collection: taxonomic analysis
PaleoDB collection 9874: authorized by Mark Patzkowsky, entered by Phil Borkow on 25.01.2001
Creative Commons license: CC BY (attribution)
Taxonomic list
unclassified | |
Lingulata | |
Lingulata indet. Gorjansky and Popov 1985 | |
Trilobita | |
"Cedaria minor" = Asaphiscus minor
"Cedaria minor" = Asaphiscus minor Walcott 1916 trilobite | |
Crepicephalus norrisicanus, Crepicephalus columbiensis, Crepicephalus snowyensis, Crepicephalus rabbitkettlei
Crepicephalus norrisicanus trilobite
Crepicephalus columbiensis trilobite
Crepicephalus snowyensis trilobite
Crepicephalus rabbitkettlei trilobite | |
Modocia dubia trilobite | |
Tricrepicephalus texanus trilobite | |
Blountia beltensis trilobite | |
Llanoaspis modesta trilobite | |
Cedaria selwyni Pratt 1992 trilobite | |
Artiopoda | |