Also known as San Miguel Canyon
Where: San Miguel County, Colorado (38.0° N, 108.0° W: paleocoordinates 8.7° N, 32.9° W)
• coordinate estimated from map
• small collection-level geographic resolution
When: Cutler Formation, Wolfcampian (298.9 - 286.0 Ma)
• about 80-90 feet below top of Cutler Fm.
•" [...] the present [...] study [...] has convinced us that the age is Early Permian beyond all reasonable doubt, equivalent to that of the Moran, Putnam, and Admiral Formations of Texas." (Lewis & Vaughn, 1965 p. C41). According to that statement the collection is of Wolfcampian age.
• group of beds-level stratigraphic resolution
Environment/lithology: fluvial-lacustrine; fine, micaceous, red siliciclastic sediments and lenticular, gray conglomerate
•greenish gray in some places. [...] Crossbedding is common. Torrential deposition took place, as shown by lateral gradation, interlensing, and interbed
•ding between sandstone and conglomerate. No individual beds of conglomerate can be traced laterally for more than a few hundred feet. Finer grained micaceous sandstone, siltstone, and shale that weather to hematite red commonly contain bleached zones from 1 to 75 mm in diameter; these zones seemingly have organic centers. These finer clastics yielded almost all the fossil vertebrates; they contain many mud cracks and raindrop and other impressions including footprints." (Lewis & Vaughn, 1965 p. C5)
Size class: macrofossils
Reposited in the MCZ, USNM
Collection methods: bulk,
Primary reference: G. E. Lewis and P. P. Vaughn. 1965. Early Permian Vertebrates from the Cutler Formation of the Placerville Area, Colorado. United States Geological Survey Professional Papers 503-C:C1-C46 [J. Mueller/T. Liebrecht/T. Liebrecht]more details
Purpose of describing collection: taxonomic analysis
PaleoDB collection 85475: authorized by Johannes Mueller, entered by Torsten Liebrecht on 29.12.2008, edited by Bryan Gee
Creative Commons license: CC BY (attribution)
Taxonomic list
Osteichthyes | |
Cutleria wilmarthi n. gen. n. sp.
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Amphibia | |
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