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Wagner Quarry Cystoid Bed, Goodhue County, Minnesota, USA
| Lat/Long (Decimal) | 44.5,-92.9 |
|---|---|
| Co-ordinates Derivation | not explained |
| Given Location | Minnesota, United States |
| Mindat.org Region (for given coordinates) | Goodhue County, Minnesota, USA |
Collections
| Collection | Reference | Stratigraphic Name | Comments | Lithology | Age |
|---|---|---|---|---|---|
| near Cannon Falls, Phylloporina Beds | Bassler R. S. (1911) | Decorah Shale | "Phylloporina Beds of the Black River (Decorah) Shale Formation", in Bassler (1911) | "shale" | 457.5 - 452.5 Ma Late/Upper Ordovician |
| Cannon Falls, Clitambonites Beds | Bassler R. S. (1911) | Prosser | "Clitambonites Bed of Lower Trenton Limestone",in Bassler (1911) | "limestone" | 460.9 - 449.5 Ma Ordovician |
| Cannon Falls, Lower Trenton Shales | Bassler R. S. (1911) | "Lower Trenton Shales", in Bassler (1911) | "shale" | 460.9 - 449.5 Ma Ordovician | |
| Cannon Falls, Nematopora Bed | Bassler R. S. (1911) | Prosser | "Nematopora Bed of Trenton Limestone",in Bassler (1911) | "limestone" | 460.9 - 449.5 Ma Ordovician |
| Clitambonites Beds, near Cannon Falls | Wahlman G.P. (1992) | Prosser | "Clitambonites Bed of Lower Trenton Limestone",in Bassler (1911) | "limestone" | 460.9 - 449.5 Ma Ordovician |
| Wagner Quarry Cystoid Bed, Goodhue County, MN | Sloan R. E., DesAutels D. A. (1987) | Cummingsville | "[T]he lower part of the type Prosser Limestone, the equivalent of the Rivoli Member of the Illinois and Iowa classification, has greatly increased in mud content and must be classed as part of the Cummingsville Formation here." | "limestone" | 460.9 - 449.5 Ma Ordovician |
| Cannon Falls | Stauffer C. R. (1937) | Shakopee | AGE: Cassinian; refined by A. Hendy (6/2009) on the basis of biostratigraphic data. | "limestone" | 478.6 - 468.1 Ma Ordovician |
Recorded Fossils
References
Data courtesy of: PBDB: The Paleobiology Database, Creative Commons CC-BY licenced. , GBIF: the Global Biodiversity Information Facility, various licences, iDigBio, various licences, and EOL: The Encyclopedia of Life (Open Data Public Domain). Because fossils are made of minerals too!
