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Loc. 21, Alberta, Canada

Lat/Long (Decimal)49.098,-112.145
Co-ordinates Derivationstated in text
Given LocationAlberta, Canada
Mindat.org Region (for given coordinates)Alberta, Canada

Collections

CollectionReferenceStratigraphic NameCommentsLithologyAge
Loc. 21, Milk River [upper Pawkowki Fm]Russell L. S., Landes R. W. (1937)PawkowkiSTRATIGRAPHIC RELATIONS: From the Pawkowki Formation, which overlies the Early Campanian Milk River Formation, is equivalent to the Lea Park Fm, and is overlain by the Judith River Fm (Late Campanian). AGE: Early Campanian on the basis of ammonite (and other groups) biostratigraphy; Baculites obtusus biozone. Early Campanian according to Dawson et el. - Geological Atlas of the Western Canada Sedimentary Basin. STRATIGRAPHIC POSITION: From the upper Pakowki Fm."shale"83.5 - 70.6 Ma
Late/Upper Cretaceous

Recorded Fossils

Accepted NameHierarchyAge
Yoldia dowlingi
species
Animalia : Mollusca : Bivalvia : Nuculanida : Yoldiidae : Yoldia : Yoldia dowlingi83.5 - 70.6 Ma
Late/Upper Cretaceous
Nucula assiniboiensis
species
Animalia : Mollusca : Bivalvia : Nuculida : Nuculidae : Nucula : Nucula assiniboiensis83.5 - 70.6 Ma
Late/Upper Cretaceous
Pteria (Oxytoma) nebrascana
species
Animalia : Mollusca : Bivalvia : Pectinida : Oxytomidae : Oxytoma : Pteria (Oxytoma) nebrascana83.5 - 70.6 Ma
Late/Upper Cretaceous
Liopistha sp.
genus
Animalia : Mollusca : Bivalvia : Poromyidae : Liopistha83.5 - 70.6 Ma
Late/Upper Cretaceous
Periploma johnseni
species
Animalia : Mollusca : Bivalvia : Periplomatidae : Periploma : Periploma johnseni83.5 - 70.6 Ma
Late/Upper Cretaceous

References

Russell L. S., Landes R. W. (1937) Geology of the Southern Alberta Plains. Part II. Paleontology of the marine formations of the Montana Group, Geological Survey of Canada Memoir 221
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!
 
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