PRG-1-1010: Campanian, Canada
List of taxa
Where & when
Geology
Taphonomy & methods
Metadata & references
Taxonomic list
Polypodiopsida
- Salviniales
- Azollaceae
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Azollopsis coccoides megaspore
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Lycopodiopsida
- Isoetales
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Minerisporites borealis megaspore
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Rhynchonellata
- Terebratulida
- Terebrataliidae
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Thomsonia pogonites megaspore
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replaced by Coptothyris | |||||||
see common names |
Geography
Country: | Canada | State/province: | Alberta |
Coordinates: | 52.7° North, 116.0° West (view map) | ||
Paleocoordinates: | 60.8° North, 78.9° West | ||
Basis of coordinate: | stated in text | ||
Geographic resolution: | outcrop |
Time
Period: | Cretaceous | Epoch: | Late/Upper Cretaceous |
Stage: | Campanian | 10 m.y. bin: | Cretaceous 7 |
*Period: | Cretaceous - Cretaceous | *Epoch: | Late - Late |
*International age/stage: | Campanian - Campanian | ||
Key time interval: | Campanian | ||
Age range of interval: | 83.60000 - 72.10000 m.y. ago | ||
* legacy (obsolete) database fields |
Stratigraphy
Formation: | Brazeau | Local bed: | 1010 | ||
Local order: | bottom to top | ||||
Stratigraphic resolution: | formation | ||||
Stratigraphy comments: The top of the section is approximately 1000 ft above the mouth of Chungo Creek; the base is delineated by the Wapiabi-Brazeau Formation contact which is found just below Brown Creek. The two creeks are less than 3 miles apart and both flow into the north side of the Blackstone River.
PRG-1-1010 is from the section of the Brazeau Formation which is Belly River Equivalent. |
Lithology and environment
Primary lithology: | "shale" |
Lithology description: shale and silty shale | |
Environment: | terrestrial indet. |
Taphonomy
Modes of preservation: | original sporopollenin |
Size of fossils: | microfossils |
Collection methods and comments
Collection methods: | surface (in situ),chemical,sieve,field collection | ||
Minimum sieve size: | 0.074 | Maximum sieve size: | 1.000 |
Reason for describing collection: | paleoecologic analysis | ||
Collection method comments: Method involved boiling 500-800 grams of rock in aqueous solution of Quaternary-O until dissolved, washing sediment through 4 screens (1000, 297, 125, 74 microns), and some additional treatment in hydrochloric and hydroflouric acids was used to remove carbonate and silicate minerals. The highly carbonized samples were oxidized with Schultze's solution and 10% potassium carbonate to lighten the spore color. The slides are now stored in the palynological collection of the Department of Geology, the University of Calgary. |
Metadata
Also known as: | Sub-Section PRG-1, Sample #1010, Alberta (Brazeau Formation) | ||
Database number: | 32997 | ||
Authorizer: | R. Lupia | Enterer: | T. Naeher |
Modifier: | T. Naeher | Research group: | paleobotany |
Created: | 2003-07-22 10:50:32 | Last modified: | 2003-07-22 14:56:34 |
Access level: | the public | Released: | 2003-07-22 10:50:32 |
Creative Commons license: | CC BY |
Reference information
Primary reference:
8836. | P. R. Gunther and L. V. Hills. 1972. Megaspores and other palynomorphs of the Brazeau Formation (Upper Cretaceous), Nordegg Area, Alberta. Geoscience and Man 4:29-48 [R. Lupia/T. Naeher/T. Naeher] |