US58, Ravenscrag Butte flora: Paleocene, Canada
List of taxa
Where & when
Geology
Taphonomy & methods
Metadata & references
Taxonomic list
unclassified
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Equisetum fluviatoides leaf, root
McIver and Basinger 1989
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Spirodela scutata leaf, root
Dawson
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Trochodendroides speciosa leaf
Berry 1930
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Nyssidium arcticum seed/fruit
Iljinskaja 1974
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Platanites canadensis leaf
McIver and Basinger 1993
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Angiospermae
- Saxifragales
- Cercidiphyllaceae
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cf. Cercidiphyllum sp. seed/fruit
Siebold and Zuccarini 1846
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cf. Cercidiphyllum sp. flower
Siebold and Zuccarini 1846
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staminate inflorescences | ||||||||||
Archeampelos acerifolia leaf
(Newberry 1868)
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Archeampelos acerifolia comb. nov. | ||||||||||
Angiospermae
- Cornales
- Cornaceae
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Cornophyllum newberryi leaf
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Cornophyllum newberryi comb. nov. | ||||||||||
Angiospermae
- Dipsacales
- Caprifoliaceae
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Viburnum sp. seed/fruit
Linnaeus 1753
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fruits | ||||||||||
Angiospermae
- Proteales
- Platanaceae
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cf. Platanus sp. non-seed repro
Linnaeus 1753
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reproductive organs | ||||||||||
Angiospermae
- Araceae
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Pistia corrugata leaf, root
Lesquereux 1874
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Angiospermae
- Magnoliales
- Myristicaceae
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cf. Myristica catahoulensis seed/fruit
Berry 1924
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Angiospermae
- Rosales
- Rhamnaceae
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Rhamnites n. gen. cleburnii leaf
McIver and Basinger 1993
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Rhamnites cleburnii comb. nov. | ||||||||||
Angiospermae
- Nymphaeales
- Nymphaeaceae
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Paranymphaea crassifolia leaf
Newberry 1935
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Magnoliopsida
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Dicotylophyllum anomalum leaf
(Ward 1887)
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Trapago angulata leaf
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Trapago angulata comb. nov. | ||||||||||
see common names |
Geography
Country: | Canada | State/province: | Saskatchewan | County: | Eastend |
Coordinates: | 49.5° North, 109.0° West (view map) | ||||
Paleocoordinates: | 55.6° North, 85.6° West | ||||
Basis of coordinate: | stated in text |
Time
Period: | Paleogene | Epoch: | Paleocene |
10 m.y. bin: | Cenozoic 1 | ||
Key time interval: | Paleocene | ||
Age range of interval: | 66 - 56 m.y. ago |
Stratigraphy
Formation: | Ravenscrag | Local bed: | US58 | ||
Local order: | no particular order | ||||
Stratigraphy comments: The stratigraphic position of the collection is given relative to the No. 1 coal zone, which is approximately at the base of the formation. US58 is located 10 m above the No. 1 coal zone, west of US5 (west face). |
Lithology and environment
Primary lithology: | sandstone |
Includes fossils? | Y |
Lithology description: The Ravenscrag Formation consists of interbedded, nonmarine clays, silts, sands, and lignite. The measured section at the Ravenscrag Butte site is about 67 m thick, and lithologically, the formation in divided into two facies; the lower 38 metres comprises the grey facies, the upper 29 metres, the buff facies. At a distance, the two facies are easily distinguishable on the basis of colour. Commonly, the buff facies are less than 31 m thick in measured sections due to erosion or cover at the top. There are four conspicuous beds of coal or coaly shale in the sections at Ravenscrag Butte, including the No. 1 coal zone. The fourth coal zone marks the transition from grey to buff facies. Locality 58 is composed of buff clays and sands. | |
Environment: | terrestrial indet. |
Geology comments: During the early Tertiary, most of southern Saskatchewan was a broad alluvial plain dominated by meandering river systems. Locally, at the Ravenscrag Butte site, small lakes or ponds, sluggish streams, swamps and lowland forests successively dominated the area over a period of perhaps 2 million years. |
Taphonomy
Modes of preservation: | adpression |
Size of fossils: | macrofossils |
Collection methods and comments
Collection methods: | salvage,surface (in situ),field collection |
Reason for describing collection: | paleoecologic analysis |
Metadata
Database number: | 34421 | ||
Authorizer: | R. Lupia | Enterer: | B. Wilborn |
Modifier: | B. Wilborn | Research group: | paleobotany |
Created: | 2003-08-31 16:01:58 | Last modified: | 2003-09-01 13:20:47 |
Access level: | the public | Released: | 2003-08-31 16:01:58 |
Creative Commons license: | CC BY |
Reference information
Primary reference:
8995. | E. E. McIver and J. F. Basinger. 1993. Flora of the Ravenscrag Formation (Paleocene), Southwestern Saskatchewan, Canada. Palaeontographica Canadiana 10:1-85 [R. Lupia/B. Wilborn/B. Wilborn] |