| 词条 | Frenchman Formation | |||||||||||||||||||||||
| 释义 |
| name = Frenchman Formation | image = | caption = | type = Geological formation | age = {{fossil range|Maastrichtian|Maastrichtian|Upper Cretaceous}} | period = Maastrichtian | prilithology = Sandstone | otherlithology = Claystone, conglomerate | namedfor = Frenchman River | namedby = Furnival, 1942 | region = Western Canada Sedimentary Basin | country = {{flag|Canada}} | coordinates = {{coord|49.49073|-108.90467|name=Frenchman Formation|display=inline,title}} | unitof = | subunits = | underlies = Ravenscrag Formation | overlies = Battle Formation, Whitemud Formation, Eastend Formation, Bearpaw Formation | thickness = up to {{convert|113|m|ft|sp=us}}[1] | extent = | area = | map = | map_caption = }} The Frenchman Formation is stratigraphic unit of Late Cretaceous (late Maastrichtian) age in the Western Canada Sedimentary Basin. It is present in southern Saskatchewan and the Cypress Hills of southeastern Alberta. The formation was defined by G.M. Furnival in 1942[1] from observations of outcrops along the Frenchman River, between Ravenscrag and Highway 37. It contains the youngest of dinosaur genera, much like the Hell Creek Formation in the United States. LithologyThe Frenchman Formation consists of olive-green to brown, fine- to coarse-grained, cross-bedded sandstone with interbedded claystone bands and minor beds and lenses of intraformational clay-clast conglomerate.[2] A conglomerate layer with well-rounded quartzite pebbles is present above the basal unconformity in some areas.[3] Thickness and distributionThe Frenchman Formation is present in southwestern Saskatchewan and the Cypress Hills area of southeastern Alberta. Its maximum reported thickness is about 113 m.[3] AgeThe Frenchman Formation is of latest Maastrichtian age, and the top of the formation coincides with the Cretaceous-Paleogene boundary, as evidenced by biostratigraphic changes and, in some areas, the presence of the terminal Cretaceous iridium anomaly.[4] Relationship to other unitsAlthough some early workers included the Frenchman Formation in the overlying Ravenscrag Formation, the two are separated by the Cretaceous-Paleogene boundary and are now treated separately. The contact is abrupt but conformable, and occurs at the base of the No. 1 or Ferris coal seam of the Ravenscrag Formation.[3] The Frenchman is separated from the underlying formations by an erosional unconformity, and depending on the depth of the erosion, the Frenchman rests on the Whitemud Formation, the Battle Formation, the Eastend Formation, or the Bearpaw Formation.[3] It is equivalent in age to the lower part of the Scollard Formation, the lower part of the Willow Creek Formation, and the lower part of the Coalspur Formation in Alberta, and the Hell Creek Formation in Montana and North Dakota. Paleontology
See also{{Portal|Earth sciences|Paleontology|Dinosaurs||}}
References1. ^Furnival, G.M., 1942. Preliminary Map, Cypress Lake, Saskatchewan; Geological Survey of Canada, Paper 42-5, contains Preliminary Map 42-5, Cypress Lake, West of Third Meridian, Saskatchewan, Scale: 1 inch to 2 miles. {{WCSB|Saskatchewan=yes}}2. ^1 {{Cite web|url=http://cgkn1.cgkn.net/weblex/weblex_litho_detail_e.pl?00053:005334|title=Frenchman Formation|author=Lexicon of Canadian Geological Units|accessdate=2010-01-17}} 3. ^1 2 3 Glass, D.J., editor, 1997. Lexicon of Canadian Stratigraphy, vol. 4, Western Canada. Canadian Society of Petroleum Geologists, Calgary, Alberta, 1423 p. on CD-ROM, {{ISBN|0-920230-23-7}}. 4. ^Lerbekmo, J.F., Sweet, A.R. and St. Louis, R.M. 1987. The relationship between the iridium anomaly and palynofloral events at three Cretaceous-Tertiary boundary localities in western Canada. Geological Society of America Bulletin, 99:25-330. 5. ^"Table 20.1," in Weishampel, et al. (2004). Page 440. 6. ^1 Campione, N.E. and Evans, D.C. (2011). "Cranial Growth and Variation in Edmontosaurs (Dinosauria: Hadrosauridae): Implications for Latest Cretaceous Megaherbivore Diversity in North America." PLoS ONE, 6(9): e25186. {{doi|10.1371/journal.pone.0025186}} 7. ^1 Tokaryk, T. 1986. Ceratopsian dinosaurs from the Frenchman Formation (Upper Cretaceous) of Saskatchewan. Canadian Field-Naturalist 100:192–196. 5 : Cretaceous Saskatchewan|Maastrichtian Stage of North America|Upper Cretaceous Series of North America|Western Canadian Sedimentary Basin|Stratigraphy of Saskatchewan |
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