Английская Википедия:Coralline Oolite Formation
Шаблон:Use dmy dates Шаблон:Infobox rockunit The Coralline Oolite Formation is a limestone formation of Oxfordian (Upper Jurassic) age, found in the Cleveland Basin of North Yorkshire, England.[1]
Coral Rag Member
The rock forms some of the hills around Oxford and was once used as building stone. Coral rag can be seen in some of the oldest buildings in that city, including the Saxon tower of St Michael at the Northgate, St George's Tower of Oxford Castle and the mediaeval walls of the city.[2]
Hambleton Oolite Member
This ooidal limestone lies above either the Yedmandale Member or the Lower Calcareous Grit Formation. It is overlain by either the Middle Calcareous Grit or Malton Oolite Members. It is distinguished from the latter by its smaller grain-size and poorer sorting.[3]
Vertebrate paleofauna
Dinosaurs
The following dinosaurs were reported from the formation, with many of them reidentified.[4]
Taxa | Location | Description | Images |
---|---|---|---|
|
Berkshire, England[4] | ||
Metriacanthosaurus
|
misidentified | Actually from the Weymouth Member.[5] | |
Sauropoda[4]
|
Oxfordshire, England[4] | "(=Cetiosaurus sp.)"[4] | |
Stegosauridae[4]
|
North Yorkshire, England.[4] | "(=Omosaurus phillipsi)"[4] "Juvenile femur."[6] | |
Theropoda[4] | North Yorkshire & Oxfordshire, England[4] | "(=Megalosaurus bucklandii)"[4]
|
References
- ↑ Шаблон:Cite web
- ↑ Шаблон:Cite web
- ↑ Шаблон:Cite web
- ↑ 4,00 4,01 4,02 4,03 4,04 4,05 4,06 4,07 4,08 4,09 4,10 4,11 4,12 4,13 4,14 4,15 4,16 4,17 4,18 4,19 Weishampel, David B; et al. (2004). "Dinosaur distribution (Late Jurassic, Europe)." In: Weishampel, David B.; Dodson, Peter; and Osmólska, Halszka (eds.): The Dinosauria, 2nd, Berkeley: University of California Press. Pp. 545–549. Шаблон:ISBN.
- ↑ Шаблон:Cite journal
- ↑ "Table 16.1," in Weishampel, et al. (2004). Page 345.
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- Oxfordian Stage
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