Note on the depth and temperature of the Gault sea as indicated by foraminifera
By: Khan, M.H
.
Material type: 
ArticleDescription: 175-180p.Subject(s): Reinterpretation - Foraminiferal evidence - Gault sea - England | Paleogeography - England | Paleontology - England | Depth and temperature - Gault sea - England
In:
Geological magazine : Vol. 87 Iss. 1-6 Year. 1950Summary: Abstract
Foraminiferal evidence in the past has been held to suggest that the Gault is a deep sea deposit—a view which conflicts with the belief held by many on geological and other palaeontological grounds that the Gault was laid down in fairly shallow water. This contradiction is due to a misinterpretation of the foraminiferal evidence which, in the opinion of the writer, favours a temperate, relatively shallow marine environment for the deposition of the Gault, at least in South-East of England.
| Item type | Current location | Collection | Call number | Status | Date due | Barcode |
|---|---|---|---|---|---|---|
Article
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Library and Information Centre Periodical Section | Bound Journal Collection | Not for loan | 002560_34 | ||
Serials/Scientific Journal
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Library and Information Centre Periodical Section | Bound Journal Collection | 550 GEO (Browse shelf) | Available | 002560 |
Abstract
Foraminiferal evidence in the past has been held to suggest that the Gault is a deep sea deposit—a view which conflicts with the belief held by many on geological and other palaeontological grounds that the Gault was laid down in fairly shallow water. This contradiction is due to a misinterpretation of the foraminiferal evidence which, in the opinion of the writer, favours a temperate, relatively shallow marine environment for the deposition of the Gault, at least in South-East of England.
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