M. H. Khan; Note on the depth and temperature of the Gault Sea as indicated by Foraminifera. Geological Magazine ; 87 (3): 175–180. doi:
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A re-interpretation of the foraminiferal evidence indicates that, in line with other paleontological and geological evidence, the Gault (Cretaceous) beds, at least in southeast England, were deposited in temperate shallow waters.
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