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Abstract

The foraminifera of the Gault Clay Formation (Middle and Upper Albian) are reviewed and their biostratigraphy compared to that of the standard ammonite-based zonation and the original bed numbers that are used by most workers on the formation. The change from an aragonitic assemblage in the Lower Gault to an assemblage dominated by agglutinated foraminifera in the Upper Gault is discussed in terms of changing palaeogeography and sea-level.

DOI

10.1016/j.pgeola.2019.10.003

Publication Date

2020-08-01

Publication Title

Proceedings of the Geologists' Association

Volume

131

First Page

386

Last Page

396

ISSN

0016-7878

Embargo Period

2024-05-18

Organisational Unit

School of Geography, Earth and Environmental Sciences

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