THE STRATIGRAPHY AND PALEONTOLOGY OF THE UPPER WEALD CLAY (BARREMIAN)AT SMOKEJACKS BRICKWORKS, OCKLEY, SURREY, ENGLAND

Authors
Citation
Aj. Ross et E. Cook, THE STRATIGRAPHY AND PALEONTOLOGY OF THE UPPER WEALD CLAY (BARREMIAN)AT SMOKEJACKS BRICKWORKS, OCKLEY, SURREY, ENGLAND, Cretaceous research, 16(6), 1995, pp. 705-716
Citations number
24
Categorie Soggetti
Paleontology,Geology
Journal title
ISSN journal
01956671
Volume
16
Issue
6
Year of publication
1995
Pages
705 - 716
Database
ISI
SICI code
0195-6671(1995)16:6<705:TSAPOT>2.0.ZU;2-B
Abstract
The stratigraphy of the Weald Clay of Surrey is summarized. The Hauter ivian/Barremian boundary is shown to correspond closely to the Lower W eald Clay/Upper Weald Clay boundary, which lies at the base of BGS (Br itish Geological Survey) Bed 3a and is close to the Ewhurst/Capel ostr acod faunicycle boundary. Detailed sections of the sediments exposed i n the pit at Smokejacks Brickworks are published for the first time. B GS Bed 5c is present at the top of the pit, which indicates that the s ediments belong to the Upper Weald Clay and suggests an early Barremia n age for this sire. The pit has yielded a diverse non-marine fossil f auna and flora consisting of the remains of insects, crustacea, bivalv es, dinosaurs (including Baryonyx walken), pterosaurs, crocodiles, sha rks, bony fish, club mosses, horsetails, ferns, conifers and a primiti ve aquatic or marsh-dwelling herbaceous plant. The extinct lacewing fa mily Brongniartiellidae is recorded from the Barremian for the first t ime. The sediments exposed in Smokejacks pit and their fossil content indicate a shallowing upwards sequence, documenting a change from a la custrine/lagoonal to a fluvial/mudplain environment. (C) 1995 Academic Press Limited.