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Journal of the Geological Society; April 1989; v. 146; no. 2; p. 311-317; DOI: 10.1144/gsjgs.146.2.0311
© 1989 Geological Society of London
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Article

The biotic response to the late Cenomanian oceanic anoxic event; integrated evidence from Dover, SE England

P. N. LEARY1, G. A. CARSON2, M. K. E. COOPER3, M. B. HART1, D. HORNE4, I. JARVIS5, A. ROSENFELD6 and B. A. TOCHER1

1 Department of Geological Sciences, Plymouth Polytechnic, Drake Circus, Plymouth PL4 8AA, UK
2Department of Earth Sciences, Liverpool University, Brownlow Street, PO Box 147, Liverpool L69 3BX, UK
3Stratigraphic Services International Ltd, Chancellor Court, 20 Priestly Road, Guildford, Surrey GU2 5YC, UK
4Department of Geology, City of London Polytechnic, Walburgh House, Bigland Street, London El 2NG, UK
5School of Geological Sciences, Kingston Polytechnic, Penrhyn Road, Kingston Upon Thames KT1 2EE, UK
6Geological Survey of Israel, 30 Malke Yisrael Street, Jerusalem 95 501, Israel

The late Cenomanian sea-level rise was coupled with an expansion of the oxygen-minimum zone. The position of its upper surface may be discerned from the sequential effects on the benthonic and planktonic biota.




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