The biotic response to the late Cenomanian oceanic anoxic event; integrated evidence from Dover, SE England
- 1 March 1989
- journal article
- Published by Geological Society of London in Journal of the Geological Society
- Vol. 146 (2) , 311-317
- https://doi.org/10.1144/gsjgs.146.2.0311
Abstract
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.This publication has 15 references indexed in Scilit:
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