The stratigraphic and palaeogeographic setting of the late Cenomanian ‘anoxic’ event
- 1 March 1989
- journal article
- Published by Geological Society of London in Journal of the Geological Society
- Vol. 146 (2) , 305-310
- https://doi.org/10.1144/gsjgs.146.2.0305
Abstract
The late Cenomanian carbon isotope excursion can be shown to be synchronous over most areas of the globe where micropalaeontological data are adequate. The sedimentological variations seen in these different areas are thought to be due to palaeobathymetry. The relationship between this ‘anoxic’ event and the major faunal change in the late Cenomanian is described.This publication has 18 references indexed in Scilit:
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