Redox conditions, glacio-eustasy, and the status of the Cenomanian–Turonian Anoxic Event: new evidence from the Upper Cretaceous Chalk of England
Author:
Publisher
Polish Academy of Sciences Chancellery
Subject
Geology
Link
https://journals.pan.pl/Content/117596/PDF/1_Jeans_et_al.pdf
Cited by 5 articles. 订阅此论文施引文献 订阅此论文施引文献,注册后可以免费订阅5篇论文的施引文献,订阅后可以查看论文全部施引文献
1. Chemostratigraphy of the lower Danubian Cretaceous Group (Cenomanian–lower Turonian, Bavaria, SE Germany)—A new carbon isotope reference curve and inter-basinal correlation;Cretaceous Research;2023-09
2. The erratic rocks of the Upper Cretaceous Chalk of England: how did they get there, ice transport or other means?;Acta Geologica Polonica;2023-07-26
3. A marker band folgen stratigraphy for the Cenomanian Chalk of England and its extension to northen Germany and France;Acta Geologica Polonica;2023-06-27
4. Evidence for changes in sea-surface circulation patterns and ~20° equatorward expansion of the Boreal bioprovince during a cold snap of Oceanic Anoxic Event 2 (Late Cretaceous);Global and Planetary Change;2022-01
5. Condensation and channelling in Cenomanian chalks of the northern Anglo-Paris Basin; The Totternhoe Stone and related deposits;Newsletters on Stratigraphy;2021-08-18
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