Two shallow water late Cenomanian to early Turonian sequences of NE Egypt have been
investigated to evaluate the response to OAE2. Age control based on calcareous …

Environmental and depositional changes across the Late Cenomanian oceanic anoxic
event (OAE2) in the Sinai, Egypt, are examined based on biostratigraphy, mineralogy, δ 13 …

Abstract Oceanic Anoxic Event 2, spanning the Cenomanian/Turonian boundary (93.9 Ma),
was an episode of major perturbations in the global carbon cycle. To investigate the …

The response of shallow‐water sequences to oceanic anoxic event 2 and mid‐Cenomanian
events 1a and 1b was investigated along the west African margin of Morocco north of Agadir …

To better understand the linkage between climate and ocean circulation under greenhouse
conditions we have studied calcareous nannofossils, palynomorphs and benthic …

Profound biotic changes accompanied the late Cenomanian δ13C excursion and OAE2 in
planktic foraminifera in the Tarfaya Basin of Morocco. Planktic foraminifera experienced a …

The occurrence of the biomarker lycopane and the enrichment patterns of redox sensitive
trace metals in black shales from Demerara Rise (western tropical Atlantic) reveal that …

Ichnological analysis of dark sediments of the Oceanic Anoxic Event at the Cenomanian–
Turonian boundary interval (OAE-2) from the Betic Cordillera, southern Spain, reveals the …

Abstract In 2013, Andra (French National Radioactive Waste Management Agency) drilled
boreholes to the south-east of the Paris Basin, to characterise Aptian and Albian clayey …

We investigated the onset and development of Cretaceous Oceanic Anoxic Event 2 (OAE2)
in a newly drilled core (SN° 4) from the Tarfaya Basin (southern Morocco), where this …