Abstract Oceanic Anoxic Event 2 (Cenomanian–Turonian: ca 94 Ma) represents a major
palaeoceanographic phenomenon that took place during an interval of extreme global …

One of the key objectives of Deep Sea Drilling Project (DSDP) Leg 75 was to shed light on
the underlying causes of Cretaceous oceanic anoxia in the South Atlantic by addressing two …

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 …

Organic carbon‐rich shales from localities in England, Italy, and Morocco, which formed
during the Cenomanian‐Turonian oceanic anoxic event (OAE), have been examined for …

The effects of the Cenomanian-Turonian Oceanic Anoxic Event (OAE) in the Chalk Sea of
NW Europe have been investigated using published macrofossil records combined with new …

The Cenomanian‐Turonian oceanic anoxic event (OAE2) is characterized by large
perturbations in the oxygen and sulfur cycles of the ocean, potentially resulting from …

We present new, detailed carbon-isotope records for bulk carbonate, total organic carbon
(TOC) and phytane from three key sections spanning the Cenomanian–Turonian boundary …

Oceanic anoxic events (OAEs) record profound changes in the climatic and
paleoceanographic state of the planet and represent major disturbances in the global …

Correlation of the δ 13C spike with the well dated occurrences of strata rich in organic
carbon detailed in Schlanger et al.(this volume), indicates that a global episode of intense …