Episodes of widespread distribution of organic-rich marine facies within relatively narrow
stratigraphic intervals have been interpreted as Oceanic Anoxic Events (OAEs). There are a …

The Cretaceous experienced numerous global and local climatic perturbations to the ocean–
atmosphere system, especially during periods of known widespread organic-carbon burial …

Lower Cretaceous pelagic sediments deposited in the Central Tethys Ocean and along its
southern continental margin and outcropping in the Swiss and Italian Alps were chosen for a …

Abstract Oceanic Anoxic Event 2 (OAE2; c. 94.5–93.9 Ma) offers insight into the mechanisms
of past climate change linked to organic productivity and carbon sequestration. It has been …

Today's disturbance of the global carbon cycle induced by anthropogenic processes has
raised new interest in the history of the global carbon cycle and its relationship to climate …

Abstract The Coniacian-Santonian (CS) was a time of differentiation in marine
sedimentation, characterized by organic carbon (OC)-rich black shales and carbonates …

We develop a recycling model using 13C/12C mass balance for net growth/loss of the
sedimentary organic carbon (Corg) reservoir, and apply it to the Neogene bulk marine …

A common feature of records of the early Aptian oceanic anoxic event (OAE) 1a is the sharp
negative δ13C excursion displayed in both carbonate and organic matter at the onset of this …

The paleoceanographic history of the Pacific Ocean during the mid-Cretaceous is poorly
constrained due to the loss of much of the contemporaneous Pacific seafloor to subduction …

Highest resolution carbon isotope stratigraphy was established for terrestrial organic carbon
through the uppermost Cenomanian in Hokkaido, Japan. The interval of the main phase of …