Cenomanian - Turonian Oceanic Anoxic Event (OAE2) in the Sakarya Zone, northwestern Turkey: Sedimentological, cyclostratigraphic, and geochemical records

2010-04-01
Yılmaz, İsmail Ömer
Altıner, Demir
TEKİN, UĞUR KAĞAN
Tuysuz, Okan
Ocakoglu, Faruk
Acikalin, Sanem
The Cenomanian/Turonian oceanic anoxic event as recorded in many parts of the world is characterized by presence of black shales and global carbon isotope peaks. Cyclic variations within the anoxic event and association with pelagic red beds are indicated by many studies. Global tectonic/volcanic controls on the origin and the chronostratigraphic position of the anoxic event within the global sea-level changes are important for understanding the paleoceanographic and paleoclimatic conditions during the deposition of Cenomanian/Turonian sediments.

Citation Formats
İ. Ö. Yılmaz, D. Altıner, U. K. TEKİN, O. Tuysuz, F. Ocakoglu, and S. Acikalin, “Cenomanian - Turonian Oceanic Anoxic Event (OAE2) in the Sakarya Zone, northwestern Turkey: Sedimentological, cyclostratigraphic, and geochemical records,” CRETACEOUS RESEARCH, vol. 31, no. 2, pp. 207–226, 2010, Accessed: 00, 2020. [Online]. Available: https://hdl.handle.net/11511/48534.