Cenomanian-Turonian boundary event

System/
Period
Series/
Epoch
Stage/
Age
Age (Ma)
Paleogene Paleocene Danian younger
Cretaceous Upper/
Late
Maastrichtian 66.0 72.1
Campanian 72.1 83.6
Santonian 83.6 86.3
Coniacian 86.3 89.8
Turonian 89.8 93.9
Cenomanian 93.9 100.5
Lower/
Early
Albian 100.5 ≈113.0
Aptian ≈113.0 ≈125.0
Barremian ≈125.0 ≈129.4
Hauterivian ≈129.4 ≈132.9
Valanginian ≈132.9 ≈139.8
Berriasian ≈139.8 ≈145.0
Jurassic Upper/
Late
Tithonian older
Subdivision of the Cretaceous system
according to the ICS, as of 2017.[1]

The Cenomanian-Turonian boundary event, also known as the Cenomanian-Turonian extinction, Cenomanian-Turonian Oceanic Anoxic Event (OAE 2), and referred to also as the Bonarelli Event or Level,[2] was an anoxic extinction event in the Cretaceous period. The Cenomanian-Turonian oceanic anoxic event is considered to be the most recent truly global oceanic anoxic event in Earth's geologic history.[3] There was a large carbon cycle disturbance during this time period,[4][5] signified by a large positive carbon isotope excursion.[6][7][8] However, apart from the carbon cycle disturbance, there were also large disturbances in the ocean's nitrogen,[9] oxygen,[10] phosphorus,[11][12][13] sulphur,[14] and iron cycles.[15]

  1. ^ "International Chronostratigraphic Chart". www.stratigraphy.org.
  2. ^ Cetean, Claudia G.; Balc, Ramona; Kaminski, Michael A.; Filipescu, Sorin (August 2008). "Biostratigraphy of the Cenomanian-Turonian boundary in the Eastern Carpathians (Dâmboviţa Valley): preliminary observations". Studia Universitatis Babeş-Bolyai, Geologia. 53 (1): 11–23. doi:10.5038/1937-8602.53.1.2.
  3. ^ Petrizzo, Maria Rose; Amaglio, Giulia; Watkins, David K.; MacLeod, Kenneth G.; Huber, Brian T.; Hasegawa, Takashi; Wolfgring, Erik (19 August 2022). "Biotic and Paleoceanographic Changes Across the Late Cretaceous Oceanic Anoxic Event 2 in the Southern High Latitudes (IODP Sites U1513 and U1516, SE Indian Ocean)". Paleoceanography and Paleoclimatology. 37 (9): e2022PA004474. Bibcode:2022PaPa...37.4474P. doi:10.1029/2022PA004474. PMC 9545577. PMID 36247808.
  4. ^ Paul, C. R. C.; Lamolda, M. A.; Mitchell, S. F.; Vaziri, M. R.; Gorostidi, A.; Marshall, J. D. (15 June 1999). "The Cenomanian–Turonian boundary at Eastbourne (Sussex, UK): a proposed European reference section". Palaeogeography, Palaeoclimatology, Palaeoecology. 150 (1–2): 83–121. Bibcode:1999PPP...150...83P. doi:10.1016/S0031-0182(99)00009-7. Retrieved 28 January 2023.
  5. ^ Arthur, Michael A.; Dean, Walter E.; Pratt, Lisa M. (20 October 1988). "Geochemical and climatic effects of increased marine organic carbon burial at the Cenomanian/Turonian boundary". Nature. 335 (6192): 714–717. Bibcode:1988Natur.335..714A. doi:10.1038/335714a0. S2CID 4277249. Retrieved 28 January 2023.
  6. ^ Cite error: The named reference GroshenyEtAl2006 was invoked but never defined (see the help page).
  7. ^ Cite error: The named reference JarvisEtAl2006 was invoked but never defined (see the help page).
  8. ^ Cite error: The named reference JarvisEtAl1988 was invoked but never defined (see the help page).
  9. ^ Cite error: The named reference JuniumAndArthur2007 was invoked but never defined (see the help page).
  10. ^ Cite error: The named reference OAE2Poland was invoked but never defined (see the help page).
  11. ^ Cite error: The named reference EnhancedPhosphorusRecycling was invoked but never defined (see the help page).
  12. ^ Cite error: The named reference EnhancedPhosphorusRecyclingApatiteAuthigenesis was invoked but never defined (see the help page).
  13. ^ Cite error: The named reference PhosphorusCycleOscillation was invoked but never defined (see the help page).
  14. ^ Cite error: The named reference renamed_from_9_on_20221219231054 was invoked but never defined (see the help page).
  15. ^ Cite error: The named reference OkhouchiEtAl1999 was invoked but never defined (see the help page).

© MMXXIII Rich X Search. We shall prevail. All rights reserved. Rich X Search