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The Cenomanian-Turonian Boundary Event (CTBE) in northern Lebanon as compared to regional data – Another set of evidences supporting a short-lived tectonic pulse coincidental with the event?

Autor: Serge Ferry, Danièle Grosheny, Bruno Granier, Yann Merran, Mustapha Mroueh, Christophe Lécuyer

Publikováno v: Palaeogeography, Palaeoclimatology, Palaeoecology
Palaeogeography, Palaeoclimatology, Palaeoecology, Elsevier, 2017, 487, pp.447--461. ⟨10.1016/j.palaeo.2017.09.031⟩
Palaeogeography, Palaeoclimatology, Palaeoecology, 2017, 487, pp.447--461. ⟨10.1016/j.palaeo.2017.09.031⟩

Constrained by both foraminifera and isotope data, the Zeitoun and Nahr Ibrahim sections in northern Lebanon record a steady flooding of the Cenomanian carbonate platform during the uppermost Cenomanian-lower Turonian interval. The flooding began jus

Externí odkaz: https://explore.openaire.eu/search/publication?articleId=doi_dedup___::c8f5d9a005cdafee712256970a252906
https://doi.org/10.1016/j.palaeo.2017.09.031

Patterns of local and global redox variability during the Cenomanian–Turonian Boundary Event (Oceanic Anoxic Event 2) recorded in carbonates and shales from central Italy

Autor: Bridget K. Lee, Dalton S. Hardisty, Zunli Lu, Christopher M. Lowery, Timothy W. Lyons, Jeremy D. Owens, Hugh C. Jenkyns

Publikováno v: Sedimentology. 64:168-185

Careful evaluation of the local geochemical conditions in past marine settings can provide a window to the average redox state of the global ocean during episodes of extensive organic-carbon deposition. These comparisons aid in identifying the interp

Externí odkaz: https://explore.openaire.eu/search/publication?articleId=doi_dedup___::e6682e2945dd01d3ebbdeebb34177ebf
https://doi.org/10.1111/sed.12352

The Cenomanian–Turonian boundary event in Egypt: Foraminiferal turnover and carbon isotopic change

Autor: Sherif M. El Baz, Ahmed A. Kassem

Publikováno v: Revue de Micropaléontologie. 69:100463

This study deals with the integration between geochemical data (carbon isotope and, total organic carbon) and foraminiferal turnover to track the Oceanic Anoxic Event 2 (OAE2) from the OCT-A8st1 well, which located in October field, central part of G

Externí odkaz: https://explore.openaire.eu/search/publication?articleId=doi_________::7c5c3e8a8a476217a041142814ab40a7
https://doi.org/10.1016/j.revmic.2020.100463

Paleoenvironmental and paleoceanographic changes across the Cenomanian–Turonian Boundary Event (Oceanic Anoxic Event 2) as indicated by foraminiferal assemblages from the eastern margin of the Cretaceous Western Interior Sea

Autor: Neil E. Tibert, Khalifa Elderbak, R. Mark Leckie

Publikováno v: Palaeogeography, Palaeoclimatology, Palaeoecology. 413:29-48

Two sites near the eastern margin of the Cretaceous Western Interior Sea (WIS) were investigated. The section at Cuba, Kansas (CK) is ~ 630 km east of the GSSP for the Cenomanian/Turonian boundary at Rock Canyon, Colorado (RC), and the section near S

Externí odkaz: https://explore.openaire.eu/search/publication?articleId=doi_________::28c0a2b9f9d39f3c0295b22450fb5cd3
https://doi.org/10.1016/j.palaeo.2014.07.002