49 citations as recorded by crossref.

1. Main controlling factors of organic matter enrichment of the Mesoproterozoic source rocks from the North China Craton J. Cai et al. 10.1002/gj.3967
2. Exploring the paleoceanographic changes registered by planktonic foraminifera across the Cenomanian-Turonian boundary interval and Oceanic Anoxic Event 2 at southern high latitudes in the Mentelle Basin (SE Indian Ocean) M. Petrizzo et al. 10.1016/j.gloplacha.2021.103595
3. Sulfur isotopes track the global extent and dynamics of euxinia during Cretaceous Oceanic Anoxic Event 2 J. Owens et al. 10.1073/pnas.1305304110
4. Climate changes as recorded in stable carbon isotopic compositions of the Late Jurassic marine sedimentary succession in the Qiangtang Basin, Northern Tibet G. Li et al. 10.1016/j.jseaes.2022.105317
5. Stripping back the modern to reveal the Cenomanian–Turonian climate and temperature gradient underneath M. Laugié et al. 10.5194/cp-16-953-2020
6. Radioisotopic chronology of Ocean Anoxic Event 1a: Framework for analysis of driving mechanisms Y. Li et al. 10.1126/sciadv.adn8365
7. Paleoceanographic changes across OAE 2 inferred from resilient foraminifera and XRF data at southern high latitudes (IODP Sites U1513 and U1516, Mentelle Basin, SW Australia) G. Amaglio et al. 10.1016/j.palaeo.2024.112578
8. Organomineral nanocomposite carbon burial during Oceanic Anoxic Event 2 S. Löhr & M. Kennedy 10.5194/bg-11-4971-2014
9. The upper Cenomanian–lower Turonian of the Preafrican Trough (Morocco): Platform configuration and palaeoenvironmental conditions V. Lebedel et al. 10.1016/j.jafrearsci.2015.03.001
10. Pre‐treatment Methods for Accurate Determination of Total Nitrogen and Organic Carbon Contents and their Stable Isotopic Compositions: Re‐evaluation from Geological Reference Materials W. Fujisaki et al. 10.1111/ggr.12410
11. Turonian and Coniacian in the territory of the Eastern Perithetys — biostratigraphy and paleogeography L. Kopaevich et al. 10.55959/MSU0579-9406-4-2024-63-6-72-81
12. The Plenus Cold Event Record in the Abyssal DSDP Site 367 (Cape Verde, Central Atlantic): Environmental Perturbations and Impacts on the Nitrogen Cycle L. Riquier et al. 10.3389/feart.2021.703282
13. Enhanced Organic Carbon Burial in Sediments of Oxygen Minimum Zones Upon Ocean Deoxygenation I. Ruvalcaba Baroni et al. 10.3389/fmars.2019.00839
14. Confounding effects of oxygen and temperature on the TEX 86 signature of marine Thaumarchaeota W. Qin et al. 10.1073/pnas.1501568112
15. Paleoceanographic importance of tri- and di-unsaturated alkenones through the early phase of Cretaceous Oceanic Anoxic Event 2 from southern high latitudes of the proto-Indian Ocean T. Hasegawa & A. Goto 10.1016/j.orggeochem.2023.104722
16. Quantifying the missing sink for global organic carbon burial during a Cretaceous oceanic anoxic event J. Owens et al. 10.1016/j.epsl.2018.07.021
17. A Re‐evaluation of the Plenus Cold Event, and the Links Between CO2, Temperature, and Seawater Chemistry During OAE 2 L. O'Connor et al. 10.1029/2019PA003631
18. Cretaceous southern high latitude benthic foraminiferal assemblages during OAE 2 at IODP Site U1516, Mentelle Basin, Indian Ocean E. Wolfgring et al. 10.1016/j.cretres.2023.105555
19. Why are the δ13Corg values in Phanerozoic black shales more negative than in modern marine organic matter? P. Meyers 10.1002/2014GC005305
20. Gradual and sustained carbon dioxide release during Aptian Oceanic Anoxic Event 1a B. Naafs et al. 10.1038/ngeo2627
21. Late Cretaceous astrochronology, organic carbon evolution, and paleoclimate inferences for the subtropical western South Atlantic, Espírito Santo Basin T. Santos et al. 10.1016/j.cretres.2021.105032
22. Changing ocean circulation and hydrothermal inputs during Ocean Anoxic Event 2 (Cenomanian–Turonian): Evidence from Nd-isotopes in the European shelf sea X. Zheng et al. 10.1016/j.epsl.2013.05.053
23. Imbalanced nutrients as triggers for black shale formation in a shallow shelf setting during the OAE 2 (Wunstorf, Germany) M. Blumenberg & F. Wiese 10.5194/bg-9-4139-2012
24. The Northern Gulf of Mexico During OAE2 and the Relationship Between Water Depth and Black Shale Development C. Lowery et al. 10.1002/2017PA003180
25. Cyanobacteria Proliferation in the Cenomanian‐Turonian Boundary Interval of the Apennine Carbonate Platform: Immediate Response to the Environmental Perturbations Associated With OAE‐2? G. Frijia et al. 10.1029/2019GC008306
26. Nitrogen and carbon cycle perturbations through the Cenomanian-Turonian oceanic anoxic event 2 (~94 Ma) in the Vocontian Basin (SE France) J. Danzelle et al. 10.1016/j.palaeo.2019.109443
27. The Late Cretaceous Western Interior Seaway as a model for oxygenation change in epicontinental restricted basins C. Lowery et al. 10.1016/j.earscirev.2017.12.001
28. An analysis of the impacts of Cretaceous oceanic anoxic events on global molluscan diversity dynamics N. Freymueller et al. 10.1017/pab.2019.10
29. An integrated stratigraphic re-evaluation of key Central Atlantic DSDP sites M. Casson et al. 10.1016/j.jafrearsci.2024.105278
30. Complete archive of late Turonian to early Campanian sedimentary deposition in newly drilled cores from the Tarfaya Basin, SW Morocco M. Aquit et al. 10.1130/B31523.1
31. Carbon Cycling During Oceanic Anoxic Event 2: Compound‐Specific Carbon Isotope Evidence From the Western Interior Seaway F. Boudinot et al. 10.1029/2021PA004287
32. Marine organic carbon burial increased forest fire frequency during Oceanic Anoxic Event 2 F. Boudinot & J. Sepúlveda 10.1038/s41561-020-0633-y
33. Intercontinental correlation of organic carbon and carbonate stable isotope records: evidence of climate and sea‐level change during the Turonian (Cretaceous) I. Jarvis et al. 10.1002/dep2.6
34. Stable Isotope Constraints on Marine Productivity Across the Cretaceous‐Paleogene Mass Extinction J. Sepúlveda et al. 10.1029/2018PA003442
35. Molecular fossils from phytoplankton reveal secular P co 2 trend over the Phanerozoic C. Witkowski et al. 10.1126/sciadv.aat4556
36. Paleoenvironment and source-rock potential of the Cenomanian-Turonian Eagle Ford Formation in the Sabinas basin, northeast Mexico J. Enciso-Cárdenas et al. 10.1016/j.jsames.2021.103184
37. Short-term eustatic sea-level changes during the Cenomanian–Turonian Supergreenhouse interval in the Kopet-Dagh Basin, NE Tethyan realm B. Kalanat et al. 10.1007/s41513-018-0060-8
38. Cretaceous oceanic anoxic events prolonged by phosphorus cycle feedbacks S. Beil et al. 10.5194/cp-16-757-2020
39. Cenomanian–Turonian carbon isotope stratigraphy of the Western Canadian Sedimentary Basin A. Prokoph et al. 10.1016/j.cretres.2013.03.005
40. Foraminiferal and nannofossil paleoecology and paleoceanography of the Cenomanian–Turonian Eagle Ford Shale of southern Texas C. Lowery et al. 10.1016/j.palaeo.2014.07.025
41. Transition from the Cretaceous ocean to Cenozoic circulation in the western South Atlantic — A twofold reconstruction G. Uenzelmann-Neben et al. 10.1016/j.tecto.2016.05.036
42. Spatio-temporal variability in microfossil and geochemical records of Cenomanian-Turonian oceanic anoxic event-2: a review C. Sooraj et al. 10.1016/j.jop.2024.06.002
43. Planktonic foraminiferal turnover across the Cenomanian – Turonian boundary (OAE2) in the northeast of the Tethys realm, Kopet-Dagh Basin B. Kalanat et al. 10.1515/geoca-2016-0028
44. Biotic response to the latest Cenomanian drowning and OAE2: A case study from the Eastern Desert of Egypt E. Nagm et al. 10.1016/j.pgeola.2020.10.001
45. Iron Isotopes reveal volcanogenic input during Oceanic Anoxic Event 2 (OAE 2 ∼ 94 Ma) L. Nana Yobo et al. 10.1016/j.gca.2024.10.023
46. Calcareous plankton and shallow-water benthic biocalcifiers: Resilience and extinction across the Cenomanian-Turonian Oceanic Anoxic Event 2 M. Petrizzo et al. 10.1016/j.palaeo.2025.112891
47. Reconstructing Late Ordovician carbon cycle variations R. Pancost et al. 10.1016/j.gca.2012.11.033
48. Astronomical constraints on global carbon-cycle perturbation during Oceanic Anoxic Event 2 (OAE2) Y. Li et al. 10.1016/j.epsl.2017.01.007
49. Paleo-CO2 variation trends and the Cretaceous greenhouse climate Y. Wang et al. 10.1016/j.earscirev.2013.11.001