35 citations as recorded by crossref.

1. Water-mass evolution in the Cretaceous Western Interior Seaway of North America and equatorial Atlantic J. Eldrett et al. 10.5194/cp-13-855-2017
2. Vegetation response to exceptional global warmth during Oceanic Anoxic Event 2 U. Heimhofer et al. 10.1038/s41467-018-06319-6
3. 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
4. Models of organic enrichment in epicontinental basins: Applications of a large organic geochemical dataset from the Cretaceous Western Interior Seaway L. Robinson & J. Whiteside 10.1016/j.cretres.2022.105160
5. DINOSTRAT: a global database of the stratigraphic and paleolatitudinal distribution of Mesozoic–Cenozoic organic-walled dinoflagellate cysts P. Bijl 10.5194/essd-14-579-2022
6. High-frequency sequences, paleogeography, and syn-depositional tectonism on a shallow clastic ramp: Doe Creek and Pouce Coupe members of the Late Cenomanian Kaskapau Formation, Western Canada Foreland Basin A. Plint & M. Kreitner 10.35767/gscpgbull.67.2.71
7. Biostratigraphy and Inoceramus survival across the Cenomanian–Turonian (Cretaceous) boundary in the Ram River section, Alberta, Canada I. Walaszczyk et al. 10.1515/agp-2016-0039
8. Palynology and calcareous nannofossil biostratigraphy of the Turonian – Coniacian boundary: The proposed boundary stratotype at Salzgitter-Salder, Germany and its correlation in NW Europe I. Jarvis et al. 10.1016/j.cretres.2021.104782
9. The Cretaceous succession of northeast Baffin Bay: Stratigraphy, sedimentology and petroleum potential H. Nøhr-Hansen et al. 10.1016/j.marpetgeo.2021.105108
10. 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
11. A dinoflagellate cyst zonation of the Cenomanian and Turonian (Upper Cretaceous) in the Western Interior, United States P. Dodsworth & J. Eldrett 10.1080/01916122.2018.1477851
12. Redox conditions and ecological resilience during Oceanic Anoxic Event 2 in the Western Interior Seaway L. Robinson et al. 10.1016/j.palaeo.2023.111496
13. Zinc- and cadmium-isotope evidence for redox-driven perturbations to global micronutrient cycles during Oceanic Anoxic Event 2 (Late Cretaceous) T. Sweere et al. 10.1016/j.epsl.2020.116427
14. 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
15. Enhanced Arctic-Tethys connectivity ended the Toarcian Oceanic Anoxic Event in NW Europe B. van de Schootbrugge et al. 10.1017/S0016756819001262
16. Evidence for changes in sea-surface circulation patterns and ~20° equatorward expansion of the Boreal bioprovince during a cold snap of Oceanic Anoxic Event 2 (Late Cretaceous) F. Falzoni & M. Petrizzo 10.1016/j.gloplacha.2021.103678
17. Benthic foraminiferal response to the Oceanic Anoxic Event 2 (Late Cretaceous) and evidence of bottom water re‐oxygenation during the Plenus Cold Event at Clot Chevalier (Vocontian Basin, SE France) G. Amaglio et al. 10.1016/j.palaeo.2023.111598
18. A 87Sr/86Sr, δ18O and δ13C record of Turonian-Santonian belemnites from lower Volga region of the East European Platform: Stratigraphic significance and palaeoenvironmental reconstructions Y. Zakharov et al. 10.1016/j.geobios.2022.07.006
19. Timing of the Greenhorn transgression and OAE2 in Central Utah using CA-TIMS U-Pb zircon dating R. Renaut et al. 10.1016/j.cretres.2022.105464
20. Isotopic evidence for changes in the zinc cycle during Oceanic Anoxic Event 2 (Late Cretaceous) T. Sweere et al. 10.1130/G40226.1
21. Low-latitude ?upper Barremian–lower Aptian palynoflora and paleovegetation of the Biyadh Formation (Arabian Plate, eastern margin of northern Gondwana): evidence for a possible cold snap H. Boukhamsin et al. 10.1016/j.cretres.2021.104995
22. High resolution osmium data record three distinct pulses of magmatic activity during cretaceous Oceanic Anoxic Event 2 (OAE-2) D. Sullivan et al. 10.1016/j.gca.2020.04.002
23. A new record of the Cenomanian–Turonian transgression preserved in the Ikorfat Fault zone, Nuussuaq Basin, West Greenland G. Pedersen et al. 10.1016/j.cretres.2023.105481
24. Basalt‐seawater interaction, the Plenus Cold Event, enhanced weathering and geochemical change: deconstructing Oceanic Anoxic Event 2 (Cenomanian–Turonian, Late Cretaceous) H. Jenkyns et al. 10.1111/sed.12305
25. Cretaceous large igneous provinces: from volcanic formation to environmental catastrophes and biological crises L. Percival et al. 10.1144/SP544-2023-88
26. High‐frequency sequences within a retrogradational deltaic succession: Upper Cenomanian Dunvegan Formation, Western Canada Foreland Basin M. Hay & A. Plint 10.1002/dep2.114
27. Late Cenomanian Plenus event in the Western Interior Seaway B. Sageman et al. 10.1016/j.cretres.2023.105798
28. Comparing Seawater Temperature Proxy Records for the Past 90 Myrs From the Shallow Shelf Record Bass River, New Jersey M. de Bar et al. 10.1029/2018PA003453
29. The expression of late Cenomanian–Coniacian episodes of accelerated global change in the sedimentary record of the Mexican Interior Basin A. Colín-Rodríguez et al. 10.1016/j.cretres.2022.105380
30. Cretaceous Oceanic Anoxic Event 2 in eastern England: further palynological and geochemical data from Melton Ross P. Dodsworth et al. 10.1144/pygs2019-017
31. Spatial heterogeneity in benthic foraminiferal assemblages tracks regional impacts of paleoenvironmental change across Cretaceous OAE2 R. Bryant & C. Belanger 10.1017/pab.2022.47
32. Anatomy of a late Cenomanian transgressive shelf system: The influence of high-frequency eustasy and crustal flexure on stratigraphy and paleogeography, basal Kaskapau Formation, Western Canada Foreland Basin A. Plint 10.35767/gscpgbull.67.1.1
33. Patterns of planktonic foraminiferal extinctions and eclipses during Oceanic Anoxic Event 2 at Eastbourne (SE England) and other mid-low latitude locations F. Falzoni & M. Petrizzo 10.1016/j.cretres.2020.104593
34. Sedimentary Mercury Enrichments as a Marker for Submarine Large Igneous Province Volcanism? Evidence From the Mid‐Cenomanian Event and Oceanic Anoxic Event 2 (Late Cretaceous) J. Scaife et al. 10.1002/2017GC007153
35. Onset and demise of Cretaceous oceanic anoxic events: The coupling of surface and bottom oceanic processes in two pelagic basins of the western Tethys G. Gambacorta et al. 10.1002/2015PA002922