50 citations as recorded by crossref.

1. 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
2. Decoupling δ13Ccarb and δ13Corg at the onset of the Ireviken Carbon Isotope Excursion: Δ13C and organic carbon burial (forg) during a Silurian oceanic anoxic event E. Hartke et al. 10.1016/j.gloplacha.2020.103373
3. 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
4. Controls On Sedimentation and Cyclicity of the Boquillas and Equivalent Eagle Ford Formation from Detailed Outcrop Studies of Western and Central Texas, U.S.A. D. Lehrmann et al. 10.2110/jsr.2019.38
5. Controls on the Cd-isotope composition of Upper Cretaceous (Cenomanian–Turonian) organic-rich mudrocks from south Texas (Eagle Ford Group) T. Sweere et al. 10.1016/j.gca.2020.02.019
6. Facies partitioning of fluvial, wave, and tidal influences across the shoreline-to-shelf architecture in the Western Interior Campanian Seaway, USA K. Minor et al. 10.1144/SP523-2022-11
7. Integrated ground-based hyperspectral imaging and geochemical study of the Eagle Ford Group in West Texas L. Sun et al. 10.1016/j.sedgeo.2017.10.012
8. LIP volcanism (not anoxia) tracked by Cr isotopes during Ocean Anoxic Event 2 in the proto-North Atlantic region L. Nana Yobo et al. 10.1016/j.gca.2022.06.016
9. Authigenic, volcanogenic, and detrital influences on the Cenomanian–Turonian clay sedimentation in the Western Interior Basin: Implications for palaeoclimatic reconstructions G. Charbonnier et al. 10.1016/j.cretres.2019.104228
10. 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
11. Spatial heterogeneity in benthic foraminiferal assemblages tracks regional impacts of paleoenvironmental change across Cretaceous OAE2 R. Bryant & C. Belanger 10.1017/pab.2022.47
12. 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
13. Unraveling short- and long-term carbon cycle variations during the Oceanic Anoxic Event 2 from the Paris Basin Chalk S. Boulila et al. 10.1016/j.gloplacha.2020.103126
14. 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
15. Cretaceous Oceanic Anoxic Event 2 in eastern England: further palynological and geochemical data from Melton Ross P. Dodsworth et al. 10.1144/pygs2019-017
16. Uranium isotope reconstruction of ocean deoxygenation during OAE 2 hampered by uncertainties in fractionation factors and local U-cycling B. McDonald et al. 10.1016/j.gca.2022.05.010
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. Sequence stratigraphical and palaeoenvironmental implications of Cenomanian–Santonian dinocyst assemblages from the Trans‐Sahara epicontinental seaway: a multivariate statistical approach M. Usman et al. 10.1002/dep2.260
19. Enhanced ocean connectivity and volcanism instigated global onset of Cretaceous Oceanic Anoxic Event 2 (OAE2) ∼94.5 million years ago Y. Li et al. 10.1016/j.epsl.2021.117331
20. 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
21. Late Cenomanian Plenus Event in the Western Interior Seaway B. Sageman et al. 10.2139/ssrn.4089095
22. 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
23. Neritic ecosystem response to Oceanic Anoxic Event 2 in the Cretaceous Western Interior Seaway, USA F. Boudinot et al. 10.1016/j.palaeo.2020.109673
24. 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
25. What happened to the organic matter from the Upper Cretaceous succession in Guatemala, Central America? W. Radmacher et al. 10.1016/j.marpetgeo.2021.105246
26. Microfossil and geochemical records reveal high-productivity paleoenvironments in the Cretaceous Western Interior Seaway during Oceanic Anoxic Event 2 R. Bryant et al. 10.1016/j.palaeo.2021.110679
27. Data-model comparison reveals key environmental changes leading to Cenomanian-Turonian Oceanic Anoxic Event 2 Y. Joo et al. 10.1016/j.earscirev.2020.103123
28. The First Occurrence of Ptychodus latissimus from the Codell Sandstone Member of the Carlile Shale in Kansas S. Hamm 10.1660/062.123.0311
29. Pliosaurid (Reptilia: Sauropterygia) remains from the Upper Cretaceous of Japan, and their biostratigraphic and paleogeographic significance T. Sato et al. 10.1016/j.cretres.2023.105593
30. 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
31. Turonian Sea Level and Paleoclimatic Events in Astronomically Tuned Records From the Tropical North Atlantic and Western Interior Seaway M. Jones et al. 10.1029/2017PA003158
32. 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
33. The Cretaceous succession of northeast Baffin Bay: Stratigraphy, sedimentology and petroleum potential H. Nøhr-Hansen et al. 10.1016/j.marpetgeo.2021.105108
34. 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
35. Changing inputs of continental and submarine weathering sources of Sr to the oceans during OAE 2 L. Nana Yobo et al. 10.1016/j.gca.2021.03.013
36. A New Fossil Marine Vertebrate Assemblage from the Upper Cretaceous Fairport Chalk Member of the Carlile Shale in Russell County, Kansas, U.S.A. L. Arroyo & K. Shimada 10.1660/062.126.0101
37. Late Cenomanian Plenus event in the Western Interior Seaway B. Sageman et al. 10.1016/j.cretres.2023.105798
38. 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
39. Centennial to millennial variability of greenhouse climate across the mid-Cenomanian event C. Ma et al. 10.1130/G48734.1
40. Quantifying large-scale continental shelf margin growth and dynamics across middle-Cretaceous Arctic Alaska with detrital zircon U-Pb dating R. Lease et al. 10.1130/G49118.1
41. Geochemistry of a thermally immature Eagle Ford Group drill core in central Texas K. French et al. 10.1016/j.orggeochem.2019.02.007
42. Regional chronostratigraphic synthesis of the Cenomanian-Turonian Oceanic Anoxic Event 2 (OAE2) interval, Western Interior Basin (USA): New Re-Os chemostratigraphy and 40Ar/39Ar geochronology M. Jones et al. 10.1130/B35594.1
43. Late Cretaceous to Palaeogene carbon isotope, calcareous nannofossil and foraminifera stratigraphy of the Chalk Group, Central North Sea J. Eldrett et al. 10.1016/j.marpetgeo.2020.104789
44. Chronostratigraphic framework and depositional environments in the organic‐rich, mudstone‐dominated Eagle Ford Group, Texas, USA D. Minisini et al. 10.1111/sed.12437
45. A new marine palynomorph from the Turonian (Upper Cretaceous) in the USA P. Dodsworth & J. Eldrett 10.1016/j.revpalbo.2018.12.003
46. Depositional environments and controls on the stratigraphic architecture of the Cenomanian Buda Limestone in west Texas, U.S.A. F. Valencia et al. 10.1016/j.marpetgeo.2021.105275
47. 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
48. Revisiting paleoenvironmental analyses and interpretations of organic-rich deposits: The importance of TOC corrections B. Hart & M. Hofmann 10.1016/j.orggeochem.2022.104434
49. Distribution of Albian dinoflagellate cyst associations along a proximal–distal transect across the Iberian margin R. Sánchez-Pellicer et al. 10.1016/j.cretres.2018.08.004
50. New Constraints on Global Geochemical Cycling During Oceanic Anoxic Event 2 (Late Cretaceous) From a 6‐Million‐year Long Molybdenum‐Isotope Record A. Dickson et al. 10.1029/2020GC009246