On the public citation graph
Basalt‐seawater interaction, the Plenus Cold Event, enhanced weathering and geochemical change: deconstructing Oceanic Anoxic Event 2 (Cenomanian–Turonian, Late Cretaceous)
0 signed · 316 inferred · view as graph
Inferred edges come from two machine sources: sweeps of open repository metadata (mostly SSRN and Zenodo), and a bulk OpenAlex citation snapshot. Every row below is labelled with the one it came from. Neither is a complete citation index — absence here is not evidence of absence.
Is this your work? Sign in with ORCID and put your name on the
claims that are yours.
Reference health. See whether every reference in this work resolves to a
known work and none has been retracted — and get a dated CiteStamped
badge you can embed.
What this work says
Outgoing claims: the papers this work cites, builds on, or argues with.
inferredcites →https://doi.org/10.1002/2014gc005528openalex-snapshot
Spatial extent and degree of oxygen depletion in the deep proto‐ N orth A tlantic basin during O ceanic A noxic E vent 2
inferredcites →https://doi.org/10.1002/2014pa002741openalex-snapshot
Upper ocean oxygenation dynamics from I/Ca ratios during the Cenomanian‐Turonian OAE 2
inferredcites →https://doi.org/10.1002/2015pa002869openalex-snapshot
Biogeochemical sulfur cycling during Cretaceous oceanic anoxic events: A comparison of OAE1a and OAE2
inferredcites →https://doi.org/10.1006/cres.1994.1007openalex-snapshot
Quantitative estimates of calcareous nannofossil changes across the Plenus Marls (latest Cenomanian), Dover, England: implications for the generation of the Cenomanian-Turonian Boundary Event
inferredcites →https://doi.org/10.1006/cres.1997.0076openalex-snapshot
Cyclicity of Cenomanian-Turonian organic-carbon-rich sediments in the Tarfaya Atlantic Coastal Basin (Morocco)
inferredcites →https://doi.org/10.1007/978-3-642-68409-8_16openalex-snapshot
Turonian Black Shales in the Moroccan Coastal Basins: First Upwelling in the Atlantic Ocean?
inferredcites →https://doi.org/10.1007/978-94-015-6861-6_6openalex-snapshot
Stratigraphy, Geochemistry, and Paleoceanography of Organic Carbon-Rich Cretaceous Sequences
inferredcites →https://doi.org/10.1007/s00531-003-0315-1openalex-snapshot
Cenomanian palaeotemperatures derived from the oxygen isotopic composition of brachiopods and belemnites: evaluation of Cretaceous palaeotemperature proxies
inferredcites →https://doi.org/10.1007/s00531-004-0440-5openalex-snapshot
Orbital-scale record of the late Cenomanian?Turonian oceanic anoxic event (OAE-2) in the Tarfaya Basin (Morocco)
inferredcites →https://doi.org/10.1016/0009-2541(66)90011-8openalex-snapshot
Isotope geochemistry of sedimentary sulfates
inferredcites →https://doi.org/10.1016/0012-821x(93)90126-topenalex-snapshot
Elemental abundance anomalies in the late Cenomanian extinction interval: a search for the source(s)
inferredcites →https://doi.org/10.1016/0016-7037(79)90095-4openalex-snapshot
Early oxidation of organic matter in pelagic sediments of the eastern equatorial Atlantic: suboxic diagenesis
inferredcites →https://doi.org/10.1016/0025-3227(86)90093-9openalex-snapshot
Global geochemical cycles of carbon, sulfur and oxygen
inferredcites →https://doi.org/10.1016/0031-0182(94)90024-8openalex-snapshot
Strontium isotope stratigraphy for Late Cretaceous time: Direct numerical calibration of the Sr isotope curve based on the US Western Interior
inferredcites →https://doi.org/10.1016/0195-6671(83)90025-3openalex-snapshot
Geochemistry of the late Cenomanian-early Turonian chalks of the Paris Basin: Manganese and carbon isotopes in carbonates as paleooceanographic indicators
inferredcites →https://doi.org/10.1016/j.chemgeo.2006.05.008openalex-snapshot
Anoxic vs dysoxic events reflected in sediment geochemistry during the Cenomanian–Turonian Boundary Event (Cretaceous) in the Umbria–Marche Basin of central Italy
inferredcites →https://doi.org/10.1016/j.chemgeo.2009.09.001openalex-snapshot
Environmental analysis of paleoceanographic systems based on molybdenum–uranium covariation
inferredcites →https://doi.org/10.1016/j.chemgeo.2011.09.009openalex-snapshot
Analysis of marine environmental conditions based onmolybdenum–uranium covariation—Applications to Mesozoic paleoceanography
inferredcites →https://doi.org/10.1016/j.cretres.2006.07.004openalex-snapshot
Fauna and palaeoecology of the Middle Cenomanian Praeactinocamax primus Event at the type locality, Wunstorf quarry, northern Germany
inferredcites →https://doi.org/10.1016/j.cretres.2008.05.020openalex-snapshot
Oceanic events and biotic effects of the Cenomanian-Turonian anoxic event, Tarfaya Basin, Morocco
inferredcites →https://doi.org/10.1016/j.cretres.2013.03.005openalex-snapshot
Cenomanian–Turonian carbon isotope stratigraphy of the Western Canadian Sedimentary Basin
inferredcites →https://doi.org/10.1016/j.cretres.2015.04.010openalex-snapshot
An astronomically calibrated stratigraphy of the Cenomanian, Turonian and earliest Coniacian from the Cretaceous Western Interior Seaway, USA: Implications for global chronostratigraphy
inferredcites →https://doi.org/10.1016/j.earscirev.2005.10.004openalex-snapshot
Reconstruction of changes in global sulfur cycling from marine sulfate isotopes
inferredcites →https://doi.org/10.1016/j.epsl.2007.01.027openalex-snapshot
Contemporaneous massive subaerial volcanism and late cretaceous Oceanic Anoxic Event 2
inferredcites →https://doi.org/10.1016/j.epsl.2008.10.020openalex-snapshot
C-isotope stratigraphy and paleoenvironmental changes across OAE2 (mid-Cretaceous) from shallow-water platform carbonates of southern Mexico
inferredcites →https://doi.org/10.1016/j.epsl.2010.02.027openalex-snapshot
A CO2 decrease-driven cooling and increased latitudinal temperature gradient during the mid-Cretaceous Oceanic Anoxic Event 2
inferredcites →https://doi.org/10.1016/j.epsl.2011.06.029openalex-snapshot
Significant increases in global weathering during Oceanic Anoxic Events 1a and 2 indicated by calcium isotopes
inferredcites →https://doi.org/10.1016/j.epsl.2012.01.037openalex-snapshot
Water mass circulation on Demerara Rise during the Late Cretaceous based on Nd isotopes
inferredcites →https://doi.org/10.1016/j.epsl.2013.05.030openalex-snapshot
Secular change in northwestern Tethyan water-mass oxygenation during the late Hauterivian–early Aptian
inferredcites →https://doi.org/10.1016/j.epsl.2013.05.053openalex-snapshot
Changing ocean circulation and hydrothermal inputs during Ocean Anoxic Event 2 (Cenomanian–Turonian): Evidence from Nd-isotopes in the European shelf sea
inferredcites →https://doi.org/10.1016/j.epsl.2013.12.024openalex-snapshot
Marine 187Os/188Os isotope stratigraphy reveals the interaction of volcanism and ocean circulation during Oceanic Anoxic Event 2
inferredcites →https://doi.org/10.1016/j.epsl.2014.07.018openalex-snapshot
Heterogeneous oxygenation states in the Atlantic and Tethys oceans during Oceanic Anoxic Event 2
inferredcites →https://doi.org/10.1016/j.epsl.2015.07.020openalex-snapshot
Pacific 187 Os/ 188 Os isotope chemistry and U–Pb geochronology: Synchroneity of global Os isotope change across OAE 2
inferredcites →https://doi.org/10.1016/j.epsl.2016.02.006openalex-snapshot
Molybdenum drawdown during Cretaceous Oceanic Anoxic Event 2
inferredcites →https://doi.org/10.1016/j.gca.2006.01.020openalex-snapshot
Secular variation in the major-ion chemistry of seawater: Evidence from fluid inclusions in Cretaceous halites
inferredcites →https://doi.org/10.1016/j.gca.2015.12.036openalex-snapshot
Basin-scale controls on the molybdenum-isotope composition of seawater during Oceanic Anoxic Event 2 (Late Cretaceous)
inferredcites →https://doi.org/10.1016/j.gca.2016.04.039openalex-snapshot
Response of the Cr isotope proxy to Cretaceous Ocean Anoxic Event 2 in a pelagic carbonate succession from the Western Interior Seaway
inferredcites →https://doi.org/10.1016/j.marmicro.2003.08.004openalex-snapshot
Age and paleoenvironment of the Cenomanian–Turonian global stratotype section and point at Pueblo, Colorado
inferredcites →https://doi.org/10.1016/j.palaeo.2005.05.011openalex-snapshot
The trace metal content of recent organic carbon-rich sediments: Implications for Cretaceous black shale formation
inferredcites →https://doi.org/10.1016/j.palaeo.2008.01.003openalex-snapshot
Strontium isotope stratigraphy in the upper Cenomanian shallow-water carbonates of the southern Apennines: Short-term perturbations of marine 87Sr/86Sr during the oceanic anoxic event 2
inferredcites →https://doi.org/10.1016/j.palaeo.2008.11.005openalex-snapshot
Paleo-redox conditions during OAE 2 reflected in Demerara Rise sediment geochemistry (ODP Leg 207)
inferredcites →https://doi.org/10.1016/j.palaeo.2009.06.012openalex-snapshot
The Cenomanian–Turonian boundary event, OAE2 and palaeoenvironmental change in epicontinental seas: New insights from the dinocyst and geochemical records
inferredcites →https://doi.org/10.1016/j.palaeo.2009.07.003openalex-snapshot
Reconstruction of water column anoxia in the equatorial Atlantic during the Cenomanian–Turonian oceanic anoxic event using biomarker and trace metal proxies
inferredcites →https://doi.org/10.1016/j.palaeo.2014.07.002openalex-snapshot
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
inferredcites →https://doi.org/10.1016/j.revmic.2006.04.003openalex-snapshot
Paleoenvironmental changes across the Cenomanian/Turonian Boundary Event (Oceanic Anoxic Event 2) as indicated by benthic foraminifera from the Demerara Rise (ODP Leg 207)
inferredcites →https://doi.org/10.1016/s0016-7878(63)80011-5openalex-snapshot
The stratigraphy of the Actinocamax plenus Subzone (Turonian) in the Anglo-Paris Basin
inferredcites →https://doi.org/10.1016/s0016-7878(75)80061-7openalex-snapshot
The petrology of the Chalk
inferredcites →https://doi.org/10.1016/s0031-0182(96)00129-0openalex-snapshot
Cenomanian-Turonian carbon isotope events recorded in terrestrial organic matter from northern Japan
inferredcites →https://doi.org/10.1016/s0031-0182(97)00069-2openalex-snapshot
Evaluation of the application of rare-earth elements to paleoceanography
inferredcites →https://doi.org/10.1016/s1631-0713(03)00006-3openalex-snapshot
On the ages of flood basalt events
inferredcites →https://doi.org/10.1017/s0016756800010451openalex-snapshot
Carbon- and oxygen-isotope stratigraphy of the English Chalk and Italian Scaglia and its palaeoclimatic significance
inferredcites →https://doi.org/10.1017/s0016756800019725openalex-snapshot
The geochemistry of the Plenus Marls at Dover, England: evidence of fluctuating oceanographic conditions and of glacial control during the development of the Cenomanian–Turonian δ13C anomaly
inferredcites →https://doi.org/10.1017/s0016756806002421openalex-snapshot
Secular variation in Late Cretaceous carbon isotopes: a new δ13C carbonate reference curve for the Cenomanian–Campanian (99.6–70.6 Ma)
inferredcites →https://doi.org/10.1029/2003pa000950openalex-snapshot
Black shale deposition on the northwest African Shelf during the Cenomanian/Turonian oceanic anoxic event: Climate coupling and global organic carbon burial
inferredcites →https://doi.org/10.1029/2004gc000850openalex-snapshot
Stable organic carbon isotope stratigraphy across Oceanic Anoxic Event 2 of Demerara Rise, western tropical Atlantic
inferredcites →https://doi.org/10.1029/2004pa001015openalex-snapshot
Midlatitude shelf seas in the Cenomanian‐Turonian greenhouse world: Temperature evolution and North Atlantic circulation
inferredcites →https://doi.org/10.1029/2004pa001093openalex-snapshot
Trace element abundances in the Rock Canyon Anticline, Pueblo, Colorado, marine sedimentary section and their relationship to Caribbean plateau construction and oxygen anoxic event 2
inferredcites →https://doi.org/10.1029/2004pa001112openalex-snapshot
Mo–total organic carbon covariation in modern anoxic marine environments: Implications for analysis of paleoredox and paleohydrographic conditions
inferredcites →https://doi.org/10.1029/2006pa001349openalex-snapshot
Tropical warming and intermittent cooling during the Cenomanian/Turonian oceanic anoxic event 2: Sea surface temperature records from the equatorial Atlantic
inferredcites →https://doi.org/10.1029/2009gc002788openalex-snapshot
Geochemistry of oceanic anoxic events
inferredcites →https://doi.org/10.1029/2010pa002081openalex-snapshot
Black shale deposition, atmospheric CO 2 drawdown, and cooling during the Cenomanian‐Turonian Oceanic Anoxic Event
inferredcites →https://doi.org/10.1029/94gl03047openalex-snapshot
Rare earth element deposition in pelagic sediment at the Cenomanian‐Turonian Boundary, Exmouth Plateau
inferredcites →https://doi.org/10.1029/jz068i014p04209openalex-snapshot
Rare-Earth distributions in the marine environment
inferredcites →https://doi.org/10.1029/pa005i005p00823openalex-snapshot
Application of the Ce anomaly as a paleoredox indicator: The ground rules
inferredcites →https://doi.org/10.1038/20659openalex-snapshot
A large and abrupt fall in atmospheric CO2 concentration during Cretaceous times
inferredcites →https://doi.org/10.1038/nature07076openalex-snapshot
Cretaceous oceanic anoxic event 2 triggered by a massive magmatic episode
inferredcites →https://doi.org/10.1038/ngeo1875openalex-snapshot
Lithium isotope evidence for enhanced weathering during Oceanic Anoxic Event 2
inferredcites →https://doi.org/10.1038/ngeo743openalex-snapshot
Volcanic triggering of a biogeochemical cascade during Oceanic Anoxic Event 2
inferredcites →https://doi.org/10.1038/ngeo757openalex-snapshot
Carbon sequestration activated by a volcanic CO2 pulse during Ocean Anoxic Event 2
inferredcites →https://doi.org/10.1046/j.1365-3121.2000.00295.xopenalex-snapshot
The marine osmium isotope record
inferredcites →https://doi.org/10.1073/pnas.1305304110openalex-snapshot
Sulfur isotopes track the global extent and dynamics of euxinia during Cretaceous Oceanic Anoxic Event 2
inferredcites →https://doi.org/10.1098/rsta.2003.1240openalex-snapshot
Evidence for rapid climate change in the Mesozoic–Palaeogene greenhouse world
inferredcites →https://doi.org/10.1111/sed.12303openalex-snapshot
A Southern Hemisphere record of global trace‐metal drawdown and orbital modulation of organic‐matter burial across the Cenomanian–Turonian boundary (Ocean Drilling Program Site 1138, Kerguelen Plateau)
inferredcites →https://doi.org/10.1126/science.1095258openalex-snapshot
Seawater Sulfur Isotope Fluctuations in the Cretaceous
inferredcites →https://doi.org/10.1126/science.1214697openalex-snapshot
Lithium Isotope History of Cenozoic Seawater: Changes in Silicate Weathering and Reverse Weathering
inferredcites →https://doi.org/10.1127/0078-0421/2008/0043-0065openalex-snapshot
The Cenomanian Turonian of the Wunstorf section (North Germany): global stratigraphic reference section and new orbital time scale for Oceanic Anoxic Event 2
inferredcites →https://doi.org/10.1127/nos/2015/0066openalex-snapshot
Carbon- and oxygen-isotope records of mid-Cretaceous Tethyan pelagic sequences from the Umbria – Marche and Belluno Basins (Italy)
inferredcites →https://doi.org/10.1130/0091-7613(1999)027<0535:siralb>2.3.co;2openalex-snapshot
Sulfur isotope records around Livello Bonarelli (northern Apennines, Italy) black shale at the Cenomanian-Turonian boundary
inferredcites →https://doi.org/10.1130/0091-7613(1999)027<0699:noiefl>2.3.co;2openalex-snapshot
New oxygen isotope evidence for long-term Cretaceous climatic change in the Southern Hemisphere
inferredcites →https://doi.org/10.1130/0091-7613(2002)030<0123:dsproe>2.0.co;2openalex-snapshot
Deep-sea paleotemperature record of extreme warmth during the Cretaceous
inferredcites →https://doi.org/10.1130/0091-7613(2002)030<0299:jtttit>2.0.co;2openalex-snapshot
Jiggling the tropical thermostat in the Cretaceous hothouse
inferredcites →https://doi.org/10.1130/2015.2511(15)openalex-snapshot
Environmental consequences of Ontong Java Plateau and Kerguelen Plateau volcanism
inferredcites →https://doi.org/10.1130/b30922.1openalex-snapshot
Testing the astronomical time scale for oceanic anoxic event 2, and its extension into Cenomanian strata of the Western Interior Basin (USA)
inferredcites →https://doi.org/10.1130/g22074.1openalex-snapshot
Orbital time scale and new C-isotope record for Cenomanian-Turonian boundary stratotype
inferredcites →https://doi.org/10.1130/g23874a.1openalex-snapshot
Mid-Cretaceous (Albian–Santonian) sea surface temperature record of the tropical Atlantic Ocean
inferredcites →https://doi.org/10.1130/g24893a.1openalex-snapshot
Stepwise extinction of larger foraminifers at the Cenomanian-Turonian boundary: A shallow-water perspective on nutrient fluctuations during Oceanic Anoxic Event 2 (Bonarelli Event)
inferredcites →https://doi.org/10.1130/g31145.1openalex-snapshot
Iodine to calcium ratios in marine carbonate as a paleo-redox proxy during oceanic anoxic events
inferredcites →https://doi.org/10.1130/g32261.1openalex-snapshot
Intercalibration of radioisotopic and astrochronologic time scales for the Cenomanian-Turonian boundary interval, Western Interior Basin, USA
inferredcites →https://doi.org/10.1130/g32701.1openalex-snapshot
Evolution of middle to Late Cretaceous oceans—A 55 m.y. record of Earth's temperature and carbon cycle
inferredcites →https://doi.org/10.1130/g34929.1openalex-snapshot
A perturbed hydrological cycle during Oceanic Anoxic Event 2
inferredcites →https://doi.org/10.1130/g35520.1openalex-snapshot
Decoupling of the carbon cycle during Ocean Anoxic Event 2
inferredcites →https://doi.org/10.1130/g35732.1openalex-snapshot
Arctic black shale formation during Cretaceous Oceanic Anoxic Event 2
inferredcites →https://doi.org/10.1130/g36837.1openalex-snapshot
A continental-weathering control on orbitally driven redox-nutrient cycling during Cretaceous Oceanic Anoxic Event 2
inferredcites →https://doi.org/10.1130/g37354.1openalex-snapshot
A climatic control on reorganization of ocean circulation during the mid-Cenomanian event and Cenomanian-Turonian oceanic anoxic event (OAE 2): Nd isotope evidence
inferredcites →https://doi.org/10.1130/spe196-p325openalex-snapshot
REE and Nd isotopes in conodont apatite: Variations with geological age and depositional environment
inferredcites →https://doi.org/10.1134/s0024490213060047openalex-snapshot
The late Cenomanian paleoecological event (OAE 2) in the eastern Caucasus basin of Northern Peri-Tethys
inferredcites →https://doi.org/10.1144/0016-764903-077openalex-snapshot
Carbon-isotope stratigraphy recorded by the Cenomanian–Turonian Oceanic Anoxic Event: correlation and implications based on three key localities
inferredcites →https://doi.org/10.1144/0016-764905-046openalex-snapshot
Upper Cretaceous carbon- and oxygen-isotope stratigraphy of hemipelagic carbonate facies from southern Tibet, China
inferredcites →https://doi.org/10.1144/gsjgs.137.2.0171openalex-snapshot
Cretaceous anoxic events: from continents to oceans
inferredcites →https://doi.org/10.1144/gsjgs.150.1.0029openalex-snapshot
Chemostratigraphy versus biostratigraphy: data from around the Cenomanian–Turonian boundary
inferredcites →https://doi.org/10.1144/gsjgs.155.4.0619openalex-snapshot
Oceanic plateau formation: a cause of mass extinction and black shale deposition around the Cenomanian–Turonian boundary?
inferredcites →https://doi.org/10.1144/gsl.sp.1987.026.01.24openalex-snapshot
The Cenomanian-Turonian Oceanic Anoxic Event, I. Stratigraphy and distribution of organic carbon-rich beds and the marine δ 13 C excursion
inferredcites →https://doi.org/10.1144/gsl.sp.1993.070.01.14openalex-snapshot
Strontium isotope stratigraphy for the Late Cretaceous: a new curve, based on the English Chalk
inferredcites →https://doi.org/10.1144/jgs.158.4.685openalex-snapshot
Geochemistry of pelagic and hemipelagic carbonates: criteria for identifying systems tracts and sea-level change
inferredcites →https://doi.org/10.1306/2f91892d-16ce-11d7-8645000102c1865dopenalex-snapshot
Carbon Isotope Fluctuations in Cretaceous Pelagic Limestones: Potential Stratigraphic and Petroleum Exploration Tool
inferredcites →https://doi.org/10.18814/epiiugs/2005/v28i2/003openalex-snapshot
The Global Boundary Stratotype Section and Point for the base of the Turonian Stage of the Cretaceous: Pueblo, Colorado, U.S.A.
inferredcites →https://doi.org/10.2110/csp.98.06.0079openalex-snapshot
Foraminiferal Paleoecology and Paleoceanography of the Greenhorn Cycle Along the Southwestern Margin of the Western Interior Sea
inferredcites →https://doi.org/10.2110/jsr.2014.38openalex-snapshot
Cenomanian To Campanian Carbon Isotope Chemostratigraphy from the Western Interior Basin, U.S.A
inferredcites →https://doi.org/10.2113/gsecongeo.91.1.36openalex-snapshot
Sedimentary geochemistry of manganese; implications for the environment of formation of manganiferous black shales
inferredcites →https://doi.org/10.2113/gsecongeo.92.7-8.836openalex-snapshot
Potential links between ocean plateau volcanism and global ocean anoxia at the Cenomanian-Turonian boundary
inferredcites →https://doi.org/10.2113/gsjfr.39.4.322openalex-snapshot
ONSET OF SEAWATER 87SR/86SR EXCURSION PRIOR TO CENOMANIAN-TURONIAN OCEANIC ANOXIC EVENT 2? NEW LATE CRETACEOUS STRONTIUM ISOTOPE CURVE FROM THE CENTRAL PACIFIC OCEAN
inferredcites →https://doi.org/10.2113/gssgfbull.vi.3.469openalex-snapshot
Preservation cyclique de la matiere organique amorphe des sediments au passage cenomanien-turonien dans le Bassin vocontien (Sud-Est France); controles paleo-oceanographiques
inferredcites →https://doi.org/10.2307/1485079openalex-snapshot
Cenomanian and Turonian Foraminifera from the Great Plains, United States
inferredcites →https://doi.org/10.2307/3515055openalex-snapshot
Timing and paleoceanography of oceanic dysoxia/anoxia in the late Barremian to early Aptian (Early Cretaceous)
inferredcites →https://doi.org/10.2475/ajs.301.2.112openalex-snapshot
Seawater strontium isotopes, oceanic anoxic events, and seafloor hydrothermal activity in the Jurassic and Cretaceous
inferredcites →https://doi.org/10.37570/bgsd-1996-43-08openalex-snapshot
Occurrence of the belemnite Actinocamax plenus in the - Cenomanian of SE France and its significance
inferredcites →https://doi.org/10.4202/app.2008.0411openalex-snapshot
Lower Turonian Record of BelemnitePraeactinocamaxfrom NW Siberia and Its Palaeogeographic Significance
inferredcites →https://doi.org/10.5169/seals-168658openalex-snapshot
Carbon-isotope stratigraphy of shallow-water limestones and implications for the timing of Late Cretaceous sea-level rise and anoxic events (Cenomanian-Turonian of the peri-Adriatic carbonate platform, Croatia)
inferredcites →https://doi.org/10.5194/bg-13-2859-2016openalex-snapshot
Equatorward phytoplankton migration during a cold spell within the Late Cretaceous super-greenhouse
inferredcites →https://doi.org/10.5194/cp-11-495-2015openalex-snapshot
Freshwater discharge controlled deposition of Cenomanian–Turonian black shales on the NW European epicontinental shelf (Wunstorf, northern Germany)
What points at this work
Incoming claims: where this work appears in other papers’ reference lists and arguments.
inferred← citeshttps://doi.org/10.2139/ssrn.4688214openalex-extracted
Reconstruction of a Deep-Time Critical Zone in Southern Patagonia (Mid-High Paleolatitude) During the Mid-Cretaceous Geenhouse
inferred← citeshttps://doi.org/10.1002/2017gc007153openalex-snapshot
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)
inferred← citeshttps://doi.org/10.1002/2017pa003146openalex-snapshot
Unraveling the onset of Cretaceous Oceanic Anoxic Event 2 in an extended sediment archive from the Tarfaya‐Laayoune Basin, Morocco
inferred← citeshttps://doi.org/10.1002/9781119507444.ch13openalex-snapshot
Assessing the Effect of Large Igneous Provinces on Global Oceanic Redox Conditions Using Non‐traditional Metal Isotopes (Molybdenum, Uranium, Thallium)
inferred← citeshttps://doi.org/10.1002/9781119507444.ch9openalex-snapshot
Phanerozoic Large Igneous Province, Petroleum System, and Source Rock Links
inferred← citeshttps://doi.org/10.1002/dep2.70033openalex-snapshot
The Cenomanian–Turonian boundary interval in the Western Canada Foreland Basin: Stratigraphy, geochemistry, geochronology and sea‐level changes recorded in expanded and condensed clastic successions
inferred← citeshttps://doi.org/10.1002/gj.70189openalex-snapshot
Mid‐Cenomanian Event Controls the Bioproductivity and Organic Preservation of Bituminous Limestones From North Jordan
inferred← citeshttps://doi.org/10.1007/978-3-031-25494-9_2openalex-snapshot
Carbonate Facies of Venezuela: From the Late Paleozoic to Modern Times
inferred← citeshttps://doi.org/10.1007/s00015-017-0296-xopenalex-snapshot
Integrated foraminifera and δ13C stratigraphy across the Cenomanian–Turonian event interval in the eastern Baltic (Lithuania)
inferred← citeshttps://doi.org/10.1007/s11430-019-9604-4openalex-snapshot
Two types of hyperthermal events in the Mesozoic-Cenozoic: Environmental impacts, biotic effects, and driving mechanisms
inferred← citeshttps://doi.org/10.1007/s11430-024-1421-8openalex-snapshot
Multi-spheric interactions driven differential formation and accumulation of hydrocarbon resources in the North Sea Basin
inferred← citeshttps://doi.org/10.1007/s11707-022-1071-5openalex-snapshot
Constraints of palaeoenvironment on organic matter of Benxi Formation shale and discussion on enrichment mechanism under different facies
inferred← citeshttps://doi.org/10.1007/s12517-016-2775-1openalex-snapshot
Chemostratigraphy of the Cenomanian-Turonian shallow-water carbonate: new correlation for the rudist levels from north Sinai, Egypt
inferred← citeshttps://doi.org/10.1007/s12517-021-09180-yopenalex-snapshot
Oceanic anoxic events in the Earth’s geological history and signature of such event in the Paleocene-Eocene Himalayan foreland basin sediment records of NW Himalaya, India
inferred← citeshttps://doi.org/10.1007/s13146-022-00768-3openalex-snapshot
Sedimentological and geochemical approaches for determination of the palaeoceanographic and palaeoclimatic conditions of Lower Cretaceous marine deposits in the eastern part of Sakarya Zone, NE Turkey
inferred← citeshttps://doi.org/10.1016/b978-0-323-99762-1.00033-4openalex-snapshot
Ocean redox evolution past and present
inferred← citeshttps://doi.org/10.1016/bs.sats.2020.08.001openalex-snapshot
Comparative carbon isotope chemostratigraphy of major Late Devonian biotic crises
inferred← citeshttps://doi.org/10.1016/j.catena.2024.108054openalex-snapshot
Reconstruction of a deep-time critical zone in southern patagonia (mid-high paleolatitude) during the mid-cretaceous greenhouse
inferred← citeshttps://doi.org/10.1016/j.chemgeo.2017.03.016openalex-snapshot
Organically bound iodine as a bottom-water redox proxy: Preliminary validation and application
inferred← citeshttps://doi.org/10.1016/j.chemgeo.2021.120399openalex-snapshot
A new view on the evolution of seawater molybdenum inventories before and during the Cretaceous Oceanic Anoxic Event 2
inferred← citeshttps://doi.org/10.1016/j.chemgeo.2023.121411openalex-snapshot
Regional conditions cause contrasting behaviour in U-isotope fractionation in black shales: Constraints for global ocean palaeo-redox reconstructions
inferred← citeshttps://doi.org/10.1016/j.chemgeo.2024.122436openalex-snapshot
Redox-sensitive metals and δ238U in red and grey shales: Exploring a new archive for palaeo-redox studies
inferred← citeshttps://doi.org/10.1016/j.chemgeo.2024.122462openalex-snapshot
Evolution of continental inputs and watermass during cretaceous oceanic anoxic event 2 in the Neo-Tethyan region: Evidence from Nd-isotopes in southern Tibet
inferred← citeshttps://doi.org/10.1016/j.chemgeo.2024.122477openalex-snapshot
Trace metal evolution of the Late Cretaceous Ocean
inferred← citeshttps://doi.org/10.1016/j.cretres.2019.07.007openalex-snapshot
Change from rimmed to ramp platform forced by regional and global events in the Cretaceous of the Friuli-Adriatic Platform (Southern Alps, Italy)
inferred← citeshttps://doi.org/10.1016/j.cretres.2019.104228openalex-snapshot
Authigenic, volcanogenic, and detrital influences on the Cenomanian–Turonian clay sedimentation in the Western Interior Basin: Implications for palaeoclimatic reconstructions
inferred← citeshttps://doi.org/10.1016/j.cretres.2020.104590openalex-snapshot
Njoerdichthys dyckerhoffi gen. et sp. nov. (Pycnodontiformes, lower Turonian) northward migration caused by the Cretaceous Thermal Maximum
inferred← citeshttps://doi.org/10.1016/j.cretres.2020.104593openalex-snapshot
Patterns of planktonic foraminiferal extinctions and eclipses during Oceanic Anoxic Event 2 at Eastbourne (SE England) and other mid-low latitude locations
inferred← citeshttps://doi.org/10.1016/j.cretres.2021.104964openalex-snapshot
The mid-Cretaceous debate: Evidence from the foraminifera
inferred← citeshttps://doi.org/10.1016/j.cretres.2021.105022openalex-snapshot
Exploring the role of High Arctic Large Igneous Province volcanism on Early Cretaceous Arctic forests
inferred← citeshttps://doi.org/10.1016/j.cretres.2022.105151openalex-snapshot
Proliferation of Chondrodonta in upper Cenomanian shallow-water limestones of the Adriatic Carbonate Platform (Croatia) as a proxy of environmental instability
inferred← citeshttps://doi.org/10.1016/j.cretres.2022.105264openalex-snapshot
Biostratigraphic and chemostratigraphic record of the Cenomanian/Turonian boundary interval of the Tellian Atlas (Algeria)
inferred← citeshttps://doi.org/10.1016/j.cretres.2022.105329openalex-snapshot
Geochemical expression of sequence stratigraphic surfaces: A case from Upper Cretaceous shallow-water carbonates of southeastern Neo-Tethys margin, SW Iran
inferred← citeshttps://doi.org/10.1016/j.cretres.2022.105380openalex-snapshot
The expression of late Cenomanian–Coniacian episodes of accelerated global change in the sedimentary record of the Mexican Interior Basin
inferred← citeshttps://doi.org/10.1016/j.cretres.2023.105555openalex-snapshot
Cretaceous southern high latitude benthic foraminiferal assemblages during OAE 2 at IODP Site U1516, Mentelle Basin, Indian Ocean
inferred← citeshttps://doi.org/10.1016/j.cretres.2023.105568openalex-snapshot
Chemostratigraphy of the lower Danubian Cretaceous Group (Cenomanian–lower Turonian, Bavaria, SE Germany)—A new carbon isotope reference curve and inter-basinal correlation
inferred← citeshttps://doi.org/10.1016/j.cretres.2023.105574openalex-snapshot
Paleoenvironmental significance of the carbon isotope record across the Cenomanian–Turonian transition and the Oceanic Anoxic Event 2 (OAE2) in the southeastern Neotethys, Zagros, Iran
inferred← citeshttps://doi.org/10.1016/j.cretres.2023.105578openalex-snapshot
Peatland wildfires in the Lower Cretaceous Damoguaihe Formation, Hailar Basin, Northeast China
inferred← citeshttps://doi.org/10.1016/j.cretres.2023.105798openalex-snapshot
Late Cenomanian Plenus event in the Western Interior Seaway
inferred← citeshttps://doi.org/10.1016/j.cretres.2024.106075openalex-snapshot
First dinosaur ichnofauna from the Bauru Group indicates Cenomanian–Turonian events led to an ‘Ornithischian Hiatus’ in the Upper Cretaceous of Southeast Brazil
inferred← citeshttps://doi.org/10.1016/j.cretres.2025.106133openalex-snapshot
Paleoenvironmental changes in the western Tethys carbonate platforms during OAE-2: Implications from phosphorus, δ18O, δ13C and facies analysis
inferred← citeshttps://doi.org/10.1016/j.cretres.2025.106162openalex-snapshot
Palaeoceanographic changes during the late Albian-early Turonian in the Sergipe-Alagoas Basin (Northeast Brazil) and their link with global events
inferred← citeshttps://doi.org/10.1016/j.cretres.2025.106204openalex-snapshot
Sea-level and paleoenvironmental changes revealed by benthic foraminifera across Oceanic Anoxic Event 2 (OAE 2) at Eastbourne (SE England)
inferred← citeshttps://doi.org/10.1016/j.cretres.2025.106213openalex-snapshot
Calcareous nannofossil biostratigraphy of the upper Cretaceous to lower Paleocene in Zagros Basin, western Iran
inferred← citeshttps://doi.org/10.1016/j.earscirev.2017.07.012openalex-snapshot
Cretaceous sea-surface temperature evolution: Constraints from TEX86 and planktonic foraminiferal oxygen isotopes
inferred← citeshttps://doi.org/10.1016/j.earscirev.2020.103123openalex-snapshot
Data-model comparison reveals key environmental changes leading to Cenomanian-Turonian Oceanic Anoxic Event 2
inferred← citeshttps://doi.org/10.1016/j.earscirev.2021.103871openalex-snapshot
Fossil evidence that increased wildfire activity occurs in tandem with periods of global warming in Earth's past
inferred← citeshttps://doi.org/10.1016/j.earscirev.2024.104851openalex-snapshot
Statistical approaches for improved definition of carbon isotope excursions
inferred← citeshttps://doi.org/10.1016/j.earscirev.2024.104903openalex-snapshot
Quantifying the pattern of organic carbon burial through Cretaceous Oceanic Anoxic Event 2
inferred← citeshttps://doi.org/10.1016/j.epsl.2018.07.029openalex-snapshot
Obliquity pacing of the hydrological cycle during the Oceanic Anoxic Event 2
inferred← citeshttps://doi.org/10.1016/j.epsl.2019.01.023openalex-snapshot
Influence of the High Arctic Igneous Province on the Cenomanian/Turonian boundary interval, Sverdrup Basin, High Canadian Arctic
inferred← citeshttps://doi.org/10.1016/j.epsl.2019.04.008openalex-snapshot
Oxygen minimum zone-type biogeochemical cycling in the Cenomanian-Turonian Proto-North Atlantic across Oceanic Anoxic Event 2
inferred← citeshttps://doi.org/10.1016/j.epsl.2019.04.028openalex-snapshot
High-resolution records of Oceanic Anoxic Event 2: Insights into the timing, duration and extent of environmental perturbations from the palaeo-South Pacific Ocean
inferred← citeshttps://doi.org/10.1016/j.epsl.2020.116427openalex-snapshot
Zinc- and cadmium-isotope evidence for redox-driven perturbations to global micronutrient cycles during Oceanic Anoxic Event 2 (Late Cretaceous)
inferred← citeshttps://doi.org/10.1016/j.epsl.2021.117331openalex-snapshot
Enhanced ocean connectivity and volcanism instigated global onset of Cretaceous Oceanic Anoxic Event 2 (OAE2) ∼94.5 million years ago
inferred← citeshttps://doi.org/10.1016/j.fuel.2019.04.095openalex-snapshot
Paleoenvironmental conditions and organic matter accumulation in Upper Paleozoic organic-rich rocks in the east margin of the Ordos Basin, China
inferred← citeshttps://doi.org/10.1016/j.gca.2020.04.002openalex-snapshot
High resolution osmium data record three distinct pulses of magmatic activity during cretaceous Oceanic Anoxic Event 2 (OAE-2)
inferred← citeshttps://doi.org/10.1016/j.gca.2021.03.013openalex-snapshot
Changing inputs of continental and submarine weathering sources of Sr to the oceans during OAE 2
inferred← citeshttps://doi.org/10.1016/j.gca.2022.05.010openalex-snapshot
Uranium isotope reconstruction of ocean deoxygenation during OAE 2 hampered by uncertainties in fractionation factors and local U-cycling
inferred← citeshttps://doi.org/10.1016/j.gca.2022.06.016openalex-snapshot
LIP volcanism (not anoxia) tracked by Cr isotopes during Ocean Anoxic Event 2 in the proto-North Atlantic region
inferred← citeshttps://doi.org/10.1016/j.gca.2024.10.023openalex-snapshot
Iron Isotopes reveal volcanogenic input during Oceanic Anoxic Event 2 (OAE 2 ∼ 94 Ma)
inferred← citeshttps://doi.org/10.1016/j.gca.2025.12.022openalex-snapshot
Late Cretaceous cerium anomalies and globally distinctive redox responses before, during and after Oceanic Anoxic Event 2
inferred← citeshttps://doi.org/10.1016/j.gloplacha.2018.04.004openalex-snapshot
The rise and fall of the Cretaceous Hot Greenhouse climate
inferred← citeshttps://doi.org/10.1016/j.gloplacha.2018.08.009openalex-snapshot
The expression of early Aptian to latest Cenomanian oceanic anoxic events in the sedimentary record of the Briançonnais domain
inferred← citeshttps://doi.org/10.1016/j.gloplacha.2019.01.020openalex-snapshot
Global bioevents and the Cretaceous/Paleogene boundary in Texas and Alabama: Stratigraphy, correlation and ocean acidification
inferred← citeshttps://doi.org/10.1016/j.gloplacha.2020.103373openalex-snapshot
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
inferred← citeshttps://doi.org/10.1016/j.gloplacha.2021.103424openalex-snapshot
Assessing the contribution of the La Luna Sea to the global sink of organic carbon during the Cenomanian-Turonian Oceanic Anoxic Event 2 (OAE2)
inferred← citeshttps://doi.org/10.1016/j.gloplacha.2021.103595openalex-snapshot
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)
inferred← citeshttps://doi.org/10.1016/j.gloplacha.2021.103678openalex-snapshot
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)
inferred← citeshttps://doi.org/10.1016/j.gloplacha.2022.103735openalex-snapshot
Enhanced hydrological cycle during Oceanic Anoxic Event 2 at southern high latitudes: New insights from IODP Site U1516
inferred← citeshttps://doi.org/10.1016/j.gloplacha.2022.103881openalex-snapshot
Isotopic evidence for changes in the mercury and zinc cycles during Oceanic Anoxic Event 2 in the northwestern Tethys, Austria
inferred← citeshttps://doi.org/10.1016/j.gloplacha.2023.104117openalex-snapshot
Phytoplankton dynamics and nitrogen cycling during Oceanic Anoxic Event 2 (Cenomanian/Turonian) in the upwelling zone of the NE proto-North Atlantic
inferred← citeshttps://doi.org/10.1016/j.gloplacha.2023.104182openalex-snapshot
The response of nitrogen and sulfur cycles to ocean deoxygenation across the Cenomanian-Turonian boundary
inferred← citeshttps://doi.org/10.1016/j.gloplacha.2024.104365openalex-snapshot
Enhanced primary productivity and perturbation of marine nitrogen cycling during the onset of the Cambrian SPICE event
inferred← citeshttps://doi.org/10.1016/j.gloplacha.2024.104494openalex-snapshot
Marine sulfate sulfur isotopic evidence for enhanced terrestrial weathering and expansion of oceanic anoxia during the Devonian-Carboniferous transition
inferred← citeshttps://doi.org/10.1016/j.gloplacha.2024.104631openalex-snapshot
Widespread upper-ocean deoxygenation in the Alpine-Mediterranean Tethys during the Toarcian Oceanic Anoxic Event
inferred← citeshttps://doi.org/10.1016/j.gloplacha.2025.104922openalex-snapshot
Nannoplankton response indicates intra-OAE2 cooling (Plenus Cold Event) in southeastern Tethys (Qiangdong, Tibet)
inferred← citeshttps://doi.org/10.1016/j.gloplacha.2025.104976openalex-snapshot
Transient modeling for ocean redox conditions during the mid-cretaceous Oceanic Anoxic Event 2
inferred← citeshttps://doi.org/10.1016/j.gloplacha.2025.105161openalex-snapshot
Astronomical calibration of Oceanic Anoxic Event 2 in the Northeastern Neo-Tethys: Insights into the cause of carbon cycle perturbations
inferred← citeshttps://doi.org/10.1016/j.gloplacha.2026.105414openalex-snapshot
Long-term variations in palaeoenvironmental conditions in the Western Tethys during the late Aptian–late Cenomanian time interval: From an unstable to a stable ocean
inferred← citeshttps://doi.org/10.1016/j.gr.2020.01.010openalex-snapshot
Oxygen level, primary productivity, and water turbulence during the OAE2 interval of Zagros Basin (SW Iran): Benthic foraminiferal variations in the carbonate microfacies
inferred← citeshttps://doi.org/10.1016/j.gr.2020.03.010openalex-snapshot
Paleocene resurrection of a crocodylomorph taxon: Biotic crises, climatic and sea level fluctuations
inferred← citeshttps://doi.org/10.1016/j.jafrearsci.2019.103641openalex-snapshot
Ammonite zonal scheme for the upper Cenomanian of the southern Tethys margin from Jordan to Tunisia, with palaeobiogeographic implications
inferred← citeshttps://doi.org/10.1016/j.jafrearsci.2023.104930openalex-snapshot
Litho-, biostratigraphy and sedimentological framework of the ‘mid’-Cretaceous crinoid-rich facies of the southern Aures Range (eastern Algeria)
inferred← citeshttps://doi.org/10.1016/j.jafrearsci.2026.106212openalex-snapshot
Microfacies Analysis, diagenetic modifications and depositional environments of the Cenomanian–Turonian carbonate Ramp of Ghardaïa (Northern Sahara, Algeria)
inferred← citeshttps://doi.org/10.1016/j.jafrearsci.2026.106248openalex-snapshot
Sedimentary and faunal dynamics during late Cenomanian–early Turonian eustatic sea-level rise along the southern Tethyan margin
inferred← citeshttps://doi.org/10.1016/j.jop.2024.06.002openalex-snapshot
Spatio-temporal variability in microfossil and geochemical records of Cenomanian-Turonian oceanic anoxic event-2: a review
inferred← citeshttps://doi.org/10.1016/j.jop.2024.07.006openalex-snapshot
Southern Tethys shelf evolution around the Cenomanian–Turonian OAE2: The Saharan Atlas (Algeria) depositional model
inferred← citeshttps://doi.org/10.1016/j.jsames.2017.10.019openalex-snapshot
High-resolution carbonate isotopic study of the Mural Formation (Cerro Pimas section), Sonora, México: Implications for early Albian oceanic anoxic events
inferred← citeshttps://doi.org/10.1016/j.jseaes.2021.104863openalex-snapshot
Evidence of Mid-Cretaceous carbon cycle perturbations and OAE2 recorded in Cenomanian to middle Campanian carbonates of the Zagros fold–thrust belt basin, Iran
inferred← citeshttps://doi.org/10.1016/j.jseaes.2023.105901openalex-snapshot
Classification of shale lithofacies with minimal data: Application to the early Permian shales in the Ordos Basin, China
inferred← citeshttps://doi.org/10.1016/j.jseaes.2024.106365openalex-snapshot
Geochemical characterization of Upper Cretaceous organic-rich deposits: Insights from the Azraq Basin in Jordan
inferred← citeshttps://doi.org/10.1016/j.marmicro.2025.102525openalex-snapshot
Size variation of Eprolithus floralis across Oceanic Anoxic Event 2 (Late Cretaceous) in the Eastbourne section
inferred← citeshttps://doi.org/10.1016/j.marpetgeo.2024.107067openalex-snapshot
Greensand formation, siliceous earth deposition and coastal metal drawdown in the Danubian Cretaceous Basin (Bavaria, Germany)
inferred← citeshttps://doi.org/10.1016/j.marpetgeo.2024.107180openalex-snapshot
High-resolution oceanic anoxic event 2 (OAE2) records from the north of eastern Tethys and evidence for short-term sea regression and wildfire at its early phase
inferred← citeshttps://doi.org/10.1016/j.marpetgeo.2025.107303openalex-snapshot
Depositional environment characteristics and mechanisms of organic carbon accumulation in the organic-rich siliceous-carbonate of the Late Devonian Domanik formation in the Volga-Ural Basin
inferred← citeshttps://doi.org/10.1016/j.marpetgeo.2025.107463openalex-snapshot
Cyclostratigraphy of the Cenomanian-Turonian boundary in Jordan
inferred← citeshttps://doi.org/10.1016/j.orggeochem.2023.104722openalex-snapshot
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
inferred← citeshttps://doi.org/10.1016/j.palaeo.2019.03.019openalex-snapshot
Terrestrial and marginal-marine record of the mid-Cretaceous Oceanic Anoxic Event 2 (OAE 2): High-resolution framework, carbon isotopes, CO2 and sea-level change
inferred← citeshttps://doi.org/10.1016/j.palaeo.2019.109238openalex-snapshot
The Cenomanian/Turonian boundary interval deep-sea deposits in the Zagros Basin (SW Iran): Bioevents, carbon isotope record and palaeoceanographic model
inferred← citeshttps://doi.org/10.1016/j.palaeo.2019.109443openalex-snapshot
Nitrogen and carbon cycle perturbations through the Cenomanian-Turonian oceanic anoxic event 2 (~94 Ma) in the Vocontian Basin (SE France)
inferred← citeshttps://doi.org/10.1016/j.palaeo.2019.109465openalex-snapshot
Orbitally driven redox fluctuations during Cretaceous Oceanic Anoxic Event 2 (OAE2) revealed by a new magnetic proxy
inferred← citeshttps://doi.org/10.1016/j.palaeo.2020.109703openalex-snapshot
Paleoecology and proliferation of the bivalve Chondrodonta joannae (Choffat) in the upper Cenomanian (Upper Cretaceous) Adriatic Carbonate Platform of Istria (Croatia)
inferred← citeshttps://doi.org/10.1016/j.palaeo.2021.110605openalex-snapshot
Turonian-Maastrichtian biostratigraphy and isotope stratigraphy of the Kopet-Dagh Basin deposits, northeastern Neo-Tethys, Iran
inferred← citeshttps://doi.org/10.1016/j.palaeo.2023.111490openalex-snapshot
A mercury and trace element geochemical record across Oceanic Anoxic Event 1b in Arctic Canada
inferred← citeshttps://doi.org/10.1016/j.palaeo.2023.111598openalex-snapshot
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)
inferred← citeshttps://doi.org/10.1016/j.palaeo.2023.111756openalex-snapshot
Carbonate uranium isotopes across Cretaceous OAE 2 in southern Mexico: New constraints on the global spread of marine anoxia and organic carbon burial
inferred← citeshttps://doi.org/10.1016/j.palaeo.2024.112578openalex-snapshot
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)
inferred← citeshttps://doi.org/10.1016/j.palaeo.2024.112678openalex-snapshot
The Cenomanian-Turonian boundary and Oceanic Anoxic Event 2 in the eastern Neotethys: A multi-proxy study of the İnişdere area of southeast Türkiye
inferred← citeshttps://doi.org/10.1016/j.palaeo.2025.112891openalex-snapshot
Calcareous plankton and shallow-water benthic biocalcifiers: Resilience and extinction across the Cenomanian-Turonian Oceanic Anoxic Event 2
inferred← citeshttps://doi.org/10.1016/j.petrol.2019.03.032openalex-snapshot
Sealing capacity of siderite-bearing strata: The effect of pore dimension on abundance and micromorphology type of siderite in the Lopingian (Late Permian) coal-bearing strata, western Guizhou province
inferred← citeshttps://doi.org/10.1016/j.petrol.2021.109627openalex-snapshot
Paleoenvironmental conditions and organic matter enrichment of the Late Paleoproterozoic Cuizhuang Formation dark shale in the Yuncheng Basin, North China
inferred← citeshttps://doi.org/10.1016/j.pgeola.2024.03.003openalex-snapshot
Stratigraphy and sedimentology of the upper Cenomanian–lower Coniacian in the Northern Aures Range (Algeria)
inferred← citeshttps://doi.org/10.1016/j.sedgeo.2019.04.010openalex-snapshot
A new terrestrial plant-rich Fossil-Lagerstätte from the middle Cenomanian (Late Cretaceous) of the Apennine Carbonate Platform (Magliano Vetere, southern Italy): Depositional and palaeoenvironmental settings
inferred← citeshttps://doi.org/10.1017/pab.2017.3openalex-snapshot
Marine life in a greenhouse world: cephalopod biodiversity and biogeography during the early Late Cretaceous
inferred← citeshttps://doi.org/10.1017/s0016756822000991openalex-snapshot
Planktonic foraminifera document palaeoceanographic changes across the middle Cenomanian carbon-isotope excursion MCE 1: new evidence from the UK chalk
inferred← citeshttps://doi.org/10.1017/s0016756824000244openalex-snapshot
A global reference for black shale geochemistry and the T-OAE revisited: upper Pliensbachian – middle Toarcian (Lower Jurassic) chemostratigraphy in the Cleveland Basin, England
inferred← citeshttps://doi.org/10.1021/acsearthspacechem.4c00002openalex-snapshot
Characteristics of Cenomanian–Turonian Oceanic Anoxic Event 2 and its Impact on Organic Carbon Accumulation in the Abu Roash (F) Organic-Rich Carbonate Rocks in the Abu Gharadig Field, Egypt
inferred← citeshttps://doi.org/10.1021/acsomega.1c06051openalex-snapshot
Controls on the Organic Matter Accumulation of the Marine–Continental Transitional Shanxi Formation Shale in the Southeastern Ordos Basin
inferred← citeshttps://doi.org/10.1029/2019gc008306openalex-snapshot
Cyanobacteria Proliferation in the Cenomanian‐Turonian Boundary Interval of the Apennine Carbonate Platform: Immediate Response to the Environmental Perturbations Associated With OAE‐2?
inferred← citeshttps://doi.org/10.1029/2019pa003631openalex-snapshot
A Re‐evaluation of the Plenus Cold Event, and the Links Between CO2, Temperature, and Seawater Chemistry During OAE 2
inferred← citeshttps://doi.org/10.1029/2020gc009246openalex-snapshot
New Constraints on Global Geochemical Cycling During Oceanic Anoxic Event 2 (Late Cretaceous) From a 6‐Million‐year Long Molybdenum‐Isotope Record
inferred← citeshttps://doi.org/10.1029/2020pa004016openalex-snapshot
Complex Interactions Between Large Igneous Province Emplacement and Global‐Temperature Changes During the Cenomanian‐Turonian Oceanic Anoxic Event (OAE 2)
inferred← citeshttps://doi.org/10.1029/2020pa004202openalex-snapshot
Exploring the Impact of Cenomanian Paleogeography and Marine Gateways on Oceanic Oxygen
inferred← citeshttps://doi.org/10.1029/2021gc010292openalex-snapshot
Volcanism‐Triggered Climatic Control on Late Cretaceous Oceans
inferred← citeshttps://doi.org/10.1029/2021pa004287openalex-snapshot
Carbon Cycling During Oceanic Anoxic Event 2: Compound‐Specific Carbon Isotope Evidence From the Western Interior Seaway
inferred← citeshttps://doi.org/10.1029/2022pa004474openalex-snapshot
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)
inferred← citeshttps://doi.org/10.1029/2026gl123945openalex-snapshot
A Shallow‐Marine Ecosystem Before Initial Tibetan Plateau Uplift
inferred← citeshttps://doi.org/10.1038/s41467-018-06319-6openalex-snapshot
Vegetation response to exceptional global warmth during Oceanic Anoxic Event 2
inferred← citeshttps://doi.org/10.1038/s41467-022-31076-yopenalex-snapshot
Hydrological control of river and seawater lithium isotopes
inferred← citeshttps://doi.org/10.1038/s41467-024-49032-3openalex-snapshot
Oceanic Anoxic Event 2 triggered by Kerguelen volcanism
inferred← citeshttps://doi.org/10.1038/s41561-020-0633-yopenalex-snapshot
Marine organic carbon burial increased forest fire frequency during Oceanic Anoxic Event 2
inferred← citeshttps://doi.org/10.1038/s41561-024-01496-0openalex-snapshot
Solid Earth forcing of Mesozoic oceanic anoxic events
inferred← citeshttps://doi.org/10.1038/s41598-022-21716-0openalex-snapshot
Evidence for the early Toarcian Carbon Isotope Excursion (T-CIE) from the shallow marine siliciclastic red beds of Arabia
inferred← citeshttps://doi.org/10.1038/s41598-023-30072-6openalex-snapshot
The Cenomanian/Turonian boundary in light of new developments in terrestrial palynology
inferred← citeshttps://doi.org/10.1038/s43247-024-01214-zopenalex-snapshot
Large igneous province activity drives oceanic anoxic event 2 environmental change across eastern Asia
inferred← citeshttps://doi.org/10.1051/bsgf/2020026openalex-snapshot
Late Cenomanian-Turonian isotopic stratigraphy in the chalk of the Paris Basin (France): a reference section between the Tethyan and Boreal realms
inferred← citeshttps://doi.org/10.1073/pnas.1715278115openalex-snapshot
Uranium isotope evidence for two episodes of deoxygenation during Oceanic Anoxic Event 2
inferred← citeshttps://doi.org/10.1080/00206814.2022.2084644openalex-snapshot
The Cenomanian–Turonian Boundary Event (CTBE) as recorded in the northern margin of Africa: palaeoceanography of the Oceanic Anoxic Event (OAE-2), North-Central Tunisia
inferred← citeshttps://doi.org/10.1080/00206814.2024.2361276openalex-snapshot
Diagenetic evolution of Upper Cretaceous carbonate sequences (Sarvak Formation) in the Abadan Plain, Iran: evidence from petrographic, elemental, stable, and strontium isotopic data
inferred← citeshttps://doi.org/10.1088/1755-1315/1300/1/012018openalex-snapshot
Determining of an oceanic anoxic event and paleoenvironmental conditions of the Gulneri Formation Kirkuk Oilfield, Northern Iraq
inferred← citeshttps://doi.org/10.1098/rsta.2017.0073openalex-snapshot
Transient cooling episodes during Cretaceous Oceanic Anoxic Events with special reference to OAE 1a (Early Aptian)
inferred← citeshttps://doi.org/10.1111/sed.12349openalex-snapshot
Mesozoic climates and oceans – a tribute to Hugh Jenkyns and Helmut Weissert
inferred← citeshttps://doi.org/10.1111/sed.12352openalex-snapshot
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
inferred← citeshttps://doi.org/10.1111/sed.12493openalex-snapshot
The Albian to Turonian carbon isotope record from the Shilaif Basin (United Arab Emirates) and its regional and intercontinental correlation
inferred← citeshttps://doi.org/10.1111/sed.13146openalex-snapshot
New insights into the palaeoenvironmental–palaeoclimatic significance and sedimentary dynamics of carbonate Lagerstätten: The lower Albian of Pietraroja (Southern Italy)
inferred← citeshttps://doi.org/10.1126/sciadv.1701020openalex-snapshot
Constraining the rate of oceanic deoxygenation leading up to a Cretaceous Oceanic Anoxic Event (OAE-2: ~94 Ma)
inferred← citeshttps://doi.org/10.1126/sciadv.aeg0341openalex-snapshot
Coupled nickel and molybdenum isotopes quantify the evolution of the ocean system since the Late Cretaceous
inferred← citeshttps://doi.org/10.1127/nos/2018/0416openalex-snapshot
Age and synchronicity of planktonic foraminiferal bioevents across the Cenomanian – Turonian boundary interval (Late Cretaceous)
inferred← citeshttps://doi.org/10.1127/zdgg/2025/0473openalex-snapshot
Integrated stratigraphy and facies development of the lower Danubian Cretaceous Group (Bavaria, SE-Germany): dissecting Cenomanian–middle Turonian onlap patterns onto the Bohemian Massif
inferred← citeshttps://doi.org/10.1130/b32057.1openalex-snapshot
Astronomical pacing of relative sea level during Oceanic Anoxic Event 2: Preliminary studies of the expanded SH#1 Core, Utah, USA
inferred← citeshttps://doi.org/10.1130/b35097.1openalex-snapshot
CO2-induced climate forcing on the fire record during the initiation of Cretaceous oceanic anoxic event 2
inferred← citeshttps://doi.org/10.1130/b35594.1openalex-snapshot
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
inferred← citeshttps://doi.org/10.1130/g40226.1openalex-snapshot
Isotopic evidence for changes in the zinc cycle during Oceanic Anoxic Event 2 (Late Cretaceous)
inferred← citeshttps://doi.org/10.1130/g45842.1openalex-snapshot
Southern Hemisphere sea-surface temperatures during the Cenomanian–Turonian: Implications for the termination of Oceanic Anoxic Event 2
inferred← citeshttps://doi.org/10.1130/g48198.1openalex-snapshot
Zinc isotope evidence for paleoenvironmental changes during Cretaceous Oceanic Anoxic Event 2
inferred← citeshttps://doi.org/10.1130/geol.s.18173069openalex-snapshot
Supplemental Material: Quantifying volcanism and organic carbon burial across Oceanic Anoxic Event 2
inferred← citeshttps://doi.org/10.1130/geol.s.18173069.v1openalex-snapshot
Supplemental Material: Quantifying volcanism and organic carbon burial across Oceanic Anoxic Event 2
inferred← citeshttps://doi.org/10.1144/pygs2017-007openalex-snapshot
The ‘Black Band’: local expression of a global event
inferred← citeshttps://doi.org/10.1144/pygs2019-017openalex-snapshot
Cretaceous Oceanic Anoxic Event 2 in eastern England: further palynological and geochemical data from Melton Ross
inferred← citeshttps://doi.org/10.1144/sp498-2018-138openalex-snapshot
Microfossil assemblages as key to reconstruct sea-level fluctuations, cooling episodes and palaeogeography: The Albian to Maastrichtian of Boreal and Peri-Tethyan Russia
inferred← citeshttps://doi.org/10.1144/sp498-2019-105openalex-snapshot
Aquifer-eustasy as the main driver of short-term sea-level fluctuations during Cretaceous hothouse climate phases
inferred← citeshttps://doi.org/10.1144/sp544-2023-60openalex-snapshot
Prologue: the founding of the Cretaceous System
inferred← citeshttps://doi.org/10.1144/sp544-2023-88openalex-snapshot
Cretaceous large igneous provinces: from volcanic formation to environmental catastrophes and biological crises
inferred← citeshttps://doi.org/10.1155/2020/8867140openalex-snapshot
Enrichment Mechanism of the Upper Carboniferous-Lower Permian Transitional Shale in the East Margin of the Ordos Basin, China: Evidence from Geochemical Proxies
inferred← citeshttps://doi.org/10.1180/clm.2022.1openalex-snapshot
Palaeoclimate, palaeosalinity and redox conditions control palygorskite claystone formation: an example from the Yangtaiwatan Basin, northwest China
inferred← citeshttps://doi.org/10.1360/tb-2021-0806openalex-snapshot
Processes and forcing mechanisms of the carbon cycle perturbation during Cretaceous Oceanic Anoxic Event 2
inferred← citeshttps://doi.org/10.14379/iodp.pr.369.2018openalex-snapshot
Australia Cretaceous climate and tectonics:tectonic, paleoclimate, and paleoceanographic history of high-latitude southern margins of Australia during the Cretaceous
inferred← citeshttps://doi.org/10.14379/iodp.proc.369.101.2019openalex-snapshot
Expedition 369 summary
inferred← citeshttps://doi.org/10.17794/rgn.2023.5.2openalex-snapshot
CHARACTERISTICS OF THE FACIES AND RADIOLITID PALEOENVIRONMENT OF THE UPPER CENOMANIAN SHALLOW-WATER SUCCESSION FROM THE SOUTHERN PART OF THE ADRIATIC CARBONATE PLATFORM, NORTHWESTERN SIDE OF KORČULA ISLAND, CROATIA
inferred← citeshttps://doi.org/10.2110/palo.2018.002openalex-snapshot
A RECORD OF SEQUESTRATION OF PLANT MATERIAL BY MARINE BURROWING ANIMALS AS A NEW FEEDING STRATEGY UNDER OLIGOTROPHIC CONDITIONS EVIDENCED BY PYRITE MICROTEXTURES
inferred← citeshttps://doi.org/10.2139/ssrn.7451249openalex-snapshot
Evolution of the Late Cenomanian-Early Turonian Mixed Carbonate-Siliciclastic Shelf: Sedimentological, Sequence Stratigraphic and Geochemical Evidence from the Dukul Formation in Yola Arm of the Northern Benue Trough, Nigeria
inferred← citeshttps://doi.org/10.24425/agp.2020.134556openalex-snapshot
Redox conditions, glacio-eustasy, and the status of the Cenomanian–Turonian Anoxic Event: new evidence from the Upper Cretaceous Chalk of England
inferred← citeshttps://doi.org/10.2475/08.2018.01openalex-snapshot
Does large igneous province volcanism always perturb the mercury cycle? Comparing the records of Oceanic Anoxic Event 2 and the end-Cretaceous to other Mesozoic events
inferred← citeshttps://doi.org/10.3389/feart.2021.703282openalex-snapshot
The Plenus Cold Event Record in the Abyssal DSDP Site 367 (Cape Verde, Central Atlantic): Environmental Perturbations and Impacts on the Nitrogen Cycle
inferred← citeshttps://doi.org/10.3389/feart.2024.1405768openalex-snapshot
Calcareous nannoplankton fluctuation within the Albian-Cenomanian Boundary Event of the Tethyan Himalaya
inferred← citeshttps://doi.org/10.3390/geosciences11090378openalex-snapshot
Carbon Isotopic Signature and Organic Matter Composition of Cenomanian High-Latitude Paleosols of Southern Patagonia
inferred← citeshttps://doi.org/10.35537/10915/154131openalex-snapshot
Relación entre procesos pedogenéticos y factores formadores de suelo durante el greenhouse Cenomaniano desde un abordaje macro-, micro-, y nanomorfológico
inferred← citeshttps://doi.org/10.4081/scie.2018.657openalex-snapshot
ITALIAN GEOLOGY AND CLIMATE CHANGE IN THE DEEP PAST
inferred← citeshttps://doi.org/10.4138/atlgeo.2025.020openalex-snapshot
Cretaceous palynoevents in the circum-Arctic region
inferred← citeshttps://doi.org/10.5194/cp-16-757-2020openalex-snapshot
Cretaceous oceanic anoxic events prolonged by phosphorus cycle feedbacks
inferred← citeshttps://doi.org/10.5724/gcs.38.001openalex-snapshot
Unique insight to the Cretaceous OAE1d, mid-Cenomanian Event, and OAE2 from long-line drillcores along the eastern cratonic margin of the Western Interior Basin
inferred← citeshttps://doi.org/10.5724/gcs.38.162openalex-snapshot
The Earth system during the Cenomanian and Turonian (Upper Cretaceous)
inferred← citeshttps://doi.org/10.70675/09e4134fzd2b3z432ez899ez6a7d9c9ac030openalex-snapshot
Organic facies variability during the Toarcian and Cenomanian— Turonian oceanic anoxic events : local versus global paleoenvironmental control
inferred← citeshttps://doi.org/10.70675/795447baze3efz460bza55az27323fb4589bopenalex-snapshot
Modélisation de l'oxygène océanique et de la productivité marine au Cénomano-Turonien avec le modèle système Terre IPSL
inferred← citeshttps://doi.org/10.70675/d4f527a8ze98dz4c91z911ezff8d242d27fdopenalex-snapshot
Caractérisation géochimique des changements paléoenvironnementaux au cours de l’Évènement Océanique Anoxique 2 (~94 Ma) dans le Bassin Vocontien (SE France)
Editorial review for independent work. ICSAC — the Institute for Complexity
Science and Advanced Computing — runs a structured editorial panel for researchers
publishing outside journals, and publishes on CiteStamp rails. Submission is free
and goes through ORCID: icsacinstitute.org/submit.