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High-resolution deep-sea carbon and oxygen isotope records of Eocene Thermal Maximum 2 and H2
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What this work says
Outgoing claims: the papers this work cites, builds on, or argues with.
inferredcites →https://doi.org/10.1017/cbo9780511564512.006openalex-snapshot
Deep-sea environments on a warm earth: latest Paleocene-early Eocene
inferredcites →https://doi.org/10.1029/2001jd001002openalex-snapshot
A simple model of multiple climate regimes
inferredcites →https://doi.org/10.1029/2001pa000733openalex-snapshot
Application of dynamic programming to the correlation of paleoclimate records
inferredcites →https://doi.org/10.1029/2003pa000908openalex-snapshot
Early Cenozoic decoupling of the global carbon and sulfur cycles
inferredcites →https://doi.org/10.1029/2003pa000909openalex-snapshot
Orbital climate forcing of δ13C excursions in the late Paleocene–early Eocene (chrons C24n–C25n)
inferredcites →https://doi.org/10.1029/2006gc001291openalex-snapshot
Microstructural and geochemical perspectives on planktic foraminiferal preservation: “Glassy” versus “Frosty”
inferredcites →https://doi.org/10.1029/2006pa001322openalex-snapshot
On the duration of magnetochrons C24r and C25n and the timing of early Eocene global warming events: Implications from the Ocean Drilling Program Leg 208 Walvis Ridge depth transect
inferredcites →https://doi.org/10.1029/2006pa001372openalex-snapshot
Interpreting transient carbonate compensation depth changes by marine sediment core modeling
inferredcites →https://doi.org/10.1029/2007pa001465openalex-snapshot
North American continental margin records of the Paleocene‐Eocene thermal maximum: Implications for global carbon and hydrological cycling
inferredcites →https://doi.org/10.1029/2008gc002116openalex-snapshot
Depth dependency of the Paleocene‐Eocene carbon isotope excursion: Paired benthic and terrestrial biomarker records (Ocean Drilling Program Leg 208, Walvis Ridge)
inferredcites →https://doi.org/10.1029/2008pa001655openalex-snapshot
Patterns and magnitude of deep sea carbonate dissolution during Eocene Thermal Maximum 2 and H2, Walvis Ridge, southeastern Atlantic Ocean
inferredcites →https://doi.org/10.1029/95pa02087openalex-snapshot
Dissociation of oceanic methane hydrate as a cause of the carbon isotope excursion at the end of the Paleocene
inferredcites →https://doi.org/10.1029/98pa00070openalex-snapshot
Reevaluation of the oxygen isotopic composition of planktonic foraminifera: Experimental results and revised paleotemperature equations
inferredcites →https://doi.org/10.1038/353225a0openalex-snapshot
Abrupt deep-sea warming, palaeoceanographic changes and benthic extinctions at the end of the Palaeocene
inferredcites →https://doi.org/10.1038/nature02566openalex-snapshot
Release of methane from a volcanic basin as a mechanism for initial Eocene global warming
inferredcites →https://doi.org/10.1038/nature03814openalex-snapshot
Astronomical pacing of late Palaeocene to early Eocene global warming events
inferredcites →https://doi.org/10.1038/nature08399openalex-snapshot
Early Palaeogene temperature evolution of the southwest Pacific Ocean
inferredcites →https://doi.org/10.1038/ngeo578openalex-snapshot
Carbon dioxide forcing alone insufficient to explain Palaeocene–Eocene Thermal Maximum warming
inferredcites →https://doi.org/10.1038/ngeo668openalex-snapshot
Warm and wet conditions in the Arctic region during Eocene Thermal Maximum 2
inferredcites →https://doi.org/10.1098/rsta.2007.2045openalex-snapshot
The Palaeocene–Eocene carbon isotope excursion: constraints from individual shell planktonic foraminifer records
inferredcites →https://doi.org/10.1126/science.1059412openalex-snapshot
Trends, Rhythms, and Aberrations in Global Climate 65 Ma to Present
inferredcites →https://doi.org/10.1126/science.1109004openalex-snapshot
Rapid Acidification of the Ocean During the Paleocene-Eocene Thermal Maximum
inferredcites →https://doi.org/10.1130/0091-7613(2002)030<1067:wtfftf>2.0.co;2openalex-snapshot
Warming the fuel for the fire: Evidence for the thermal dissociation of methane hydrate during the Paleocene-Eocene thermal maximum
inferredcites →https://doi.org/10.1130/g22545.1openalex-snapshot
Evolution of Atlantic thermohaline circulation: Early Oligocene onset of deep-water production in the North Atlantic
inferredcites →https://doi.org/10.1130/g23648a.1openalex-snapshot
Multiple early Eocene hyperthermals: Their sedimentary expression on the New Zealand continental margin and in the deep sea
inferredcites →https://doi.org/10.2973/odp.proc.ir.194.2002openalex-snapshot
Proceedings of the Ocean Drilling Program, 194 Initial Reports
inferredcites →https://doi.org/10.2973/odp.proc.sr.113.123.1990openalex-snapshot
Late Cretaceous through Neogene Deep-Sea Benthic Foraminifers (Maud Rise|Weddell Sea|Antarctica)
What points at this work
Incoming claims: where this work appears in other papers’ reference lists and arguments.
inferred← citeshttps://doi.org/10.11646/zootaxa.3636.2.5zenodo-depositor-declared
The first Aleyrodidae from the Lowermost Eocene Oise amber (Hemiptera: Sternorrhyncha)
inferred← citeshttps://doi.org/10.1002/2013gc004960openalex-snapshot
Orbital pacing of Eocene climate during the Middle Eocene climate optimum and the chron C19r event - missing link found in the tropical western Atlantic
inferred← citeshttps://doi.org/10.1002/2013pa002567openalex-snapshot
A transient deep‐sea circulation switch during Eocene Thermal Maximum 2
inferred← citeshttps://doi.org/10.1002/2014gl059808openalex-snapshot
Early Eocene carbon isotope excursions: Evidence from the terrestrial coal seam in the Fushun Basin, Northeast China
inferred← citeshttps://doi.org/10.1002/2014pa002651openalex-snapshot
Pliocene switch in orbital‐scale carbon cycle/climate dynamics
inferred← citeshttps://doi.org/10.1002/2014pa002670openalex-snapshot
The middle Eocene climatic optimum (MECO): A multiproxy record of paleoceanographic changes in the southeast Atlantic (ODP Site 1263, Walvis Ridge)
inferred← citeshttps://doi.org/10.1002/2014pa002702openalex-snapshot
I/Ca evidence for upper ocean deoxygenation during the PETM
inferred← citeshttps://doi.org/10.1002/2015pa002821openalex-snapshot
Changes in benthic ecosystems and ocean circulation in the Southeast Atlantic across Eocene Thermal Maximum 2
inferred← citeshttps://doi.org/10.1002/2015pa002837openalex-snapshot
Late Paleocene‐middle Eocene benthic foraminifera on a Pacific seamount (Allison Guyot, ODP Site 865): Greenhouse climate and superimposed hyperthermal events
inferred← citeshttps://doi.org/10.1002/2016pa002940openalex-snapshot
Environmental perturbations at the early Eocene ETM2, H2, and I1 events as inferred by Tethyan calcareous plankton (Terche section, northeastern Italy)
inferred← citeshttps://doi.org/10.1002/2017gc007240openalex-snapshot
Late Lutetian Thermal Maximum—Crossing a Thermal Threshold in Earth's Climate System?
inferred← citeshttps://doi.org/10.1002/2017pa003138openalex-snapshot
Did Photosymbiont Bleaching Lead to the Demise of Planktic ForaminiferMorozovellaat the Early Eocene Climatic Optimum?
inferred← citeshttps://doi.org/10.1002/ggge.20293openalex-snapshot
Orbital pacing of Eocene climate during the Middle Eocene Climate Optimum and the chron C19r event: Missing link found in the tropical western Atlantic
inferred← citeshttps://doi.org/10.1002/gj.4285openalex-snapshot
Hyperthermal events recorded in the Palaeogene carbonate sequence of southern Gulf of Mexico—Santa Elena borehole, Yucatan Peninsula
inferred← citeshttps://doi.org/10.1007/s00531-020-01972-zopenalex-snapshot
Planktic foraminiferal response to an early Paleocene transient warming event and biostratigraphic implications
inferred← citeshttps://doi.org/10.1016/b978-0-08-095975-7.01314-0openalex-snapshot
Greenhouse Climates
inferred← citeshttps://doi.org/10.1016/b978-0-12-821575-3.00028-1openalex-snapshot
The variation of the Earth's movements (orbital, tilt, and precession) and climate change
inferred← citeshttps://doi.org/10.1016/j.chemgeo.2023.121861openalex-snapshot
Phosphate δ13Corg chemostratigraphy from the Gantour basin, Morocco: A proof of concept from the K–Pg transition to mid-Thanetian
inferred← citeshttps://doi.org/10.1016/j.epsl.2013.04.037openalex-snapshot
Recognition of Early Eocene global carbon isotope excursions using lipids of marine Thaumarchaeota
inferred← citeshttps://doi.org/10.1016/j.epsl.2014.05.054openalex-snapshot
A high-resolution benthic stable-isotope record for the South Atlantic: Implications for orbital-scale changes in Late Paleocene–Early Eocene climate and carbon cycling
inferred← citeshttps://doi.org/10.1016/j.epsl.2014.07.029openalex-snapshot
High latitude hydrological changes during the Eocene Thermal Maximum 2
inferred← citeshttps://doi.org/10.1016/j.epsl.2017.08.038openalex-snapshot
Atmospheric pCO2 reconstructed across five early Eocene global warming events
inferred← citeshttps://doi.org/10.1016/j.epsl.2019.115865openalex-snapshot
A lower to middle Eocene astrochronology for the Mentelle Basin (Australia) and its implications for the geologic time scale
inferred← citeshttps://doi.org/10.1016/j.epsl.2022.117589openalex-snapshot
Paleoenvironmental evolution during the Early Eocene Climate Optimum in the Chicxulub impact crater
inferred← citeshttps://doi.org/10.1016/j.gca.2022.05.022openalex-snapshot
Enhanced continental chemical weathering during the multiple early Eocene hyperthermals: New constraints from the southern Indian Ocean
inferred← citeshttps://doi.org/10.1016/j.gexplo.2025.107889openalex-snapshot
Geochemistry and economic evaluation of REE + Y potential in the fine-grained matrix of sedimentary phosphorites from the Tebessa region, eastern Algeria
inferred← citeshttps://doi.org/10.1016/j.gloplacha.2017.09.007openalex-snapshot
Planktic foraminiferal response to early Eocene carbon cycle perturbations in the southeast Atlantic Ocean (ODP Site 1263)
inferred← citeshttps://doi.org/10.1016/j.gloplacha.2018.08.011openalex-snapshot
Towards determination of the source and magnitude of atmospheric pCO2 change across the early Paleogene hyperthermals
inferred← citeshttps://doi.org/10.1016/j.gloplacha.2019.04.012openalex-snapshot
Arctic vegetation, temperature, and hydrology during Early Eocene transient global warming events
inferred← citeshttps://doi.org/10.1016/j.gloplacha.2020.103372openalex-snapshot
Turnover and stability in the deep sea: Benthic foraminifera as tracers of Paleogene global change
inferred← citeshttps://doi.org/10.1016/j.gloplacha.2021.103634openalex-snapshot
Dextral to sinistral coiling switch in planktic foraminifer Morozovella during the Early Eocene Climatic Optimum
inferred← citeshttps://doi.org/10.1016/j.gloplacha.2022.103875openalex-snapshot
Reconstruction of the early Eocene paleoclimate and paleoenvironment of the southeastern Neo-Tethys Ocean
inferred← citeshttps://doi.org/10.1016/j.gloplacha.2025.104800openalex-snapshot
Eccentricity pacing of the Paleocene-Eocene Thermal Maximum: Multi-section astrochronology and statistical insights in China
inferred← citeshttps://doi.org/10.1016/j.gr.2013.04.004openalex-snapshot
First carbon isotope chemostratigraphy of the Ouled Abdoun phosphate Basin, Morocco; implications for dating and evolution of earliest African placental mammals
inferred← citeshttps://doi.org/10.1016/j.gsf.2020.07.014openalex-snapshot
Carbon cycle variability in tropical Atlantic across two Early Eocene hyperthermals
inferred← citeshttps://doi.org/10.1016/j.gsf.2024.101838openalex-snapshot
A transient shift in equatorial hydrology and vegetation during the Eocene Thermal Maximum 2
inferred← citeshttps://doi.org/10.1016/j.jseaes.2017.04.030openalex-snapshot
Lignite deposits of the Kutch Basin, western India: Carbon isotopic and palynological signatures of the early Eocene hyperthermal event ETM2
inferred← citeshttps://doi.org/10.1016/j.jseaes.2022.105401openalex-snapshot
Early Paleogene continental temperature patterns and gradients over eastern Eurasia
inferred← citeshttps://doi.org/10.1016/j.margeo.2024.107447openalex-snapshot
Impact of Paleocene–Eocene tectonic and climatic forcing on Arctic sediment transfer variability: SW Barents Sea, Norway
inferred← citeshttps://doi.org/10.1016/j.marmicro.2012.02.006openalex-snapshot
Multiple early Eocene benthic foraminiferal assemblage and δ13C fluctuations at DSDP Site 401 (Bay of Biscay — NE Atlantic)
inferred← citeshttps://doi.org/10.1016/j.marmicro.2012.09.001openalex-snapshot
Multispiral growth in Nummulites
inferred← citeshttps://doi.org/10.1016/j.marmicro.2013.12.004openalex-snapshot
Temporally variable diagenetic overgrowth on deep-sea nannofossil carbonates across Palaeogene hyperthermals and implications for isotopic analyses
inferred← citeshttps://doi.org/10.1016/j.marmicro.2016.11.001openalex-snapshot
Contrasting response of the calcareous nannoplankton communities after the Eocene hyperthermal events in the tropical Atlantic Ocean
inferred← citeshttps://doi.org/10.1016/j.marmicro.2018.12.001openalex-snapshot
The planktonic foraminiferal response to the Paleocene-Eocene thermal maximum on the Atlantic coastal plain
inferred← citeshttps://doi.org/10.1016/j.marmicro.2019.04.004openalex-snapshot
Benthic foraminiferal biotic events related to the Paleocene–Eocene Thermal Maximum along the California margin
inferred← citeshttps://doi.org/10.1016/j.marmicro.2019.101795openalex-snapshot
Do different extraction techniques impact planktic foraminiferal assemblages? An early Eocene case study
inferred← citeshttps://doi.org/10.1016/j.marmicro.2022.102131openalex-snapshot
Integrated stratigraphy of the lower Eocene successions on the southern Tethys margin (Egypt): Emphases on the hyperthermal events
inferred← citeshttps://doi.org/10.1016/j.palaeo.2010.10.029openalex-snapshot
Constraints on ocean acidification associated with rapid and massive carbon injections: The early Paleogene record at ocean drilling program site 1215, equatorial Pacific Ocean
inferred← citeshttps://doi.org/10.1016/j.palaeo.2011.10.016openalex-snapshot
Paleogene temperature gradient, seasonal variation and climate evolution of northeast China
inferred← citeshttps://doi.org/10.1016/j.palaeo.2012.02.006openalex-snapshot
Enhanced siliceous plankton productivity in response to middle Eocene warming at Southern Ocean ODP Sites 748 and 749
inferred← citeshttps://doi.org/10.1016/j.palaeo.2012.10.004openalex-snapshot
Diversity and climate change in the middle-late Wasatchian (early Eocene) Willwood Formation, central Bighorn Basin, Wyoming
inferred← citeshttps://doi.org/10.1016/j.palaeo.2012.10.011openalex-snapshot
Coupled CO2-climate response during the Early Eocene Climatic Optimum
inferred← citeshttps://doi.org/10.1016/j.palaeo.2013.03.018openalex-snapshot
Paleoenvironmental changes during the Middle Eocene Climatic Optimum (MECO) and its aftermath: The benthic foraminiferal record from the Alano section (NE Italy)
inferred← citeshttps://doi.org/10.1016/j.palaeo.2013.07.008openalex-snapshot
Do the large carbon isotopic excursions in terrestrial organic matter across Paleocene–Eocene boundary in India indicate intensification of tropical precipitation?
inferred← citeshttps://doi.org/10.1016/j.palaeo.2013.08.013openalex-snapshot
New Paleogene paleoclimate analysis of western Washington using physiognomic characteristics from fossil leaves
inferred← citeshttps://doi.org/10.1016/j.palaeo.2014.10.023openalex-snapshot
Deep-sea benthic foraminiferal turnover during the early–middle Eocene transition at Walvis Ridge (SE Atlantic)
inferred← citeshttps://doi.org/10.1016/j.palaeo.2016.03.010openalex-snapshot
Deep-sea benthic foraminiferal turnover across early Eocene hyperthermal events at Northeast Atlantic DSDP Site 550
inferred← citeshttps://doi.org/10.1016/j.palaeo.2016.09.013openalex-snapshot
Microfossil turnover across the uppermost Danian at Caravaca, Spain: Paleoenvironmental inferences and identification of the latest Danian event
inferred← citeshttps://doi.org/10.1016/j.palaeo.2017.07.030openalex-snapshot
The micropaleontological record of marine early Eocene oil shales from Jordan
inferred← citeshttps://doi.org/10.1016/j.palaeo.2021.110410openalex-snapshot
Benthic foraminiferal turnover across the Dan-C2 event in the eastern South Atlantic Ocean (ODP Site 1262)
inferred← citeshttps://doi.org/10.1016/j.palaeo.2022.110925openalex-snapshot
Some like it cool: Benthic foraminiferal response to Paleogene warming events
inferred← citeshttps://doi.org/10.1016/j.palaeo.2023.111712openalex-snapshot
Benthic biota (nummulites) response to a hyperthermal event: Eccentricity-modulated precession control on climate during the middle Eocene warming in the Southern Mediterranean
inferred← citeshttps://doi.org/10.1016/j.palaeo.2025.112867openalex-snapshot
Evaluating planktic foraminiferal resilience during the Middle Eocene Climatic Optimum (MECO) in the Atlantic Ocean
inferred← citeshttps://doi.org/10.1016/j.palaeo.2025.113238openalex-snapshot
Vegetation dynamics and carbon isotope responses to the early eocene hyperthermals
inferred← citeshttps://doi.org/10.1016/j.palaeo.2025.113298openalex-snapshot
Assessing Milankovitch forcing during and in the aftermath of the Early Eocene Climate Optimum: Dammam Formation, Saudi Arabia
inferred← citeshttps://doi.org/10.1016/j.petsci.2025.08.005openalex-snapshot
Terrestrial paleoenvironmental response of Early Eocene Climate Optimum: Implications for organic matter enrichment in the South China Sea
inferred← citeshttps://doi.org/10.1016/j.sedgeo.2020.105705openalex-snapshot
Eocene carbonate accumulation in the north-central Pacific Ocean: new insights from Ocean Drilling Program Site 1209, Shatsky Rise
inferred← citeshttps://doi.org/10.1017/s0016756826100697openalex-snapshot
Paleoenvironmental reconstruction of Bohai Bay Basin, Northern China, during the Paleocene–Eocene thermal maximum (PETM): insights from mineralogy, geochemistry and microfossils
inferred← citeshttps://doi.org/10.1021/acsomega.2c02445openalex-snapshot
Eocene Paleoclimate Evolution under the Background of Warmhouse–Hothouse Conditions in the Continental Fushun Basin: Implications from Magnetic Susceptibility and Color Reflectance
inferred← citeshttps://doi.org/10.1029/2010gc003097openalex-snapshot
Coherent pattern and timing of the carbon isotope excursion and warming during Eocene Thermal Maximum 2 as recorded in planktic and benthic foraminifera
inferred← citeshttps://doi.org/10.1029/2010pa002028openalex-snapshot
Stable carbon isotope patterns of marine biomarker lipids in the Arctic Ocean during Eocene Thermal Maximum 2
inferred← citeshttps://doi.org/10.1029/2011gb004224openalex-snapshot
Assessing offsets between the δ13C of sedimentary components and the global exogenic carbon pool across early Paleogene carbon cycle perturbations
inferred← citeshttps://doi.org/10.1029/2012pa002300openalex-snapshot
An early Lutetian carbon‐cycle perturbation: Insights from the Gorrondatxe section (western Pyrenees, Bay of Biscay)
inferred← citeshttps://doi.org/10.1029/2012pa002346openalex-snapshot
A molybdenum isotope record of Eocene Thermal Maximum 2: Implications for global ocean redox during the early Eocene
inferred← citeshttps://doi.org/10.1029/2017pa003306openalex-snapshot
Global Extent of Early Eocene Hyperthermal Events: A New Pacific Benthic Foraminiferal Isotope Record From Shatsky Rise (ODP Site 1209)
inferred← citeshttps://doi.org/10.1029/2018pa003375openalex-snapshot
Early Eocene Thermal Maximum 3: Biotic Response at Walvis Ridge (SE Atlantic Ocean)
inferred← citeshttps://doi.org/10.1029/2018pa003422openalex-snapshot
Orbitally Paced Carbon and Deep‐Sea Temperature Changes at the Peak of the Early Eocene Climatic Optimum
inferred← citeshttps://doi.org/10.1029/2019pa003556openalex-snapshot
A High‐Fidelity Benthic Stable Isotope Record of Late Cretaceous–Early Eocene Climate Change and Carbon‐Cycling
inferred← citeshttps://doi.org/10.1029/2019pa003699openalex-snapshot
The Magnitude of Surface Ocean Acidification and Carbon Release During Eocene Thermal Maximum 2 (ETM‐2) and the Paleocene‐Eocene Thermal Maximum (PETM)
inferred← citeshttps://doi.org/10.1029/2019pa003806openalex-snapshot
Paleoenvironmental Changes at ODP Site 702 (South Atlantic): Anatomy of the Middle Eocene Climatic Optimum
inferred← citeshttps://doi.org/10.1029/2020pa004053openalex-snapshot
Bentho‐Pelagic Decoupling: The Marine Biological Carbon Pump During Eocene Hyperthermals
inferred← citeshttps://doi.org/10.1029/2021pa004329openalex-snapshot
Early Eocene Ocean Meridional Overturning Circulation: The Roles of Atmospheric Forcing and Strait Geometry
inferred← citeshttps://doi.org/10.1029/2023pa004762openalex-snapshot
Extreme Planktic Foraminiferal Dwarfism Across the ETM2 in the Tethys Realm in Response to Warming
inferred← citeshttps://doi.org/10.1029/2023pa004801openalex-snapshot
Apparent Diachroneity of Calcareous Nannofossil Datums During the Early Eocene in the High‐Latitude South Pacific Ocean
inferred← citeshttps://doi.org/10.1029/2023pa004829openalex-snapshot
Multi‐Elemental Statistical Features of Early Paleogene Sediments From the Mid‐Latitude Eastern Indian Ocean
inferred← citeshttps://doi.org/10.1029/2024pa004907openalex-snapshot
Orbital (Hydro)Climate Variability in the Ice‐Free Early Eocene Arctic
inferred← citeshttps://doi.org/10.1038/nature09826openalex-snapshot
Eocene global warming events driven by ventilation of oceanic dissolved organic carbon
inferred← citeshttps://doi.org/10.1038/ngeo1301openalex-snapshot
Abundant Early Palaeogene marine gas hydrates despite warm deep-ocean temperatures
inferred← citeshttps://doi.org/10.1038/ngeo1427openalex-snapshot
Terrestrial carbon isotope excursions and biotic change during Palaeogene hyperthermals
inferred← citeshttps://doi.org/10.1038/s41467-020-17887-xopenalex-snapshot
Proxy evidence for state-dependence of climate sensitivity in the Eocene greenhouse
inferred← citeshttps://doi.org/10.1038/s41561-022-01006-0openalex-snapshot
Eocene emergence of highly calcifying coccolithophores despite declining atmospheric CO2
inferred← citeshttps://doi.org/10.1038/s41586-019-1590-8openalex-snapshot
Diversity decoupled from ecosystem function and resilience during mass extinction recovery
inferred← citeshttps://doi.org/10.1038/s41598-017-11470-zopenalex-snapshot
Earth system feedback statistically extracted from the Indian Ocean deep-sea sediments recording Eocene hyperthermals
inferred← citeshttps://doi.org/10.1038/s41598-019-45763-2openalex-snapshot
Carbon cycle instability and orbital forcing during the Middle Eocene Climatic Optimum
inferred← citeshttps://doi.org/10.1038/s41598-025-99045-1openalex-snapshot
First evidence of Limoniidae (Diptera: Nematocera) in French amber from Oise
inferred← citeshttps://doi.org/10.1038/s43247-022-00350-8openalex-snapshot
Warm deep-sea temperatures across Eocene Thermal Maximum 2 from clumped isotope thermometry
inferred← citeshttps://doi.org/10.1073/pnas.1300579110openalex-snapshot
Surviving rapid climate change in the deep sea during the Paleogene hyperthermals
inferred← citeshttps://doi.org/10.1086/666743openalex-snapshot
Large-Amplitude Variations in Carbon Cycling and Terrestrial Weathering during the Latest Paleocene and Earliest Eocene: The Record at Mead Stream, New Zealand
inferred← citeshttps://doi.org/10.1111/j.1365-3121.2012.01076.xopenalex-snapshot
An integrated stratigraphic record of the Palaeocene–lower Eocene at Gubbio (Italy): new insights into the early Palaeogene hyperthermals and carbon isotope excursions
inferred← citeshttps://doi.org/10.1111/sed.12243openalex-snapshot
Climate‐modulated sequence development in a tropical rift basin during the Late Palaeocene to Early Eocene super greenhouse Earth
inferred← citeshttps://doi.org/10.1111/ter.12250openalex-snapshot
Differential response at the seafloor during Palaeocene and Eocene ocean warming events at Walvis Ridge, Atlantic Ocean ( ODP Site 1262)
inferred← citeshttps://doi.org/10.1126/sciadv.1601430openalex-snapshot
Repetitive mammalian dwarfing during ancient greenhouse warming events
inferred← citeshttps://doi.org/10.1126/science.aba6853openalex-snapshot
An astronomically dated record of Earth’s climate and its predictability over the last 66 million years
inferred← citeshttps://doi.org/10.1127/nos/2016/0077openalex-snapshot
Astronomically tuned age model for the early Eocene carbon isotope events: A new high-resolution δ13 Cbenthic record of ODP Site 1263 between ~ 49 and ~ 54 Ma
inferred← citeshttps://doi.org/10.1130/2018.2541(27)openalex-snapshot
Evidence for subtropical warmth in the Canadian Arctic (Beaufort-Mackenzie, Northwest Territories, Canada) during the early Eocene
inferred← citeshttps://doi.org/10.1130/2019.2542(07)openalex-snapshot
Multiproxy Cretaceous-Paleogene boundary event stratigraphy: An Umbria-Marche basinwide perspective
inferred← citeshttps://doi.org/10.1130/2021.1217(12)openalex-snapshot
Global biotic events evident in the Paleogene marine strata of the eastern San Francisco Bay area, California
inferred← citeshttps://doi.org/10.1130/b31515.1openalex-snapshot
Clay mineralogical constraints on weathering in response to early Eocene hyperthermal events in the Bighorn Basin, Wyoming (Western Interior, USA)
inferred← citeshttps://doi.org/10.1130/b37650.1openalex-snapshot
Patterns of carbon-isotope excursions recorded in lacustrine sedimentary rocks of Central China during Paleocene–Eocene hyperthermals
inferred← citeshttps://doi.org/10.1130/b37957.1openalex-snapshot
SedST: An updated chronological database for ocean sediments
inferred← citeshttps://doi.org/10.1130/g39658.1openalex-snapshot
Subtropical sea-surface warming and increased salinity during Eocene Thermal Maximum 2
inferred← citeshttps://doi.org/10.1130/ges02398.1openalex-snapshot
Geochemical indications for the Paleocene-Eocene Thermal Maximum (PETM) and Eocene Thermal Maximum 2 (ETM-2) hyperthermals in terrestrial sediments of the Canadian Arctic
inferred← citeshttps://doi.org/10.1134/s0869593822050069openalex-snapshot
Integrated Paleocene–Eocene Nannofossil and Stable Isotope Stratigraphy in the Northern Caucasus, Russia
inferred← citeshttps://doi.org/10.1186/s42501-020-00076-8openalex-snapshot
The formation of authigenic deposits during Paleogene warm climatic intervals: a review
inferred← citeshttps://doi.org/10.1371/journal.pone.0193167openalex-snapshot
Early Eocene deep-sea benthic foraminiferal faunas: Recovery from the Paleocene Eocene Thermal Maximum extinction in a greenhouse world
inferred← citeshttps://doi.org/10.14379/iodp.sp.388.2019openalex-snapshot
Expedition 388 Scientific Prospectus: Equatorial Atlantic Gateway: origin, evolution, and paleoenvironment of the Equatorial Atlantic Gateway
inferred← citeshttps://doi.org/10.15697/fk20022openalex-snapshot
WITHDRAWN: Using Synthetic Data Trained Convolutional Neural Network For Predicting Sub-Resolution Thin Layers From Seismic Data
inferred← citeshttps://doi.org/10.15697/fk2v59gopenalex-snapshot
WITHDRAWN: Using Synthetic Data Trained Convolutional Neural Network For Predicting Sub-Resolution Thin Layers From Seismic Data
inferred← citeshttps://doi.org/10.1594/pangaea.857761openalex-snapshot
Stable carbon isotope record of Nuttallides truempyi of ODP Site 208-1263
inferred← citeshttps://doi.org/10.1594/pangaea.884585openalex-snapshot
Late Maastrichtian-early Eocene benthic stable carbon and oxygen isotope records from ODP Site 208-1262, South Atlantic
inferred← citeshttps://doi.org/10.1594/pangaea.893894openalex-snapshot
Benthic stable isotope record of ODP Site 208-1263
inferred← citeshttps://doi.org/10.2110/palo.2010.p10-109ropenalex-snapshot
CORRELATION OF EARLY PALEOGENE GLOBAL DIVERSITY PATTERNS OF LARGE BENTHIC FORAMINIFERA WITH PALEOCENE AND EOCENE CLIMATIC EVENTS
inferred← citeshttps://doi.org/10.2113/gsjfr.53.4.378openalex-snapshot
Exploring Early Eocene Hyperthermals on the New Jersey Paleoshelf (ODP 174AX)
inferred← citeshttps://doi.org/10.21203/rs.3.rs-1955221/v1openalex-snapshot
Evolution of the Eocene shallow carbonate platform in Tunisia: Carbon isotopes stratigraphy and petroleum implications
inferred← citeshttps://doi.org/10.2204/iodp.proc.320321.212.2013openalex-snapshot
Data report: early to middle Eocene benthic foraminifers at Sites U1331 and U1333, equatorial central Pacific Ocean, Expedition 320/321
inferred← citeshttps://doi.org/10.31223/x5nc9hopenalex-snapshot
Independent constraints on deep-sea temperatures across two early Eocene hyperthermals from clumped isotope thermometry
inferred← citeshttps://doi.org/10.5194/bg-9-4679-2012openalex-snapshot
Scaled biotic disruption during early Eocene global warming events
inferred← citeshttps://doi.org/10.5194/cp-11-1223-2015openalex-snapshot
Mammal faunal change in the zone of the Paleogene hyperthermals ETM2 and H2
inferred← citeshttps://doi.org/10.5194/cp-11-1313-2015openalex-snapshot
Frequency, magnitude and character of hyperthermal events at the onset of the Early Eocene Climatic Optimum
inferred← citeshttps://doi.org/10.5194/cp-11-473-2015openalex-snapshot
Early Paleogene variations in the calcite compensation depth: new constraints using old borehole sediments from across Ninetyeast Ridge, central Indian Ocean
inferred← citeshttps://doi.org/10.5194/cp-12-1151-2016openalex-snapshot
Environmental impact and magnitude of paleosol carbonate carbon isotope excursions marking five early Eocene hyperthermals in the Bighorn Basin, Wyoming
inferred← citeshttps://doi.org/10.5194/cp-12-455-2016openalex-snapshot
A model–model and data–model comparison for the early Eocene hydrological cycle
inferred← citeshttps://doi.org/10.5194/cp-13-1129-2017openalex-snapshot
Astronomical calibration of the Ypresian timescale: implications for seafloor spreading rates and the chaotic behavior of the solar system?
inferred← citeshttps://doi.org/10.5194/cp-14-1515-2018openalex-snapshot
Reduced carbon cycle resilience across the Palaeocene–Eocene Thermal Maximum
inferred← citeshttps://doi.org/10.5194/cp-15-1741-2019openalex-snapshot
Paleoenvironmental response of midlatitudinal wetlands to Paleocene–early Eocene climate change (Schöningen lignite deposits, Germany)
inferred← citeshttps://doi.org/10.5194/cp-16-227-2020openalex-snapshot
Alluvial record of an early Eocene hyperthermal within the Castissent Formation, the Pyrenees, Spain
inferred← citeshttps://doi.org/10.5194/cp-17-1315-2021openalex-snapshot
Optimizing sampling strategies in high-resolution paleoclimate records
inferred← citeshttps://doi.org/10.5194/cp-18-681-2022openalex-snapshot
Terrestrial carbon isotope stratigraphy and mammal turnover during post-PETM hyperthermals in the Bighorn Basin, Wyoming, USA
inferred← citeshttps://doi.org/10.5194/cp-19-1677-2023openalex-snapshot
Assessing environmental change associated with early Eocene hyperthermals in the Atlantic Coastal Plain, USA
inferred← citeshttps://doi.org/10.5194/cp-20-1303-2024openalex-snapshot
Polar amplification of orbital-scale climate variability in the early Eocene greenhouse world
inferred← citeshttps://doi.org/10.5194/cp-2023-70-supplementopenalex-snapshot
Supplementary material to "Polar amplification of orbital-scale climate variability in the early Eocene greenhouse world"
inferred← citeshttps://doi.org/10.5194/cp-7-47-2011openalex-snapshot
Southern ocean warming, sea level and hydrological change during the Paleocene-Eocene thermal maximum
inferred← citeshttps://doi.org/10.5194/cp-8-977-2012openalex-snapshot
Productivity response of calcareous nannoplankton to Eocene Thermal Maximum 2 (ETM2)
inferred← citeshttps://doi.org/10.5194/egusphere-2023-58-rc1openalex-snapshot
Comment on egusphere-2023-58
inferred← citeshttps://doi.org/10.5194/egusphere-2023-58-rc2openalex-snapshot
Comment on Rush et al. manuscript
inferred← citeshttps://doi.org/10.5670/oceanog.2019.122openalex-snapshot
Astronomical Time Keeping of Earth History: An Invaluable Contribution of Scientific Ocean Drilling
inferred← citeshttps://doi.org/10.58998/jnr2219openalex-snapshot
Paleogene Calcareous Nannofossils of the South Dover Bridge core, Southern Maryland (USA).
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