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Causes and consequences of globally warm climates in the early Paleogene
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inferred← citeshttps://doi.org/10.5252/geodiversitas2023v45a9zenodo-depositor-declared
Early Eocene hippomorph perissodactyls (Mammalia) from the Paris Basin
inferred← citeshttps://doi.org/10.1002/2017pa003314openalex-snapshot
Diagenetic Attenuation of Carbon Isotope Excursion Recorded by Planktic Foraminifers During the Paleocene‐Eocene Thermal Maximum
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New fossils of the oldest North American euprimate Teilhardina brandti (Omomyidae) from the paleocene–eocene thermal maximum
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Orbital pacing of Eocene climate during the Middle Eocene Climate Optimum and the chron C19r event: Missing link found in the tropical western Atlantic
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Continental Paleobiogeography as Phylogenetic Evidence
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Physiognomic and chemical characters in wood as palaeoclimate proxies
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Climatic and Environmental Changes During Paleocene-Eocene Thermal Maximum in Egypt: An Overview
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Paläoökologie der Auenbiotope
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inferred← citeshttps://doi.org/10.1007/s00114-005-0043-4openalex-snapshot
A new scincomorph lizard from the Palaeocene of Belgium and the origin of Scincoidea in Europe
inferred← citeshttps://doi.org/10.1007/s00114-012-0912-6openalex-snapshot
A long-bodied centriscoid fish from the basal Eocene of Kabardino-Balkaria, northern Caucasus, Russia
inferred← citeshttps://doi.org/10.1007/s00114-013-1069-7openalex-snapshot
Bird species migration ratio in East Asia, Australia, and surrounding islands
inferred← citeshttps://doi.org/10.1007/s00531-006-0144-0openalex-snapshot
Reappraisal of early Paleogene CCD curves: foraminiferal assemblages and stable carbon isotopes across the carbonate facies of Perth Abyssal Plain
inferred← citeshttps://doi.org/10.1007/s10347-005-0070-9openalex-snapshot
A paleoenvironmental standard section for Early Ilerdian tropical carbonate factories (Corbieres, France; Pyrenees, Spain)
inferred← citeshttps://doi.org/10.1007/s11430-010-4095-8openalex-snapshot
Early Paleogene stratigraphic sequences, mammalian evolution and its response to environmental changes in Erlian Basin, Inner Mongolia, China
inferred← citeshttps://doi.org/10.1007/s11430-011-4267-1openalex-snapshot
Trend of Santonian (Late Cretaceous) atmospheric CO2 and global mean land surface temperature: Evidence from plant fossils
inferred← citeshttps://doi.org/10.1007/s11692-011-9138-3openalex-snapshot
Impacts of Paleo-Oxygen Levels on the Size, Development, Reproduction, and Tracheal Systems of Blatella germanica
inferred← citeshttps://doi.org/10.1007/s12038-009-0062-yopenalex-snapshot
Evidence of Late Palaeocene-Early Eocene equatorial rain forest refugia in southern Western Ghats, India
inferred← citeshttps://doi.org/10.1007/s12229-012-9116-1openalex-snapshot
Fossil Records in the Lythraceae
inferred← citeshttps://doi.org/10.1007/s12517-013-1050-yopenalex-snapshot
Influence of the halokinesis on the clay mineral repartition of upper Maastrichtian–Ypresian in the Meknassy-Mezzouna basin, centerwestern Tunisia
inferred← citeshttps://doi.org/10.1007/s12517-013-1066-3openalex-snapshot
Mid-Paleocene event at Gabal Nezzazat, Sinai, Egypt: planktonic foraminiferal biostratigraphy, mineralogy and geochemistry
inferred← citeshttps://doi.org/10.1007/s13146-025-01077-1openalex-snapshot
Inferring paleoenvironmental changes from integrated facies analysis of the late Paleocene-early Eocene succession, Salt Range, Pakistan
inferred← citeshttps://doi.org/10.1007/s42990-021-00059-4openalex-snapshot
The first record of genus Linderina Schlumberger (foraminifera) from the Ypresian of Neo-Tethys: data from the Kozaklı Basin, Nevşehir, Central Turkey
inferred← citeshttps://doi.org/10.1007/s43217-022-00117-3openalex-snapshot
Floodplain evolution during the early Paleogene within the Piceance Creek Basin, northwest Colorado, U.S.A
inferred← citeshttps://doi.org/10.1016/b978-0-08-095975-7.01311-5openalex-snapshot
Atmospheric CO2 and O2 During the Phanerozoic: Tools, Patterns, and Impacts
inferred← citeshttps://doi.org/10.1016/b978-0-08-095975-7.01314-0openalex-snapshot
Greenhouse Climates
inferred← citeshttps://doi.org/10.1016/b978-0-323-85937-0.00002-9openalex-snapshot
Global coal endowment and coalbed gas potential
inferred← citeshttps://doi.org/10.1016/b978-0-444-59425-9.00028-7openalex-snapshot
The Paleogene Period
inferred← citeshttps://doi.org/10.1016/bs.sats.2023.08.006openalex-snapshot
Late Paleocene to Early Eocene integrated biostratigraphic framework, chronostratigraphy and Paleocene/Eocene boundary in the Salt Range, Pakistan
inferred← citeshttps://doi.org/10.1016/j.cageo.2010.07.011openalex-snapshot
Solid modeling of fossil small mammal teeth
inferred← citeshttps://doi.org/10.1016/j.chemgeo.2005.08.008openalex-snapshot
Barium cycling in shallow sediment above active mud volcanoes in the Gulf of Mexico
inferred← citeshttps://doi.org/10.1016/j.chemgeo.2005.08.012openalex-snapshot
Influence of maceral content on δ13C and δ15N in a Middle Pennsylvanian coal
inferred← citeshttps://doi.org/10.1016/j.chemgeo.2011.04.004openalex-snapshot
Fluvial discharge and sea-level changes controlling black shale deposition during the Paleocene–Eocene Thermal Maximum in the Dababiya Quarry section, Egypt
inferred← citeshttps://doi.org/10.1016/j.chemgeo.2025.123079openalex-snapshot
Introduction of isotopically heavy barium from back-arc basin hydrothermal systems into the ocean
inferred← citeshttps://doi.org/10.1016/j.coal.2017.08.009openalex-snapshot
Paleoenvironment of Eocene lignite bearing succession from Bikaner-Nagaur Basin, western India: Organic petrography, palynology, palynofacies and geochemistry
inferred← citeshttps://doi.org/10.1016/j.cretres.2008.08.004openalex-snapshot
High resolution estimates of paleo-CO2 levels through the Campanian (Late Cretaceous) based on Ginkgo cuticles
inferred← citeshttps://doi.org/10.1016/j.cretres.2014.11.004openalex-snapshot
Paleoclimatic reconstruction for the Albian–Cenomanian transition based on a dominantly angiosperm flora from the Cedar Mountain Formation, Utah, USA
inferred← citeshttps://doi.org/10.1016/j.cretres.2019.02.016openalex-snapshot
The Cretaceous–Paleogene (K/Pg) boundary in the Dababiya Borehole, southern Egypt: An organic-walled dinoflagellate cyst approach
inferred← citeshttps://doi.org/10.1016/j.crpv.2017.01.001openalex-snapshot
First occurrence of Palaeotheriidae (Perissodactyla) from the late–middle Eocene of eastern Thrace (Greece)
inferred← citeshttps://doi.org/10.1016/j.dsr2.2007.01.007openalex-snapshot
Marine barite: Recorder of variations in ocean export productivity
inferred← citeshttps://doi.org/10.1016/j.earscirev.2004.06.001openalex-snapshot
From greenhouse to icehouse; organic-walled dinoflagellate cysts as paleoenvironmental indicators in the Paleogene
inferred← citeshttps://doi.org/10.1016/j.earscirev.2005.09.003openalex-snapshot
Unit stratotypes for global stages: The Neogene perspective
inferred← citeshttps://doi.org/10.1016/j.earscirev.2008.07.002openalex-snapshot
Late Paleocene–early Eocene Tethyan carbonate platform evolution — A response to long- and short-term paleoclimatic change
inferred← citeshttps://doi.org/10.1016/j.earscirev.2009.03.004openalex-snapshot
Quantitative paleoenvironmental and paleoclimatic reconstruction using paleosols
inferred← citeshttps://doi.org/10.1016/j.earscirev.2013.11.001openalex-snapshot
Paleo-CO2 variation trends and the Cretaceous greenhouse climate
inferred← citeshttps://doi.org/10.1016/j.earscirev.2014.07.001openalex-snapshot
Stratigraphic distribution of large flightless birds in the Palaeogene of Europe and its palaeobiological and palaeogeographical implications
inferred← citeshttps://doi.org/10.1016/j.earscirev.2014.08.017openalex-snapshot
Total organic carbon, organic phosphorus, and biogenic barium fluxes as proxies for paleomarine productivity
inferred← citeshttps://doi.org/10.1016/j.earscirev.2018.09.003openalex-snapshot
The evolution of hydroclimate in Asia over the Cenozoic: A stable-isotope perspective
inferred← citeshttps://doi.org/10.1016/j.earscirev.2020.103403openalex-snapshot
Evolution of deep-sea sediments across the Paleocene-Eocene and Eocene-Oligocene boundaries
inferred← citeshttps://doi.org/10.1016/j.envsoft.2012.10.003openalex-snapshot
New developments and applications in the ANUCLIM spatial climatic and bioclimatic modelling package
inferred← citeshttps://doi.org/10.1016/j.epsl.2004.06.017openalex-snapshot
Basaltic explosive volcanism, but no comet impact, at the Paleocene–Eocene boundary: high-resolution chemical and isotopic records from Egypt, Spain and Denmark
inferred← citeshttps://doi.org/10.1016/j.epsl.2007.03.037openalex-snapshot
Coccolithophore productivity response to greenhouse event of the Paleocene–Eocene Thermal Maximum
inferred← citeshttps://doi.org/10.1016/j.epsl.2007.04.024openalex-snapshot
The Paleocene–Eocene carbon isotope excursion in higher plant organic matter: Differential fractionation of angiosperms and conifers in the Arctic
inferred← citeshttps://doi.org/10.1016/j.epsl.2007.07.021openalex-snapshot
Magnitude of the carbon isotope excursion at the Paleocene–Eocene thermal maximum: The role of plant community change
inferred← citeshttps://doi.org/10.1016/j.epsl.2007.08.008openalex-snapshot
Closing the Mid-Palaeocene gap: Toward a complete astronomically tuned Palaeocene Epoch and Selandian and Thanetian GSSPs at Zumaia (Basque Basin, W Pyrenees)
inferred← citeshttps://doi.org/10.1016/j.epsl.2007.10.040openalex-snapshot
Transient ocean warming and shifts in carbon reservoirs during the early Danian
inferred← citeshttps://doi.org/10.1016/j.epsl.2008.03.009openalex-snapshot
An integrated stratigraphic record from the Paleocene of the Chijiang Basin, Jiangxi Province (China): Implications for mammalian turnover and Asian block rotations
inferred← citeshttps://doi.org/10.1016/j.epsl.2008.07.030openalex-snapshot
Large terrestrial and marine carbon and hydrogen isotope excursions in a new Paleocene/Eocene boundary section from Tanzania
inferred← citeshttps://doi.org/10.1016/j.epsl.2009.02.025openalex-snapshot
The Paleocene–Eocene Thermal Maximum record in the organic matter of the Claret and Tendruy continental sections (South-central Pyrenees, Lleida, Spain)
inferred← citeshttps://doi.org/10.1016/j.epsl.2010.06.031openalex-snapshot
The Dan-C2 hyperthermal event at Gubbio (Italy): Global implications, environmental effects, and cause(s)
inferred← citeshttps://doi.org/10.1016/j.epsl.2010.12.043openalex-snapshot
Sea-level and salinity fluctuations during the Paleocene–Eocene thermal maximum in Arctic Spitsbergen
inferred← citeshttps://doi.org/10.1016/j.epsl.2011.08.045openalex-snapshot
Coupled high-resolution marine and terrestrial records of carbon and hydrologic cycles variations during the Paleocene–Eocene Thermal Maximum (PETM)
inferred← citeshttps://doi.org/10.1016/j.epsl.2012.06.024openalex-snapshot
Early Paleogene temperature history of the Southwest Pacific Ocean: Reconciling proxies and models
inferred← citeshttps://doi.org/10.1016/j.epsl.2012.08.011openalex-snapshot
Marine and terrestrial environmental changes in NW Europe preceding carbon release at the Paleocene–Eocene transition
inferred← citeshttps://doi.org/10.1016/j.epsl.2014.03.017openalex-snapshot
Persistent environmental change after the Paleocene–Eocene Thermal Maximum in the eastern North Atlantic
inferred← citeshttps://doi.org/10.1016/j.epsl.2014.06.024openalex-snapshot
Early Eocene carbon isotope excursions and landscape destabilization at eccentricity minima: Green River Formation of Wyoming
inferred← citeshttps://doi.org/10.1016/j.epsl.2014.09.005openalex-snapshot
Quantifying the isotopic ‘continental effect’
inferred← citeshttps://doi.org/10.1016/j.epsl.2014.10.027openalex-snapshot
Structure of the carbon isotope excursion in a high-resolution lacustrine Paleocene–Eocene Thermal Maximum record from central China
inferred← citeshttps://doi.org/10.1016/j.epsl.2016.01.012openalex-snapshot
Improving the Ginkgo CO2 barometer: Implications for the early Cenozoic atmosphere
inferred← citeshttps://doi.org/10.1016/j.epsl.2017.10.019openalex-snapshot
Controls on the barium isotope compositions of marine sediments
inferred← citeshttps://doi.org/10.1016/j.epsl.2018.06.031openalex-snapshot
Ocean and climate response to North Atlantic seaway changes at the onset of long-term Eocene cooling
inferred← citeshttps://doi.org/10.1016/j.epsl.2018.12.036openalex-snapshot
Increased export production during recovery from the Paleocene–Eocene thermal maximum constrained by sedimentary Ba isotopes
inferred← citeshttps://doi.org/10.1016/j.epsl.2019.116044openalex-snapshot
Carbon isotope and mammal recovery from extreme greenhouse warming at the Paleocene–Eocene boundary in astronomically-calibrated fluvial strata, Bighorn Basin, Wyoming, USA
inferred← citeshttps://doi.org/10.1016/j.flora.2006.07.006openalex-snapshot
Major vegetation trends in the Tertiary of Patagonia (Argentina): A qualitative paleoclimatic approach based on palynological evidence
inferred← citeshttps://doi.org/10.1016/j.gca.2003.10.010openalex-snapshot
The effect of dissolved barium on biogeochemical processes at cold seeps
inferred← citeshttps://doi.org/10.1016/j.gca.2014.05.026openalex-snapshot
Assessment of the clumped isotope composition of fossil bone carbonate as a recorder of subsurface temperatures
inferred← citeshttps://doi.org/10.1016/j.gca.2017.01.038openalex-snapshot
Introducing global peat-specific temperature and pH calibrations based on brGDGT bacterial lipids
inferred← citeshttps://doi.org/10.1016/j.geobios.2005.05.001openalex-snapshot
A new basal tapiromorph (Perissodactyla, Mammalia) from the middle Eocene of Myanmar
inferred← citeshttps://doi.org/10.1016/j.gexplo.2007.06.001openalex-snapshot
Labile barite contents and dissolved barium concentrations on Blake Ridge: New perspectives on barium cycling above gas hydrate systems
inferred← citeshttps://doi.org/10.1016/j.gloplacha.2004.03.004openalex-snapshot
A method for using a fully coupled climate system model to generate detailed surface boundary conditions for paleoclimate modeling investigations: an early Paleogene example
inferred← citeshttps://doi.org/10.1016/j.gloplacha.2005.08.001openalex-snapshot
Reconstructing a lost Eocene paradise: Part I. Simulating the change in global floral distribution at the initial Eocene thermal maximum
inferred← citeshttps://doi.org/10.1016/j.gloplacha.2013.07.001openalex-snapshot
Up in smoke: A role for organic carbon feedbacks in Paleogene hyperthermals
inferred← citeshttps://doi.org/10.1016/j.gloplacha.2014.07.014openalex-snapshot
The global vegetation pattern across the Cretaceous–Paleogene mass extinction interval: A template for other extinction events
inferred← citeshttps://doi.org/10.1016/j.gloplacha.2017.07.014openalex-snapshot
Hydrological and associated biogeochemical consequences of rapid global warming during the Paleocene-Eocene Thermal Maximum
inferred← citeshttps://doi.org/10.1016/j.gloplacha.2019.03.013openalex-snapshot
What caused Earth's largest mass extinction event? New evidence from the Permian-Triassic boundary in northeastern Utah
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.2019.04.018openalex-snapshot
Microcodium-rich turbidites in hemipelagic sediments during the Paleocene–Eocene Thermal Maximum: Evidence for extreme precipitation events in a Mediterranean climate (Río Gor section, southern Spain)
inferred← citeshttps://doi.org/10.1016/j.gloplacha.2019.05.006openalex-snapshot
The potential of biomarker proxies to trace climate, vegetation, and biogeochemical processes in peat: A review
inferred← citeshttps://doi.org/10.1016/j.gloplacha.2019.103049openalex-snapshot
Constraining the magnitude of the carbon isotope excursion during the Paleocene-Eocene thermal maximum using larger benthic foraminifera
inferred← citeshttps://doi.org/10.1016/j.gloplacha.2021.103716openalex-snapshot
Changes in sulfur cycling in a large lake during the Paleocene-Eocene Thermal Maximum and implications for lake deoxygenation
inferred← citeshttps://doi.org/10.1016/j.gloplacha.2022.103786openalex-snapshot
Key traits of living fossil Ginkgo biloba are highly variable but not influenced by climate – Implications for palaeo-pCO2 reconstructions and climate sensitivity
inferred← citeshttps://doi.org/10.1016/j.gloplacha.2025.104882openalex-snapshot
Astrochronology of the Paleocene–Eocene Thermal Maximum on the East Tasman Plateau
inferred← citeshttps://doi.org/10.1016/j.gr.2015.10.018openalex-snapshot
The Paleocene of Antarctica: Dinoflagellate cyst biostratigraphy, chronostratigraphy and implications for the palaeo-Pacific margin of Gondwana
inferred← citeshttps://doi.org/10.1016/j.gr.2018.05.007openalex-snapshot
The formation of microbial-metazoan bioherms and biostromes following the latest Permian mass extinction
inferred← citeshttps://doi.org/10.1016/j.jafrearsci.2008.07.004openalex-snapshot
Biostratigraphy and paleoenvironment of the Danian/Selandian (D/S) transition in the Southern Tethys: A case study from north Eastern Desert, Egypt
inferred← citeshttps://doi.org/10.1016/j.jafrearsci.2010.11.001openalex-snapshot
Shallow marine ostracode turnover in response to environmental change during the Paleocene–Eocene thermal maximum in northwest Tunisia
inferred← citeshttps://doi.org/10.1016/j.jafrearsci.2015.10.013openalex-snapshot
Paleocene stratigraphy in Egypt
inferred← citeshttps://doi.org/10.1016/j.jafrearsci.2015.11.004openalex-snapshot
Differential dissolution susceptibility of Paleocene foraminiferal assemblage from Farafra Oasis, Egypt
inferred← citeshttps://doi.org/10.1016/j.jafrearsci.2015.11.021openalex-snapshot
Calcareous nannofossils and paleoenvironments of the Paleocene–Eocene thermal maximum (PETM) interval in central Egypt
inferred← citeshttps://doi.org/10.1016/j.jafrearsci.2016.02.020openalex-snapshot
Sedimentology, diagenesis, clay mineralogy and sequential analysis model of Upper Paleocene evaporite-carbonate ramp succession from Tamerza area (Gafsa Basin: Southern Tunisia)
inferred← citeshttps://doi.org/10.1016/j.jafrearsci.2016.06.003openalex-snapshot
Thanetian transgressive-regressive sequences based on foraminiferal paleobathymetry at Gebel Matulla, west-central Sinai, Egypt
inferred← citeshttps://doi.org/10.1016/j.jafrearsci.2017.02.022openalex-snapshot
Palaeogeographical type of the geological heritage of Egypt: A new evidence
inferred← citeshttps://doi.org/10.1016/j.jafrearsci.2017.05.008openalex-snapshot
Anatomy of a mountain: The Thebes Limestone Formation (Lower Eocene) at Gebel Gurnah, Luxor, Nile Valley, Upper Egypt
inferred← citeshttps://doi.org/10.1016/j.jafrearsci.2019.103645openalex-snapshot
Biostratigraphy and geochemistry of the Cretaceous-Paleogene (K/Pg) and early danian event (Dan-C2), a possible link to deccan volcanism: New insights from Red Sea, Egypt
inferred← citeshttps://doi.org/10.1016/j.jafrearsci.2022.104569openalex-snapshot
Nature of the Paleocene/Eocene boundary (the Dababiya Quarry Member) at El-Ballas area, Qena region, Egypt
inferred← citeshttps://doi.org/10.1016/j.jaridenv.2006.01.009openalex-snapshot
Cenozoic climatic change and the development of the arid vegetation in Australia
inferred← citeshttps://doi.org/10.1016/j.jhevol.2013.04.006openalex-snapshot
Systematics of Paleogene Micromomyidae (Euarchonta, Primates) from North America
inferred← citeshttps://doi.org/10.1016/j.jsames.2014.02.001openalex-snapshot
Controls on clay minerals assemblages in an early paleogene nonmarine succession: Implications for the volcanic and paleoclimatic record of extra-andean patagonia, Argentina
inferred← citeshttps://doi.org/10.1016/j.jsames.2023.104587openalex-snapshot
Eocene paleoceanographic and paleoclimatic events recognized by assemblages of dinoflagellate cysts in the Southwest Atlantic Ocean
inferred← citeshttps://doi.org/10.1016/j.jseaes.2022.105361openalex-snapshot
Origin of ooids, peloids and micro-oncoids of marine ironstone deposits in Western Siberia (Russia)
inferred← citeshttps://doi.org/10.1016/j.jvolgeores.2008.12.017openalex-snapshot
Nonexplosive and explosive magma/wet-sediment interaction during emplacement of Eocene intrusions into Cretaceous to Eocene strata, Trans-Pecos igneous province, West Texas
inferred← citeshttps://doi.org/10.1016/j.jvolgeores.2015.01.001openalex-snapshot
WITHDRAWN: Volcano-sedimentary characteristics in the Abu Treifiya Basin, Cairo–Suez District, Egypt: Example of dynamics and fluidization over sedimentary and volcaniclastic beds by emplacement of syn-volcanic basaltic rocks
inferred← citeshttps://doi.org/10.1016/j.jvolgeores.2015.10.023openalex-snapshot
Volcano-sedimentary characteristics in the Abu Treifiya Basin, Cairo–Suez District, Egypt: Example of dynamics and fluidization over sedimentary and volcaniclastic beds by emplacement of syn-volcanic basaltic rocks
inferred← citeshttps://doi.org/10.1016/j.margeo.2011.02.009openalex-snapshot
Impact of the Paleocene–Eocene Thermal Maximum on the macrobenthic community: Ichnological record from the Zumaia section, northern Spain
inferred← citeshttps://doi.org/10.1016/j.margeo.2011.06.008openalex-snapshot
Reconstructing changes in seep activity by means of pore water and solid phase Sr/Ca and Mg/Ca ratios in pockmark sediments of the Northern Congo Fan
inferred← citeshttps://doi.org/10.1016/j.margeo.2012.02.003openalex-snapshot
Carbonate saturation dynamics during the Paleocene–Eocene thermal maximum: Bathyal constraints from ODP sites 689 and 690 in the Weddell Sea (South Atlantic)
inferred← citeshttps://doi.org/10.1016/j.marmicro.2004.04.002openalex-snapshot
Nannofossil assemblage fluctuations during the Paleocene–Eocene Thermal Maximum at Sites 213 (Indian Ocean) and 401 (North Atlantic Ocean): palaeoceanographic implications
inferred← citeshttps://doi.org/10.1016/j.marmicro.2005.01.001openalex-snapshot
Paleocene sea-level and productivity changes at the southern Tethyan margin (El Kef, Tunisia)
inferred← citeshttps://doi.org/10.1016/j.marmicro.2005.05.002openalex-snapshot
Environmental change across the Paleocene–Eocene transition from eastern New Zealand: A marine palynological approach
inferred← citeshttps://doi.org/10.1016/j.marmicro.2006.02.008openalex-snapshot
Paleoenvironmental change at the Danian–Selandian transition in Tunisia: Foraminifera, organic-walled dinoflagellate cyst and calcareous nannofossil records
inferred← citeshttps://doi.org/10.1016/j.marmicro.2006.03.002openalex-snapshot
Environmental perturbation in the southern Tethys across the Paleocene/Eocene boundary (Dababiya, Egypt): Foraminiferal and clay mineral records
inferred← citeshttps://doi.org/10.1016/j.marmicro.2006.08.006openalex-snapshot
Danian/Selandian boundary stratigraphy, paleoenvironment and Ostracoda from Sidi Nasseur, Tunisia
inferred← citeshttps://doi.org/10.1016/j.marmicro.2006.10.002openalex-snapshot
Responses of calcareous nannofossil assemblages, mineralogy and geochemistry to the environmental perturbations across the Paleocene/Eocene boundary in the Venetian Pre-Alps
inferred← citeshttps://doi.org/10.1016/j.marmicro.2007.05.001openalex-snapshot
The Paleocene–Eocene Thermal Maximum as recorded by Tethyan planktonic foraminifera in the Forada section (northern Italy)
inferred← citeshttps://doi.org/10.1016/j.marmicro.2007.05.003openalex-snapshot
High-resolution nannofossil biochronology of middle Paleocene to early Eocene at ODP Site 1262: Implications for calcareous nannoplankton evolution
inferred← citeshttps://doi.org/10.1016/j.marmicro.2007.05.004openalex-snapshot
Calcareous nannofossils from the Paleocene–Eocene Thermal Maximum of the equatorial Atlantic (ODP Site 1260B): Evidence for tropical warming
inferred← citeshttps://doi.org/10.1016/j.marmicro.2007.08.004openalex-snapshot
Danian/Selandian boundary criteria and North Sea Basin–Tethys correlations based on calcareous nannofossil and foraminiferal trends in SW France
inferred← citeshttps://doi.org/10.1016/j.marmicro.2008.01.010openalex-snapshot
Size variations of the calcareous nannofossil taxon Discoaster multiradiatus (Incertae sedis) across the Paleocene–Eocene thermal maximum in ocean drilling program holes 690B and 1209B
inferred← citeshttps://doi.org/10.1016/j.marmicro.2008.09.001openalex-snapshot
Palaeoenvironmental turnover across the Ypresian–Lutetian transition at the Agost section, Southastern Spain: In search of a marker event to define the Stratotype for the base of the Lutetian Stage
inferred← citeshttps://doi.org/10.1016/j.marmicro.2008.11.003openalex-snapshot
Perturbation at the sea floor during the Paleocene–Eocene Thermal Maximum: Evidence from benthic foraminifera at Contessa Road, Italy
inferred← citeshttps://doi.org/10.1016/j.marmicro.2009.03.007openalex-snapshot
High resolution calcareous nannofossil biostratigraphy and paleoecology across the Latest Danian Event (LDE) in central Eastern Desert, Egypt
inferred← citeshttps://doi.org/10.1016/j.marmicro.2012.01.001openalex-snapshot
Characterization of the Latest Danian Event by means of benthic foraminiferal assemblages along a depth transect at the southern Tethyan margin (Nile Basin, Egypt)
inferred← citeshttps://doi.org/10.1016/j.marmicro.2012.02.003openalex-snapshot
Deep-sea ostracode turnovers through the Paleocene–Eocene thermal maximum in DSDP Site 401, Bay of Biscay, North Atlantic
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.2012.02.007openalex-snapshot
Sea-level rise and coastal circulation controlled Holocene groundwater development in Bermuda and caused a meteoric lens to collapse 1600years ago
inferred← citeshttps://doi.org/10.1016/j.marmicro.2013.09.004openalex-snapshot
Can the morphology of deep-sea benthic foraminifera reveal what caused their extinction during the mid-Pleistocene Climate Transition?
inferred← citeshttps://doi.org/10.1016/j.marmicro.2014.11.003openalex-snapshot
Early Eocene environmental development in the northern Peri-Tethys (Aktulagay, Kazakhstan) based on benthic foraminiferal assemblages and stable isotopes (O, C)
inferred← citeshttps://doi.org/10.1016/j.marmicro.2014.12.001openalex-snapshot
Paleocene–Eocene Thermal Maximum environmental change in the New Jersey Coastal Plain: benthic foraminiferal biotic events
inferred← citeshttps://doi.org/10.1016/j.marmicro.2015.10.002openalex-snapshot
Stable seafloor conditions, sea level and food supply during the latest Maastrichtian at Brazos River, Texas
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.2024.102433openalex-snapshot
High-resolution Danian–Selandian benthic foraminifera-based paleoenvironmental reconstruction and response to sequence stratigraphy: Inferences from the Elles section, El Kef Basin, Tunisia
inferred← citeshttps://doi.org/10.1016/j.marmicro.2025.102487openalex-snapshot
Response of calcareous nannofossils during the Danian-Thanetian isotopic events in the Elles Section, Central Tunisia
inferred← citeshttps://doi.org/10.1016/j.marpetgeo.2023.106504openalex-snapshot
The Paleocene-Eocene transition in the Gulf of Guinea: Evidence of the PETM in the Douala basin, Cameroon
inferred← citeshttps://doi.org/10.1016/j.orggeochem.2014.09.005openalex-snapshot
High frequency floral changes at the Paleocene–Eocene boundary revealed by comparative biomarker and palynological studies
inferred← citeshttps://doi.org/10.1016/j.palaeo.2003.11.014openalex-snapshot
Changes in atmospheric CO2 concentrations and climate from the Late Eocene to Early Miocene: palaeobotanical reconstruction based on fossil floras from Saxony, Germany
inferred← citeshttps://doi.org/10.1016/j.palaeo.2004.09.004openalex-snapshot
Taxonomic turnover and abundance in Cretaceous to Tertiary wood floras of Antarctica: implications for changes in forest ecology
inferred← citeshttps://doi.org/10.1016/j.palaeo.2004.09.011openalex-snapshot
The Paleocene–Eocene transition at Mead Stream, New Zealand: a southern Pacific record of early Cenozoic global change
inferred← citeshttps://doi.org/10.1016/j.palaeo.2005.01.005openalex-snapshot
Palaeoenvironmental changes across the Danian–Selandian boundary in the North Sea Basin
inferred← citeshttps://doi.org/10.1016/j.palaeo.2005.03.011openalex-snapshot
A multi-proxy approach to determine Antarctic terrestrial palaeoclimate during the Late Cretaceous and Early Tertiary
inferred← citeshttps://doi.org/10.1016/j.palaeo.2005.03.040openalex-snapshot
Bolide summer: The Paleocene/Eocene thermal maximum as a response to an extraterrestrial trigger
inferred← citeshttps://doi.org/10.1016/j.palaeo.2005.05.006openalex-snapshot
Changes in calcareous nannofossil assemblages across the Paleocene/Eocene transition from the paleo-equatorial Pacific Ocean
inferred← citeshttps://doi.org/10.1016/j.palaeo.2005.05.013openalex-snapshot
Palynology and organic-carbon isotope ratios across a terrestrial Palaeocene/Eocene boundary section in the Williston Basin, North Dakota, USA
inferred← citeshttps://doi.org/10.1016/j.palaeo.2005.07.037openalex-snapshot
The ocean circulation in the southern hemisphere and its climatic impacts in the Eocene
inferred← citeshttps://doi.org/10.1016/j.palaeo.2005.10.013openalex-snapshot
Covarying sedimentary and biotic fluctuations in Lower–Middle Eocene Pyrenean deep-sea deposits: Palaeoenvironmental implications
inferred← citeshttps://doi.org/10.1016/j.palaeo.2005.11.006openalex-snapshot
Amphisbaenian paleobiogeography: Evidence of vicariance and geodispersal patterns
inferred← citeshttps://doi.org/10.1016/j.palaeo.2006.09.011openalex-snapshot
Transient drying during the Paleocene–Eocene Thermal Maximum (PETM): Analysis of paleosols in the bighorn basin, Wyoming
inferred← citeshttps://doi.org/10.1016/j.palaeo.2006.10.022openalex-snapshot
Eocene vegetation patterns reconstructed from plant diversity — A global perspective
inferred← citeshttps://doi.org/10.1016/j.palaeo.2006.12.007openalex-snapshot
The Campo section (Pyrenees, Spain) revisited: Implications for changing benthic carbonate assemblages across the Paleocene–Eocene boundary
inferred← citeshttps://doi.org/10.1016/j.palaeo.2007.09.016openalex-snapshot
Astronomical calibration of the Paleocene time
inferred← citeshttps://doi.org/10.1016/j.palaeo.2007.12.007openalex-snapshot
Timing and magnitude of early Aptian extreme warming: Unraveling primary δ18O variation in indurated pelagic carbonates at Deep Sea Drilling Project Site 463, central Pacific Ocean
inferred← citeshttps://doi.org/10.1016/j.palaeo.2008.07.005openalex-snapshot
Rare earth elements and stable isotope geochemistry (δ13C and δ18O) of phosphorite deposits in the Gafsa Basin, Tunisia
inferred← citeshttps://doi.org/10.1016/j.palaeo.2008.12.007openalex-snapshot
The first microbialite - coral mounds in the Cenozoic (Uppermost Paleocene) from the Northern Tethys (Slovenia): Environmentally-triggered phase shifts preceding the PETM?
inferred← citeshttps://doi.org/10.1016/j.palaeo.2009.05.009openalex-snapshot
Extinction and recovery of benthic foraminifera across the Paleocene–Eocene Thermal Maximum at the Alamedilla section (Southern Spain)
inferred← citeshttps://doi.org/10.1016/j.palaeo.2009.06.018openalex-snapshot
Filling the North European Early/Middle Eocene (Ypresian/Lutetian) boundary gap: Insights from the Pyrenean continental to deep-marine record
inferred← citeshttps://doi.org/10.1016/j.palaeo.2009.08.019openalex-snapshot
Extinction, dwarfing and the Lilliput effect
inferred← citeshttps://doi.org/10.1016/j.palaeo.2010.03.029openalex-snapshot
Ecological and evolutionary response of Tethyan planktonic foraminifera to the middle Eocene climatic optimum (MECO) from the Alano section (NE Italy)
inferred← citeshttps://doi.org/10.1016/j.palaeo.2010.05.034openalex-snapshot
Changing CO2 conditions during the end-Triassic inferred from stomatal frequency analysis on Lepidopteris ottonis (Goeppert) Schimper and Ginkgoites taeniatus (Braun) Harris
inferred← citeshttps://doi.org/10.1016/j.palaeo.2011.01.022openalex-snapshot
Increasing restriction of the Egyptian shelf during the Early Eocene? — New insights from a southern Tethyan carbonate platform
inferred← citeshttps://doi.org/10.1016/j.palaeo.2011.03.001openalex-snapshot
A New Zealand record of sea level rise and environmental change during the Paleocene–Eocene Thermal Maximum
inferred← citeshttps://doi.org/10.1016/j.palaeo.2011.04.005openalex-snapshot
Dynamic response of the shallow marine benthic ecosystem to regional and pan-Tethyan environmental change at the Paleocene–Eocene boundary
inferred← citeshttps://doi.org/10.1016/j.palaeo.2011.06.017openalex-snapshot
Atmospheric paleo-CO2 estimates based on Taxodium distichum (Cupressaceae) fossils from the Miocene and Pliocene of Eastern North America
inferred← citeshttps://doi.org/10.1016/j.palaeo.2011.12.010openalex-snapshot
The evolution of mid Paleocene-early Eocene coral communities: How to survive during rapid global warming
inferred← citeshttps://doi.org/10.1016/j.palaeo.2012.04.021openalex-snapshot
The fidelity of oxygen and strontium isotope values from shallow shelf settings: Implications for temperature and age reconstructions
inferred← citeshttps://doi.org/10.1016/j.palaeo.2012.05.001openalex-snapshot
Sedimentology, palynostratigraphy and palynofacies of the late Oligocene Makum Coalfield, Assam, India: A window on lowland tropical vegetation during the most recent episode of significant global warmth
inferred← citeshttps://doi.org/10.1016/j.palaeo.2012.05.009openalex-snapshot
Mallee model for mammal communities of the early Cenozoic and Mesozoic
inferred← citeshttps://doi.org/10.1016/j.palaeo.2012.06.004openalex-snapshot
Dwarfing of ostracodes during the Paleocene–Eocene Thermal Maximum at DSDP Site 401 (Bay of Biscay, North Atlantic) and its implication for changes in organic carbon cycle in deep-sea benthic ecosystem
inferred← citeshttps://doi.org/10.1016/j.palaeo.2012.09.008openalex-snapshot
Northward range extension of a diminutive-sized mammal (Ectocion parvus) and the implication of body size change during the Paleocene–Eocene Thermal Maximum
inferred← citeshttps://doi.org/10.1016/j.palaeo.2012.10.019openalex-snapshot
Isotopic and palynological evidence for a new Early Jurassic environmental perturbation
inferred← citeshttps://doi.org/10.1016/j.palaeo.2013.01.018openalex-snapshot
In search of the Latest Danian Event in a paleobathymetric transect off Kasserine Island, north-central Tunisia
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.2013.10.016openalex-snapshot
Sea-level changes across the Paleocene–Eocene interval in the Spanish Pyrenees, and their possible relationship with North Atlantic magmatism
inferred← citeshttps://doi.org/10.1016/j.palaeo.2014.07.015openalex-snapshot
Deriving temperature estimates from Southern Hemisphere leaves
inferred← citeshttps://doi.org/10.1016/j.palaeo.2014.09.002openalex-snapshot
Integrated bio-chemostratigraphical correlations and climatic evolution across the Danian–Selandian boundary at low latitudes
inferred← citeshttps://doi.org/10.1016/j.palaeo.2015.01.015openalex-snapshot
Paleoceanographic, and paleoclimatic constraints on the global Eocene diatom and silicoflagellate record
inferred← citeshttps://doi.org/10.1016/j.palaeo.2015.03.009openalex-snapshot
High-resolution chemostratigraphy of the late Aptian–early Albian oceanic anoxic event (OAE 1b) from the Poggio le Guaine section (Umbria–Marche Basin, central Italy)
inferred← citeshttps://doi.org/10.1016/j.palaeo.2015.03.026openalex-snapshot
Effect of global warming on diversity pattern in Nypa mangroves across Paleocene–Eocene transition in the paleo-equatorial region of the Indian sub-continent
inferred← citeshttps://doi.org/10.1016/j.palaeo.2015.04.003openalex-snapshot
New geochemical constraints on the Paleocene–Eocene thermal maximum: Dababiya GSSP, Egypt
inferred← citeshttps://doi.org/10.1016/j.palaeo.2015.06.021openalex-snapshot
Alluvial response to the Paleocene–Eocene Thermal Maximum climatic event, Polecat Bench, Wyoming (U.S.A.)
inferred← citeshttps://doi.org/10.1016/j.palaeo.2015.08.011openalex-snapshot
Climatic implications of Ginkgoites waarrensis Douglas emend. from the south polar Tupuangi flora, Late Cretaceous (Cenomanian), Chatham Islands
inferred← citeshttps://doi.org/10.1016/j.palaeo.2015.08.019openalex-snapshot
Evidence for weathering and volcanism during the PETM from Arctic Ocean and Peri-Tethys osmium isotope records
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.2016.05.006openalex-snapshot
Environmental dynamics during the Paleocene–Eocene thermal maximum (PETM) in the northeastern Peri-Tethys revealed by high-resolution micropalaeontological and geochemical studies of a Caucasian key section
inferred← citeshttps://doi.org/10.1016/j.palaeo.2016.07.029openalex-snapshot
A siliciclastic braid delta within a lower Paleogene carbonate platform (Ordesa-Monte Perdido National Park, southern Pyrenees, Spain): Record of the Paleocene–Eocene Thermal Maximum perturbation
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.2018.02.013openalex-snapshot
Low-latitude vegetation and climate dynamics at the Paleocene-Eocene transition – A study based on multiple proxies from the Jathang section in northeastern India
inferred← citeshttps://doi.org/10.1016/j.palaeo.2018.02.018openalex-snapshot
Environmental instability during the latest Paleocene at Zumaia (Basque-Cantabric Basin): The bellwether of the Paleocene-Eocene Thermal Maximum
inferred← citeshttps://doi.org/10.1016/j.palaeo.2018.07.004openalex-snapshot
Eocene to Oligocene dinoflagellate cysts from the Tattofte section, western External Rif, northwestern Morocco: Biostratigraphy, paleoenvironments and paleoclimate
inferred← citeshttps://doi.org/10.1016/j.palaeo.2020.110138openalex-snapshot
Woody dicot leaf traits as a palaeoclimate proxy: 100 years of development and application
inferred← citeshttps://doi.org/10.1016/j.palaeo.2021.110293openalex-snapshot
Atmospheric rivers in high-resolution simulations of the Paleocene Eocene Thermal Maximum (PETM)
inferred← citeshttps://doi.org/10.1016/j.palaeo.2021.110450openalex-snapshot
Larger benthic foraminiferal response to the PETM in the Potwar Basin (Eastern Neotethys, Pakistan)
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