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A Transient Rise in Tropical Sea Surface Temperature During the Paleocene-Eocene Thermal Maximum

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What this work says

Outgoing claims: the papers this work cites, builds on, or argues with.

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Reconstructing past sea surface temperatures: Correcting for diagenesis of bulk marine carbonate

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An alternative age model for the Paleocene–Eocene thermal maximum using extraterrestrial 3He

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Climate model sensitivity to atmospheric CO2 levels in the Early–Middle Paleogene

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Evolutionary consequences of the latest Paleocene thermal maximum for tropical planktonic foraminifera

inferredcites →https://doi.org/10.1017/s0094837300012847openalex-snapshot

Stable isotopic signals and photosymbiosis in Late Paleocene planktic foraminifera

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Incorporation and preservation of Mg in Globigerinoides sacculifer: implications for reconstructing the temperature and 18O/16O of seawater

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New evidence for subtropical warming during the Late Paleocene thermal maximum: Stable isotopes from Deep Sea Drilling Project Site 527, Walvis Ridge

inferredcites →https://doi.org/10.1029/2001gc000200openalex-snapshot

Core top calibration of Mg/Ca in tropical foraminifera: Refining paleotemperature estimation

inferredcites →https://doi.org/10.1029/2001pa000749openalex-snapshot

Accurate estimation of sea surface temperatures using dissolution‐corrected calibrations for Mg/Ca paleothermometry

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Atmospheric composition, radiative forcing, and climate change as a consequence of a massive methane release from gas hydrates

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Correction to “Evidence of surface water oligotrophy during the Paleocene‐Eocene thermal maximum: Nannofossil assemblage data from Ocean Drilling Program Site 690, Maud Rise, Weddell Sea” by Timothy J. Bralower

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Calibration of Mg/Ca thermometry in planktonic foraminifera from a sediment trap time series

inferredcites →https://doi.org/10.1029/2003gc000525openalex-snapshot

Application of a radially viewed inductively coupled plasma‐optical emission spectrophotometer to simultaneous measurement of Mg/Ca, Sr/Ca, and Mn/Ca ratios in marine biogenic carbonates

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Higher temperatures and lower oceanic pCO2: A climate enigma at the end of the Paleocene Epoch

inferredcites →https://doi.org/10.1029/93pa03266openalex-snapshot

Evolution of Early Cenozoic marine temperatures

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

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Abrupt deep-sea warming, palaeoceanographic changes and benthic extinctions at the end of the Palaeocene

inferredcites →https://doi.org/10.1038/37333openalex-snapshot

Effect of seawater carbonate concentration on foraminiferal carbon and oxygen isotopes

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Trends, Rhythms, and Aberrations in Global Climate 65 Ma to Present

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Paleobotanical Evidence for Near Present-Day Levels of Atmospheric CO 2 During Part of the Tertiary

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Antarctic subtropical humid episode at the Paleocene-Eocene boundary: Clay-mineral evidence

inferredcites →https://doi.org/10.1130/0091-7613(1996)024<0423:rdopfi>2.3.co;2openalex-snapshot

Rapid diversification of planktonic foraminifera in the tropical Pacific (ODP Site 865) during the late Paleocene thermal maximum

inferredcites →https://doi.org/10.1130/0091-7613(1997)025<0259:abogit>2.3.co;2openalex-snapshot

A blast of gas in the latest Paleocene: Simulating first-order effects of massive dissociation of oceanic methane hydrate

inferredcites →https://doi.org/10.1130/0091-7613(1997)025<0963:hrrotl>2.3.co;2openalex-snapshot

High-resolution records of the late Paleocene thermal maximum and circum-Caribbean volcanism: Is there a causal link?

inferredcites →https://doi.org/10.1130/0091-7613(2000)028<0927:ncftlp>2.3.co;2openalex-snapshot

New chronology for the late Paleocene thermal maximum and its environmental implications

inferredcites →https://doi.org/10.1130/0091-7613(2001)029<0315:gdeawt>2.0.co;2openalex-snapshot

Global dinoflagellate event associated with the late Paleocene 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/10.1144/gsl.sp.1996.101.01.20openalex-snapshot

The Paleocene-Eocene benthic foraminiferal extinction and stable isotope anomalies

inferredcites →https://doi.org/10.2113/gsjfr.15.4.302openalex-snapshot

Carbon and oxygen isotopic composition of planktonic foraminifera from laboratory culture, plankton tows and Recent sediment; implications for the reconstruction of paleoclimatic conditions and of the global carbon cycle

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Coccolithophore productivity response to greenhouse event of the Paleocene–Eocene Thermal Maximum

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The Paleocene–Eocene carbon isotope excursion in higher plant organic matter: Differential fractionation of angiosperms and conifers in the Arctic

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Calcium carbonate veins in ocean crust record a threefold increase of seawater Mg/Ca in the past 30 million years

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.2014.05.047openalex-snapshot

Devils Hole paleotemperatures and implications for oxygen isotope equilibrium fractionation

inferred← citeshttps://doi.org/10.1016/j.epsl.2014.05.055openalex-snapshot

Impact of dissolution on the sedimentary record of the Paleocene–Eocene thermal maximum

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.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.2015.11.027openalex-snapshot

Development of a novel empirical framework for interpreting geological carbon isotope excursions, with implications for the rate of carbon injection across the PETM

inferred← citeshttps://doi.org/10.1016/j.epsl.2016.01.013openalex-snapshot

Planktic foraminifera shell chemistry response to seawater chemistry: Pliocene–Pleistocene seawater Mg/Ca, temperature and sea level change

inferred← citeshttps://doi.org/10.1016/j.epsl.2017.09.011openalex-snapshot

Redox-controlled carbon and phosphorus burial: A mechanism for enhanced organic carbon sequestration during the PETM

inferred← citeshttps://doi.org/10.1016/j.epsl.2020.116164openalex-snapshot

Simulation of early Eocene water isotopes using an Earth system model and its implication for past climate reconstruction

inferred← citeshttps://doi.org/10.1016/j.epsl.2020.116414openalex-snapshot

Coupled evolution of temperature and carbonate chemistry during the Paleocene–Eocene; new trace element records from the low latitude Indian Ocean

inferred← citeshttps://doi.org/10.1016/j.epsl.2021.117340openalex-snapshot

Large-scale, astronomically paced sediment input to the North Sea Basin during the Paleocene Eocene Thermal Maximum

inferred← citeshttps://doi.org/10.1016/j.epsl.2022.117926openalex-snapshot

Mercury isotope evidence for protracted North Atlantic magmatism during the Paleocene-Eocene Thermal Maximum

inferred← citeshttps://doi.org/10.1016/j.epsl.2023.118164openalex-snapshot

The large decline in carbonate δ238U from a PETM section at Tingri (South Tibet) was driven by local sea-level changes, not global oceanic anoxia

inferred← citeshttps://doi.org/10.1016/j.epsl.2026.119931openalex-snapshot

Enhanced erosion of the Laramide ranges during the Paleocene–Eocene Thermal Maximum, Bighorn Basin, Wyoming

inferred← citeshttps://doi.org/10.1016/j.gca.2010.03.039openalex-snapshot

An extraterrestrial 3He-based timescale for the Paleocene–Eocene thermal maximum (PETM) from Walvis Ridge, IODP Site 1266

inferred← citeshttps://doi.org/10.1016/j.gca.2010.07.030openalex-snapshot

Application of calcite Mg partitioning functions to the reconstruction of paleocean Mg/Ca

inferred← citeshttps://doi.org/10.1016/j.gca.2020.01.015openalex-snapshot

Constraining multiple controls on planktic foraminifera Mg/Ca

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.geogeo.2025.100465openalex-snapshot

Paleoenvironmental and vegetation evolution during the PETM in the Gulf of Guinea: A study based on integrated palynological and chemostratigraphic analysis of the Miang section in the Douala Basin, Cameroon

inferred← citeshttps://doi.org/10.1016/j.geothermics.2023.102868openalex-snapshot

Seismic expression of paleokarst morphologies and associated Siderolithic infill in the Geneva Basin, Switzerland: Implications for geothermal exploration

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.2013.06.011openalex-snapshot

Re-evaluating modern and Palaeogene GDGT distributions: Implications for SST reconstructions

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.2016.08.010openalex-snapshot

The demise of the early Eocene greenhouse – Decoupled deep and surface water cooling in the eastern North Atlantic

inferred← citeshttps://doi.org/10.1016/j.gloplacha.2017.08.011openalex-snapshot

Fluvial-system response to climate change: The Paleocene-Eocene Tremp Group, Pyrenees, Spain

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.2019.04.018openalex-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.2019.103049openalex-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.2020.103313openalex-snapshot

Spatial change of precipitation in response to the Paleocene-Eocene thermal Maximum warming in China

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.2022.103794openalex-snapshot

Mercury enrichments of the Pyrenean foreland basins sediments support enhanced volcanism during the Paleocene-Eocene thermal maximum (PETM)

inferred← citeshttps://doi.org/10.1016/j.gloplacha.2022.103918openalex-snapshot

Response of calcareous nannoplankton to the Paleocene–Eocene Thermal Maximum in the Paratethys Seaway (Tarim Basin, West China)

inferred← citeshttps://doi.org/10.1016/j.gloplacha.2023.104206openalex-snapshot

Continuous measurements in North China and culture experiments reveal the potential of leaf n-alkane carbon isotopes in paleoclimate studies

inferred← citeshttps://doi.org/10.1016/j.gloplacha.2023.104289openalex-snapshot

Tropical ocean temperatures and changes in terrigenous flux during the Paleocene-Eocene Thermal Maximum in southern Tibet

inferred← citeshttps://doi.org/10.1016/j.gloplacha.2025.104774openalex-snapshot

A link between the paleoenvironment and PETM via trace element proxies in Southwest Atlantic sediments

inferred← citeshttps://doi.org/10.1016/j.gloplacha.2026.105493openalex-snapshot

Astronomical and volcanic forcing of Paleocene carbon cycle perturbations in the Norwegian Sea Basin

inferred← citeshttps://doi.org/10.1016/j.gloplacha.2026.105586openalex-snapshot

Volcanism-driven redox and productivity responses during the Paleocene–Eocene Thermal Maximum in the western Atlantic

inferred← citeshttps://doi.org/10.1016/j.gloplacha.2026.105624openalex-snapshot

Hafnium-neodymium isotopic evidence for latitudinal heterogeneity in continental silicate weathering during the Paleocene-Eocene thermal maximum

inferred← citeshttps://doi.org/10.1016/j.gloplacha.2026.105751openalex-snapshot

Multi-stressor-driven biotic upheaval across the PETM: A perspective from elemental and isotope ratios of foraminiferal and bulk carbonate in the southern Tethyan shelf

inferred← citeshttps://doi.org/10.1016/j.gr.2016.09.007openalex-snapshot

A stem lepidosireniform lungfish (Sarcopterygia: Dipnoi) from the Upper Eocene of Libya, North Africa and implications for Cenozoic lungfish evolution

inferred← citeshttps://doi.org/10.1016/j.gr.2017.02.016openalex-snapshot

Structure and magnitude of the carbon isotope excursion during the Paleocene-Eocene thermal maximum

inferred← citeshttps://doi.org/10.1016/j.gr.2017.12.002openalex-snapshot

Environmental changes during the Cretaceous-Paleogene mass extinction and Paleocene-Eocene Thermal Maximum: Implications for the Anthropocene

inferred← citeshttps://doi.org/10.1016/j.gr.2026.05.012openalex-snapshot

Spatial heterogeneity of the Middle Eocene Climate Optimum: Review and perspectives

inferred← citeshttps://doi.org/10.1016/j.gsf.2010.08.003openalex-snapshot

Biostratigraphy of a Paleocene–Eocene Foreland Basin boundary in southern Tibet

inferred← citeshttps://doi.org/10.1016/j.gsf.2018.04.002openalex-snapshot

Calcareous nannofossil changes linked to climate deterioration during the Paleocene–Eocene thermal maximum in Tarim Basin, NW China

inferred← citeshttps://doi.org/10.1016/j.heliyon.2023.e15221openalex-snapshot

An animal crisis caused by pollution, deforestation, and warming in the late 21st century and exacerbation by nuclear war

inferred← citeshttps://doi.org/10.1016/j.icarus.2005.02.021openalex-snapshot

Evaluation of the possible presence of clathrate hydrates in Europa's icy shell or seafloor

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.2015.07.011openalex-snapshot

Foraminifera from Paleocene –early Eocene rocks of Bir El Markha section (West Central Sinai), Egypt: Paleobathymetric and paleotemperature significance

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.2017.07.029openalex-snapshot

The nummulithoclast event within the Lower Eocene in the Southern Tethyan margin: Mechanisms involved, analogy with the filament event and climate implication (Kairouan, Central Tunisia)

inferred← citeshttps://doi.org/10.1016/j.jafrearsci.2018.07.013openalex-snapshot

The Paleocene/Eocene (P/E) boundary along the eastern plateau of Kharga-Baris oases, Western Desert, Egypt

inferred← citeshttps://doi.org/10.1016/j.jafrearsci.2021.104125openalex-snapshot

Study of the Upper Paleocene-Lower Ypresian phosphate succession in El Guettar out crop (Gafsa area, central Tunisia)

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.jafrearsci.2022.104609openalex-snapshot

Calcareous nannofossil biostratigraphy of the Eocene succession in West Central Sinai, Egypt

inferred← citeshttps://doi.org/10.1016/j.jafrearsci.2024.105483openalex-snapshot

Paleoenvironmental and sea level changes across the Paleocene-lower Eocene interval at the central and southwestern Sinai, Egypt

inferred← citeshttps://doi.org/10.1016/j.jafrearsci.2026.106365openalex-snapshot

Paleocene-Eocene oyster patch reefs, northern Subatlas Zone (Morocco): Genesis and palaeoenvironmental controls

inferred← citeshttps://doi.org/10.1016/j.jembe.2008.07.024openalex-snapshot

Predicting the impact of ocean acidification on benthic biodiversity: What can animal physiology tell us?

inferred← citeshttps://doi.org/10.1016/j.jhevol.2016.04.001openalex-snapshot

Cranial anatomy of Paleogene Micromomyidae and implications for early primate evolution

inferred← citeshttps://doi.org/10.1016/j.jop.2024.11.004openalex-snapshot

Mass organic matter accumulation induced by rapid redox variations in lakes: Evidence from the Miaoxi area, Bohai Bay Basin, China

inferred← citeshttps://doi.org/10.1016/j.jop.2026.100414openalex-snapshot

Ichnological analysis of the Paleocene–Eocene Thermal Maximum along a continental–marine transect reveals a protracted recovery at deep marine settings

inferred← citeshttps://doi.org/10.1016/j.jsames.2021.103209openalex-snapshot

Paleoclimate and changing composition of the Paleogene-Neogene shallow Molluscan Assemblages of Patagonia

inferred← citeshttps://doi.org/10.1016/j.jseaes.2018.05.027openalex-snapshot

Precursors of the Paleocene–Eocene Thermal Maximum (PETM) in the Subathu Group, NW sub-Himalaya, India

inferred← citeshttps://doi.org/10.1016/j.jseaes.2018.07.035openalex-snapshot

Early Eocene leaves of northwestern India and their response to climate change

inferred← citeshttps://doi.org/10.1016/j.jseaes.2024.106137openalex-snapshot

Multidisciplinary study on the stratigraphy of the upper Cretaceous-Paleogene successions in the western Tajik Basin, Uzbekistan

inferred← citeshttps://doi.org/10.1016/j.jseaes.2026.107268openalex-snapshot

Stable isotopes and larger benthic foraminiferal response to the Paleocene-Eocene Thermal Maximum in the shallow-water carbonates of the Lower Indus Basin (Eastern Tethys, Pakistan)

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.margeo.2012.10.010openalex-snapshot

Seismic-scale funnel-shaped collapse features from the Paleocene–Eocene of the North West Shelf of Australia

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.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.2006.10.002openalex-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.2006.11.007openalex-snapshot

The onset of the Paleocene–Eocene Thermal Maximum (PETM) at Sites 1209 and 1210 (Shatsky Rise, Pacific Ocean) as recorded by planktonic foraminifera

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.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.2008.07.002openalex-snapshot

Response of calcareous nannofossils to the Paleocene–Eocene Thermal Maximum: Observations on composition, preservation and calcification in sediments from ODP Site 1263 (Walvis Ridge — SW Atlantic)

inferred← citeshttps://doi.org/10.1016/j.marmicro.2009.03.003openalex-snapshot

Distinguishing the influence of diagenesis on the paleoecological reconstruction of nannoplankton across the Paleocene/Eocene Thermal Maximum: An example from the Kerguelen Plateau, southern Indian Ocean

inferred← citeshttps://doi.org/10.1016/j.marmicro.2009.10.005openalex-snapshot

Experimental dissolution of a fossil foraminiferal assemblage (Paleocene–Eocene Thermal Maximum, Dababiya, Egypt): Implications for paleoenvironmental reconstructions

inferred← citeshttps://doi.org/10.1016/j.marmicro.2011.06.006openalex-snapshot

Shifts in North Atlantic planktic foraminifer biogeography and subtropical gyre circulation during the mid-Piacenzian warm period

inferred← citeshttps://doi.org/10.1016/j.marmicro.2011.07.001openalex-snapshot

Dissolution susceptibility of Paleocene–Eocene planktic foraminifera: Implications for palaeoceanographic reconstructions

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.2012.05.003openalex-snapshot

Calcareous nannofossil assemblage changes across the Paleocene–Eocene Thermal Maximum: Evidence from a shelf setting

inferred← citeshttps://doi.org/10.1016/j.marmicro.2016.07.003openalex-snapshot

Response of calcareous nannofossils to the Paleocene-Eocene thermal maximum from a shelf section in Jordan

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.2017.12.004openalex-snapshot

Chamber formation and trace element distribution in the calcite walls of laboratory cultured planktonic foraminifera ( Globigerina bulloides and Globigerinoides ruber )

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.2023.102221openalex-snapshot

Changes in calcareous nannofossil assemblages linked to dramatic climate change over the Paleocene–Eocene Thermal Maximum in the Taramsa Section, Central Nile Valley, Egypt

inferred← citeshttps://doi.org/10.1016/j.marmicro.2026.102555openalex-snapshot

Foraminiferal biostratigraphy, paleoenvironmental interpretation, and sequence stratigraphy of the latest Maastrichtian–Thanetian succession in the Southern Galala Plateau, Eastern Desert, Egypt

inferred← citeshttps://doi.org/10.1016/j.marmicro.2026.102579openalex-snapshot

Calcareous nannofossil assemblage changes in the Surprise Hill core and their implications for floral response to the Paleocene-Eocene Thermal Maximum across the Salisbury Embayment of Virginia, USA

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