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Eocene greenhouse climate revealed by coupled clumped isotope-Mg/Ca thermometry
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What this work says
Outgoing claims: the papers this work cites, builds on, or argues with.
inferredcites →https://doi.org/10.1002/2014pa002723openalex-snapshot
Descent toward the Icehouse: Eocene sea surface cooling inferred from GDGT distributions
inferredcites →https://doi.org/10.1016/0016-7037(95)00105-9openalex-snapshot
Reconstructing past sea surface temperatures: Correcting for diagenesis of bulk marine carbonate
inferredcites →https://doi.org/10.1016/j.epsl.2009.07.026openalex-snapshot
Climate sensitivity to Arctic seaway restriction during the early Paleogene
inferredcites →https://doi.org/10.1016/j.epsl.2012.06.024openalex-snapshot
Early Paleogene temperature history of the Southwest Pacific Ocean: Reconciling proxies and models
inferredcites →https://doi.org/10.1016/j.epsl.2013.07.026openalex-snapshot
A revised calibration of the clumped isotope thermometer
inferredcites →https://doi.org/10.1016/j.epsl.2013.08.035openalex-snapshot
Eocene seasonality and seawater alkaline earth reconstruction using shallow-dwelling large benthic foraminifera
inferredcites →https://doi.org/10.1016/j.epsl.2015.01.003openalex-snapshot
The Mg isotopic composition of Cenozoic seawater – evidence for a link between Mg-clays, seawater Mg/Ca, and climate
inferredcites →https://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
inferredcites →https://doi.org/10.1016/j.gca.2005.11.014openalex-snapshot
13C–18O bonds in carbonate minerals: A new kind of paleothermometer
inferredcites →https://doi.org/10.1016/j.gca.2010.05.027openalex-snapshot
New indices and calibrations derived from the distribution of crenarchaeal isoprenoid tetraether lipids: Implications for past sea surface temperature reconstructions
inferredcites →https://doi.org/10.1016/j.gca.2011.09.025openalex-snapshot
Defining an absolute reference frame for ‘clumped’ isotope studies of CO2
inferredcites →https://doi.org/10.1016/j.gca.2013.07.028openalex-snapshot
The influence of salinity on Mg/Ca in planktic foraminifers – Evidence from cultures, core-top sediments and complementary δ18O
inferredcites →https://doi.org/10.1016/j.gca.2013.11.026openalex-snapshot
A Bayesian, spatially-varying calibration model for the TEX86 proxy
inferredcites →https://doi.org/10.1016/j.gca.2014.03.005openalex-snapshot
Evaluation of kinetic effects on clumped isotope fractionation (Δ47) during inorganic calcite precipitation
inferredcites →https://doi.org/10.1016/j.gca.2014.09.039openalex-snapshot
Mg/Ca-temperature and seawater-test chemistry relationships in the shallow-dwelling large benthic foraminifera Operculina ammonoides
inferredcites →https://doi.org/10.1016/j.gca.2015.03.018openalex-snapshot
Fossil corals as an archive of secular variations in seawater chemistry since the Mesozoic
inferredcites →https://doi.org/10.1016/j.gca.2015.12.034openalex-snapshot
Last glacial-Holocene temperatures and hydrology of the Sea of Galilee and Hula Valley from clumped isotopes in Melanopsis shells
inferredcites →https://doi.org/10.1016/j.marmicro.2005.10.004openalex-snapshot
Large benthic foraminifera from the deep photic zone of a mixed siliciclastic-carbonate shelf off East Kalimantan, Indonesia
inferredcites →https://doi.org/10.1016/j.palaeo.2006.03.044openalex-snapshot
Evaporites and the salinity of the ocean during the Phanerozoic: Implications for climate, ocean circulation and life
inferredcites →https://doi.org/10.1016/j.palaeo.2014.07.011openalex-snapshot
Cool tropics in the Middle Eocene: Evidence from the Changchang Flora, Hainan Island, China
inferredcites →https://doi.org/10.1016/s0009-2541(99)00088-1openalex-snapshot
Effects of diagenesis on the isotopic record of late paleogene tropical sea surface temperatures
inferredcites →https://doi.org/10.1016/s0016-7037(01)00884-5openalex-snapshot
Chemical evolution of seawater during the Phanerozoic
inferredcites →https://doi.org/10.1016/s0031-0182(98)00109-6openalex-snapshot
Secular oscillations in the carbonate mineralogy of reef-building and sediment-producing organisms driven by tectonically forced shifts in seawater chemistry
inferredcites →https://doi.org/10.1029/2003pa000937openalex-snapshot
Tropical sea‐surface temperature reconstruction for the early Paleogene using Mg/Ca ratios of planktonic foraminifera
inferredcites →https://doi.org/10.1029/2007pa001495openalex-snapshot
Arctic late Paleocene–early Eocene paleoenvironments with special emphasis on the Paleocene‐Eocene thermal maximum (Lomonosov Ridge, Integrated Ocean Drilling Program Expedition 302)
inferredcites →https://doi.org/10.1029/2008gl035758openalex-snapshot
Greenland ice sheet motion coupled with daily melting in late summer
inferredcites →https://doi.org/10.1029/2009gl039849openalex-snapshot
Global warming, convective threshold and false thermostats
inferredcites →https://doi.org/10.1029/2010pa002056openalex-snapshot
Planktonic foraminiferal oxygen isotope analysis by ion microprobe technique suggests warm tropical sea surface temperatures during the Early Paleogene
inferredcites →https://doi.org/10.1029/2011jc007255openalex-snapshot
Late Cretaceous–Neogene trends in deep ocean temperature and continental ice volume: Reconciling records of benthic foraminiferal geochemistry ( δ 18 O and Mg/Ca) with sea level history
inferredcites →https://doi.org/10.1029/2012pa002315openalex-snapshot
Deep time foraminifera Mg/Ca paleothermometry: Nonlinear correction for secular change in seawater Mg/Ca
inferredcites →https://doi.org/10.1038/35097000openalex-snapshot
Warm tropical sea surface temperatures in the Late Cretaceous and Eocene epochs
inferredcites →https://doi.org/10.1038/nature08399openalex-snapshot
Early Palaeogene temperature evolution of the southwest Pacific Ocean
inferredcites →https://doi.org/10.1038/nature17423openalex-snapshot
Changing atmospheric CO2 concentration was the primary driver of early Cenozoic climate
inferredcites →https://doi.org/10.1038/nclimate3190openalex-snapshot
Climate goals and computing the future of clouds
inferredcites →https://doi.org/10.1038/ngeo2763openalex-snapshot
Flat meridional temperature gradient in the early Eocene in the subsurface rather than surface ocean
inferredcites →https://doi.org/10.1039/b805995kopenalex-snapshot
Initial performance metrics of a new custom-designed ArF excimer LA-ICPMS system coupled to a two-volume laser-ablation cell
inferredcites →https://doi.org/10.1073/pnas.1220872110openalex-snapshot
Eocene cooling linked to early flow across the Tasmanian Gateway
inferredcites →https://doi.org/10.1073/pnas.1321441111openalex-snapshot
Pronounced zonal heterogeneity in Eocene southern high-latitude sea surface temperatures
inferredcites →https://doi.org/10.1098/rsta.2010.0317openalex-snapshot
Are there pre-Quaternary geological analogues for a future greenhouse warming?
inferredcites →https://doi.org/10.1098/rsta.2013.0093openalex-snapshot
Sensitivity of the Palaeocene–Eocene Thermal Maximum climate to cloud properties
inferredcites →https://doi.org/10.1098/rsta.2013.0123openalex-snapshot
The Early Eocene equable climate problem: can perturbations of climate model parameters identify possible solutions?
inferredcites →https://doi.org/10.1098/rsta.2013.0146openalex-snapshot
Warm climates of the past—a lesson for the future?
inferredcites →https://doi.org/10.1126/sciadv.1600891openalex-snapshot
Extreme warmth and heat-stressed plankton in the tropics during the Paleocene-Eocene Thermal Maximum
inferredcites →https://doi.org/10.1126/science.1182252openalex-snapshot
Reconstructing Past Seawater Mg/Ca and Sr/Ca from Mid-Ocean Ridge Flank Calcium Carbonate Veins
inferredcites →https://doi.org/10.1130/0-8137-2332-9.1openalex-snapshot
Alternative global Cretaceous paleogeography
inferredcites →https://doi.org/10.1130/g23175a.1openalex-snapshot
Stable warm tropical climate through the Eocene Epoch
inferredcites →https://doi.org/10.1130/g25200a.1openalex-snapshot
Tropical sea temperatures in the high-latitude South Pacific during the Eocene
inferredcites →https://doi.org/10.1130/g31184.1openalex-snapshot
CO2-driven ocean circulation changes as an amplifier of Paleocene-Eocene thermal maximum hydrate destabilization
inferredcites →https://doi.org/10.1130/g32054.1openalex-snapshot
Warm, not super-hot, temperatures in the early Eocene subtropics
inferredcites →https://doi.org/10.1130/g35637.1openalex-snapshot
Extreme warming of tropical waters during the Paleocene–Eocene Thermal Maximum
inferredcites →https://doi.org/10.1144/gsjgs.138.2.0153openalex-snapshot
The climate of the Eocene ocean
inferredcites →https://doi.org/10.1175/2009jcli3113.1openalex-snapshot
Climate Response at the Paleocene–Eocene Thermal Maximum to Greenhouse Gas Forcing—A Model Study with CCSM3
inferredcites →https://doi.org/10.2475/ajs.289.10.1158openalex-snapshot
Sedimentary carbonate record of calcium-magnesium cycling
inferredcites →https://doi.org/10.5194/cp-12-819-2016openalex-snapshot
Revisiting carbonate chemistry controls on planktic foraminifera Mg / Ca: implications for sea surface temperature and hydrology shifts over the Paleocene–Eocene Thermal Maximum and Eocene–Oligocene transition
inferredcites →https://doi.org/10.5194/cp-5-785-2009openalex-snapshot
Warm Paleocene/Eocene climate as simulated in ECHAM5/MPI-OM
inferredcites →https://doi.org/10.5194/cp-7-603-2011openalex-snapshot
The early Eocene equable climate problem revisited
inferredcites →https://doi.org/10.5194/cp-8-1717-2012openalex-snapshot
A model–data comparison for a multi-model ensemble of early Eocene atmosphere–ocean simulations: EoMIP
inferredcites →https://doi.org/10.5194/gmd-10-889-2017openalex-snapshot
The DeepMIP contribution to PMIP4: experimental design for model simulations of the EECO, PETM, and pre-PETM (version 1.0)
What points at this work
Incoming claims: where this work appears in other papers’ reference lists and arguments.
inferred← citeshttps://doi.org/10.1093/zoolinnean/zlae117zenodo-depositor-declared
A new family of freshwater snails with Cretaceous origin from Yunnan, China
inferred← citeshttps://doi.org/10.2139/ssrn.4585263openalex-extracted
Paleogene Sea Subsurface Temperatures: A Multi-Proxy Analysis Based on Planktonic Foraminifera
inferred← citeshttps://doi.org/10.5070/p939257077zenodo-depositor-declared
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Global Warming and Mass Extinctions Associated With Large Igneous Province Volcanism
inferred← citeshttps://doi.org/10.1002/dep2.70039openalex-snapshot
Mechanisms of near‐normal sea water dolomitisation: Mesohaline‐reflux or syn‐depositional?
inferred← citeshttps://doi.org/10.1002/ece3.70701openalex-snapshot
Earth's Climate History Explains Life's Temperature Optima
inferred← citeshttps://doi.org/10.1002/essoar.10512308.1openalex-snapshot
Global- and regional-scale hydrological response to early Eocene warmth
inferred← citeshttps://doi.org/10.1002/qj.3660openalex-snapshot
Changes in mean flow and atmospheric wave activity in the North Atlantic sector
inferred← citeshttps://doi.org/10.1002/rcm.8678openalex-snapshot
Effects of different constants and standards on the reproducibility of carbonate clumped isotope (Δ 47 ) measurements: Insights from a long‐term dataset
inferred← citeshttps://doi.org/10.1002/rcm.9692openalex-snapshot
Accurate measurement of K/Ca in low‐[K] carbonate samples using laser‐ablation sector‐field inductively coupled plasma mass spectrometry
inferred← citeshttps://doi.org/10.1007/978-3-032-22801-7_1openalex-snapshot
Origins and Evolution of Bats in the Americas
inferred← citeshttps://doi.org/10.1007/s11430-024-1439-yopenalex-snapshot
Paleoclimate data assimilation: Principles and prospects
inferred← citeshttps://doi.org/10.1007/s12549-019-00377-4openalex-snapshot
Paleogene climate dynamics in the Primorye Region, Far East of Russia, based on a Coexistence Approach analysis of palaeobotanical data
inferred← citeshttps://doi.org/10.1007/s12549-025-00692-zopenalex-snapshot
Diversity and biolithostratigraphy of foraminifera from the upper Eocene–lower Oligocene Malishka section, Armenia
inferred← citeshttps://doi.org/10.1007/s13146-025-01066-4openalex-snapshot
Architectural development of early Eocene third-order dolomite-anhydrite sequences, Sirte Basin, Libya—Sequence stratigraphy and controlling factors
inferred← citeshttps://doi.org/10.1016/b978-0-08-102908-4.00174-0openalex-snapshot
Approaches to Paleoclimate Reconstruction
inferred← citeshttps://doi.org/10.1016/b978-0-12-823957-5.00006-8openalex-snapshot
Foraminifera—witness of the evolving Earth
inferred← citeshttps://doi.org/10.1016/b978-0-12-823957-5.00007-xopenalex-snapshot
Signals of deep-time climate change
inferred← citeshttps://doi.org/10.1016/b978-0-12-823957-5.00008-1openalex-snapshot
Geochemical proxies of climate and environment
inferred← citeshttps://doi.org/10.1016/j.apgeochem.2024.105925openalex-snapshot
Reconstructing the temperature and origin of CO2 mineralisation in CarbFix calcite using clumped, carbon and oxygen isotopes
inferred← citeshttps://doi.org/10.1016/j.cretres.2025.106258openalex-snapshot
Seawater properties based on clumped isotope analyses of macrofossil assemblages from the Upper Cretaceous–lower Paleocene Type-Maastrichtian area
inferred← citeshttps://doi.org/10.1016/j.earscirev.2019.01.025openalex-snapshot
The evolution of latitudinal temperature gradients from the latest Cretaceous through the Present
inferred← citeshttps://doi.org/10.1016/j.earscirev.2019.102961openalex-snapshot
Climatic and environmental changes across the early Eocene climatic optimum at mid-Waipara River, Canterbury Basin, New Zealand
inferred← citeshttps://doi.org/10.1016/j.earscirev.2021.103546openalex-snapshot
Evolution of paleo-climate and seawater pH from the late Permian to postindustrial periods recorded by boron isotopes and B/Ca in biogenic carbonates
inferred← citeshttps://doi.org/10.1016/j.earscirev.2024.105036openalex-snapshot
Global vegetation zonation and terrestrial climate of the warm Early Eocene
inferred← citeshttps://doi.org/10.1016/j.epsl.2019.05.025openalex-snapshot
Evidence for seasonality in early Eocene high latitude sea-surface temperatures
inferred← citeshttps://doi.org/10.1016/j.epsl.2019.115824openalex-snapshot
Evaluating the planktic foraminiferal B/Ca proxy for application to deep time paleoceanography
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.2022.117589openalex-snapshot
Paleoenvironmental evolution during the Early Eocene Climate Optimum in the Chicxulub impact crater
inferred← citeshttps://doi.org/10.1016/j.epsl.2023.118313openalex-snapshot
Clumped isotopes in globally distributed Holocene coccoliths reveal their habitat depth
inferred← citeshttps://doi.org/10.1016/j.epsl.2023.118565openalex-snapshot
Enhanced volcanic activity and long-term warmth in the middle Eocene revealed by mercury and osmium isotopes from IODP Expedition 369 Site U1514
inferred← citeshttps://doi.org/10.1016/j.epsl.2024.118981openalex-snapshot
Eocene climate and hydrology of eastern Asia controlled by orbital forcing and Tibetan Plateau uplift
inferred← citeshttps://doi.org/10.1016/j.epsl.2026.119863openalex-snapshot
Seasonal upper ocean temperatures from coccolith clumped isotopes and a proxy-model comparison for the late Early Eocene Climatic Optimum
inferred← citeshttps://doi.org/10.1016/j.gca.2018.03.010openalex-snapshot
Coupled Mg/Ca and clumped isotope analyses of foraminifera provide consistent water temperatures
inferred← citeshttps://doi.org/10.1016/j.gca.2018.07.038openalex-snapshot
The clumped (13C18O) isotope composition of echinoid calcite: Further evidence for “vital effects” in the clumped isotope proxy
inferred← citeshttps://doi.org/10.1016/j.gca.2019.05.005openalex-snapshot
Sensitivity of clumped isotope temperatures in fossil benthic and planktic foraminifera to diagenetic alteration
inferred← citeshttps://doi.org/10.1016/j.gca.2019.07.055openalex-snapshot
Kinetic clumped isotope fractionation in the DIC-H2O-CO2 system: Patterns, controls, and implications
inferred← citeshttps://doi.org/10.1016/j.gca.2019.11.022openalex-snapshot
A robust calibration of the clumped isotopes to temperature relationship for foraminifers
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.2022.10.030openalex-snapshot
On the combination of the planktonic foraminiferal Mg/Ca, clumped (Δ47) and conventional (δ18O) stable isotope paleothermometers in palaeoceanographic studies
inferred← citeshttps://doi.org/10.1016/j.gca.2023.04.020openalex-snapshot
Controls on potassium incorporation in foraminifera and other marine calcifying organisms
inferred← citeshttps://doi.org/10.1016/j.gca.2024.06.020openalex-snapshot
Boron isotope pH calibration of a shallow dwelling benthic nummulitid foraminifera
inferred← citeshttps://doi.org/10.1016/j.gca.2025.10.008openalex-snapshot
Most bivalves and gastropods calcify indistinguishably from dual clumped isotope equilibrium
inferred← citeshttps://doi.org/10.1016/j.gca.2025.10.023openalex-snapshot
Clumped isotope thermometry (Δ47) measurements in marine gastropods suggest equilibrium precipitation
inferred← citeshttps://doi.org/10.1016/j.geobios.2022.07.005openalex-snapshot
Systematics and phylogenetic interpretation of a new bathyal spatangoid echinoid from the Eocene of Spain: Habanaster itzae nov. sp
inferred← citeshttps://doi.org/10.1016/j.gloplacha.2018.08.017openalex-snapshot
Temperature dependency of metabolic rates in the upper ocean: A positive feedback to global climate change?
inferred← citeshttps://doi.org/10.1016/j.gloplacha.2023.104352openalex-snapshot
Influence of plate reference frames on deep-time climate simulations
inferred← citeshttps://doi.org/10.1016/j.gloplacha.2026.105547openalex-snapshot
Low elevation and humid climate in the Eocene Gerze basin, central Tibet: Insights from multi-proxy isotopic analyses
inferred← citeshttps://doi.org/10.1016/j.gr.2018.12.001openalex-snapshot
Modelling the long-term carbon cycle, atmospheric CO2, and Earth surface temperature from late Neoproterozoic to present day
inferred← citeshttps://doi.org/10.1016/j.isci.2025.113430openalex-snapshot
Eocene amber fossils reveal how complex trophic interactions shaped tropical rainforest biodiversity
inferred← citeshttps://doi.org/10.1016/j.jafrearsci.2025.105889openalex-snapshot
Anatomy of Early Eocene dolomite-anhydrite sequences developed on a detached carbonate platform during greenhouse conditions, NW Sirte Basin, Libya: Sequence stratigraphic architecture and key factors
inferred← citeshttps://doi.org/10.1016/j.jafrearsci.2026.106354openalex-snapshot
Micropalaeontology and geochemistry of outcropping Paleogene and Neogene marine sediments of southern Tanzania
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.jseaes.2023.105975openalex-snapshot
Carbonate clumped isotopes and blocking temperatures of marbles from the Backbone Range, Taiwan
inferred← citeshttps://doi.org/10.1016/j.jseaes.2025.106604openalex-snapshot
Biodiversity and paleoenvironments of vertebrate-rich Eocene marine deposits (Lutetian) of the tropical western Neotethys: New insights from the Arabian Platform
inferred← citeshttps://doi.org/10.1016/j.palaeo.2020.109777openalex-snapshot
Carbonate clumped isotope evidence for latitudinal seawater temperature gradients and the oxygen isotope composition of Early Cretaceous seas
inferred← citeshttps://doi.org/10.1016/j.palaeo.2021.110528openalex-snapshot
Carbon and oxygen isotope variations in shell beds from the Upper Ordovician (mid-Cincinnatian: Maysvillian to early Richmondian) of Ontario: Evaluation of the Warm Saline Deep Ocean hypothesis, paleoceanographic changes, and Milankovitch orbital cycles in the transition to the Hirnantian glaciation
inferred← citeshttps://doi.org/10.1016/j.palaeo.2023.111729openalex-snapshot
Chromium isotopic compositions of a reef in the South China Sea: Biological effects and influence from early diagenetic Mn-oxides reduction
inferred← citeshttps://doi.org/10.1016/j.palaeo.2023.111762openalex-snapshot
High rainfall afforded resilience to tropical rainforests during Early Eocene Climatic Optimum
inferred← citeshttps://doi.org/10.1016/j.palaeo.2024.112627openalex-snapshot
Making sense of variation in sclerochronological stable isotope profiles of mollusks and fish otoliths from the early Eocene southern North Sea Basin
inferred← citeshttps://doi.org/10.1016/j.palaeo.2024.112660openalex-snapshot
Planktic foraminiferal response to the Early Eocene Climatic Optimum (EECO) from southern mid-to-high latitudes
inferred← citeshttps://doi.org/10.1016/j.palaeo.2025.113108openalex-snapshot
Fish tooth oxygen isotopes as indicators of Lutetian seawater paleotemperatures and paleoecology in the tropical Neo-Tethys (Arabian Platform)
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.palaeo.2025.113350openalex-snapshot
Intra-annually-resolved sea surface temperature variability at the onset of the Oligocene icehouse based on Nummulites geochemistry
inferred← citeshttps://doi.org/10.1016/j.palaeo.2026.113960openalex-snapshot
Size-driven dietary partitioning in Archaeotherium (the North American “Hell Pig”) revealed through dental microwear texture analysis
inferred← citeshttps://doi.org/10.1016/j.quascirev.2021.107223openalex-snapshot
Eastern Mediterranean climate change deduced from the Soreq Cave fluid inclusion stable isotopes and carbonate clumped isotopes record of the last 160 ka
inferred← citeshttps://doi.org/10.1016/j.ringeo.2020.100004openalex-snapshot
Petrogenesis of Siletzia: The world's youngest oceanic plateau
inferred← citeshttps://doi.org/10.1016/j.scib.2024.02.028openalex-snapshot
Cenozoic Indo-Pacific warm pool controlled by both atmospheric CO2 and paleogeography
inferred← citeshttps://doi.org/10.1016/j.sedgeo.2025.106940openalex-snapshot
From Platform to Burial: Tectonic and climatic imprints on the diagenetic evolution of shallow-marine carbonate deposits (Middle Eocene), Bombay Offshore Basin, India
inferred← citeshttps://doi.org/10.1017/s0016756823000377openalex-snapshot
Cenozoic evolution of the Tripolitza carbonate platform in the Tethyan realm: new age constraints on deposition, diagenesis, metamorphism and nappe emplacement based on U-Pb and Rb-Sr dating (External Hellenides, Crete)
inferred← citeshttps://doi.org/10.1029/2017gc007385openalex-snapshot
Reducing Uncertainties in Carbonate Clumped Isotope Analysis Through Consistent Carbonate‐Based Standardization
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/10.1029/2018pa003391openalex-snapshot
Warm Terrestrial Subtropics During the Paleocene and Eocene: Carbonate Clumped Isotope (Δ47) Evidence From the Tornillo Basin, Texas (USA)
inferred← citeshttps://doi.org/10.1029/2018pa003453openalex-snapshot
Comparing Seawater Temperature Proxy Records for the Past 90 Myrs From the Shallow Shelf Record Bass River, New Jersey
inferred← citeshttps://doi.org/10.1029/2019av000159openalex-snapshot
A Decrease to Low Carbonate Clumped Isotope Temperatures in Cryogenian Strata
inferred← citeshttps://doi.org/10.1029/2019gc008794openalex-snapshot
The Giant Marine Gastropod Campanile Giganteum (Lamarck, 1804) as a High‐Resolution Archive of Seasonality in the Eocene Greenhouse World
inferred← citeshttps://doi.org/10.1029/2019pa003638openalex-snapshot
Midlatitude Temperature Variations in the Oligocene to Early Miocene
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/10.1029/2019pa003744openalex-snapshot
Bayesian Calibration of the Mg/Ca Paleothermometer in Planktic Foraminifera
inferred← citeshttps://doi.org/10.1029/2019pa003811openalex-snapshot
Enhanced Poleward Flux of Atmospheric Moisture to the Weddell Sea Region (ODP Site 690) During the Paleocene‐Eocene Thermal Maximum
inferred← citeshttps://doi.org/10.1029/2019tc005545openalex-snapshot
Thermotectonic History of the Kluane Ranges and Evolution of the Eastern Denali Fault Zone in Southwestern Yukon, Canada
inferred← citeshttps://doi.org/10.1029/2020gc009443openalex-snapshot
Intratest Variations in Trace Element Composition of Amphistegina lessonii Using Femtosecond‐Laser Ablation‐ICP‐Mass Spectrometry: A Field Study From Akajima, Okinawa Prefecture, Japan
inferred← citeshttps://doi.org/10.1029/2020gl089044openalex-snapshot
A Dynamical Framework for Interpreting Ancient Sea Surface Temperatures
inferred← citeshttps://doi.org/10.1029/2020pa003873openalex-snapshot
Constraints on Earth System Functioning at the Paleocene‐Eocene Thermal Maximum From the Marine Silicon Cycle
inferred← citeshttps://doi.org/10.1029/2020pa003920openalex-snapshot
Initiation of the Western Pacific Warm Pool at the Middle Miocene Climate Transition?
inferred← citeshttps://doi.org/10.1029/2020pa003927openalex-snapshot
Warm Middle Miocene Indian Ocean Bottom Water Temperatures: Comparison of Clumped Isotope and Mg/Ca‐Based Estimates
inferred← citeshttps://doi.org/10.1029/2020pa003932openalex-snapshot
A Warm, Stratified, and Restricted Labrador Sea Across the Middle Eocene and Its Climatic Optimum
inferred← citeshttps://doi.org/10.1029/2020pa004165openalex-snapshot
Tropical Sea Surface Temperatures Following the Middle Miocene Climate Transition From Laser‐Ablation ICP‐MS Analysis of Glassy Foraminifera
inferred← citeshttps://doi.org/10.1029/2021pa004218openalex-snapshot
Salinity Effect on Trace Element Incorporation in Cultured Shells of the Large Benthic Foraminifer Operculinaammonoides
inferred← citeshttps://doi.org/10.1029/2021pa004278openalex-snapshot
Evidence of a South Asian Proto‐Monsoon During the Oligocene‐Miocene Transition
inferred← citeshttps://doi.org/10.1029/2021pa004375openalex-snapshot
Variations on a Pathway to an Early Eocene Climate
inferred← citeshttps://doi.org/10.1029/2022gc010742openalex-snapshot
Temperature Calibration of Elevated Mg/Ca in Planktic Foraminifera Shells From the Hypersaline Gulf of Aqaba
inferred← citeshttps://doi.org/10.1029/2022pa004418openalex-snapshot
Plant Proxy Evidence for High Rainfall and Productivity in the Eocene of Australia
inferred← citeshttps://doi.org/10.1029/2022pa004529openalex-snapshot
Revisiting the Geographical Extent of Exceptional Warmth in the Early Paleogene Southern Ocean
inferred← citeshttps://doi.org/10.1029/2022pa004542openalex-snapshot
Global and Zonal‐Mean Hydrological Response to Early Eocene Warmth
inferred← citeshttps://doi.org/10.1029/2022pa004569openalex-snapshot
Atmospheric CO2 Estimates for the Late Oligocene and Early Miocene Using Multi‐Species Cross‐Calibrations of Boron Isotopes
inferred← citeshttps://doi.org/10.1029/2022pa004607openalex-snapshot
Meridional Heat Transport in the DeepMIP Eocene Ensemble: Non‐CO 2 and CO 2 Effects
inferred← citeshttps://doi.org/10.1029/2022rg000775openalex-snapshot
Comparison and Synthesis of Sea‐Level and Deep‐Sea Temperature Variations Over the Past 40 Million Years
inferred← citeshttps://doi.org/10.1029/2023gl105448openalex-snapshot
Surface Ocean Cooling in the Eocene North Atlantic Coincides With Declining Atmospheric CO2
inferred← citeshttps://doi.org/10.1029/2023pa004613openalex-snapshot
Calibrating Non‐Thermal Effects on Planktic Foraminiferal Mg/Ca for Application Across the Cenozoic
inferred← citeshttps://doi.org/10.1029/2023pa004650openalex-snapshot
Transient Deep Ocean Cooling in the Eastern Equatorial Pacific Ocean at the Eocene‐Oligocene Transition
inferred← citeshttps://doi.org/10.1029/2023pa004788openalex-snapshot
The Temperature of the Deep Ocean Is a Robust Proxy for Global Mean Surface Temperature During the Cenozoic
inferred← citeshttps://doi.org/10.1029/2023pa004822openalex-snapshot
The Role of Tidal Mixing in Shaping Early Eocene Deep Ocean Circulation and Oxygenation
inferred← citeshttps://doi.org/10.1029/2024gl108623openalex-snapshot
Magnesium Isotopes of Carbonate Reveal Seasonal Climate Variation in the Central East Asia During the Middle Eocene
inferred← citeshttps://doi.org/10.1029/2024pa004907openalex-snapshot
Orbital (Hydro)Climate Variability in the Ice‐Free Early Eocene Arctic
inferred← citeshttps://doi.org/10.1029/2024pa005038openalex-snapshot
Major Shifts in Equatorial Atlantic and Pacific Calcareous Nannofossil Assemblages Across the Early Eocene Climatic Optimum (EECO; ∼53–49 Ma)
inferred← citeshttps://doi.org/10.1029/2025pa005129openalex-snapshot
Habitat Specific Growth Rate Adaptation in Oysters During Early Bartonian: Effects of High Temperature and Low Seasonality in the Indian Palaeotropics
inferred← citeshttps://doi.org/10.1029/2025pa005176openalex-snapshot
Thermal and Non‐Thermal Controls on Benthic Foraminiferal Mg/Ca, Sr/Ca, B/Ca, and Mg/Li: Global Core‐Top Compilation, Revised Calibrations, and Application to the Geologic Record
inferred← citeshttps://doi.org/10.1038/s41467-018-05303-4openalex-snapshot
No substantial long-term bias in the Cenozoic benthic foraminifera oxygen-isotope record
inferred← citeshttps://doi.org/10.1038/s41467-018-06319-6openalex-snapshot
Vegetation response to exceptional global warmth during Oceanic Anoxic Event 2
inferred← citeshttps://doi.org/10.1038/s41467-019-11110-2openalex-snapshot
Evolution of tropical cyclone genesis regions during the Cenozoic era
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/s41467-020-18558-7openalex-snapshot
Cold spells in the Nordic Seas during the early Eocene Greenhouse
inferred← citeshttps://doi.org/10.1038/s41467-023-37781-6openalex-snapshot
What the geological past can tell us about the future of the ocean’s twilight zone
inferred← citeshttps://doi.org/10.1038/s41467-025-64241-0openalex-snapshot
A European monsoon-like climate in a warmhouse world
inferred← citeshttps://doi.org/10.1038/s41561-018-0199-0openalex-snapshot
High temperatures in the terrestrial mid-latitudes during the early Palaeogene
inferred← citeshttps://doi.org/10.1038/s41561-020-00648-2openalex-snapshot
Spatial pattern of super-greenhouse warmth controlled by elevated specific humidity
inferred← citeshttps://doi.org/10.1038/s41561-021-00859-1openalex-snapshot
Poleward expansion of tropical cyclone latitudes in warming climates
inferred← citeshttps://doi.org/10.1038/s41561-023-01234-yopenalex-snapshot
Enhanced clay formation key in sustaining the Middle Eocene Climatic Optimum.
inferred← citeshttps://doi.org/10.1038/s41561-025-01878-yopenalex-snapshot
Oligocene deep ocean oxygen isotope variations primarily driven by temperature
inferred← citeshttps://doi.org/10.1038/s41586-018-0272-2openalex-snapshot
Synchronous tropical and polar temperature evolution in the Eocene
inferred← citeshttps://doi.org/10.1038/s41597-022-01826-0openalex-snapshot
The PhanSST global database of Phanerozoic sea surface temperature proxy data
inferred← citeshttps://doi.org/10.1038/s41598-019-41013-7openalex-snapshot
Climate- and gateway-driven cooling of Late Eocene to earliest Oligocene sea surface temperatures in the North Sea Basin
inferred← citeshttps://doi.org/10.1038/s41598-020-60379-7openalex-snapshot
Divergent mammalian body size in a stable Eocene greenhouse climate
inferred← citeshttps://doi.org/10.1038/s41598-022-11493-1openalex-snapshot
Ocean temperatures through the Phanerozoic reassessed
inferred← citeshttps://doi.org/10.1038/s41598-024-58377-0openalex-snapshot
Largest known madtsoiid snake from warm Eocene period of India suggests intercontinental Gondwana dispersal
inferred← citeshttps://doi.org/10.1038/s41598-024-79779-0openalex-snapshot
Spatiotemporal changes in riverine input into the Eocene North Sea revealed by strontium isotope and barium analysis of bivalve shells
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/10.1038/s43247-024-01531-3openalex-snapshot
Paleoclimate data provide constraints on climate models' large-scale response to past CO2 changes
inferred← citeshttps://doi.org/10.1038/s43247-025-02288-zopenalex-snapshot
Persistent greenhouse conditions in Eocene North America point to lower climate sensitivity
inferred← citeshttps://doi.org/10.1038/s43247-025-02479-8openalex-snapshot
Substantial continental temperature rise over the Paleocene-Eocene Thermal Maximum in the Pyrenees
inferred← citeshttps://doi.org/10.1038/s43247-026-03770-yopenalex-snapshot
Dual clumped isotopes in foraminiferal calcite reveal kinetic bias in some species
inferred← citeshttps://doi.org/10.1051/bsgf/2022002openalex-snapshot
Hydrological differences between the Lutetian Paris and Hampshire basins revealed by stable isotopes of conid gastropods
inferred← citeshttps://doi.org/10.1073/pnas.2111332119openalex-snapshot
The latitudinal temperature gradient and its climate dependence as inferred from foraminiferal δ 18 O over the past 95 million years
inferred← citeshttps://doi.org/10.1073/pnas.2318779121openalex-snapshot
Long- and short-term coupling of sea surface temperature and atmospheric CO 2 during the late Paleocene and early Eocene
inferred← citeshttps://doi.org/10.1073/pnas.2511781122openalex-snapshot
The major ion chemistry of seawater was closely coupled to the long-term carbon cycle during the Cenozoic
inferred← citeshttps://doi.org/10.1080/10256016.2023.2271127openalex-snapshot
Isotopic history of seawater: the stable isotope character of the global ocean at present and in the geological past
inferred← citeshttps://doi.org/10.1088/1748-9326/ac9c74openalex-snapshot
Elevation-dependent temperature response in early Eocene using paleoclimate model experiment
inferred← citeshttps://doi.org/10.1093/icb/icy111openalex-snapshot
Loss of Biodiversity Dimensions through Shifting Climates and Ancient Mass Extinctions
inferred← citeshttps://doi.org/10.1093/nsr/nwaa101openalex-snapshot
Large shift of the Pacific Walker Circulation across the Cenozoic
inferred← citeshttps://doi.org/10.1093/sysbio/syaa006openalex-snapshot
Tropical Niche Conservatism Explains the Eocene Migration from India to Southeast Asia in Ochyroceratid Spiders
inferred← citeshttps://doi.org/10.1101/2021.03.24.436109openalex-snapshot
gen3sis: the general engine for eco-evolutionary simulations on the origins of biodiversity
inferred← citeshttps://doi.org/10.1111/evo.14209openalex-snapshot
Climatic effects on niche evolution in a passerine bird clade depend on paleoclimate reconstruction method
inferred← citeshttps://doi.org/10.1111/geb.13503openalex-snapshot
Origin of the tropical–polar biodiversity contrast
inferred← citeshttps://doi.org/10.1111/ggr.12351openalex-snapshot
Potassium and Calcium K‐Edge XANES in Chemical Compounds and Minerals: Implications for Geological Phase Identification
inferred← citeshttps://doi.org/10.1111/sed.12982openalex-snapshot
Extensive recrystallization of Cenozoic dolomite during shallow burial: A case study from the Palaeocene–Eocene Umm er Radhuma formation and a global meta‐analysis
inferred← citeshttps://doi.org/10.1111/sed.70059openalex-snapshot
Some record it hot: Clumped isotope temperatures from Middle Jurassic molluscan aragonite
inferred← citeshttps://doi.org/10.1111/ter.70056openalex-snapshot
Paleoclimate Controls on the Formation of Quartz and Calcite Concretions in Shallow‐Marine Dolomitized Ypresian Deposits of the Arabian Platform
inferred← citeshttps://doi.org/10.1126/sciadv.aar5690openalex-snapshot
An early Cambrian greenhouse climate
inferred← citeshttps://doi.org/10.1126/sciadv.aax1874openalex-snapshot
Simulation of Eocene extreme warmth and high climate sensitivity through cloud feedbacks
inferred← citeshttps://doi.org/10.1126/sciadv.aax9361openalex-snapshot
Eggshell geochemistry reveals ancestral metabolic thermoregulation in Dinosauria
inferred← citeshttps://doi.org/10.1126/sciadv.aba1951openalex-snapshot
The lightness of water vapor helps to stabilize tropical climate
inferred← citeshttps://doi.org/10.1126/sciadv.abf5326openalex-snapshot
Sea level and deep-sea temperature reconstructions suggest quasi-stable states and critical transitions over the past 40 million years
inferred← citeshttps://doi.org/10.1126/sciadv.abg1025openalex-snapshot
Surface ocean warming and acidification driven by rapid carbon release precedes Paleocene-Eocene Thermal Maximum
inferred← citeshttps://doi.org/10.1126/sciadv.abm3875openalex-snapshot
Slow-growing reef corals as climate archives: A case study of the Middle Eocene Climatic Optimum 40 Ma ago
inferred← citeshttps://doi.org/10.1126/sciadv.abq0110openalex-snapshot
North Atlantic surface ocean warming and salinization in response to middle Eocene greenhouse warming
inferred← citeshttps://doi.org/10.1126/sciadv.adm9798openalex-snapshot
Phanerozoic icehouse climates as the result of multiple solid-Earth cooling mechanisms
inferred← citeshttps://doi.org/10.1130/b36280.1openalex-snapshot
Deoxygenation and organic carbon sequestration in the Tethyan realm associated with the middle Eocene climatic optimum
inferred← citeshttps://doi.org/10.1130/b38743.1openalex-snapshot
Record of Cenozoic climatic events from a paleolake in eastern China: Astrochronology and isotopic stratigraphy perspectives
inferred← citeshttps://doi.org/10.1130/g49984.1openalex-snapshot
Apparent preservation of primary foraminiferal Mg/Ca ratios and Mg-banding in recrystallized foraminifera
inferred← citeshttps://doi.org/10.1130/g51330.1openalex-snapshot
Warming, acidification, and calcification feedback during the first hyperthermal of the Cenozoic—The Latest Danian Event
inferred← citeshttps://doi.org/10.1130/geol.s.19386218.v1openalex-snapshot
Supplemental Material: Apparent preservation of primary foraminiferal Mg/Ca ratios and Mg-banding in recrystallized foraminifera
inferred← citeshttps://doi.org/10.1144/jgs2021-006openalex-snapshot
The Eocene−Oligocene transition in Nanggulan, Java: lithostratigraphy, biostratigraphy and foraminiferal stable isotopes
inferred← citeshttps://doi.org/10.1144/jgs2021-102openalex-snapshot
Assessing Nummulites geochemistry as a proxy for early Eocene palaeotemperature evolution in the North Sea Basin
inferred← citeshttps://doi.org/10.1146/annurev-earth-032320-100333openalex-snapshot
Modeling Past Hothouse Climates as a Means for Assessing Earth System Models and Improving the Understanding of Warm Climates
inferred← citeshttps://doi.org/10.1146/annurev-earth-040523-114630openalex-snapshot
The Causes and Consequences of Ordovician Cooling
inferred← citeshttps://doi.org/10.1146/annurev-earth-082420-063026openalex-snapshot
Atmospheric CO 2 over the Past 66 Million Years from Marine Archives
inferred← citeshttps://doi.org/10.1162/artl_a_00470openalex-snapshot
Ecology, Spatial Structure, and Selection Pressure Induce Strong Signatures in Phylogenetic Structure
inferred← citeshttps://doi.org/10.1175/jcli-d-18-0551.1openalex-snapshot
The Strength of Low-Cloud Feedbacks and Tropical Climate: A CESM Sensitivity Study
inferred← citeshttps://doi.org/10.1175/jcli-d-21-0131.1openalex-snapshot
Reduced High-Latitude Land Seasonality in Climates with Very High Carbon Dioxide
inferred← citeshttps://doi.org/10.1177/05529360251408963openalex-snapshot
Additional Eocene echinoids from the Sylhet Limestone of Mikir Hills, Assam, Northeast India: Deeper insights into Neo-Tethys palaeobiogeography
inferred← citeshttps://doi.org/10.1201/9781003288602-5openalex-snapshot
Hotspots of Cenozoic Tropical Marine Biodiversity
inferred← citeshttps://doi.org/10.1371/journal.pbio.3001340openalex-snapshot
gen3sis: A general engine for eco-evolutionary simulations of the processes that shape Earth’s biodiversity
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/10.20341/gbcp.vol3openalex-snapshot
6th International Geologica Belgica Congress: 12-14 September 2018 – Leuven, Belgium
inferred← citeshttps://doi.org/10.20341/gbcp.vol4openalex-snapshot
7th International Geologica Belgica Meeting: 15-17 September 2021 – AfricaMuseum Tervuren (Belgium)
inferred← citeshttps://doi.org/10.2110/jsr.2020.056openalex-snapshot
Multi-episodic recrystallization and isotopic resetting of early-diagenetic dolomites in near-surface settings
inferred← citeshttps://doi.org/10.2110/jsr.2022.016openalex-snapshot
Environmental and microbial influence on chemistry and dolomite formation in an ancient lake, Green River Formation (Eocene), Uinta basin, Utah, U.S.A.
inferred← citeshttps://doi.org/10.2110/palo.2020.029openalex-snapshot
THE HIGH-MAGNESIUM CALCITE ORIGIN OF NUMMULITID FORAMINIFERA AND IMPLICATIONS FOR THE IDENTIFICATION OF CALCITE DIAGENESIS
inferred← citeshttps://doi.org/10.2113/gsjfr.51.1.4openalex-snapshot
Late Paleocene-Early Eocene Foraminiferal Assemblage and Carbon Isotope Excursion Indicating Hyperthermal Events in Paleotropical Succession of Northwestern India
inferred← citeshttps://doi.org/10.2113/gsjfr.52.1.40openalex-snapshot
Larger Benthic Foraminifera and Microfacies of Late Paleocene - Early Eocene Sections in Meghalaya, Northeast India
inferred← citeshttps://doi.org/10.21248/gups.84416openalex-snapshot
Long-term variability of ocean chemistry : implications for deep-time palaeothermometry and the carbon cycle
inferred← citeshttps://doi.org/10.22541/essoar.169091906.62444464/v1openalex-snapshot
Surface ocean cooling in the Eocene North Atlantic coincides with declining atmospheric CO 2
inferred← citeshttps://doi.org/10.22541/essoar.170196814.47982364/v1openalex-snapshot
Impacts of tidally driven internal mixing in the Early Eocene Ocean
inferred← citeshttps://doi.org/10.31223/osf.io/5tk8gopenalex-snapshot
Ancient siderites reveal hot and humid super-greenhouse climate
inferred← citeshttps://doi.org/10.31223/osf.io/8527zopenalex-snapshot
Global mean surface temperature and climate sensitivity of the EECO, PETM and latest Paleocene
inferred← citeshttps://doi.org/10.31223/osf.io/zaj4gopenalex-snapshot
Ancient siderites reveal hot and humid super-greenhouse climate
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/10.32493/eaj.v6i3.y2023.p209-221openalex-snapshot
The Effect of Financial Performance as Moderating on Good Corporate Governance, Media Exposure and Disclosure of Sustainability Reports
inferred← citeshttps://doi.org/10.3390/geosciences11100419openalex-snapshot
Advances and Challenges in Palaeoenvironmental Studies Based on Oxygen Isotope Composition of Skeletal Carbonates and Phosphates
inferred← citeshttps://doi.org/10.3390/min12121611openalex-snapshot
Non-Linear Clumped Isotopes from DIC Endmember Mixing and Kinetic Isotope Fractionation in High pH Anthropogenic Tufa
inferred← citeshttps://doi.org/10.3390/plants13071008openalex-snapshot
Origin and Early Evolution of Hydrocharitaceae and the Ancestral Role of Stratiotes
inferred← citeshttps://doi.org/10.35414/akufemubid.1105170openalex-snapshot
Clumped Isotope Signatures of Dolomites as Reservoir Rocks, Southeast Anatolia
inferred← citeshttps://doi.org/10.3755/jcrs.26.59openalex-snapshot
Public symposium “Biogenic Reefs: Past and Future”
inferred← citeshttps://doi.org/10.5070/p939054415openalex-snapshot
The earliest Ancistrolepis (Gastropoda: Buccinidae) and its geologic implications
inferred← citeshttps://doi.org/10.5194/cp-14-1391-2018openalex-snapshot
Temperature seasonality in the North American continental interior during the Early Eocene Climatic Optimum
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