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Tectonic degassing drove global temperature trends since 20 Ma
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What this work says
Outgoing claims: the papers this work cites, builds on, or argues with.
inferredcites →https://doi.org/10.1002/2014gb004986openalex-snapshot
The effects of secular calcium and magnesium concentration changes on the thermodynamics of seawater acid/base chemistry: Implications for Eocene and Cretaceous ocean carbon chemistry and buffering
inferredcites →https://doi.org/10.1002/2014pa002752openalex-snapshot
Growth of the Maritime Continent and its possible contribution to recurring Ice Ages
inferredcites →https://doi.org/10.1002/2017pa003201openalex-snapshot
BAYSPLINE: A New Calibration for the Alkenone Paleothermometer
inferredcites →https://doi.org/10.1007/978-1-4615-5935-1_18openalex-snapshot
Global Chemical Erosion during the Cenozoic: Weatherability Balances the Budgets
inferredcites →https://doi.org/10.1016/0016-7037(94)90016-7openalex-snapshot
Chemical weathering rate laws and global geochemical cycles
inferredcites →https://doi.org/10.1016/0016-7037(95)00078-eopenalex-snapshot
Effects of climate on chemical_ weathering in watersheds
inferredcites →https://doi.org/10.1016/b978-0-444-59425-9.00029-9openalex-snapshot
The Neogene Period
inferredcites →https://doi.org/10.1016/j.csr.2007.10.014openalex-snapshot
A comparative overview of weathering intensity and HCO3− flux in the world's major rivers with emphasis on the Changjiang, Huanghe, Zhujiang (Pearl) and Mississippi Rivers
inferredcites →https://doi.org/10.1016/j.epsl.2005.03.020openalex-snapshot
Tectonic and climatic controls on silicate weathering
inferredcites →https://doi.org/10.1016/j.epsl.2007.07.026openalex-snapshot
Orbitally-paced climate evolution during the middle Miocene “Monterey” carbon-isotope excursion
inferredcites →https://doi.org/10.1016/j.epsl.2007.10.046openalex-snapshot
Himalayan metamorphic CO2 fluxes: Quantitative constraints from hydrothermal springs
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.2017.07.038openalex-snapshot
Late Miocene climate and time scale reconciliation: Accurate orbital calibration from a deep-sea perspective
inferredcites →https://doi.org/10.1016/j.epsl.2018.06.017openalex-snapshot
Constraining the evolution of Neogene ocean carbonate chemistry using the boron isotope pH proxy
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.2012.10.014openalex-snapshot
Evolution of carbon cycle over the past 100 million years
inferredcites →https://doi.org/10.1016/j.quascirev.2019.01.012openalex-snapshot
Upregulation of phytoplankton carbon concentrating mechanisms during low CO2 glacial periods and implications for the phytoplankton pCO2 proxy
inferredcites →https://doi.org/10.1016/s0012-821x(01)00317-xopenalex-snapshot
Erosion of Deccan Traps determined by river geochemistry: impact on the global climate and the 87Sr/86Sr ratio of seawater
inferredcites →https://doi.org/10.1016/s0016-7037(98)00097-0openalex-snapshot
Calibration of the alkenone paleotemperature index U37K′ based on core-tops from the eastern South Atlantic and the global ocean (60°N-60°S)
inferredcites →https://doi.org/10.1016/s0016-7037(99)00251-3openalex-snapshot
Direct measurement of the combined effects of lichen, rainfall, and temperature onsilicate weathering
inferredcites →https://doi.org/10.1029/1999rg000066openalex-snapshot
What caused the glacial/interglacial atmospheric p CO 2 cycles?
inferredcites →https://doi.org/10.1029/2005gc001148openalex-snapshot
Trends and rhythms in global seafloor generation rate
inferredcites →https://doi.org/10.1029/2018pa003496openalex-snapshot
100‐kyr Paced Climate Change in the Pliocene Warm Period, Southwest Pacific
inferredcites →https://doi.org/10.1029/2018tc005462openalex-snapshot
A Global Plate Model Including Lithospheric Deformation Along Major Rifts and Orogens Since the Triassic
inferredcites →https://doi.org/10.1029/2019gl083574openalex-snapshot
Climate Sensitivity on Geological Timescales Controlled by Nonlinear Feedbacks and Ocean Circulation
inferredcites →https://doi.org/10.1029/2019pa003638openalex-snapshot
Midlatitude Temperature Variations in the Oligocene to Early Miocene
inferredcites →https://doi.org/10.1029/2019pa003720openalex-snapshot
Plio‐Pleistocene Hemispheric (A)Symmetries in the Northern and Southern Hemisphere Midlatitudes
inferredcites →https://doi.org/10.1029/2019rg000678openalex-snapshot
An Assessment of Earth's Climate Sensitivity Using Multiple Lines of Evidence
inferredcites →https://doi.org/10.1029/2020pa003858openalex-snapshot
Comparison of Late Neogene Uk′37 and TEX86 Paleotemperature Records From the Eastern Equatorial Pacific at Orbital Resolution
inferredcites →https://doi.org/10.1029/2020pa003920openalex-snapshot
Initiation of the Western Pacific Warm Pool at the Middle Miocene Climate Transition?
inferredcites →https://doi.org/10.1029/2020pa003925openalex-snapshot
Decreasing Atmospheric CO 2 During the Late Miocene Cooling
inferredcites →https://doi.org/10.1029/2020pa003927openalex-snapshot
Warm Middle Miocene Indian Ocean Bottom Water Temperatures: Comparison of Clumped Isotope and Mg/Ca‐Based Estimates
inferredcites →https://doi.org/10.1029/2020pa003935openalex-snapshot
Bihemispheric Warming in the Miocene Climatic Optimum as Seen From the Danish North Sea
inferredcites →https://doi.org/10.1029/2020pa004054openalex-snapshot
Simulating Miocene Warmth: Insights From an Opportunistic Multi‐Model Ensemble (MioMIP1)
inferredcites →https://doi.org/10.1029/2022gl097937openalex-snapshot
Evidence for a Global Slowdown in Seafloor Spreading Since 15 Ma
inferredcites →https://doi.org/10.1029/91jb01898openalex-snapshot
The effect of silicate weathering on global temperature and atmospheric CO2
inferredcites →https://doi.org/10.1029/92jb01202openalex-snapshot
A new geomagnetic polarity time scale for the Late Cretaceous and Cenozoic
inferredcites →https://doi.org/10.1029/92jb01749openalex-snapshot
Oceanic crustal thickness from seismic measurements and rare earth element inversions
inferredcites →https://doi.org/10.1029/95pa02022openalex-snapshot
Middle Miocene deepwater paleoceanography in the southwest Pacific: Relations with East Antarctic Ice Sheet development
inferredcites →https://doi.org/10.1029/jc086ic10p09776openalex-snapshot
A negative feedback mechanism for the long‐term stabilization of Earth's surface temperature
inferredcites →https://doi.org/10.1038/359117a0openalex-snapshot
Tectonic forcing of late Cenozoic climate
inferredcites →https://doi.org/10.1038/nature01073openalex-snapshot
Vapour undersaturation in primitive mid-ocean-ridge basalt and the volatile content of Earth's upper mantle
inferredcites →https://doi.org/10.1038/nature07337openalex-snapshot
Thresholds for Cenozoic bipolar glaciation
inferredcites →https://doi.org/10.1038/ncomms15423openalex-snapshot
Constraining climate sensitivity and continental versus seafloor weathering using an inverse geological carbon cycle model
inferredcites →https://doi.org/10.1038/ngeo2813openalex-snapshot
Late Miocene global cooling and the rise of modern ecosystems
inferredcites →https://doi.org/10.1038/ngeo706openalex-snapshot
Earth system sensitivity inferred from Pliocene modelling and data
inferredcites →https://doi.org/10.1038/s41467-017-02609-7openalex-snapshot
Southern Ocean warming and Wilkes Land ice sheet retreat during the mid-Miocene
inferredcites →https://doi.org/10.1038/s41561-017-0003-6openalex-snapshot
Potential links between continental rifting, CO2 degassing and climate change through time
inferredcites →https://doi.org/10.1038/s41561-018-0182-9openalex-snapshot
Transient temperature asymmetry between hemispheres in the Palaeogene Atlantic Ocean
inferredcites →https://doi.org/10.1038/s41586-019-1332-yopenalex-snapshot
Neogene cooling driven by land surface reactivity rather than increased weathering fluxes
inferredcites →https://doi.org/10.1073/pnas.1507889112openalex-snapshot
Reevaluating carbon fluxes in subduction zones, what goes down, mostly comes up
inferredcites →https://doi.org/10.1073/pnas.1516030113openalex-snapshot
Antarctic ice sheet sensitivity to atmospheric CO 2 variations in the early to mid-Miocene
inferredcites →https://doi.org/10.1073/pnas.1615440114openalex-snapshot
Evolution of the early Antarctic ice ages
inferredcites →https://doi.org/10.1073/pnas.2011033117openalex-snapshot
Emergence of the Southeast Asian islands as a driver for Neogene cooling
inferredcites →https://doi.org/10.1093/gji/ggw277openalex-snapshot
Preserved history of global mean spreading rate: 83 Ma to present
inferredcites →https://doi.org/10.1093/gji/ggw305openalex-snapshot
High-resolution reconstructions of Pacific–North America plate motion: 20 Ma to present
inferredcites →https://doi.org/10.1093/gji/ggz508openalex-snapshot
High-resolution reconstructions and GPS estimates of India–Eurasia and India–Somalia plate motions: 20 Ma to the present
inferredcites →https://doi.org/10.1111/j.1365-246x.2008.03761.xopenalex-snapshot
A high-resolution model for Eurasia-North America plate kinematics since 20 Ma
inferredcites →https://doi.org/10.1126/sciadv.aat8223openalex-snapshot
Rapid eruption of the Columbia River flood basalt and correlation with the mid-Miocene climate optimum
inferredcites →https://doi.org/10.1126/science.1059412openalex-snapshot
Trends, Rhythms, and Aberrations in Global Climate 65 Ma to Present
inferredcites →https://doi.org/10.1126/science.1100061openalex-snapshot
Middle Miocene Southern Ocean Cooling and Antarctic Cryosphere Expansion
inferredcites →https://doi.org/10.1126/science.290.5500.2288openalex-snapshot
Upwelling Intensification As Part of the Pliocene-Pleistocene Climate Transition
inferredcites →https://doi.org/10.1126/science.aad5787openalex-snapshot
Continental arc volcanism as the principal driver of icehouse-greenhouse variability
inferredcites →https://doi.org/10.1126/science.aav5300openalex-snapshot
Arc-continent collisions in the tropics set Earth’s climate state
inferredcites →https://doi.org/10.1130/0016-7606(2002)114<0927:ropcad>2.0.co;2openalex-snapshot
Rate of plate creation and destruction: 180 Ma to present
inferredcites →https://doi.org/10.1130/0091-7613(1993)021<1059:tdoswi>2.3.co;2openalex-snapshot
Temperature dependence of silicate weathering in nature: How strong a negative feedback on long-term accumulation of atmospheric CO2 and global greenhouse warming?
inferredcites →https://doi.org/10.1130/g22759a.1openalex-snapshot
Faster seafloor spreading and lithosphere production during the mid-Cenozoic
inferredcites →https://doi.org/10.1130/g30139a.1openalex-snapshot
Palynomorphs from a sediment core reveal a sudden remarkably warm Antarctica during the middle Miocene
inferredcites →https://doi.org/10.1130/g31328.1openalex-snapshot
Flux rates for water and carbon during greenschist facies metamorphism
inferredcites →https://doi.org/10.1130/g36317.1openalex-snapshot
Global perturbation of the carbon cycle at the onset of the Miocene Climatic Optimum
inferredcites →https://doi.org/10.1130/g38663.1openalex-snapshot
Alternating Southern and Northern Hemisphere climate response to astronomical forcing during the past 35 m.y.
inferredcites →https://doi.org/10.1130/g39013.1openalex-snapshot
Monsoonal upwelling in the western Arabian Sea since the middle Miocene
inferredcites →https://doi.org/10.1130/g40228.1openalex-snapshot
North Atlantic temperature and pCO2 coupling in the early-middle Miocene
inferredcites →https://doi.org/10.1130/ges00822.1openalex-snapshot
Continental arc-island arc fluctuations, growth of crustal carbonates, and long-term climate change
inferredcites →https://doi.org/10.1130/l1027.1openalex-snapshot
Oceanic axial depth and age-depth distribution of oceanic lithosphere: Comparison of magnetic anomaly picks versus age-grid models
inferredcites →https://doi.org/10.1146/annurev-earth-082420-063026openalex-snapshot
Atmospheric CO 2 over the Past 66 Million Years from Marine Archives
inferredcites →https://doi.org/10.2475/08.2013.02openalex-snapshot
How to think about the evolution of the ratio of Mg to Ca in seawater
inferredcites →https://doi.org/10.2475/ajs.283.7.641openalex-snapshot
The carbonate-silicate geochemical cycle and its effect on atmospheric carbon dioxide over the past 100 million years
inferredcites →https://doi.org/10.2475/ajs.299.7-9.611openalex-snapshot
Global chemical erosion over the last 250 my; variations due to changes in paleogeography, paleoclimate, and paleogeology
inferredcites →https://doi.org/10.2475/ajs.301.2.182openalex-snapshot
GEOCARB III: A revised model of atmospheric CO2 over Phanerozoic time
inferredcites →https://doi.org/10.5194/cp-9-525-2013openalex-snapshot
Modulation of Late Cretaceous and Cenozoic climate by variable drawdown of atmospheric p CO 2 from weathering of basaltic provinces on continents drifting through the equatorial humid belt
inferredcites →https://doi.org/10.5194/gmd-5-149-2012openalex-snapshot
LOSCAR: Long-term Ocean-atmosphere-Sediment CArbon cycle Reservoir Model v2.0.4
What points at this work
Incoming claims: where this work appears in other papers’ reference lists and arguments.
inferred← citeshttps://doi.org/10.2139/ssrn.4857477openalex-extracted
The Flora, Fauna, and Paleoenvironment of the Late Middle Miocene Quebrada Honda, Bolivia (Eastern Cordillera, Central Andes)
inferred← citeshttps://doi.org/10.1002/9781394213764.ch21openalex-snapshot
Paleo sea ice reconstruction in the Southern Ocean: Ancient warm periods
inferred← citeshttps://doi.org/10.1002/spp2.1514openalex-snapshot
The last horned armadillos: phylogeny and decline of Peltephilidae (Xenarthra, Cingulata)
inferred← citeshttps://doi.org/10.1007/s11430-025-1919-6openalex-snapshot
Progress and prospects in paleoclimate modeling
inferred← citeshttps://doi.org/10.1007/s11430-026-2009-5openalex-snapshot
Differential responses of silicate, carbonate, and sulfide weathering to erosion drive CO2 release in the Lancang River, southeastern Tibetan Plateau
inferred← citeshttps://doi.org/10.1016/b978-0-323-99762-1.00060-7openalex-snapshot
Regulation of the carbon cycle on geological timescales
inferred← citeshttps://doi.org/10.1016/j.apm.2022.09.032openalex-snapshot
Biome stability and fragmentation under critical environmental temperature change
inferred← citeshttps://doi.org/10.1016/j.chemgeo.2023.121335openalex-snapshot
Biomarker evidence for late Miocene temperature and moisture from the Alagu planation surface, NE Tibetan Plateau
inferred← citeshttps://doi.org/10.1016/j.chemgeo.2024.122106openalex-snapshot
The impact of Himalayan-Tibetan erosion on silicate weathering and organic carbon burial
inferred← citeshttps://doi.org/10.1016/j.epsl.2023.118343openalex-snapshot
Timing and tempo of organic carbon burial in the Monterey Formation of the Santa Barbara Basin and relationships with Miocene climate
inferred← citeshttps://doi.org/10.1016/j.epsl.2025.119811openalex-snapshot
A model for Cenozoic seawater chemistry and carbon cycling
inferred← citeshttps://doi.org/10.1016/j.gca.2026.06.028openalex-snapshot
Lithologic controls on silicate weathering in a tropical arc-continent collision zone: multi-isotopic evidence
inferred← citeshttps://doi.org/10.1016/j.gloplacha.2023.104095openalex-snapshot
Evolution of silicate weathering in South China since 30 Ma: Controlling factors and global implications
inferred← citeshttps://doi.org/10.1016/j.gloplacha.2024.104431openalex-snapshot
Pliocene CO2 rise due to sea-level fall as a mechanism for the delayed ice age
inferred← citeshttps://doi.org/10.1016/j.gloplacha.2024.104691openalex-snapshot
Enhanced aridity in the interior of Asia after the Middle Miocene Climatic Optimum driven by global cooling
inferred← citeshttps://doi.org/10.1016/j.gloplacha.2025.104807openalex-snapshot
Evolution of silicate weathering in the Yangtze River Basin since 3.5 Ma as archived in the East China Seas: Controlling factors and global significance
inferred← citeshttps://doi.org/10.1016/j.gloplacha.2025.104808openalex-snapshot
Refining paleoelevation estimates of the European Alps by simulating Middle Miocene climate and δ 18 O responses to diachronous surface uplift scenarios
inferred← citeshttps://doi.org/10.1016/j.gloplacha.2025.104901openalex-snapshot
Control of temperature on the weathering of slow-eroding post-orogenic terrains
inferred← citeshttps://doi.org/10.1016/j.gloplacha.2025.105235openalex-snapshot
Miocene carbonate crash in the eastern Pacific: A catalyst for early rare earth element enrichment
inferred← citeshttps://doi.org/10.1016/j.gloplacha.2026.105530openalex-snapshot
Stepwise tropical island-arc weathering driven by uplift and climate over Southeast Asia since the Pliocene
inferred← citeshttps://doi.org/10.1016/j.gloplacha.2026.105548openalex-snapshot
Coupling of enhanced precipitation at the East Asian monsoon front and intensified aridification in the Asian interior since 2.7 Ma
inferred← citeshttps://doi.org/10.1016/j.jseaes.2023.105916openalex-snapshot
Redox evolution in the subtropical Northwest Pacific across the Middle Miocene Climate Transition
inferred← citeshttps://doi.org/10.1016/j.palaeo.2023.111516openalex-snapshot
Landform evolution in Asia during the Cenozoic revealed by formation of drainages of Wei River and Indus River
inferred← citeshttps://doi.org/10.1016/j.palaeo.2023.111541openalex-snapshot
Modeling the effects of global cooling and the Tethyan Seaway closure on North African and South Asian climates during the Middle Miocene Climate Transition
inferred← citeshttps://doi.org/10.1016/j.palaeo.2024.112156openalex-snapshot
Simulating surface warming in Earth's three polar regions during the Middle Miocene Climatic Optimum using isotopic and non-isotopic versions of the Community Earth System Model
inferred← citeshttps://doi.org/10.1016/j.palaeo.2024.112517openalex-snapshot
Large river expansion and global cooling controlled the Plio-Pleistocene weathering intensity records in East Asian margin
inferred← citeshttps://doi.org/10.1016/j.palaeo.2024.112518openalex-snapshot
The flora, fauna, and paleoenvironment of the late Middle Miocene Quebrada Honda Basin, Bolivia (Eastern Cordillera, Central Andes)
inferred← citeshttps://doi.org/10.1016/j.palaeo.2025.113248openalex-snapshot
Stable Isotope Ecology of the Early Miocene Rusinga Island Mammalian Communities from the Hiwegi and Kulu Formations (Nyanza Province, Western Kenya)
inferred← citeshttps://doi.org/10.1016/j.scib.2023.03.007openalex-snapshot
Dynamic link between Neo-Tethyan subduction and atmospheric CO2 changes: insights from seismic tomography reconstruction
inferred← citeshttps://doi.org/10.1016/j.scib.2023.12.052openalex-snapshot
Accelerated marine carbon cycling forced by tectonic degassing over the Miocene Climate Optimum
inferred← citeshttps://doi.org/10.1029/2022gb007541openalex-snapshot
Increased Biogenic Calcification and Burial Under Elevated p CO 2 During the Miocene: A Model‐Data Comparison
inferred← citeshttps://doi.org/10.1029/2022pa004438openalex-snapshot
The Impact of Different Atmospheric CO2 Concentrations on Large Scale Miocene Temperature Signatures
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/10.1029/2023pa004615openalex-snapshot
A Humid East Asia During the Early Pliocene Indicated by Calcite Nodules From the Chinese Loess Plateau
inferred← citeshttps://doi.org/10.1029/2023pa004726openalex-snapshot
A Model‐Data Comparison of the Hydrological Response to Miocene Warmth: Leveraging the MioMIP1 Opportunistic Multi‐Model Ensemble
inferred← citeshttps://doi.org/10.1029/2023pa004769openalex-snapshot
Reconstruction of Cenozoic δ 11 B sw Using a Gaussian Process
inferred← citeshttps://doi.org/10.1029/2024gc011713openalex-snapshot
Solid Earth Carbon Degassing and Sequestration Since 1 Billion Years Ago
inferred← citeshttps://doi.org/10.1029/2024gc011773openalex-snapshot
Consequences of a Global Slowdown in Seafloor Spreading for Sea Level and Mantle Heat Loss
inferred← citeshttps://doi.org/10.1029/2024gl114500openalex-snapshot
Tectonics Modulated Long‐Term Weathering Inputs From the East Asian Continent and Tropical Island Arc to the South China Sea Since the Late Oligocene
inferred← citeshttps://doi.org/10.1029/2024jb028802openalex-snapshot
Organic and Inorganic Carbon Sinks Reduce Long‐Term Deep Carbon Emissions in the Continental Collision Margin of the Southern Tibetan Plateau: Implications for Cenozoic Climate Cooling
inferred← citeshttps://doi.org/10.1029/2024pa004872openalex-snapshot
Reconciling the Apparent Discrepancy Between Cenozoic Deep‐Sea Temperatures From Proxies and From Benthic Oxygen Isotope Deconvolution
inferred← citeshttps://doi.org/10.1029/2024pa004894openalex-snapshot
Two‐Stage Climate and Vegetation Change at the East Asian Monsoonal Margin Across the Miocene Climatic Optimum
inferred← citeshttps://doi.org/10.1029/2024pa004936openalex-snapshot
Cause‐and‐Effect Relationships Between Sea Surface Temperature Changes in Different Regions During the Past 4.5 Million Years
inferred← citeshttps://doi.org/10.1029/2025jb033130openalex-snapshot
A Late Cretaceous‐Eocene Geomagnetic Polarity Time Scale (MM26) That Combines Marine Magnetic Anomaly Records, Radioisotopic Dates, and Astrochronology
inferred← citeshttps://doi.org/10.1029/2025pa005100openalex-snapshot
Approaching the Miocene Climatic Optimum in Patagonia (Southern Argentina): Temperature Seasonality and a Potential Role for the Opening Drake Passage
inferred← citeshttps://doi.org/10.1029/2025pa005120openalex-snapshot
Enhanced Deep‐Water Oxygenation in the South China Sea Driven by Middle Miocene Climate Cooling
inferred← citeshttps://doi.org/10.1029/2025pa005243openalex-snapshot
Early‐Middle Miocene Low‐Latitude Pelagic Sedimentation: A Response to Climatic Evolution
inferred← citeshttps://doi.org/10.1029/2025pa005380openalex-snapshot
Neogene Stable Carbon Isotopic Evolution of the Atmosphere and Low‐Latitude Surface Ocean
inferred← citeshttps://doi.org/10.1029/2025pa005388openalex-snapshot
Evidence for Limited Atmospheric CO 2 Rise at the Miocene Climatic Optimum
inferred← citeshttps://doi.org/10.1038/s41467-023-43106-4openalex-snapshot
Reconciling Southern Ocean fronts equatorward migration with minor Antarctic ice volume change during Miocene cooling
inferred← citeshttps://doi.org/10.1038/s41467-024-52516-xopenalex-snapshot
Re-organization of Pacific overturning circulation across the Miocene Climate Optimum
inferred← citeshttps://doi.org/10.1038/s41467-026-74516-9openalex-snapshot
Algal δ13C reveals climate changes during the Cambrian Explosion
inferred← citeshttps://doi.org/10.1038/s41561-024-01496-0openalex-snapshot
Solid Earth forcing of Mesozoic oceanic anoxic events
inferred← citeshttps://doi.org/10.1038/s41561-024-01610-2openalex-snapshot
Rapid rise in atmospheric CO2 marked the end of the Late Palaeozoic Ice Age
inferred← citeshttps://doi.org/10.1038/s41586-023-06777-zopenalex-snapshot
Landscape dynamics and the Phanerozoic diversification of the biosphere
inferred← citeshttps://doi.org/10.1038/s43247-023-00684-xopenalex-snapshot
Enhanced magmatism played a dominant role in triggering the Miocene Climatic Optimum
inferred← citeshttps://doi.org/10.1038/s43247-023-00721-9openalex-snapshot
Stepwise increased spatial provenance contrast on the Chinese Loess Plateau over late Miocene-Pleistocene
inferred← citeshttps://doi.org/10.1038/s43247-025-02695-2openalex-snapshot
The editors’ highlights for the five-year anniversary
inferred← citeshttps://doi.org/10.1038/s43247-026-03457-4openalex-snapshot
Andean volcanism, ocean fertilization, marine ecosystem turnover, and global cooling in the Late Miocene
inferred← citeshttps://doi.org/10.1051/bioconf/20235601002openalex-snapshot
Role of foliar biostimulants (of plant origin) on grapevine adaptation to climate change
inferred← citeshttps://doi.org/10.1073/pnas.2306492120openalex-snapshot
The rise of New Guinea and the fall of Neogene global temperatures
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/10.1111/nph.19067openalex-snapshot
Do Southeast Asia's paleo‐Antarctic trees cool the planet?
inferred← citeshttps://doi.org/10.1126/sciadv.adf3141openalex-snapshot
Accelerated mafic weathering in Southeast Asia linked to late Neogene cooling
inferred← citeshttps://doi.org/10.1126/sciadv.adm8270openalex-snapshot
East Asian winter monsoon intensification over the Northwest Pacific Ocean driven by late Miocene atmospheric CO 2 decline
inferred← citeshttps://doi.org/10.1126/sciadv.ads4268openalex-snapshot
Vegetation feedbacks accelerated the late Miocene climate transition
inferred← citeshttps://doi.org/10.1126/sciadv.adu5030openalex-snapshot
Terrestrial temperature history reveals Late Miocene rapid uplift of the northern Tibetan Plateau
inferred← citeshttps://doi.org/10.1126/sciadv.adx6682openalex-snapshot
Eccentricity rhythms in the Oligocene-Miocene carbon cycle regulated by weathering and carbonate burial
inferred← citeshttps://doi.org/10.1126/sciadv.adz2555openalex-snapshot
Ocean circulation changes rather than global warming drove temperature trends across the Miocene Climatic Optimum
inferred← citeshttps://doi.org/10.1126/science.abq6542openalex-snapshot
Can the Miocene climate inform the future?
inferred← citeshttps://doi.org/10.1126/science.add2922openalex-snapshot
How temperature-dependent silicate weathering acts as Earth’s geological thermostat
inferred← citeshttps://doi.org/10.1126/science.adg1366openalex-snapshot
Oxygen isotope ensemble reveals Earth’s seawater, temperature, and carbon cycle history
inferred← citeshttps://doi.org/10.1126/science.adi1908openalex-snapshot
Global and regional temperature change over the past 4.5 million years
inferred← citeshttps://doi.org/10.1130/b38014.1openalex-snapshot
Fish tooth U-Pb dating reveals the late Miocene REY enrichment of the Clarion-Clipperton Fracture Zone
inferred← citeshttps://doi.org/10.1130/g52255.1openalex-snapshot
High-precision U-Pb geochronology for the Miocene Climate Optimum and a novel approach for calibrating age models in deep-sea sediment cores
inferred← citeshttps://doi.org/10.1130/g52432.1openalex-snapshot
North Pacific warmth synchronous with the Miocene Climatic Optimum
inferred← citeshttps://doi.org/10.1175/jcli-d-25-0038.1openalex-snapshot
Effects of Tide-Induced Mixing on the Equator-to-Pole Surface Temperature Gradient during the Middle Miocene Climate Optimum
inferred← citeshttps://doi.org/10.1360/tb-2023-0187openalex-snapshot
Links between deep Earth processes and hyperthermal and extreme cooling events
inferred← citeshttps://doi.org/10.21203/rs.3.rs-3184669/v1openalex-snapshot
Reconciling equatorward migration of Southern Ocean fronts with minor ice volume change during Miocene cooling
inferred← citeshttps://doi.org/10.2138/gselements.22.1.18openalex-snapshot
Igneous and Metamorphic CO2 Sources: How Large and How Variable?
inferred← citeshttps://doi.org/10.2138/gselements.22.1.24openalex-snapshot
Continental Weathering as Climate Stabilizer
inferred← citeshttps://doi.org/10.2139/ssrn.5122980openalex-snapshot
Stable Isotope Ecology of the Early Miocene Rusinga Island Mammalian Communities from the Kulu and Hiwegi Formations
inferred← citeshttps://doi.org/10.3390/geosciences14090238openalex-snapshot
Cenozoic Carbon Dioxide: The 66 Ma Solution
inferred← citeshttps://doi.org/10.3847/psj/ad7856openalex-snapshot
Substantial Extension of the Lifetime of the Terrestrial Biosphere
inferred← citeshttps://doi.org/10.5194/cp-19-1461-2023openalex-snapshot
The effect of the Pliocene temperature pattern on silicate weathering and Pliocene–Pleistocene cooling
inferred← citeshttps://doi.org/10.5194/cp-21-2501-2025openalex-snapshot
Insights into the Middle–Late Miocene palaeoceanographic development of Cyprus (eastern Mediterranean) from a new δ 18 O and δ 13 C stable isotope composite record
inferred← citeshttps://doi.org/10.5194/cp-21-405-2025openalex-snapshot
Impact of the Late Miocene Cooling on the loss of coral reefs in the Central Indo-Pacific
inferred← citeshttps://doi.org/10.5194/egusphere-2023-16-rc1openalex-snapshot
Comment on egusphere-2023-16
inferred← citeshttps://doi.org/10.5194/egusphere-2023-16-rc2openalex-snapshot
Comment on egusphere-2023-16
inferred← citeshttps://doi.org/10.5194/egusphere-2023-16-rc3openalex-snapshot
Comment on egusphere-2023-16
inferred← citeshttps://doi.org/10.59717/j.xinn-geo.2023.100020openalex-snapshot
Formation and evolution of the Asian landscape during the Cenozoic
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