Paleoceanography and Paleoclimatology

Papers
(The median citation count of Paleoceanography and Paleoclimatology is 2. The table below lists those papers that are above that threshold based on CrossRef citation counts [max. 250 papers]. The publications cover those that have been published in the past four years, i.e., from 2022-08-01 to 2026-08-01.)
ArticleCitations
Issue Information48
Enhanced North Pacific Subpolar Gyre Circulation Led to Hypoxia Events During Last Deglacial Warm Periods45
The Hydroclimate and Environmental Response to Middle Miocene Warming in the Southwestern USA: Stable Isotope Evidence40
Isotopic Expression of Millennial‐Scale Climate Events in the Central United States During the Last Glacial Period32
The Late Miocene Ocean Carbon Cycle Changes: New Evidence From the South Atlantic IODP Expeditions29
Indonesian Seas Circulation Linked to Mean Climate State Reversals28
Issue Information27
Westerlies Influenced Monsoonal Climate: Reconstructions of Summer/Winter Temperature and Precipitation Based on Japan Sea Shelf Late Holocene Sediments Geochemistry27
Assessing Seasonal and Inter‐Annual Marine Sediment Climate Proxy Data26
Cause‐and‐Effect Relationships Between Sea Surface Temperature Changes in Different Regions During the Past 4.5 Million Years26
Shell Reworking Impacts on Climate Variability Reconstructions Using Individual Foraminiferal Analyses22
Orbital Forcing and Evolution of the Southern African Monsoon From Late Miocene to Early Pliocene21
Tropical Warming and Intensification of the West African Monsoon During the Miocene Climatic Optimum21
Climate, Fjord Morphology, and Oceanographic Controls on Glacier Retreat and Sedimentation in Bellsund, Southwestern Svalbard21
Sea‐Level and Frontal Controls on Diatom Deposition During the Mid‐Pleistocene Transition, Southern Cape Basin20
Archaeal Tetraether Lipids as Tracers for Past Marine Environmental Change20
Intense Changes in the Main Source of Organic Carbon to the Gulf Coastal Plain Following the Cretaceous‐Paleogene Boundary20
High‐Resolution, Multiproxy Speleothem Record of the 8.2 ka Event From Mainland Southeast Asia19
Issue Information19
Atmospheric Transmission of Temperature and Precipitation Change in Florida During North Atlantic Heinrich Events19
Central European Hydroclimate Since the Younger Dryas Inferred From Vegetation‐Corrected Sedimentary Plant Wax δ 2 H Values18
Tropical Leaf Wax n‐Alkane and n‐Alkanoic Acid Reflect δD of Precipitation During Early Stages of Leaf Growth: Insights From an Isotope Labeling Experiment18
Stable Middle Miocene Seawater Isotopes in the Eastern North Atlantic Ocean17
Enhanced Tropical Pacific Foraminiferal Carbonate Pump During the Last Deglaciation Linked to Ocean Warming17
Reconstructing Environmental and Microbial Ecosystem Changes Across the Permian–Triassic Mass Extinction at Lusitaniadalen, Svalbard16
Amplified North Atlantic Little Ice Age Cooling Inferred From Inversion of Benthic Foraminiferal Records16
Paleoceanographic Implications of Diatom Seasonal Laminations in the Upper Miocene Pisco Formation (Ica Desert, Peru) and Their Clues on the Development of the Pisco Fossil‐Lagerstätte16
The Toba Eruption 74,000 Years ago Strengthened the Indian Winter Monsoon‐Evidence From Coccolithophores15
15
Regime Shifts in Holocene Paleohydrology as Recorded by Asian Speleothems15
A Proxy System Modeling Approach to Combining Tree‐Ring and Sediment‐Based Paleotempestological Records15
Decomposition of Deglacial Pacific Radiocarbon Age Controls Using an Isotope‐Enabled Ocean Model15
Pyleoclim: Paleoclimate Timeseries Analysis and Visualization With Python15
Issue Information15
Ecological and Environmental Stability in Offshore Southern California Marine Basins Through the Holocene14
Unraveling the Deep‐Sea Sedimentary Record of Ice Sheet History14
Pliocene Weakening of Gradients in Temperature but Not in Productivity in the Eastern Equatorial Pacific14
Precession Controls on Climate and Water Isotope Signals in Northern Africa14
Clumped Isotope Temperatures of Coccolithophores From Global Sediment Traps14
Revisiting the Early Late Cretaceous Equable Climate Problem Through a Model‐Data Perspective14
A Comprehensive Evaluation of Machine Learning on Coral Trace Element Paleothermometers for Sea Surface Temperature Reconstruction14
The Late Miocene‐Early Pliocene Biogenic Bloom: An Integrated Study in the Tasman Sea14
Evaluating Glacial CO 2 System Reconstructions From Benthic Proxies in Earth System Simulations14
The Paleocene‐Eocene Thermal Maximum Recognized in Distal Alluvial Fan Strata of the Sevier Fold‐And‐Thrust Belt (Southwestern Wyoming, USA)13
Correction of the IRD Influence for Paleo‐Current Flow Speed Reconstructions in Hemipelagic Sediments13
Early Pleistocene Orbital‐Scale Variability in Australian Northwest Shelf Sediments13
Global Speleothem Analysis Reveals State‐Dependent Hydrological Response to Orbital Forcing13
Tropical South American Climate Variability During Late MIS 3: Low‐Latitude Controls and High‐Latitude Influences in the Community Earth System Model Version 2 (CESM2)13
Coral Sr‐U Thermometry Tracks Ocean Temperature and Reconciles Sr/Ca Discrepancies Caused by Rayleigh Fractionation13
Issue Information13
A Warming Southern Gulf of Mexico: Reconstruction of Anthropogenic Environmental Changes From a Siderastrea siderea Coral on the Northern Coast of Cuba13
Oceanography of the Eastern Equatorial Pacific Ocean Across the Oligocene‐Miocene Transition12
Eocene‐Oligocene Intensification of the Deep Western Boundary Current in the North Atlantic Ocean12
Dissolution Effects on Clumped Isotope Signatures in Planktic Foraminifera12
Issue Information12
The Franks Model CO 2 Proxy: Do Assimilation Rate Values or Isotopic Corrections Optimize CO 2 Rec12
12
Evolution of Ocean Circulation in the North Atlantic Ocean During the Miocene: Impact of the Greenland Ice Sheet and the Eastern Tethys Seaway12
Issue Information11
Tropical Atlantic Temperature and Hydrologic Change During the Paleocene‐Eocene Thermal Maximum11
11
Transient Response of Southern Ocean Ecosystems During Heinrich Stadials11
Climate Variability in the Gulf of California Over the Last 1,300 years11
Expanded Composite Coral Indices of South Pacific Convergence Zone Oceanographic Variability Since 1848 CE11
Biomarker Preservation and Paleoclimate From Late Neogene Marine Sediments From DSDP Site 467, Offshore Los Angeles11
Evidence for Long‐Term Coupling of Deep Ocean Carbon Storage and Global Climate Over the Past 4.5 Million Years11
20th Century Warming in the Western Florida Keys Was Dominated by Increasing Winter Temperatures10
Morphological Insights From Benthic Foraminifera for Environmental Conditions in the Baltic Sea During the Last Interglacial10
Retraction: Earth System Model Analysis of How Astronomical Forcing Is Imprinted Onto the Marine Geological Record: The Role of the Inorganic (Carbonate) Carbon Cycle and Feedbacks10
Multiproxy Reconstruction of Pliocene North Atlantic Sea Surface Temperatures and Implications for Rainfall in North Africa10
A Comparison of New and Established Foraminiferal Dissolution Proxies in Tropical Indian Ocean Deep‐Sea Sediments10
High‐Resolution Annual Cycles of the Sr/Ca Ratio in Florida Bay Seawater Sampled With Osmotic Pumps10
The Impact of Different Atmospheric CO2 Concentrations on Large Scale Miocene Temperature Signatures9
9
Weakening of the Summer Monsoon Over the Past 150 Years Shown by a Tree‐Ring Record From Shandong, Eastern China, and the Potential Role of North Atlantic Climate9
Unsteady Gypsum Cycling as a Driver of Cryptic Perturbations in the Ancient Carbon Cycle9
Milankovitch Record From Middle Jurassic Platform Supports Moderate Coolhouse Glaciation9
Cryospheric and Oceanographic Evolution in the Arctic Makarov Basin Since the Early Pleistocene Revealed by Bulk Mineral Assemblages9
9
Floods Enhanced the Terrestrial and Marine Organic Carbon Burial in the East China Sea9
Colpophyllia natans From Tobago, a Novel Paleoclimate Archive for Reconstructing Sea Surface Temperature in the Tropical Atlantic9
Miocene Ocean Gyre Circulation and Gateway Transports—MioMIP1 Ocean Intercomparison9
Evolution of West‐East Contrast in the Subarctic Pacific Gyre During the Plio‐Pleistocene Based on Palynological Evidence at ODP Sites 882 and 8878
Toward New and Independent Constraints on Global Mean Sea‐Level Highstands During the Last Glaciation (Marine Isotope Stage 3, 5a, and 5c)8
Spatial and Temporal Bayesian Hierarchical Model Over Large Domains With Application to Holocene Sea Surface Temperature Reconstruction in the Equatorial Pacific8
Bayesian Calibration for the Arctic Sea Ice Biomarker IP258
Ocean Oxygenation Changes in the Arabian Sea Oxygen Minimum Zone During the Penultimate Glacial Cycle8
Spatial and Temporal Patterns in Petrogenic Organic Carbon Mobilization During the Paleocene‐Eocene Thermal Maximum8
Palynofloral Change Through the Paleocene‐Eocene Thermal Maximum in the Bighorn Basin, Wyoming8
Calcareous Nannofossils, Carbonate Compensation Depth Changes, and Geochemical Proxies Across the Eocene‐Oligocene Transition: Insights From IODP Site U14388
Isotopic Analyses of Marl Sediments From an Antarctic Lake Reveal Large‐Scale Hydrologic Changes Over the Last Glacial‐Interglacial Cycle8
Model Sensitivity to Insolation Forcing and Uncertainties in Holocene Temperature Simulations8
Issue Information8
Impacts of the Early Eocene Climatic Optimum (EECO, ∼53‐49 Ma) on Planktic Foraminiferal Resilience8
Retraction Statement: Plio‐Pleistocene Indonesian Throughflow Variability Drove Eastern Indian Ocean Sea Surface Temperatures8
Warming‐Induced Intensification of the Angolan Oxygen Minimum Zone Over the Past 43,000 Years8
7
Regional Variations of the Azores High Across Glacial‐Interglacial Timescales7
Issue Information7
Westerlies and Monsoon Climate Systems Shape Holocene Moisture Patterns in the Southern Tibetan Plateau: Evidence From Aeolian Sedimentary Records7
Issue Information7
Recording Kimmeridgian Palaeoclimate Changes Using Biofacial and Isotopic Analyses of Benthic Foraminifers From Normandy (Northwest France)7
7
Thank You to Our 2022 Peer Reviewers7
Authigenic and Detrital Carbonate Nd Isotope Records Reflect Pulses of Detrital Material Input to the Labrador Sea During the Heinrich Stadials7
Terrestrial Ecosystem Response to Changing Temperature and Seasonality in the Paleocene‐Eocene Thermal Maximum: Shallow Marine Records From the Salisbury Embayment, USA7
Low Chemical Weathering Intensity, Enhanced Erosion, and Euxinic Conditions Along the Norwegian Margin During the Paleocene‐Eocene Thermal Maximum7
A Systematic Role for Extreme Ocean‐Atmosphere Oscillations in the Development of Glacial Conditions Since the Mid Pleistocene Transition7
Shelf Ecosystems Along the U.S. Atlantic Coastal Plain Prior to and During the Paleocene‐Eocene Thermal Maximum: Insights Into the Stratigraphic Architecture7
Magnetic Response to the Source‐To‐Sink Environmental Changes in the Bay of Bengal Since ∼60 ka7
High‐Resolution Lake Deposits Record Temperature Variability During the Middle Eocene Greenhouse in Central Europe7
Early to Middle Miocene Astronomically Paced Climate Dynamics in the Eastern Equatorial Atlantic6
Bayesian Errors‐in‐Variables Estimation of Specific Climate Sensitivity6
Last Glacial Maximum Reconstructions of Rwenzori Mountain Glaciers6
Shifts in Fossil Benthic Foraminiferal Community Trajectories During the Last Deglaciation Along the European Margin6
Exploring Spatiotemporal Paleoenvironmental and Paleoceanographic Changes on the Continental Shelf Using Authigenic Greigite: A Case Study From the East China Sea6
Cenozoic Proxy Constraints on Earth System Sensitivity to Greenhouse Gases6
A brGDGT‐Based Reconstruction of Terrestrial Temperature From the Maritime Continent Spanning the Last Glacial Maximum6
6
Issue Information6
Paired X‐Ray Micro CT Scanning and Individual Foraminifera Isotopic Analysis Reveal (De)coupled Changes in Carbonate Preservation and Temperature6
Influence of a Rapidly Uplifting Orogen on the Preservation of Climate Oscillations6
Mid–Miocene Palaeofire and Its Complex Relationship With Vegetation Changes in the Wushan Basin, Northeastern Tibetan Plateau, China: Evidence From a High–Resolution Charcoal Record6
Influence of the Late Ordovician‐Early Silurian Paleoenvironment and Related Geological Processes on the Organic Matter Accumulation and Carbon Isotope Excursion6
Micrometer‐Scale Sediment Grain‐Size Prediction Using X‐Ray Fluorescence Geochemistry and Computed Tomography Density Scanning Data6
Evidence for Poleward Migration of the Asian Monsoon During the Paleocene‐Eocene Thermal Maximum6
Millennial‐Scale Climate Variability Potentially Shaped the Early Interglacial Optimum in Southern Europe6
Spatiotemporal Variations of Asian Summer Monsoon Subsystems During the Late Miocene‐Early Pliocene6
Multi‐Year ENSO Events Over the Last Two Millennia6
Coccolithophore Assemblage Response to Indian Monsoon–ENSO Teleconnections During the Last Century6
Hydroclimate and Ecosystem Changes in the Colorado Rocky Mountains Since the Last Glacial Maximum5
A Spatiotemporal Assessment of Extreme Cold in Northwestern North America Following the Unidentified 1809 CE Volcanic Eruption5
Pacific and Atlantic Modes of Overturning in the Miocene Climatic Optimum5
Significant Sea‐Level Fluctuations in the Western Tropical Pacific During the Mid‐Holocene5
Issue Information5
5
Contrasting Scenarios for Upper Ocean Temperature Changes at the Last Glacial Maximum Inferred From Inorganic and Organic Paleothermometers: A Case Study From the Eastern Tropical Indian Ocean5
Orbital Scale Kuroshio Current Variations of the Northwestern Pacific Ocean in the Early Pleistocene (Marine Isotope Stage 40–36) Based on Calcareous Nannofossil Records5
Calcareous Nannofossils and Paleoclimatic Evolution Across the Eocene‐Oligocene Transition at IODP Site U1509, Tasman Sea, Southwest Pacific Ocean5
Detecting Paleoclimate Transitions With Laplacian Eigenmaps of Recurrence Matrices (LERM)5
5
Milanković Forcing in Deep Time5
Evolution of the East Antarctic Ice Sheet Since Glacial Inception From Seismic Stratigraphic Records in Vincennes Bay5
A Process‐Based Model of Precipitation Isotopes, Orographic Lifting and Leaf Wax δ 2 H Across the Tibetan Plateau and South Asia5
Slope Water Intrusions Onto Canadian Atlantic Continental Shelf During the Past 1800 Years5
Hydroclimate Change Enhanced Landscape Erosion During the Early Permian Deglacial Warming5
Calibrating Non‐Thermal Effects on Planktic Foraminiferal Mg/Ca for Application Across the Cenozoic5
Issue Information5
Iron Sources and Cycling During Diagenetic Transformations of Negev Phosphorites (Israel)5
Paleobotanical Evidence for Mediterranean Climates in the Western Canadian Paleoarctic During the Late Middle Eocene5
A Pliocene Precipitation Isotope Proxy‐Model Comparison Assessing the Hydrological Fingerprints of Sea Surface Temperature Gradients5
Impact of Deep Water Formation on Antarctic Circumpolar Transport During Gateway Opening5
Chasing Interannual Marine Paleovariability5
Climate and Vegetation of the Miocene of Tierra del Fuego: Filaret Formation5
How Hot Is Too Hot? Disentangling Mid‐Cretaceous Hothouse Paleoclimate From Diagenesis5
The Loop Current Circulation Over the MIS 9 to MIS 5 Based on Planktonic Foraminifera Assemblages From the Gulf of Mexico5
Temporal, Morphological, and Taxonomic Frameworks for Calibrating Benthic Foraminiferal Pore Patterns as a Paleoxygenation Proxy5
New Insights Into the Surface‐Ocean Dynamics of the Northeastern Atlantic Ocean Across the Marine Isotope Stage 75
Spatial and Temporal Variability of Eastern Pacific Radiocarbon and Carbon Chemistry From the Ice Age to Today5
Timing Is Everything5
Western Pacific Warm Pool Warming and Salinity Front Expansion Since 1821 Reconstructed From Paired Coral δ18O, Sr/Ca, and Reconstructed δ18Osw5
MioVeg1: A Global Middle Miocene Vegetation Reconstruction for Climate Modeling5
Millennial‐Scale Climate Oscillations Triggered by Deglacial Meltwater Discharge in Last Glacial Maximum Simulations5
Issue Information5
5
Issue Information5
Climate‐Induced Variability in Sedimentary Mercury Deposition in the Southern Scotia Sea, Antarctic Zone, Over the Last 35 Kyr5
Late Miocene to Present Paleoclimatic and Paleoenvironmental Evolution of the South China Sea Recorded in the Magneto‐Cyclostratigraphy of IODP Site U15055
Significant Sea‐Level Fluctuations and Transgression During the Holocene in the Bohai Sea, Northern China5
Millennial‐Scale Carbon Flux Variability in the Subantarctic Pacific During Marine Isotope Stage 3 (57–29 ka)4
Constraints on Marine Isotope Stage 3 and 5 Sea Level From the Flooding History of the Karimata Strait in Indonesia4
Two‐Stage Climate and Vegetation Change at the East Asian Monsoonal Margin Across the Miocene Climatic Optimum4
4
Issue Information4
Clumped Isotope Thermometry in Plant‐Derived Carbonates4
Atmospheric CO2 Estimates for the Late Oligocene and Early Miocene Using Multi‐Species Cross‐Calibrations of Boron Isotopes4
Simulated Terrestrial Warming at the Last Interglacial Due to Vegetation Change4
Capturing Equatorial Pacific Variability With Multivariate Sr‐U Coral Thermometry4
Coral Data Reveal the Impact of the Great Acceleration on the Carbon Cycle in the Western Tropical South Atlantic4
Reconstructing the Tropical Thermocline From Oxygen‐Isotopes in Planktonic and Benthic Foraminifera4
Evidence for Persistent Drought Over Mesoamerica Between 1400 and 1600 CE4
Transient Shoaling, Over‐Deepening and Settling of the Calcite Compensation Depth at the Eocene‐Oligocene Transition4
North American Glaciations and Pacific Inputs in the Nd and Sr Isotope Pleistocene Record From the Western Arctic Ocean4
Incoherency in Central American Hydroclimate Proxy Records Spanning the Last Millennium4
Stagnant North Atlantic Deep Water Heat Uptake With Reduced Atlantic Meridional Overturning Circulation During the Last Deglaciation4
Issue Information4
Application of Nitrogen Isotopic Systematics in Different N Forms for the Reconstruction of Redox Conditions: An Example From the Songliao Basin4
Antarctic Intermediate Water Variability in the South Atlantic Over the Last 600,000 years4
Seismic Stratigraphy of Contourite Drift Deposits Associated With the Loop Current on the Eastern Campeche Bank, Gulf of Mexico4
Earth System Model Analysis of How Astronomical Forcing Is Imprinted Onto the Marine Geological Record: The Role of the Inorganic (Carbonate) Carbon Cycle and Feedbacks4
Habitat Specific Growth Rate Adaptation in Oysters During Early Bartonian: Effects of High Temperature and Low Seasonality in the Indian Palaeotropics4
Geochemical Variations in Sedimentary Records of Oxygen‐Depleted Marine Environments in Representative Geological Periods: New Perspectives From an Independent Component Analysis4
The Zonal Patterns in Late Quaternary Tropical South American Precipitation4
Changes in Sea Surface Temperatures and Primary Productivity in the Northern Japan Sea Since the Pliocene4
Tracing the Migration of Fronts in the Pacific Southern Ocean Across the Mid‐Pleistocene Transition4
Issue Information4
Phytoplankton Dynamics and Environmental Variability in the Eastern Equatorial Pacific Over Glacial‐Interglacial Timescales4
Exploring Icehouse Cyclicity Pattern and Seawater Dynamics on an Ancient Carbonate Platform With Nd Isotopes (Carboniferous, Southern Kazakhstan)4
Plio‐Pleistocene Antarctic Bottom Water Production in the Ross Sea Reconstructed From Hillary Canyon Levee Turbidites4
Tracking via Coccolith Assemblages the East Asian Monsoon and Carbonate Production in the South China Sea During Termination II and Marine Isotope Stage 5e4
Early Holocene Atmospheric Circulation Changes Over Northern Europe Based on Isotopic and Biomarker Evidence From Kola Peninsula4
Paleoclimate Changes in the Pacific Northwest Over the Past 36,000 Years From Clumped Isotope Measurements and Model Analysis4
Biomarker and Pollen Evidence for Late Pleistocene Pluvials in the Mojave Desert4
Elevated Post K‐Pg Export Productivity in the Gulf of Mexico and Caribbean4
Enhanced CO2 Degassing From the Tropical Indian Ocean During Cold Climatic Events of the Last Glacial Cycle4
Enhancing Astronomical Signal Detection in Cyclostratigraphy by Superimposed Averaging of Paleoclimate Proxies4
The Variable Impact of Heinrich Events on the Benthic Environment of the Porcupine Abyssal Plain4
Introduction to a Special Collection—Illuminating a Warmer World: Insights From the Paleogene4
Pacific‐Indian Ocean Intermediate Water Exchange Since the Middle Miocene: From Indonesian Throughflow to Tasman Leakage4
Brazil Margin Stable Isotope Profiles for the Last Glacial Cycle: Implications for Watermass Geometry and Oceanic Carbon Storage4
A Tropically Hot Late Jurassic North American Sundance Sea: Evidence for the Oxfordian Warm Interval4
Evolution of Global Ocean Tide Levels Since the Last Glacial Maximum4
Latitudinal Variance in the Drivers and Pacing of Warmth During Mid‐Pleistocene MIS 31 in the Antarctic Zone of the Southern Ocean4
Plio‐Pleistocene Evolution of the Benguela and Agulhas Currents4
Nitrogen Isotope Record From a Mid‐oceanic Paleo‐Atoll Limestone to Constrain the Redox State of the Panthalassa Ocean in the Capitanian (Late Guadalupian, Permian)4
REY Enrichment Mechanism in Bioapatite and Its Implications for Sr Isotope Chronometry During the Paleocene‐Eocene Thermal Maximum4
4
A Sequential Leaching Protocol for δ11B and Trace Element Analyses of Multi‐Phase Carbonate Rocks3
Estimating Plio‐Pleistocene North African Monsoon Runoff Into the Mediterranean Sea and Temperature Impacts3
Deglacial and Holocene Evolution of North Pacific Upper and Intermediate Ocean Circulation3
Tracing West Antarctic Subglacial Weathering Fluxes Across the MPT Using Osmium Isotopes3
Diverse Orbital‐Scale Variations of Precipitation Oxygen Isotopes in the Northern Hemisphere Mid‐Latitudes: A Comparative Study Between East Asia and North America3
Deciphering Paleocene‐Eocene Thermal Maximum Climatic Dynamics: Insights From Oxygen and Hydrogen Isotopes in Clay Minerals of Paleosols From the Southern Pyrenees3
Zonal Indian Ocean Variability Drives Millennial‐Scale Precipitation Changes in Northern Madagascar3
Spectral Divergence in Hydroclimate and Temperature Between Models and Reconstructions Over the Common Era3
A Late Miocene Cold Spell in Zealandia: Evidence From the Whitianga Group, Coromandel, New Zealand3
Evaluating the Drivers of Quaternary Dust Fluxes to the Western North Pacific: East Asian Dustiness and Northern Hemisphere Gustiness3
Neogene Stable Carbon Isotopic Evolution of the Atmosphere and Low‐Latitude Surface Ocean3
Unique C‐Ring Methylated Hopene Biomarkers in a Paleocene Lake3
High‐Latitude, Indian Ocean, and Orbital Influences on Eastern African Hydroclimate Across the Plio‐Pleistocene Boundary3
Issue Information3
3
Late Pleistocene Evolution of Tides and Tidal Dissipation3
Increased North African Dust Fluxes and Higher Productivity in the Eastern Equatorial Atlantic Ocean Linked to Stronger Trade Winds From About 2.7 Million Years ago3
3
3
Evidence for Limited Atmospheric CO 2 Rise at the Miocene Climatic Optimum3
Deglacial Changes in Mediterranean Water Properties and Their Link With Mediterranean Outflow3
Plant Diversity in a Mesothermal Climate: Insights From the Rio San Pedro Formation (Late Eocene, South‐Central Chile, 39°S)3
Oceanographic Influences and High Productivity Recorded in a Coastal Bay of the Amundsen Sea, West Antarctica, During the Holocene3
Century‐Long Records of Sedimentary Input on a Caribbean Reef From Coral Ba/Ca Ratios3
Sedimentary Organic Nitrogen Isotopic Constraints on the Mid‐Holocene Transition in the Nitrogen Dynamics of the Northern South China Sea3
Leaf Wax Hydrogen Isotopes Reflect Storm Track Position Over Western North America3
Competing Influences of Land Use and Greenhouse Gas Emissions on Mississippi River Basin Hydroclimate Simulated Over the Last Millennium3
Regional Millennial‐Scale Summer Monsoon Fluctuations From Southeast Asia During Heinrich Stadials3
Earth System Model Analysis of How Astronomical Forcing Is Imprinted Onto the Marine Geological Record: The Role of the Marine Organic Carbon Cycle and Feedbacks3
A 3.3‐Million‐Year Record of Antarctic Iceberg Rafted Debris and Ice Sheet Evolution Quantified by Machine Learning3
Influence of Growing Season Length on Orbital‐Scale Temperature Evolution Across the Chinese Loess Plateau3
Distinguishing Between Insolation‐Driven and Phase‐Locked 100‐Kyr Ice Age Scenarios Using Example Models3
3
0.11054491996765