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A Cenozoic record of the equatorial Pacific carbonate compensation depth

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What this work says

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

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A Cenozoic seawater Sr/Ca record from benthic foraminiferal calcite and its application in determining global weathering fluxes

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A new, mechanistic model for organic carbon fluxes in the ocean based on the quantitative association of POC with ballast minerals

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Neogene carbonate burial in the Pacific Ocean

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An end to the “rain ratio” reign?

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Missing organic carbon in Eocene marine sediments: Is metabolism the biological feedback that maintains end‐member climates?

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Pacific Ocean and Cenozoic evolution of climate

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Eocene biogenic silica accumulation rates at the Pacific equatorial divergence zone

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Influence of terrestrial weathering on ocean acidification and the next glacial inception

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Coupled greenhouse warming and deep‐sea acidification in the middle Eocene

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Ocean chemistry and atmospheric CO2sensitivity to carbon perturbations throughout the Cenozoic

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Organic carbon burial following the middle Eocene climatic optimum in the central western Tethys

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Modeling the calcite lysocline

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The role of CaCO3 compensation in the glacial to interglacial atmospheric CO2 change

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Effect of deep-sea sedimentary calcite preservation on atmospheric CO2 concentration

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Rapid stepwise onset of Antarctic glaciation and deeper calcite compensation in the Pacific Ocean

inferredcites →https://doi.org/10.1038/nature06053openalex-snapshot

No extreme bipolar glaciation during the main Eocene calcite compensation shift

inferredcites →https://doi.org/10.1038/nature06588openalex-snapshot

An early Cenozoic perspective on greenhouse warming and carbon-cycle dynamics

inferredcites →https://doi.org/10.1038/nature06853openalex-snapshot

Eocene/Oligocene ocean de-acidification linked to Antarctic glaciation by sea-level fall

inferredcites →https://doi.org/10.1038/ngeo1186openalex-snapshot

Convergent Cenozoic CO2 history

inferredcites →https://doi.org/10.1038/ngeo755openalex-snapshot

Past constraints on the vulnerability of marine calcifiers to massive carbon dioxide release

inferredcites →https://doi.org/10.1046/j.1365-3121.2000.00295.xopenalex-snapshot

The marine osmium isotope record

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.1182252openalex-snapshot

Reconstructing Past Seawater Mg/Ca and Sr/Ca from Mid-Ocean Ridge Flank Calcium Carbonate Veins

inferredcites →https://doi.org/10.1126/science.1203909openalex-snapshot

The Role of Carbon Dioxide During the Onset of Antarctic Glaciation

inferredcites →https://doi.org/10.1126/science.1214697openalex-snapshot

Lithium Isotope History of Cenozoic Seawater: Changes in Silicate Weathering and Reverse Weathering

inferredcites →https://doi.org/10.1126/science.258.5088.1594openalex-snapshot

Himalayan Tectonics, Weathering Processes, and the Strontium Isotope Record in Marine Limestones

inferredcites →https://doi.org/10.1130/g24474a.1openalex-snapshot

Sedimentary response to Paleocene-Eocene Thermal Maximum carbon release: A model-data comparison

inferredcites →https://doi.org/10.2204/iodp.proc.320321.101.2010openalex-snapshot

Pacific Equatorial Age Transect

inferredcites →https://doi.org/10.2204/iodp.proc.320321.201.2012openalex-snapshot

Revised composite depth scales and integration of IODP Sites U1331U1334 and ODP Sites 12181220

inferredcites →https://doi.org/10.2204/iodp.proc.320321.2010openalex-snapshot

Pacific Equatorial Age Transect : expeditions 320 and 321 of the riserless drilling platform from and to Honolulu, Hawaii (USA), Sites U1331–U1336, 5 March–4 May 2009 and Honolulu, Hawaii (USA), to San Diego, California (USA), Sites U1337–U1338, 4 May–22 June 2009

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.284.10.1175openalex-snapshot

Comments on the BLAG model; The carbonate-silicate geochemical cycle and its effect on atmospheric carbon dioxide over the past 100 million years

inferredcites →https://doi.org/10.2973/odp.proc.sr.115.163.1991openalex-snapshot

Late Cenozoic Carbonate Accumulation and the History of the Carbonate Compensation Depth in the Western Equatorial Indian Ocean

inferredcites →https://doi.org/10.2973/odp.proc.sr.138.157.1995openalex-snapshot

The Late Miocene (11-8 Ma) Eastern Pacific Carbonate Crash: Evidence for Reorganization of Deep-Water Circulation by the Closure of the Panama Gateway

inferredcites →https://doi.org/10.2973/odp.proc.sr.199.219.2005openalex-snapshot

Biogenic Sedimentation in the Eocene Equatorial Pacific-The Stuttering Greenhouse and Eocene Carbonate Compensation Depth

inferredcites →https://doi.org/10.5194/bg-4-87-2007openalex-snapshot

Marine geochemical data assimilation in an efficient Earth System Model of global biogeochemical cycling

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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.

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Visual Bibliometric Analysis of the Research on Marine Ecological Compensation Based on Citespace

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Orbital pacing of Eocene climate during the Middle Eocene climate optimum and the chron C19r event - missing link found in the tropical western Atlantic

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Middle Eocene to Late Oligocene Antarctic glaciation/deglaciation and Southern Ocean productivity

inferred← citeshttps://doi.org/10.1002/2013pa002567openalex-snapshot

A transient deep‐sea circulation switch during Eocene Thermal Maximum 2

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Cenozoic climate changes: A review based on time series analysis of marine benthic δ18O records

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inferred← citeshttps://doi.org/10.1002/2014pa002656openalex-snapshot

Equatorial Pacific productivity changes near the Eocene‐Oligocene boundary

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Episodes of intensified biological productivity in the subtropical Atlantic Ocean during the termination of the Middle Eocene Climatic Optimum (MECO)

inferred← citeshttps://doi.org/10.1002/2015pa002777openalex-snapshot

Evidence for changes in subsurface circulation in the late Eocene equatorial Pacific from radiolarian‐bound nitrogen isotope values

inferred← citeshttps://doi.org/10.1002/2015pa002818openalex-snapshot

Global carbon cycle perturbation across the Eocene‐Oligocene climate transition

inferred← citeshttps://doi.org/10.1002/2015pa002820openalex-snapshot

Global change across the Oligocene-Miocene transition: High-resolution stable isotope records from IODP Site U1334 (equatorial Pacific Ocean)

inferred← citeshttps://doi.org/10.1002/2015pa002822openalex-snapshot

Minimal influence of recrystallization on middle Miocene benthic foraminiferal stable isotope stratigraphy in the eastern equatorial Pacific

inferred← citeshttps://doi.org/10.1002/2015pa002825openalex-snapshot

Carbon and oxygen isotopes of bulk carbonate in sediment deposited beneath the eastern equatorial Pacific over the last 8 million years

inferred← citeshttps://doi.org/10.1002/2015pa002829openalex-snapshot

Dust, volcanic ash, and the evolution of the South Pacific Gyre through the Cenozoic

inferred← citeshttps://doi.org/10.1002/2015pa002837openalex-snapshot

Late Paleocene‐middle Eocene benthic foraminifera on a Pacific seamount (Allison Guyot, ODP Site 865): Greenhouse climate and superimposed hyperthermal events

inferred← citeshttps://doi.org/10.1002/2015pa002881openalex-snapshot

Evaluating climatic response to external radiative forcing during the late Miocene to early Pliocene: New perspectives from eastern equatorial Pacific (IODP U1338) and North Atlantic (ODP 982) locations

inferred← citeshttps://doi.org/10.1002/2015pa002899openalex-snapshot

Plio‐Pleistocene glacial‐interglacial productivity changes in the eastern equatorial Pacific upwelling system

inferred← citeshttps://doi.org/10.1002/2015pa002914openalex-snapshot

Evolution of the North Pacific Subtropical Gyre during the past 190 kyr through the interaction of the Kuroshio Current with the surface and intermediate waters

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Processes of multibathyal aragonite undersaturation in the Arctic Ocean

inferred← citeshttps://doi.org/10.1002/2016pa002950openalex-snapshot

Changes in the depth habitat of the Oligocene planktic foraminifera (Dentoglobigerina venezuelana) induced by thermocline deepening in the eastern equatorial Pacific

inferred← citeshttps://doi.org/10.1002/2016pa002972openalex-snapshot

Evidence for a heavily glaciated Antarctica during the late Oligocene “warming” (27.8–24.5 Ma): Stable isotope records from ODP Site 690

inferred← citeshttps://doi.org/10.1002/2016pa002988openalex-snapshot

Eccentricity pacing of eastern equatorial Pacific carbonate dissolution cycles during the Miocene Climatic Optimum

inferred← citeshttps://doi.org/10.1002/2016pa003058openalex-snapshot

Vertical thermal gradient history in the eastern equatorial Pacific during the early to middle Miocene: Implications for the equatorial thermocline development

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The onset of modern‐like A tlantic meridional overturning circulation at the E ocene‐ O ligocene transition: Evidence, causes, and possible implications for global cooling

inferred← citeshttps://doi.org/10.1002/2017gc007386openalex-snapshot

Effects of Dynamic Topography on the Cenozoic Carbonate Compensation Depth

inferred← citeshttps://doi.org/10.1002/2017pa003115openalex-snapshot

Silicate Weathering and Carbon Cycle Controls on the Oligocene‐Miocene Transition Glaciation

inferred← citeshttps://doi.org/10.1002/2017pa003211openalex-snapshot

Meridional Contrasts in Productivity Changes Driven by the Opening of Drake Passage

inferred← citeshttps://doi.org/10.1002/2017pa003245openalex-snapshot

Deciphering the State of the Late Miocene to Early Pliocene Equatorial Pacific

inferred← citeshttps://doi.org/10.1002/9781118897362.ch10openalex-snapshot

The Pulse of the Earth

inferred← citeshttps://doi.org/10.1002/9781118897362.ch11openalex-snapshot

Numerical Climate Models and Case Histories

inferred← citeshttps://doi.org/10.1002/9781119507444.ch17openalex-snapshot

The Monterey Event and the Paleocene‐Eocene Thermal Maximum

inferred← citeshttps://doi.org/10.1002/9781394229185.ch9openalex-snapshot

Low‐Temperature Ridge Flank Heat and Fluid Fluxes, Contributions to Global Biogeochemical Cycles, and Archives of Changing Global Conditions

inferred← citeshttps://doi.org/10.1002/essoar.10512673.1openalex-snapshot

The Late Miocene Biogenic Bloom : A globally distributed but not an ubiquitous event

inferred← citeshttps://doi.org/10.1002/ggge.20064openalex-snapshot

Rock‐magnetic artifacts on long‐term relative paleointensity variations in sediments

inferred← citeshttps://doi.org/10.1002/ggge.20293openalex-snapshot

Orbital pacing of Eocene climate during the Middle Eocene Climate Optimum and the chron C19r event: Missing link found in the tropical western Atlantic

inferred← citeshttps://doi.org/10.1002/jqs.2677openalex-snapshot

Coccolithophore carbonate during the last 450 ka in the NW Pacific Ocean (ODP site 1209B, Shatsky Rise)

inferred← citeshttps://doi.org/10.1002/palo.20027openalex-snapshot

Erosion and reworking of Pacific sediments near the Eocene‐Oligocene boundary

inferred← citeshttps://doi.org/10.1002/palo.20045openalex-snapshot

Testing the impact of diagenesis on the δ18O and δ13C of benthic foraminiferal calcite from a sediment burial depth transect in the equatorial Pacific

inferred← citeshttps://doi.org/10.1002/palo.20060openalex-snapshot

Understanding long-term carbon cycle trends: The late Paleocene through the early Eocene

inferred← citeshttps://doi.org/10.1007/978-94-007-6238-1_46openalex-snapshot

Carbonate Dissolution

inferred← citeshttps://doi.org/10.1007/978-94-007-6238-1_53openalex-snapshot

Deep-sea Sediments

inferred← citeshttps://doi.org/10.1007/978-94-007-6644-0_204-1openalex-snapshot

Ocean Drilling

inferred← citeshttps://doi.org/10.1007/978-94-007-6644-0_204-2openalex-snapshot

Ocean Drilling

inferred← citeshttps://doi.org/10.1007/978-94-007-6644-0_204-3openalex-snapshot

Ocean Drilling

inferred← citeshttps://doi.org/10.1007/978-94-007-6644-0_204-4openalex-snapshot

Ocean Drilling

inferred← citeshttps://doi.org/10.1007/978-94-007-6644-0_46-1openalex-snapshot

Carbonate Dissolution

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Carbonate Dissolution

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Deep-Sea Sediments

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Deep-Sea Sediments

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Marine Microfossils

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Deep-sea benthic foraminiferal response to the early Oligocene cooling: a study from the Southern Ocean ODP Hole 1138A

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Indian Ocean carbonate compensation depth since the Late Oligocene

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Unraveling the Cenozoic carbon cycle by reconstructing carbonate compensation depth (CCD)

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Driving force behind global cooling in the Cenozoic: an ongoing mystery

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Deepwater sedimentary processes

inferred← citeshttps://doi.org/10.1016/b978-0-323-99762-1.00060-7openalex-snapshot

Regulation of the carbon cycle on geological timescales

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Earth system carbon cycle dynamics through time

inferred← citeshttps://doi.org/10.1016/b978-0-444-62617-2.00001-3openalex-snapshot

Major Scientific Achievements of the Integrated Ocean Drilling Program

inferred← citeshttps://doi.org/10.1016/b978-0-444-62617-2.00013-xopenalex-snapshot

The Pacific Equatorial Age Transect

inferred← citeshttps://doi.org/10.1016/b978-0-444-62617-2.00014-1openalex-snapshot

North Atlantic Paleoceanography from Integrated Ocean Drilling Program Expeditions (2003–2013)

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Links between geochemical weathering on the NE Tibetan Plateau and global climate change since the Last Deglacial

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The zinc isotopic composition of siliceous marine sponges: Investigating nature's sediment traps

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Geomorphological and geochemical evidence (230Th anomalies) for cross-equatorial currents in the central Pacific

inferred← citeshttps://doi.org/10.1016/j.earscirev.2017.06.004openalex-snapshot

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inferred← citeshttps://doi.org/10.1016/j.earscirev.2020.103154openalex-snapshot

An assessment of reef coral calcification over the late Cenozoic

inferred← citeshttps://doi.org/10.1016/j.earscirev.2020.103298openalex-snapshot

Silicate weathering as a feedback and forcing in Earth's climate and carbon cycle

inferred← citeshttps://doi.org/10.1016/j.earscirev.2020.103403openalex-snapshot

Evolution of deep-sea sediments across the Paleocene-Eocene and Eocene-Oligocene boundaries

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Subduction initiation as recorded in the Izu-Bonin-Mariana forearc

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Millennial-scale changes in marine lithofacies during the Paleocene-Eocene Thermal Maximum: A deep-time analog for Anthropocene hydrologic and acidification impacts

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Opening the gateways for diatoms primes Earth for Antarctic glaciation

inferred← citeshttps://doi.org/10.1016/j.epsl.2013.04.038openalex-snapshot

A middle Miocene relative paleointensity record from the Equatorial Pacific

inferred← citeshttps://doi.org/10.1016/j.epsl.2013.11.028openalex-snapshot

Oligocene–Miocene relative (geomagnetic) paleointensity correlated from the equatorial Pacific (IODP Site U1334 and ODP Site 1218) to the South Atlantic (ODP Site 1090)

inferred← citeshttps://doi.org/10.1016/j.epsl.2013.12.014openalex-snapshot

Aridification in continental Asia after the Middle Eocene Climatic Optimum (MECO)

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A high-resolution benthic stable-isotope record for the South Atlantic: Implications for orbital-scale changes in Late Paleocene–Early Eocene climate and carbon cycling

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Estimating the impact of the cryptic degassing of Large Igneous Provinces: A mid-Miocene case-study

inferred← citeshttps://doi.org/10.1016/j.epsl.2014.09.013openalex-snapshot

Synchronous mid-Miocene upper and deep oceanic δ13C changes in the east equatorial Pacific linked to ocean cooling and ice sheet expansion

inferred← citeshttps://doi.org/10.1016/j.epsl.2016.06.035openalex-snapshot

Cenozoic carbon cycle imbalances and a variable weathering feedback

inferred← citeshttps://doi.org/10.1016/j.epsl.2017.06.005openalex-snapshot

Retrodiction of secular variations in deep-sea CaCO3 burial during the Cenozoic

inferred← citeshttps://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

inferred← citeshttps://doi.org/10.1016/j.epsl.2018.01.003openalex-snapshot

Towards a robust and consistent middle Eocene astronomical timescale

inferred← citeshttps://doi.org/10.1016/j.epsl.2018.06.017openalex-snapshot

Constraining the evolution of Neogene ocean carbonate chemistry using the boron isotope pH proxy

inferred← citeshttps://doi.org/10.1016/j.epsl.2019.02.004openalex-snapshot

Secular variations in the carbonate chemistry of the oceans over the Cenozoic

inferred← citeshttps://doi.org/10.1016/j.epsl.2022.117801openalex-snapshot

Carbonate weathering, CO2 redistribution, and Neogene CCD and pCO2 evolution

inferred← citeshttps://doi.org/10.1016/j.epsl.2023.118375openalex-snapshot

Kerguelen carbonatite tuff sourced from deep recycled material

inferred← citeshttps://doi.org/10.1016/j.epsl.2024.119097openalex-snapshot

The sulfur isotopic composition of Cenozoic pyrite is affected by methane content and depositional environment

inferred← citeshttps://doi.org/10.1016/j.epsl.2026.120256openalex-snapshot

Decoupling of biological pump strength and efficiency in the eastern equatorial Pacific during the Middle Miocene Climate Optimum

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Wildland fire emissions, carbon, and climate: Science overview and knowledge needs

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Variability of carbonate diagenesis in equatorial Pacific sediments deduced from radiogenic and stable Sr isotopes

inferred← citeshttps://doi.org/10.1016/j.gca.2019.02.041openalex-snapshot

History of carbonate ion concentration over the last 100 million years II: Revised calculations and new data

inferred← citeshttps://doi.org/10.1016/j.gca.2021.07.007openalex-snapshot

Iron isotope signature of magnetofossils and oceanic biogeochemical changes through the Middle Eocene Climatic Optimum

inferred← citeshttps://doi.org/10.1016/j.gca.2023.03.008openalex-snapshot

Millimetre-scale biomarker heterogeneity in lacustrine shale identifies the nature of signal-averaging and demonstrates anaerobic respiration control on organic matter preservation and dolomitization

inferred← citeshttps://doi.org/10.1016/j.gca.2025.10.005openalex-snapshot

The Nd isotope composition of oxic pore waters of marine sediments and implications for its use as a past water mass proxy

inferred← citeshttps://doi.org/10.1016/j.gexplo.2026.108246openalex-snapshot

Geochemistry of hematite-quartz schist in the Sanbagawa metamorphic belt, Japan: A metamorphosed umber deposit

inferred← citeshttps://doi.org/10.1016/j.gloplacha.2014.04.004openalex-snapshot

The role of ocean gateways on cooling climate on long time scales

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Downsizing the pelagic carbonate factory: Impacts of calcareous nannoplankton evolution on carbonate burial over the past 17 million years

inferred← citeshttps://doi.org/10.1016/j.gloplacha.2020.103258openalex-snapshot

Changes in upper ocean hydrography and productivity across the Middle Eocene Climatic Optimum: Local insights and global implications from the Northwest Atlantic

inferred← citeshttps://doi.org/10.1016/j.gloplacha.2021.103510openalex-snapshot

Southern Ocean carbonate dissolution paced by Antarctic Ice-Sheet expansion in the early Miocene

inferred← citeshttps://doi.org/10.1016/j.gloplacha.2021.103723openalex-snapshot

Ice sheet and terrestrial input impacts on the 100-kyr ocean carbon cycle during the Middle Miocene

inferred← citeshttps://doi.org/10.1016/j.gloplacha.2024.104564openalex-snapshot

Enhanced deep-water circulation facilitated rare earth elements enrichment in pelagic sediments from the northwestern Pacific Ocean

inferred← citeshttps://doi.org/10.1016/j.gloplacha.2025.104744openalex-snapshot

Late Eocene-Early Miocene paleoenvironmental shifts in the NW south American margin: Tectonic and climatic drivers inferred from benthic foraminifera

inferred← citeshttps://doi.org/10.1016/j.gloplacha.2025.105056openalex-snapshot

Coupled forcing of long eccentricity and silicate weathering on the carbonate dissolution in Southern Ocean during the late Eocene

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.2026.105601openalex-snapshot

Climate–ocean changes across late Eocene-early Oligocene recorded at IODP Site U1553 (Southern Pacific Ocean)

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

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

inferred← citeshttps://doi.org/10.1016/j.jafrearsci.2018.02.013openalex-snapshot

Paleoenvironmental and ecological changes during the Eocene-Oligocene transition based on foraminifera from the Cap Bon Peninsula in North East Tunisia

inferred← citeshttps://doi.org/10.1016/j.jsames.2021.103682openalex-snapshot

Why do calcareous microfossils preferentially occur in tuffaceous sandstones of the Santa Marta formation (James Ross Island, Antarctica)?

inferred← citeshttps://doi.org/10.1016/j.jseaes.2014.07.005openalex-snapshot

Geochemistry and mineralogy of REY-rich mud in the eastern Indian Ocean

inferred← citeshttps://doi.org/10.1016/j.margeo.2016.06.005openalex-snapshot

Dynamic carbonate sedimentation on the Northern Line Islands Ridge, Palmyra Basin

inferred← citeshttps://doi.org/10.1016/j.margeo.2017.07.017openalex-snapshot

Sediment waves in the Caroline Basin suggest evidence for Miocene shifts in bottom water flow in the western equatorial Pacific

inferred← citeshttps://doi.org/10.1016/j.margeo.2021.106548openalex-snapshot

How volcanically active is an abyssal plain? Evidence for recent volcanism on 20 Ma Nazca Plate seafloor

inferred← citeshttps://doi.org/10.1016/j.margeo.2024.107430openalex-snapshot

Spatial heterogeneity of sediments on a topographically diverse descending plate at convergent margins: An example from the outer slope of the Mariana Trench

inferred← citeshttps://doi.org/10.1016/j.margeo.2026.107721openalex-snapshot

Variations in thermocline depth and their response to the East Asian Monsoon in the Northern South China Sea during the Early-Middle Miocene: Evidence from planktonic foraminifera

inferred← citeshttps://doi.org/10.1016/j.marmicro.2014.06.003openalex-snapshot

Deep-sea Ostracoda from the Eastern Equatorial Pacific (ODP Site 1238) over the last 460ka

inferred← citeshttps://doi.org/10.1016/j.marmicro.2015.02.002openalex-snapshot

Radiolarian stratigraphy near the Eocene–Oligocene boundary

inferred← citeshttps://doi.org/10.1016/j.marmicro.2015.06.001openalex-snapshot

Middle Eocene-Lower Oligocene calcareous nannofossil biostratigraphy and paleoceanographic implications from Site 711 (equatorial Indian Ocean)

inferred← citeshttps://doi.org/10.1016/j.marmicro.2017.05.002openalex-snapshot

Eastern equatorial Pacific benthic foraminiferal distribution and deep water temperature changes during the early to middle Miocene

inferred← citeshttps://doi.org/10.1016/j.marmicro.2021.102051openalex-snapshot

Integrated calcareous nannofossil and magnetostratigraphic record of ODP Site 709: Middle Eocene to late Oligocene paleoclimate and paleoceanography of the Equatorial Indian Ocean

inferred← citeshttps://doi.org/10.1016/j.marmicro.2023.102272openalex-snapshot

No dramatic changes observed in subtropical radiolarian plankton assemblages during the Middle Eocene Climatic Optimum (MECO); evidence from the North Atlantic ODP Site 1051

inferred← citeshttps://doi.org/10.1016/j.marpetgeo.2020.104337openalex-snapshot

A comparative study of methods for determining carbonate content in marine and terrestrial sediments

inferred← citeshttps://doi.org/10.1016/j.marpetgeo.2023.106148openalex-snapshot

Stratigraphy of the Cenozoic succession in eastern Azerbaijan: Implications for petroleum systems and paleogeography in the Caspian basin

inferred← citeshttps://doi.org/10.1016/j.oregeorev.2024.106338openalex-snapshot

Long-term variations of factors controlling REE-rich mud formation based on ocean–sediment Nd mass balance modeling

inferred← citeshttps://doi.org/10.1016/j.orggeochem.2014.07.004openalex-snapshot

Stable carbon isotopic variation of long chain n-alkanoic acids in the equatorial Pacific sediments over the last 40Ma: Implications for expansion of C4 grassland in South America

inferred← citeshttps://doi.org/10.1016/j.palaeo.2013.09.012openalex-snapshot

Cenozoic history of phosphogenesis recorded in the ferromanganese crusts of central and western Pacific seamounts: Implications for deepwater circulation and phosphorus budgets

inferred← citeshttps://doi.org/10.1016/j.palaeo.2014.04.004openalex-snapshot

Changes in Southern Ocean bottom water environments associated with the Middle Eocene Climatic Optimum (MECO)

inferred← citeshttps://doi.org/10.1016/j.palaeo.2014.04.016openalex-snapshot

Productivity and sea-surface temperature changes recorded during the late Eocene–early Oligocene at DSDP Site 511 (South Atlantic)

inferred← citeshttps://doi.org/10.1016/j.palaeo.2014.07.024openalex-snapshot

Cenozoic bathyal and abyssal ostracods beneath the oligotrophic South Pacific Gyre (IODP Expedition 329 Sites U1367, U1368 and U1370)

inferred← citeshttps://doi.org/10.1016/j.palaeo.2014.08.009openalex-snapshot

Enhanced primary productivity and magnetotactic bacterial production in response to middle Eocene warming in the Neo-Tethys Ocean

inferred← citeshttps://doi.org/10.1016/j.palaeo.2014.10.004openalex-snapshot

Benthic foraminiferal response to the Middle Eocene Climatic Optimum (MECO) in the South-Eastern Atlantic (ODP Site 1263)

inferred← citeshttps://doi.org/10.1016/j.palaeo.2015.04.001openalex-snapshot

Biogenic sediment regimes in the Neogene equatorial Pacific, IODP Site U1338: Burial, production, and diatom community

inferred← citeshttps://doi.org/10.1016/j.palaeo.2015.06.029openalex-snapshot

Environmental magnetic implications of magnetofossil occurrence during the Middle Eocene Climatic Optimum (MECO) in pelagic sediments from the equatorial Indian Ocean

inferred← citeshttps://doi.org/10.1016/j.palaeo.2016.03.018openalex-snapshot

Late Cenozoic sea level and the rise of modern rimmed atolls

inferred← citeshttps://doi.org/10.1016/j.palaeo.2016.05.006openalex-snapshot

Environmental dynamics during the Paleocene–Eocene thermal maximum (PETM) in the northeastern Peri-Tethys revealed by high-resolution micropalaeontological and geochemical studies of a Caucasian key section

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

Climatic instability before the Miocene Climatic Optimum reflected in a Central European lacustrine record from the Most Basin in the Czech Republic

inferred← citeshttps://doi.org/10.1016/j.palaeo.2017.08.028openalex-snapshot

Reconstruction of oceanic circulation patterns in the tropical Pacific across the early/middle Miocene boundary as inferred from radiolarian assemblages

inferred← citeshttps://doi.org/10.1016/j.palaeo.2017.09.015openalex-snapshot

Variations to calcareous nannofossil CaCO3 content during the middle Eocene C21r-H6 hyperthermal event (~ 47.4 Ma) in the Gorrondatxe section (Bay of Biscay, western Pyrenees)

inferred← citeshttps://doi.org/10.1016/j.palaeo.2017.11.003openalex-snapshot

Calcareous nannofossil fluxes and size fluctuations in the middle Eocene (48–39 Ma) from Ocean Drilling Program (ODP) Site 1209 in the tropical Pacific Ocean

inferred← citeshttps://doi.org/10.1016/j.palaeo.2018.05.003openalex-snapshot

Eocene (Bartonian) benthic foraminifera and paleoenvironmental changes in the Western Tethys

inferred← citeshttps://doi.org/10.1016/j.palaeo.2018.09.016openalex-snapshot

Oligocene paleoceanographic changes based on an interbasinal comparison of Cibicidoides spp. δ18O records and a new compilation of data

inferred← citeshttps://doi.org/10.1016/j.palaeo.2018.10.034openalex-snapshot

Orbital forcing and abrupt events in a continental weathering proxy from central Europe (Most Basin, Czech Republic, 17.7–15.9 Ma) recorded beginning of the Miocene Climatic Optimum

inferred← citeshttps://doi.org/10.1016/j.palaeo.2019.01.006openalex-snapshot

Influence of increasing carbonate saturation in Atlantic bottom water during the late Miocene

inferred← citeshttps://doi.org/10.1016/j.palaeo.2020.109623openalex-snapshot

High calcification rates and inferred metabolic trade-offs in the largest turritellid gastropod, Turritella abrupta (Neogene)

inferred← citeshttps://doi.org/10.1016/j.palaeo.2021.110511openalex-snapshot

Impacts of the Middle Miocene Climatic Transition on deep-water carbonate preservation and oxygenation in the equatorial Indian Ocean

inferred← citeshttps://doi.org/10.1016/j.palaeo.2021.110563openalex-snapshot

Orbital tuning for the middle Eocene to early Oligocene Monte Cagnero Section (Central Italy): Paleoenvironmental and paleoclimatic implications

inferred← citeshttps://doi.org/10.1016/j.palaeo.2021.110567openalex-snapshot

(Bio)stratigraphic overview and paleoclimatic-paleoceanographic implications of the middle-upper Eocene deposits from the Ica River Valley (East Pisco Basin, Peru)

inferred← citeshttps://doi.org/10.1016/j.palaeo.2021.110591openalex-snapshot

A dynamic ocean driven by changes in CO2 and Antarctic ice-sheet in the middle Miocene

inferred← citeshttps://doi.org/10.1016/j.palaeo.2021.110604openalex-snapshot

Foraminiferal stratigraphy and paleoenvironments of a high latitude marginal marine basin – A Late Cretaceous record from IODP Site U1512 (Great Australian Bight)

inferred← citeshttps://doi.org/10.1016/j.palaeo.2023.111436openalex-snapshot

East Asian hydroclimate responses to the Eocene-Oligocene transition in the Weihe Basin, central China

inferred← citeshttps://doi.org/10.1016/j.palaeo.2023.111778openalex-snapshot

Calcareous nannofossils across the Eocene-Oligocene transition: Preservation signals and biostratigraphic remarks from ODP Site 1209 (NW Pacific, Shatsky Rise) and IODP Hole U1411B (NW Atlantic Ocean, Newfoundland Ridge)

inferred← citeshttps://doi.org/10.1016/j.palaeo.2025.112748openalex-snapshot

Revised astrochronology for the Lower to Middle Miocene of IODP site U1337. Implications for the Cenozoic megasplice (CENOGRID)

inferred← citeshttps://doi.org/10.1016/j.palaeo.2025.112961openalex-snapshot

Dust supply to the West Philippine Sea since the Middle Pleistocene and distinct influences of the Westerlies after the Mid-Brunhes Event

inferred← citeshttps://doi.org/10.1016/j.palaeo.2025.113106openalex-snapshot

Editorial preface to special issue: Biocalcifier resilience and response during Phanerozoic global climate changes

inferred← citeshttps://doi.org/10.1016/j.palaeo.2026.113590openalex-snapshot

Abyssal record of the Middle Eocene Climatic Optimum in the Tasman Sea: Insights from benthic foraminiferal and clay mineral assemblages

inferred← citeshttps://doi.org/10.1016/j.palaeo.2026.113730openalex-snapshot

Hydroclimate-driven variability in Middle Miocene deep-marine deposits of the Eastern Equatorial Pacific of Colombia: a multi-proxy sedimentological, ichnological, and geochemical reconstruction

inferred← citeshttps://doi.org/10.1016/j.pocean.2013.01.003openalex-snapshot

Modeling vertical carbon flux from zooplankton respiration

inferred← citeshttps://doi.org/10.1016/j.pocean.2019.102144openalex-snapshot

Review of Ostracoda (Crustacea) living below the Carbonate Compensation Depth and the deepest record of a calcified ostracod

inferred← citeshttps://doi.org/10.1016/j.quascirev.2019.106114openalex-snapshot

Timing of Quaternary geomagnetic reversals and excursions in volcanic and sedimentary archives

inferred← citeshttps://doi.org/10.1016/j.scib.2022.12.032openalex-snapshot

The formation of supercritical carbon dioxide hydrothermal vents in the Okinawa Trough

inferred← citeshttps://doi.org/10.1016/j.sedgeo.2020.105705openalex-snapshot

Eocene carbonate accumulation in the north-central Pacific Ocean: new insights from Ocean Drilling Program Site 1209, Shatsky Rise

inferred← citeshttps://doi.org/10.1016/j.sedgeo.2022.106092openalex-snapshot

3D seismic geomorphology of Early Cenozoic incised channels, Gippsland Basin, SE Australia: Evidence for submarine origin

inferred← citeshttps://doi.org/10.1016/j.tecto.2018.11.014openalex-snapshot

Multiphase magmatic and tectonic evolution of a large igneous province - Evidence from the crustal structure of the Manihiki Plateau, western Pacific

inferred← citeshttps://doi.org/10.1017/pab.2022.24openalex-snapshot

Small but mighty: how overlooked small species maintain community structure through middle Eocene climate change

inferred← citeshttps://doi.org/10.1017/s0016756821000960openalex-snapshot

The Nazca Drift System – palaeoceanographic significance of a giant sleeping on the SE Pacific Ocean floor

inferred← citeshttps://doi.org/10.1017/s1089332600002965openalex-snapshot

Late Proterozoic Transitions in Climate, Oxygen, and Tectonics, and the Rise of Complex Life

inferred← citeshttps://doi.org/10.1029/2012gc004429openalex-snapshot

Oligocene‐Miocene magnetic stratigraphy carried by biogenic magnetite at sites U1334 and U1335 (equatorial Pacific Ocean)

inferred← citeshttps://doi.org/10.1029/2017gc007313openalex-snapshot

PyBacktrack 1.0: A Tool for Reconstructing Paleobathymetry on Oceanic and Continental Crust

inferred← citeshttps://doi.org/10.1029/2017pa003278openalex-snapshot

Eccentricity‐Paced Southern Hemisphere Glacial‐Interglacial Cyclicity Preceding the Middle Miocene Climatic Transition

inferred← citeshttps://doi.org/10.1029/2017pa003309openalex-snapshot

Neodymium Evidence for Increased Circumpolar Deep Water Flow to the North Pacific During the Middle Miocene Climate Transition

inferred← citeshttps://doi.org/10.1029/2018pa003380openalex-snapshot

Assessing Mechanisms and Uncertainty in Modeled Climatic Change at the Eocene‐Oligocene Transition

inferred← citeshttps://doi.org/10.1029/2018pa003384openalex-snapshot

Paleoproductivity Reconstructions for the Paleogene Southern Ocean: A Direct Comparison of Geochemical and Micropaleontological Proxies

inferred← citeshttps://doi.org/10.1029/2018pa003482openalex-snapshot

The Middle to Late Miocene “Carbonate Crash” in the Equatorial Indian Ocean

inferred← citeshttps://doi.org/10.1029/2019gc008716openalex-snapshot

Geographic and Oceanographic Influences on Ferromanganese Crust Composition Along a Pacific Ocean Meridional Transect, 14 N to 14S

inferred← citeshttps://doi.org/10.1029/2019pa003586openalex-snapshot

Understanding Bulk Sediment Stable Isotope Records in the Eastern Equatorial Pacific, From Seven Million Years Ago to Present Day

inferred← citeshttps://doi.org/10.1029/2019pa003601openalex-snapshot

Early Cenozoic Decoupling of Climate and Carbonate Compensation Depth Trends

inferred← citeshttps://doi.org/10.1029/2019pa003685openalex-snapshot

Multiproxy Reduced‐Dimension Reconstruction of Pliocene Equatorial Pacific Sea Surface Temperatures

inferred← citeshttps://doi.org/10.1029/2019pa003713openalex-snapshot

Revisiting the Middle Eocene Climatic Optimum “Carbon Cycle Conundrum” With New Estimates of Atmospheric pCO2 From Boron Isotopes

inferred← citeshttps://doi.org/10.1029/2019pa003812openalex-snapshot

The Benthic B/Ca Record at Site 806: New Constraints on the Temperature of the West Pacific Warm Pool and the “El Padre” State in the Pliocene

inferred← citeshttps://doi.org/10.1029/2020gl087742openalex-snapshot

Himalayan‐Tibetan Erosion Is Not the Cause of Neogene Global Cooling

inferred← citeshttps://doi.org/10.1029/2020pa003915openalex-snapshot

Shifts in Phytoplankton Composition and Stepwise Climate Change During the Middle Miocene

inferred← citeshttps://doi.org/10.1029/2020pa003924openalex-snapshot

Temperature Gradients Across the Pacific Ocean During the Middle Miocene

inferred← citeshttps://doi.org/10.1029/2020pa003965openalex-snapshot

Stable Biological Production in the Eastern Equatorial Pacific Across the Plio‐Pleistocene Transition (∼3.35–2.0 Ma)

inferred← citeshttps://doi.org/10.1029/2020pa004132openalex-snapshot

Size‐Fraction‐Specific Stable Isotope Variations as a Framework for Interpreting Early Eocene Bulk Sediment Carbon Isotope Records

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/10.1029/2020pa004168openalex-snapshot

Middle to Late Eocene Changes of the Ocean Carbonate Cycle

inferred← citeshttps://doi.org/10.1029/2021av000386openalex-snapshot

Arid Coastal Carbonates and the Phanerozoic Record of Carbonate Chemistry

inferred← citeshttps://doi.org/10.1029/2021gc009729openalex-snapshot

Secular Variations in Provenance of Sedimentary Components in the Western North Pacific Ocean Constrained by Sr Isotopic Features of Deep‐Sea Sediments

inferred← citeshttps://doi.org/10.1029/2021gc009835openalex-snapshot

A Biogeochemical Imprint of the Panama Basin in the North Andean Arc

inferred← citeshttps://doi.org/10.1029/2021jb021966openalex-snapshot

Paleobathymetry of Submarine Lavas in the Samail and Troodos Ophiolites: Insights From Volatiles in Glasses and Implications for Hydrothermal Systems

inferred← citeshttps://doi.org/10.1029/2021pa004313openalex-snapshot

The Late Miocene‐Early Pliocene Biogenic Bloom in the Eastern Equatorial Pacific: New Insights From Integrated Ocean Drilling Program Site U1335

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