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Opening the gateways for diatoms primes Earth for Antarctic glaciation
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What this work says
Outgoing claims: the papers this work cites, builds on, or argues with.
inferredcites →https://doi.org/10.1016/0031-0182(92)90185-8openalex-snapshot
Sedimentological evidence for the formation of an East Antarctic ice sheet in Eocene/Oligocene time
inferredcites →https://doi.org/10.1016/0031-0182(95)00067-vopenalex-snapshot
Middle Eocene to early Oligocene paleoceanography of the Antarctic Ocean (Maud Rise, ODP Leg 113, Site 689): change from a low to a high productivity ocean
inferredcites →https://doi.org/10.1016/j.chemgeo.2006.06.006openalex-snapshot
New sample preparation techniques for the determination of Si isotopic compositions using MC-ICPMS
inferredcites →https://doi.org/10.1016/j.csr.2004.09.017openalex-snapshot
A new method for the measurement of biogenic silica in suspended matter of coastal waters: using Si:Al ratios to correct for the mineral interference
inferredcites →https://doi.org/10.1016/j.epsl.2004.05.035openalex-snapshot
Opal sedimentation shifts in the World Ocean over the last 15 Myr
inferredcites →https://doi.org/10.1016/j.epsl.2010.02.005openalex-snapshot
Deep ocean nutrients during the Last Glacial Maximum deduced from sponge silicon isotopic compositions
inferredcites →https://doi.org/10.1016/j.gca.2011.12.010openalex-snapshot
The relationship between silicon isotope fractionation in sponges and silicic acid concentration: Modern and core-top studies of biogenic opal
inferredcites →https://doi.org/10.1016/j.gca.2012.08.002openalex-snapshot
Diatom silicon isotopes as a proxy for silicic acid utilisation: A Southern Ocean core top calibration
inferredcites →https://doi.org/10.1016/j.gca.2012.09.038openalex-snapshot
Factors controlling the silicon isotope distribution in waters and surface sediments of the Peruvian coastal upwelling
inferredcites →https://doi.org/10.1016/j.gca.2012.10.057openalex-snapshot
Species-dependent silicon isotope fractionation by marine diatoms
inferredcites →https://doi.org/10.1016/j.marchem.2006.04.006openalex-snapshot
Silicon isotopes in spring Southern Ocean diatoms: Large zonal changes despite homogeneity among size fractions
inferredcites →https://doi.org/10.1016/j.marchem.2010.08.005openalex-snapshot
Isotopic constraints on the Si-biogeochemical cycle of the Antarctic Zone in the Kerguelen area (KEOPS)
inferredcites →https://doi.org/10.1016/j.margeo.2004.11.016openalex-snapshot
Sensitivity of silicon isotopes to whole-ocean changes in the silica cycle
inferredcites →https://doi.org/10.1016/j.palaeo.2004.06.018openalex-snapshot
Regional differences in pelagic productivity in the late Eocene to early Oligocene—a comparison of southern high latitudes and lower latitudes
inferredcites →https://doi.org/10.1016/s0016-7037(97)00300-1openalex-snapshot
Fractionation of silicon isotopes by marine diatoms during biogenic silica formation
inferredcites →https://doi.org/10.1016/s0031-0182(98)00093-5openalex-snapshot
Latest Eocene–Early Oligocene climate change and Southern Ocean fertility: inferences from sediment accumulation and stable isotope data
inferredcites →https://doi.org/10.1016/s0304-4203(99)00037-7openalex-snapshot
Determination of the Zn/Si ratio in diatom opal: a method for the separation, cleaning and dissolution of diatoms
inferredcites →https://doi.org/10.1016/s0921-8181(00)00052-7openalex-snapshot
A review of the Si cycle in the modern ocean: recent progress and missing gaps in the application of biogenic opal as a paleoproductivity proxy
inferredcites →https://doi.org/10.1016/s0967-0645(01)00089-3openalex-snapshot
Upper ocean export of particulate organic carbon and biogenic silica in the Southern Ocean along 170°W
inferredcites →https://doi.org/10.1016/s1434-4610(99)70006-4openalex-snapshot
Diatoms and the Ocean Carbon Cycle
inferredcites →https://doi.org/10.1017/s0954102004002202openalex-snapshot
Changing Southern Ocean palaeocirculation and effects on global climate
inferredcites →https://doi.org/10.1017/s0954102010000593openalex-snapshot
Silicon isotopes in Antarctic sponges: an interlaboratory comparison
inferredcites →https://doi.org/10.1023/b:jopl.0000021854.70714.6bopenalex-snapshot
Cleaning of lake sediment samples for diatom oxygen isotope analysis
inferredcites →https://doi.org/10.1029/2003gb002140openalex-snapshot
Biological fractionation of silicon isotopes in Southern Ocean surface waters
inferredcites →https://doi.org/10.1029/2004pa001022openalex-snapshot
Timing and nature of the deepening of the Tasmanian Gateway
inferredcites →https://doi.org/10.1029/2004pa001043openalex-snapshot
Middle Eocene to early Oligocene paleoceanography from Agulhas Ridge, Southern Ocean (Ocean Drilling Program Leg 177, Site 1090)
inferredcites →https://doi.org/10.1029/2005gc001224openalex-snapshot
Drake Passage and Cenozoic climate: An open and shut case?
inferredcites →https://doi.org/10.1029/2005gl023021openalex-snapshot
The Antarctic Circumpolar Productivity Belt
inferredcites →https://doi.org/10.1029/2007pa001576openalex-snapshot
Opal (Zn/Si) ratios as a nearshore geochemical proxy in coastal Antarctica
inferredcites →https://doi.org/10.1029/2008gm000845openalex-snapshot
Glacial-interglacial variability in atmospheric CO2
inferredcites →https://doi.org/10.1029/2008pa001683openalex-snapshot
Ocean overturning since the Late Cretaceous: Inferences from a new benthic foraminiferal isotope compilation
inferredcites →https://doi.org/10.1029/2010gb003856openalex-snapshot
Causes and biogeochemical implications of regional differences in silicification of marine diatoms
inferredcites →https://doi.org/10.1029/2010pa001950openalex-snapshot
Deep water temperature, carbonate ion, and ice volume changes across the Eocene‐Oligocene climate transition
inferredcites →https://doi.org/10.1029/2011gb004099openalex-snapshot
Global patterns in efficiency of particulate organic carbon export and transfer to the deep ocean
inferredcites →https://doi.org/10.1029/2011pa002143openalex-snapshot
Effect of the deepening of the Tasman Gateway on the global ocean
inferredcites →https://doi.org/10.1029/94jb03098openalex-snapshot
Revised calibration of the geomagnetic polarity timescale for the Late Cretaceous and Cenozoic
inferredcites →https://doi.org/10.1029/94pa03060openalex-snapshot
Late Pleistocene oxygen isotope records of biogenic silica from the Atlantic sector of the Southern Ocean
inferredcites →https://doi.org/10.1029/95gb01070openalex-snapshot
Production and dissolution of biogenic silica in the ocean: Revised global estimates, comparison with regional data and relationship to biogenic sedimentation
inferredcites →https://doi.org/10.1029/97gb03366openalex-snapshot
The decoupling of production and particulate export in the surface ocean
inferredcites →https://doi.org/10.1038/nature01290openalex-snapshot
Rapid Cenozoic glaciation of Antarctica induced by declining atmospheric CO2
inferredcites →https://doi.org/10.1038/nature02127openalex-snapshot
High-latitude controls of thermocline nutrients and low latitude biological productivity
inferredcites →https://doi.org/10.1038/nature02131openalex-snapshot
The long-term carbon cycle, fossil fuels and atmospheric composition
inferredcites →https://doi.org/10.1038/nature03135openalex-snapshot
Rapid stepwise onset of Antarctic glaciation and deeper calcite compensation in the Pacific Ocean
inferredcites →https://doi.org/10.1038/nature04883openalex-snapshot
The Southern Ocean biogeochemical divide
inferredcites →https://doi.org/10.1038/nature07435openalex-snapshot
Diversity dynamics of marine planktonic diatoms across the Cenozoic
inferredcites →https://doi.org/10.1038/nature11360openalex-snapshot
A Cenozoic record of the equatorial Pacific carbonate compensation depth
inferredcites →https://doi.org/10.1038/nprot.2008.200openalex-snapshot
Separation of sedimentary micron-sized particles for palaeoceanography and calcareous nannoplankton biogeochemistry
inferredcites →https://doi.org/10.1039/b616755aopenalex-snapshot
An inter-laboratory comparison of Si isotope reference materials
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.1120044openalex-snapshot
Timing and Climatic Consequences of the Opening of Drake Passage
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.268.5209.375openalex-snapshot
The Silica Balance in the World Ocean: A Reestimate
inferredcites →https://doi.org/10.1126/science.281.5374.200openalex-snapshot
Biogeochemical Controls and Feedbacks on Ocean Primary Production
inferredcites →https://doi.org/10.1130/0016-7606(2003)115<0607:etmmba>2.0.co;2openalex-snapshot
Eocene to Miocene magnetostratigraphy, biostratigraphy, and chemostratigraphy at ODP Site 1090 (sub-Antarctic South Atlantic)
inferredcites →https://doi.org/10.1130/0091-7613(2003)031<0423:sifbms>2.0.co;2openalex-snapshot
Silicon isotope fractionation by marine sponges and the reconstruction of the silicon isotope composition of ancient deep water
inferredcites →https://doi.org/10.1130/b25541.1openalex-snapshot
Eocene-Oligocene magnetobiochronology of ODP Sites 689 and 690, Maud Rise, Weddell Sea, Antarctica
inferredcites →https://doi.org/10.1130/g24584a.1openalex-snapshot
Cooling and ice growth across the Eocene-Oligocene transition
inferredcites →https://doi.org/10.1175/1520-0485(1992)022<0093:rowmfi>2.0.co;2openalex-snapshot
Rates of Water Mass Formation in the North Atlantic Ocean
inferredcites →https://doi.org/10.1175/1520-0485(2000)030<3212:tddc>2.0.co;2openalex-snapshot
The Diabatic Deacon Cell*
inferredcites →https://doi.org/10.2307/3514743openalex-snapshot
Secular change in chert distribution; a reflection of evolving biological participation in the silica cycle
inferredcites →https://doi.org/10.2973/odp.proc.sr.113.182.1990openalex-snapshot
Cenozoic Magnetostratigraphy of Leg 113 Drill Sites|Maud Rise|Weddell Sea|Antarctica
inferredcites →https://doi.org/10.3354/meps274123openalex-snapshot
Historical climate change and ocean turbulence as selective agents for two key phytoplankton functional groups
inferredcites →https://doi.org/10.5194/bg-9-2443-2012openalex-snapshot
Processes controlling the Si-isotopic composition in the Southern Ocean and application for paleoceanography
inferredcites →https://doi.org/10.5194/os-7-533-2011openalex-snapshot
Silicon pool dynamics and biogenic silica export in the Southern Ocean inferred from Si-isotopes
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.4679510openalex-extracted
The Rise of Biogenic Silicon Cycling and Microbial Silicification Promoted Mesoproterozoic Chert Deposition
inferred← citeshttps://doi.org/10.1002/2013pa002518openalex-snapshot
Middle Eocene to Late Oligocene Antarctic glaciation/deglaciation and Southern Ocean productivity
inferred← citeshttps://doi.org/10.1002/2013rg000440openalex-snapshot
Cenozoic climate changes: A review based on time series analysis of marine benthic δ18O records
inferred← citeshttps://doi.org/10.1002/2014pa002656openalex-snapshot
Equatorial Pacific productivity changes near the Eocene‐Oligocene boundary
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/10.1002/2015pa002793openalex-snapshot
The silicon isotope composition of Ethmodiscus rex laminated diatom mats from the tropical West Pacific: Implications for silicate cycling during the Last Glacial Maximum
inferred← citeshttps://doi.org/10.1002/2016rg000531openalex-snapshot
A revised budget for Cenozoic sedimentary carbon subduction
inferred← citeshttps://doi.org/10.1002/2017gc006826openalex-snapshot
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/10.1002/2017pa003090openalex-snapshot
Enrichment of dissolved silica in the deep equatorial Pacific during the Eocene‐Oligocene
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/essoar.10504265.1openalex-snapshot
Assessment of C, N and Si isotope tracers associated to past ocean productivity
inferred← citeshttps://doi.org/10.1007/s10533-013-9944-zopenalex-snapshot
Lack of steady-state in the global biogeochemical Si cycle: emerging evidence from lake Si sequestration
inferred← citeshttps://doi.org/10.1007/s11430-023-1335-8openalex-snapshot
Vegetation changes across the Eocene-Oligocene transition: Global signals vs. regional development
inferred← citeshttps://doi.org/10.1016/b978-0-323-99762-1.00039-5openalex-snapshot
Tools to trace past productivity and ocean nutrients
inferred← citeshttps://doi.org/10.1016/j.chemgeo.2013.06.025openalex-snapshot
The zinc isotopic composition of siliceous marine sponges: Investigating nature's sediment traps
inferred← citeshttps://doi.org/10.1016/j.chemgeo.2016.01.020openalex-snapshot
The continental Si cycle and its impact on the ocean Si isotope budget
inferred← citeshttps://doi.org/10.1016/j.chemgeo.2021.120171openalex-snapshot
Drake Passage gateway opening and Antarctic Circumpolar Current onset 31 Ma ago: The message of foraminifera and reconsideration of the Neodymium isotope record
inferred← citeshttps://doi.org/10.1016/j.chemgeo.2021.120201openalex-snapshot
Pelagic clays as archives of marine iron isotope chemistry
inferred← citeshttps://doi.org/10.1016/j.earscirev.2020.103403openalex-snapshot
Evolution of deep-sea sediments across the Paleocene-Eocene and Eocene-Oligocene boundaries
inferred← citeshttps://doi.org/10.1016/j.epsl.2014.10.036openalex-snapshot
Refining our estimate of atmospheric CO 2 across the Eocene–Oligocene climatic transition
inferred← citeshttps://doi.org/10.1016/j.epsl.2016.08.006openalex-snapshot
A silicon depleted North Atlantic since the Palaeogene: Evidence from sponge and radiolarian silicon isotopes
inferred← citeshttps://doi.org/10.1016/j.gloplacha.2014.03.011openalex-snapshot
Emplacement of Antarctic ice sheet mass affects circumpolar ocean flow
inferred← citeshttps://doi.org/10.1016/j.gloplacha.2018.05.012openalex-snapshot
The Eocene–Oligocene transition in the C-isotope record of the carbonate successions in the Central Mediterranean
inferred← citeshttps://doi.org/10.1016/j.gloplacha.2021.103581openalex-snapshot
Eocene-Oligocene paleoenvironmental changes in the South Orkney Microcontinent (Antarctica) linked to the opening of Powell Basin
inferred← citeshttps://doi.org/10.1016/j.gloplacha.2026.105374openalex-snapshot
Glaucony formation during warm phases of Earth history: Lessons learnt from Upper Cretaceous greensand giants
inferred← citeshttps://doi.org/10.1016/j.margeo.2020.106168openalex-snapshot
Rethinking the chronology of early Paleogene sediments in the western North Atlantic using diatom biostratigraphy
inferred← citeshttps://doi.org/10.1016/j.marmicro.2024.102435openalex-snapshot
Morphometric analysis of coccolithophore genus Reticulofenestra: Insights into taxonomy and evolution during late Eocene to early Oligocene
inferred← citeshttps://doi.org/10.1016/j.marmicro.2025.102452openalex-snapshot
Phyletic evolution of calcareous nannofossil species Reticulofenestra oamaruensis: An example of microevolution preserved at IODP Site U1553 (Southern Pacific Ocean)
inferred← citeshttps://doi.org/10.1016/j.palaeo.2015.01.015openalex-snapshot
Paleoceanographic, and paleoclimatic constraints on the global Eocene diatom and silicoflagellate record
inferred← citeshttps://doi.org/10.1016/j.palaeo.2020.109896openalex-snapshot
Early Paleogene biosiliceous sedimentation in the Atlantic Ocean: Testing the inorganic origin hypothesis for Paleocene and Eocene chert and porcellanite
inferred← citeshttps://doi.org/10.1016/j.palaeo.2023.111971openalex-snapshot
Biogenic silica accumulation and diatom assemblage variations through the Eocene-Oligocene Transition: A Southern Indian Ocean versus South Atlantic perspective
inferred← citeshttps://doi.org/10.1016/j.palaeo.2024.112405openalex-snapshot
The rise of biogenic silicon cycling and microbial silicification promoted Mesoproterozoic chert deposition
inferred← citeshttps://doi.org/10.1016/j.palaeo.2025.113164openalex-snapshot
Opening of South China Sea in the Western Pacific forcing the climate cooling and lake level rise at Eocene–Oligocene transition
inferred← citeshttps://doi.org/10.1016/j.quascirev.2019.02.017openalex-snapshot
Silicon isotopic systematics of deep-sea sponge grounds in the North Atlantic
inferred← citeshttps://doi.org/10.1017/pab.2023.20openalex-snapshot
Inferred nutrient forcing on the late middle Eocene to early Oligocene (~40–31 Ma) evolution of the coccolithophore Reticulofenestra (order Isochrysidales)
inferred← citeshttps://doi.org/10.1029/2019pa003597openalex-snapshot
Low‐Latitude Calcareous Nannofossil Response in the Indo‐Pacific Warm Pool Across the Eocene‐Oligocene Transition of Java, Indonesia
inferred← citeshttps://doi.org/10.1029/2020gb006775openalex-snapshot
Assessment of C, N, and Si Isotopes as Tracers of Past Ocean Nutrient and Carbon Cycling
inferred← citeshttps://doi.org/10.1029/2020pa004168openalex-snapshot
Middle to Late Eocene Changes of the Ocean Carbonate Cycle
inferred← citeshttps://doi.org/10.1029/2021pa004298openalex-snapshot
Middle Miocene (∼14 Ma) and Late Miocene (∼6 Ma) Paleogeographic Boundary Conditions
inferred← citeshttps://doi.org/10.1029/2022gc010746openalex-snapshot
High‐Resolution Coccolithophore Morphological Changes in Response to Orbital Forcings During the Early Oligocene
inferred← citeshttps://doi.org/10.1029/2024pa004965openalex-snapshot
Eocene Shark Teeth From Peninsular Antarctica: Windows to Habitat Use and Paleoceanography
inferred← citeshttps://doi.org/10.1038/s41467-017-00853-5openalex-snapshot
Cenozoic global cooling and increased seawater Mg/Ca via reduced reverse weathering
inferred← citeshttps://doi.org/10.1038/s41467-022-34623-9openalex-snapshot
Southern Ocean biogenic blooms freezing-in Oligocene colder climates
inferred← citeshttps://doi.org/10.1038/s41561-020-0540-2openalex-snapshot
No state change in pelagic fish production and biodiversity during the Eocene–Oligocene transition
inferred← citeshttps://doi.org/10.1038/s41598-019-46253-1openalex-snapshot
Late Eocene onset of the Proto-Antarctic Circumpolar Current
inferred← citeshttps://doi.org/10.1051/bsgf/2020028openalex-snapshot
Thai amber: insights into early diatom history?
inferred← citeshttps://doi.org/10.1073/pnas.1608100113openalex-snapshot
Equatorial heat accumulation as a long-term trigger of permanent Antarctic ice sheets during the Cenozoic
inferred← citeshttps://doi.org/10.1073/pnas.2103517118openalex-snapshot
Revisiting the sedimentary record of the rise of diatoms
inferred← citeshttps://doi.org/10.1073/pnas.2424082123openalex-snapshot
High-latitude teleconnections drive subtropical marine bioproductivity at the dawn of the Antarctic ice sheet
inferred← citeshttps://doi.org/10.1080/0269249x.2017.1395366openalex-snapshot
Typification of Eocene–Oligocene diatom taxa proposed by Grove & Sturt (1886–1887) from the Oamaru Diatomite
inferred← citeshttps://doi.org/10.1080/10420940.2026.2699670openalex-snapshot
Ichnofabric analysis of deep-ocean sediment cores from the South Atlantic ocean: Eocene–Oligocene transition (IODP expeditions 390 and 393)
inferred← citeshttps://doi.org/10.1093/jxb/erw163openalex-snapshot
Large variation in the Rubisco kinetics of diatoms reveals diversity among their carbon-concentrating mechanisms
inferred← citeshttps://doi.org/10.1093/jxb/erx130openalex-snapshot
The potential for co-evolution of CO2-concentrating mechanisms and Rubisco in diatoms
inferred← citeshttps://doi.org/10.1111/gbi.12442openalex-snapshot
The influence of elevated SiO2(aq) on intracellular silica uptake and microbial metabolism
inferred← citeshttps://doi.org/10.1111/gbi.12449openalex-snapshot
Isotopic analyses of Ordovician–Silurian siliceous skeletons indicate silica‐depleted Paleozoic oceans
inferred← citeshttps://doi.org/10.1111/pala.12615openalex-snapshot
Diversity dynamics of microfossils from the Cretaceous to the Neogene show mixed responses to events
inferred← citeshttps://doi.org/10.1127/nos/2022/0725openalex-snapshot
Calcareous nannofossils across the Eocene-Oligocene transition at Site 756 (Ninetyeast Ridge, Indian Ocean): implications for biostratigraphy and paleoceanographic clues
inferred← citeshttps://doi.org/10.1127/pip/2016/0050openalex-snapshot
The geological story of marine diatoms and the last generation of fossil fuels
inferred← citeshttps://doi.org/10.1130/g52016.1openalex-snapshot
Bacterial magnetofossil evidence for enhanced Pacific Ocean respired carbon storage during buildup of Antarctic glaciation
inferred← citeshttps://doi.org/10.1144/sp483.1openalex-snapshot
A history of the Asian monsoon and its interactions with solid Earth tectonics in Cenozoic South Asia
inferred← citeshttps://doi.org/10.1144/sp523-2021-54openalex-snapshot
The opening and closure of oceanic seaways during the Cenozoic: pacemaker of global climate change?
inferred← citeshttps://doi.org/10.1360/csb-2025-0232openalex-snapshot
Global climate and vegetation changes during the Eocene-Oligocene Transition: a review of recent progress
inferred← citeshttps://doi.org/10.1371/journal.pone.0084857openalex-snapshot
Cenozoic Planktonic Marine Diatom Diversity and Correlation to Climate Change
inferred← citeshttps://doi.org/10.2138/gselements.14.6.397openalex-snapshot
Discovering the Ocean’s Past through Geochemistry
inferred← citeshttps://doi.org/10.3389/feart.2017.00112openalex-snapshot
A Review of the Stable Isotope Bio-geochemistry of the Global Silicon Cycle and Its Associated Trace Elements
inferred← citeshttps://doi.org/10.3389/fmars.2017.00397openalex-snapshot
Biosilicification Drives a Decline of Dissolved Si in the Oceans through Geologic Time
inferred← citeshttps://doi.org/10.3389/fmars.2018.00022openalex-snapshot
Competition between Silicifiers and Non-silicifiers in the Past and Present Ocean and Its Evolutionary Impacts
inferred← citeshttps://doi.org/10.3410/f.726323376.793537797openalex-snapshot
Faculty Opinions recommendation of Large variation in the Rubisco kinetics of diatoms reveals diversity among their carbon-concentrating mechanisms.
inferred← citeshttps://doi.org/10.5194/bg-13-6003-2016openalex-snapshot
Quantifying the Cenozoic marine diatom deposition history: links to the C and Si cycles
inferred← citeshttps://doi.org/10.5194/cp-17-1937-2021openalex-snapshot
North Atlantic marine biogenic silica accumulation through the early to middle Paleogene: implications for ocean circulation and silicate weathering feedback
inferred← citeshttps://doi.org/10.5194/cp-20-1327-2024openalex-snapshot
Late Eocene to early Oligocene productivity events in the proto-Southern Ocean and correlation to climate change
inferred← citeshttps://doi.org/10.5194/cp-21-2283-2025openalex-snapshot
Increasing opal productivity in the Late Eocene Southern Ocean: Evidence for increased carbon export preceding the Eocene-Oligocene glaciation
inferred← citeshttps://doi.org/10.5194/jm-44-601-2025openalex-snapshot
Low-latitude biostratigraphy and diversity of planktonic foraminifera from the middle Eocene to early Oligocene
inferred← citeshttps://doi.org/10.5194/jm-45-177-2026openalex-snapshot
Unraveling Southern Ocean diatom diversity across the Eocene–Oligocene transition
inferred← citeshttps://doi.org/10.70675/02b65afcz2215z4790z828az541ccc06579copenalex-snapshot
Impact de la transition climatique Eocène - Oligocène sur les écosystèmes continentaux : Etude du bassin de Rennes
inferred← citeshttps://doi.org/10.70675/5b187077ze3cbz44b5z9c3cze36b865c23c5openalex-snapshot
Impacts de l'ouverture du Passage de Drake, des changements de pCO2 et de l'englacement de l'Antarctique sur l'évolution du climat et de l'océan global de l'Eocène à l'Oligocène
inferred← citeshttps://doi.org/10.70675/c22589f9z8476z44e9z83e6za83e1df6472eopenalex-snapshot
Rôle de la biodiversité des diatomées dans la modulation des flux biogéochimiques du carbone et du silicium dans les milieux polaires
inferred← citeshttps://doi.org/10.70675/c6900fa3zf792z4b7fzb3beze6ecc0e3849fopenalex-snapshot
Contraindre la transition greenhouse-icehouse du Paléogène par la géochimie des coccolithes
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