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Evolution of the stable carbon isotope composition of atmospheric CO2 over the last glacial cycle
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Outgoing claims: the papers this work cites, builds on, or argues with.
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The Southern Glacial Maximum 65,000 years ago and its Unfinished Termination
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inferredcites →https://doi.org/10.1038/nature14059openalex-snapshot
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inferredcites →https://doi.org/10.1038/nature14155openalex-snapshot
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inferredcites →https://doi.org/10.1038/nature14330openalex-snapshot
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inferredcites →https://doi.org/10.1038/nature14401openalex-snapshot
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inferredcites →https://doi.org/10.1038/nature16514openalex-snapshot
Covariation of deep Southern Ocean oxygenation and atmospheric CO2 through the last ice age
inferredcites →https://doi.org/10.1038/ngeo1026openalex-snapshot
Expression of the bipolar see-saw in Antarctic climate records during the last deglaciation
inferredcites →https://doi.org/10.1038/ngeo442openalex-snapshot
Glacial terminations as southern warmings without northern control
inferredcites →https://doi.org/10.1073/pnas.1104772108openalex-snapshot
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inferredcites →https://doi.org/10.1073/pnas.1204069109openalex-snapshot
Mode change of millennial CO 2 variability during the last glacial cycle associated with a bipolar marine carbon seesaw
inferredcites →https://doi.org/10.1073/pnas.1323922111openalex-snapshot
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inferredcites →https://doi.org/10.1098/rsta.2013.0054openalex-snapshot
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inferredcites →https://doi.org/10.1111/j.1600-0889.2005.00167.xopenalex-snapshot
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inferredcites →https://doi.org/10.1126/science.1064618openalex-snapshot
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inferredcites →https://doi.org/10.1126/science.1141038openalex-snapshot
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inferredcites →https://doi.org/10.1126/science.1160832openalex-snapshot
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inferredcites →https://doi.org/10.1126/science.1167441openalex-snapshot
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inferredcites →https://doi.org/10.1126/science.1169473openalex-snapshot
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inferredcites →https://doi.org/10.1126/science.1178068openalex-snapshot
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inferredcites →https://doi.org/10.1126/science.1183627openalex-snapshot
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inferredcites →https://doi.org/10.1126/science.1217161openalex-snapshot
Carbon Isotope Constraints on the Deglacial CO 2 Rise from Ice Cores
inferredcites →https://doi.org/10.1126/science.1227545openalex-snapshot
Two Modes of Change in Southern Ocean Productivity Over the Past Million Years
inferredcites →https://doi.org/10.1126/science.1246848openalex-snapshot
Iron Fertilization of the Subantarctic Ocean During the Last Ice Age
inferredcites →https://doi.org/10.1126/science.1262005openalex-snapshot
Enhanced tropical methane production in response to iceberg discharge in the North Atlantic
inferredcites →https://doi.org/10.1126/science.242.4886.1675openalex-snapshot
Gravitational Separation of Gases and Isotopes in Polar Ice Caps
inferredcites →https://doi.org/10.1126/science.290.5498.1947openalex-snapshot
Rapid Changes in the Hydrologic Cycle of the Tropical Atlantic During the Last Glacial
inferredcites →https://doi.org/10.1126/science.291.5501.109openalex-snapshot
Timing of Millennial-Scale Climate Change in Antarctica and Greenland During the Last Glacial Period
inferredcites →https://doi.org/10.1126/science.291.5501.112openalex-snapshot
Atmospheric CO 2 Concentrations over the Last Glacial Termination
inferredcites →https://doi.org/10.3189/172756500781833359openalex-snapshot
Reconstructing past atmospheric CO2 concentration based on ice-core analyses: open questions due to in situ production of CO2 in the ice
inferredcites →https://doi.org/10.3189/2014aog68a023openalex-snapshot
A review of the brittle ice zone in polar ice cores
inferredcites →https://doi.org/10.5194/amt-4-1445-2011openalex-snapshot
A sublimation technique for high-precision measurements of δ 13 CO 2 and mixing ratios of CO 2 and N 2 O from air trapped in ice cores
inferredcites →https://doi.org/10.5194/cp-10-903-2014openalex-snapshot
NGRIP CH 4 concentration from 120 to 10 kyr before present and its relation to a δ 15 N temperature reconstruction from the same ice core
inferredcites →https://doi.org/10.5194/cp-11-153-2015openalex-snapshot
The WAIS Divide deep ice core WD2014 chronology – Part 1: Methane synchronization (68–31 ka BP) and the gas age–ice age difference
inferredcites →https://doi.org/10.5194/cp-2-57-2006openalex-snapshot
Simulating low frequency changes in atmospheric CO 2 during the last 740 000 years
inferredcites →https://doi.org/10.5194/cp-6-645-2010openalex-snapshot
A synthesis of marine sediment core δ 13 C data over the last 150 000 years
inferredcites →https://doi.org/10.5194/cp-7-1-2011openalex-snapshot
TALDICE-1 age scale of the Talos Dome deep ice core, East Antarctica
inferredcites →https://doi.org/10.5194/cp-7-319-2011openalex-snapshot
Fingerprints of changes in the terrestrial carbon cycle in response to large reorganizations in ocean circulation
inferredcites →https://doi.org/10.5194/cp-8-589-2012openalex-snapshot
Systematic study of the impact of fresh water fluxes on the glacial carbon cycle
inferredcites →https://doi.org/10.5194/cp-8-609-2012openalex-snapshot
Centennial mineral dust variability in high-resolution ice core data from Dome C, Antarctica
inferredcites →https://doi.org/10.5194/cp-9-1715-2013openalex-snapshot
An optimized multi-proxy, multi-site Antarctic ice and gas orbital chronology (AICC2012): 120–800 ka
inferredcites →https://doi.org/10.5194/cp-9-1733-2013openalex-snapshot
The Antarctic ice core chronology (AICC2012): an optimized multi-parameter and multi-site dating approach for the last 120 thousand years
inferredcites →https://doi.org/10.5194/cp-9-2507-2013openalex-snapshot
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inferredcites →https://doi.org/10.5194/cp-9-2789-2013openalex-snapshot
High-resolution mineral dust and sea ice proxy records from the Talos Dome ice core
What points at this work
Incoming claims: where this work appears in other papers’ reference lists and arguments.
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inferred← citeshttps://doi.org/10.1017/qua.2024.41openalex-snapshot
Pedogenic carbonate as a transient soil component in a humid, temperate forest (Michigan, USA)
inferred← citeshttps://doi.org/10.1017/s0954102024000075openalex-snapshot
Palaeo-environmental significance of evaporative calcite crusts in the Untersee Oasis, East Antarctica
inferred← citeshttps://doi.org/10.1029/2018gl077881openalex-snapshot
Controls on Millennial‐Scale Atmospheric CO2 Variability During the Last Glacial Period
inferred← citeshttps://doi.org/10.1029/2020gl089110openalex-snapshot
Millennial‐Scale Changes in Terrestrial and Marine Nitrous Oxide Emissions at the Onset and Termination of Marine Isotope Stage 4
inferred← citeshttps://doi.org/10.1029/2020pa003876openalex-snapshot
Constraining Millennial‐Scale Changes in Northern Component Water Ventilation in the Western Tropical South Atlantic
inferred← citeshttps://doi.org/10.1029/2021pa004314openalex-snapshot
Toward Reconciling Radiocarbon Production Rates With Carbon Cycle Changes of the Last 55,000 Years
inferred← citeshttps://doi.org/10.1029/2021pa004386openalex-snapshot
The Origin of Tree‐Ring Reconstructed Summer Cooling in Northern Europe During the 18th Century Eruption of Laki
inferred← citeshttps://doi.org/10.1029/2022pa004577openalex-snapshot
Carbon Cycle Responses to Changes in Weathering and the Long‐Term Fate of Stable Carbon Isotopes
inferred← citeshttps://doi.org/10.1029/2023pa004629openalex-snapshot
Multi‐Proxy Evidence for Atlantic Meridional Overturning Circulation (AMOC) Weakening During Deglaciations of the Past 150,000 Years
inferred← citeshttps://doi.org/10.1029/2023pa004635openalex-snapshot
Brazil Margin Stable Isotope Profiles for the Last Glacial Cycle: Implications for Watermass Geometry and Oceanic Carbon Storage
inferred← citeshttps://doi.org/10.1029/2023pa004775openalex-snapshot
Ocean Oxygen, Preformed Nutrients, and the Cause of the Lower Carbon Dioxide Concentration in the Atmosphere of the Last Glacial Maximum
inferred← citeshttps://doi.org/10.1029/2023pa004777openalex-snapshot
Constraining Plio‐Pleistocene Shifts in Northwest African Hydroclimate, Ecosystem Distributions, and Marine Productivity: New Paleo‐Records Across the Mid‐Pleistocene Transition
inferred← citeshttps://doi.org/10.1029/2024gb008287openalex-snapshot
Glacial‐Interglacial and Millennial‐Scale Changes in Nitrous Oxide Emissions Pathways and Source Regions
inferred← citeshttps://doi.org/10.1029/2024gc011489openalex-snapshot
Snapshots of Coastal Ecology Using Multiproxy Analysis Reveals Insights Into the Preservation of Swamp and Marsh Environments Since the Late Pleistocene
inferred← citeshttps://doi.org/10.1029/2025gc012660openalex-snapshot
Springtime Formation of Laminated Soil Carbonate Rinds and Changes in Fluvial Terrace Soils on Orbital Timescales at Rio Mesa, Utah, USA
inferred← citeshttps://doi.org/10.1029/2025gl118490openalex-snapshot
Oceanic δ 13 C Fingerprints Caused by Laurentice Ice Sheet Discharges: Model‐Data Comparison During Heinrich Event 4
inferred← citeshttps://doi.org/10.1029/2025jd045900openalex-snapshot
Triple Isotopes of Oxygen as a Proxy for Carbon Dioxide in Altered Early Pleistocene Ice Core Samples
inferred← citeshttps://doi.org/10.1029/2025pa005357openalex-snapshot
Plant Wax Isotopic Reconstructions Reveal Thermodynamic Drivers of Hydroclimate Over the Last Two Glacial Cycles at Great Salt Lake and Bear Lake, Utah
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/10.1038/s41467-017-02691-xopenalex-snapshot
Atmospheric CO2 effect on stable carbon isotope composition of terrestrial fossil archives
inferred← citeshttps://doi.org/10.1038/s41467-018-05574-xopenalex-snapshot
An atmospheric chronology for the glacial-deglacial Eastern Equatorial Pacific
inferred← citeshttps://doi.org/10.1038/s41467-020-15739-2openalex-snapshot
Exceptionally high biosphere productivity at the beginning of Marine Isotopic Stage 11
inferred← citeshttps://doi.org/10.1038/s41467-022-31120-xopenalex-snapshot
Pleistocene drivers of Northwest African hydroclimate and vegetation
inferred← citeshttps://doi.org/10.1038/s41467-022-33166-3openalex-snapshot
Multiple carbon cycle mechanisms associated with the glaciation of Marine Isotope Stage 4
inferred← citeshttps://doi.org/10.1038/s41467-024-52360-zopenalex-snapshot
Carbon isotope budget indicates biological disequilibrium dominated ocean carbon storage at the Last Glacial Maximum
inferred← citeshttps://doi.org/10.1038/s41467-024-55184-zopenalex-snapshot
Asynchronicity of deglacial permafrost thawing controlled by millennial-scale climate variability
inferred← citeshttps://doi.org/10.1038/s41561-020-00680-2openalex-snapshot
Abrupt changes in the global carbon cycle during the last glacial period
inferred← citeshttps://doi.org/10.1038/s41586-019-1692-3openalex-snapshot
Two-million-year-old snapshots of atmospheric gases from Antarctic ice
inferred← citeshttps://doi.org/10.1038/s41586-025-10032-yopenalex-snapshot
Broadly stable atmospheric CO2 and CH4 levels over the past 3 million years
inferred← citeshttps://doi.org/10.1038/s41598-020-69116-6openalex-snapshot
Sources of solutes and carbon cycling in perennially ice-covered Lake Untersee, Antarctica
inferred← citeshttps://doi.org/10.1038/s41598-021-90795-2openalex-snapshot
Multi-isotope evidence of population aggregation in the Natufian and scant migration during the early Neolithic of the Southern Levant
inferred← citeshttps://doi.org/10.1038/s41598-024-69056-5openalex-snapshot
Contextualizing wild cereal harvesting at Middle Palaeolithic Ghar-e Boof in the southern Zagros
inferred← citeshttps://doi.org/10.1038/s43247-021-00280-xopenalex-snapshot
Glacial lake outburst floods enhance benthic microbial productivity in perennially ice-covered Lake Untersee (East Antarctica)
inferred← citeshttps://doi.org/10.1038/s43247-025-03053-yopenalex-snapshot
Persistent El Niño-like conditions over the western Pacific during the Bølling–Allerød interstadial
inferred← citeshttps://doi.org/10.1038/s43247-026-03925-xopenalex-snapshot
Long-term ecological stability in the Pleistocene central Levantine corridor revealed by enamel isotopes from Lebanon
inferred← citeshttps://doi.org/10.1073/pnas.1613883114openalex-snapshot
Glacial/interglacial wetland, biomass burning, and geologic methane emissions constrained by dual stable isotopic CH 4 ice core records
inferred← citeshttps://doi.org/10.1073/pnas.1902469117openalex-snapshot
Early Last Interglacial ocean warming drove substantial ice mass loss from Antarctica
inferred← citeshttps://doi.org/10.1073/pnas.2201871119openalex-snapshot
Evidence for massive methane hydrate destabilization during the penultimate interglacial warming
inferred← citeshttps://doi.org/10.1073/pnas.2423057122openalex-snapshot
Multiple sources of atmospheric CO 2 activated by AMOC recovery at the onset of interglacial MIS 9
inferred← citeshttps://doi.org/10.1088/1748-9326/11/12/124016openalex-snapshot
Using the Suess effect on the stable carbon isotope to distinguish the future from the past in radiocarbon
inferred← citeshttps://doi.org/10.1111/bor.12472openalex-snapshot
Palaeoenvironmental conditions during MIS 6/MIS 5 transition recorded in speleothems from the Tatra Mountains
inferred← citeshttps://doi.org/10.1111/nph.17030openalex-snapshot
C3 plant carbon isotope discrimination does not respond to CO2 concentration on decadal to centennial timescales
inferred← citeshttps://doi.org/10.1126/sciadv.adh9513openalex-snapshot
Early sea ice decline off East Antarctica at the last glacial–interglacial climate transition
inferred← citeshttps://doi.org/10.1126/science.aai8464openalex-snapshot
Regional and global sea-surface temperatures during the last interglaciation
inferred← citeshttps://doi.org/10.1126/science.aau2728openalex-snapshot
Plio-Pleistocene decline of African megaherbivores: No evidence for ancient hominin impacts
inferred← citeshttps://doi.org/10.1126/science.aay8178openalex-snapshot
Abrupt CO 2 release to the atmosphere under glacial and early interglacial climate conditions
inferred← citeshttps://doi.org/10.1146/annurev-earth-100821-081832openalex-snapshot
The Isotopic Ecology of the Mammoth Steppe
inferred← citeshttps://doi.org/10.1371/journal.pone.0330032openalex-snapshot
Fluctuations of viti- and oleiculture traditions in the Bronze and Iron Age Levant
inferred← citeshttps://doi.org/10.1594/pangaea.859179openalex-snapshot
2) Compilation of carbon dioxide in the EDML and Talos Dome ice cores
inferred← citeshttps://doi.org/10.1594/pangaea.859180openalex-snapshot
3) Monte Carlo average of stable carbon isotope ratio of atmospheric CO2 from three Antarctic ice cores, 155-0.6 ka BP
inferred← citeshttps://doi.org/10.1594/pangaea.859209openalex-snapshot
1) δ¹³C-CO2 and d15N-N2 isotope ratios in EDC, EDML and Talos Dome ice cores measured by sublimation extraction
inferred← citeshttps://doi.org/10.3319/tao.2017.07.31.01openalex-snapshot
Provenance discrimination of the last glacial sediments from the northeastern South China Sea and its paleoenvironmental indications
inferred← citeshttps://doi.org/10.3389/feart.2023.1154544openalex-snapshot
High-resolution record of stable isotopes in soil carbonates reveals environmental dynamics in an arid region (central Iran) during the last 32 ka
inferred← citeshttps://doi.org/10.3390/bios13060609openalex-snapshot
Raman Spectroscopy for Urea Breath Test
inferred← citeshttps://doi.org/10.3390/sci6040062openalex-snapshot
Comment on Koutsoyiannis, D. Net Isotopic Signature of Atmospheric CO2 Sources and Sinks: No Change Since the Little Ice Age. Sci 2024, 6, 17
inferred← citeshttps://doi.org/10.3390/sci6040063openalex-snapshot
Definite Change Since the Formation of the Earth. Reply to Kleber, A. Comment on “Koutsoyiannis, D. Net Isotopic Signature of Atmospheric CO2 Sources and Sinks: No Change Since the Little Ice Age. Sci 2024, 6, 17”
inferred← citeshttps://doi.org/10.5194/amt-13-6703-2020openalex-snapshot
New technique for high-precision, simultaneous measurements of CH 4 , N 2 O and CO 2 concentrations; isotopic and elemental ratios of N 2 , O 2 and Ar; and total air content in ice cores by wet extraction
inferred← citeshttps://doi.org/10.5194/amt-16-355-2023openalex-snapshot
Laser-induced sublimation extraction for centimeter-resolution multi-species greenhouse gas analysis on ice cores
inferred← citeshttps://doi.org/10.5194/bg-14-2641-2017openalex-snapshot
20th century changes in carbon isotopes and water-use efficiency: tree-ring-based evaluation of the CLM4.5 and LPX-Bern models
inferred← citeshttps://doi.org/10.5194/bg-15-7155-2018openalex-snapshot
Bipolar carbon and hydrogen isotope constraints on the Holocene methane budget
inferred← citeshttps://doi.org/10.5194/bg-15-7205-2018openalex-snapshot
Southern Ocean controls of the vertical marine δ 13 C gradient – a modelling study
inferred← citeshttps://doi.org/10.5194/bg-21-4413-2024openalex-snapshot
Palaeoecology of ungulates in northern Iberia during the Late Pleistocene through isotopic analysis of teeth
inferred← citeshttps://doi.org/10.5194/cp-13-1695-2017openalex-snapshot
Simulation of climate, ice sheets and CO 2 evolution during the last four glacial cycles with an Earth system model of intermediate complexity
inferred← citeshttps://doi.org/10.5194/cp-13-345-2017openalex-snapshot
δ 13 C decreases in the upper western South Atlantic during Heinrich Stadials 3 and 2
inferred← citeshttps://doi.org/10.5194/cp-14-1229-2018openalex-snapshot
Deglacial carbon cycle changes observed in a compilation of 127 benthic δ 13 C time series (20–6 ka)
inferred← citeshttps://doi.org/10.5194/cp-14-1755-2018openalex-snapshot
Connecting the Greenland ice-core and U∕Th timescales via cosmogenic radionuclides: testing the synchroneity of Dansgaard–Oeschger events
inferred← citeshttps://doi.org/10.5194/cp-15-849-2019openalex-snapshot
Low terrestrial carbon storage at the Last Glacial Maximum: constraints from multi-proxy data
inferred← citeshttps://doi.org/10.5194/cp-16-1159-2020openalex-snapshot
Mysteriously high Δ 14 C of the glacial atmosphere: influence of 14 C production and carbon cycle changes
inferred← citeshttps://doi.org/10.5194/cp-16-423-2020openalex-snapshot
Modeling the evolution of pulse-like perturbations in atmospheric carbon and carbon isotopes: the role of weathering–sedimentation imbalances
inferred← citeshttps://doi.org/10.5194/cp-17-1507-2021openalex-snapshot
The atmospheric bridge communicated the δ 13 C decline during the last deglaciation to the global upper ocean
inferred← citeshttps://doi.org/10.5194/cp-17-171-2021openalex-snapshot
Sequential changes in ocean circulation and biological export productivity during the last glacial–interglacial cycle: a model–data study
inferred← citeshttps://doi.org/10.5194/cp-18-1579-2022openalex-snapshot
The role of ice-sheet topography in the Alpine hydro-climate at glacial times
inferred← citeshttps://doi.org/10.5194/cp-19-1559-2023openalex-snapshot
Impact of iron fertilisation on atmospheric CO 2 during the last glaciation
inferred← citeshttps://doi.org/10.5194/cp-20-991-2024openalex-snapshot
No detectable influence of the carbonate ion effect on changes in stable carbon isotope ratios ( δ 13 C) of shallow dwelling planktic foraminifera over the past 160 kyr
inferred← citeshttps://doi.org/10.5194/cp-21-1043-2025openalex-snapshot
Closing the Plio-Pleistocene 13 C cycle in the 405 kyr periodicity by isotopic signatures of geological sources
inferred← citeshttps://doi.org/10.5194/cp-21-571-2025openalex-snapshot
Sediment fluxes dominate glacial–interglacial changes in ocean carbon inventory: results from factorial simulations over the past 780 000 years
inferred← citeshttps://doi.org/10.5194/gmd-16-3501-2023openalex-snapshot
The Earth system model CLIMBER-X v1.0 – Part 2: The global carbon cycle
inferred← citeshttps://doi.org/10.70675/0ea23effzdbc9z4f25z8f98z758aa1f1eac5openalex-snapshot
Coherent dating of deep polar ice cores and implications for understanding climate mechanisms
inferred← citeshttps://doi.org/10.70675/9f3a7c49ze17bz4c96zab17z72a889cc5eeaopenalex-snapshot
Le bois, archive des changements climatiques entre mer et montagne du Paléolithique moyen au Mésolithique : Composition isotopique (13C/12C), reconstitutions paléoclimatiques, histoire des forêts et interactions hommes/milieux
inferred← citeshttps://doi.org/10.70675/d20e68fczfc03z48b1zb23dz3178d8500839openalex-snapshot
Les changements majeurs de la productivité biologique au cours du Quaternaire et leurs impacts sur les cycles du carbone et de l’oxygène
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