| scholarly article | Q13442814 |
| P6179 | Dimensions Publication ID | 1002616529 |
| P356 | DOI | 10.1038/NATURE06950 |
| P698 | PubMed publication ID | 18480822 |
| P5875 | ResearchGate publication ID | 5370385 |
| P50 | author | Valérie Masson-Delmotte | Q3554288 |
| Dominique Raynaud | Q62729125 | ||
| Renato Spahni | Q114415686 | ||
| Thomas F. Stocker | Q15120866 | ||
| Jérôme Chappellaz | Q33105806 | ||
| Thomas Blunier | Q44077609 | ||
| Jean-Marc Barnola | Q52115679 | ||
| P2093 | author name string | Adrian Schilt | |
| Bénédicte Lemieux | |||
| Laetitia Loulergue | |||
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| P433 | issue | 7193 | |
| P407 | language of work or name | English | Q1860 |
| P921 | main subject | methane | Q37129 |
| P304 | page(s) | 383-386 | |
| P577 | publication date | 2008-05-01 | |
| P1433 | published in | Nature | Q180445 |
| P1476 | title | Orbital and millennial-scale features of atmospheric CH4 over the past 800,000 years | |
| P478 | volume | 453 |
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| Q58113865 | A modeling assessment of the interplay between aeolian iron fluxes and iron-binding ligands in controlling carbon dioxide fluctuations during Antarctic warm events |
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| Q59308927 | Acquiring High to Ultra-High Resolution Geological Records of Past Climate Change by Scientific Drilling |
| Q97620910 | An assessment of Earth's climate sensitivity using multiple lines of evidence |
| Q21093487 | An optimized multi-proxy, multi-site Antarctic ice and gas orbital chronology (AICC2012): 120–800 ka |
| Q21128943 | An optimized multi-proxy, multi-site Antarctic ice and gas orbital chronology (AICC2012): 120–800 ka |
| Q57250879 | Analytical constraints on layered gas trapping and smoothing of atmospheric variability in ice under low-accumulation conditions |
| Q56340173 | Antarctic and global climate history viewed from ice cores |
| Q38603076 | Arctic Ocean sea ice cover during the penultimate glacial and the last interglacial. |
| Q42374961 | Arctic cryosphere and Milankovitch forcing of Great Basin paleoclimate |
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| Q58052069 | Atmospheric CH4in the first decade of the 21st century: Inverse modeling analysis using SCIAMACHY satellite retrievals and NOAA surface measurements |
| Q30949666 | Atmospheric composition 1 million years ago from blue ice in the Allan Hills, Antarctica. |
| Q47196516 | Atmospheric science: Ancient ice and the global methane cycle |
| Q58053640 | Atmosphericδ13CO2and its relation topCO2and deep oceanδ13C during the late Pleistocene |
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| Q55298337 | Bayesian Analysis of the Glacial-Interglacial Methane Increase Constrained by Stable Isotopes and Earth System Modeling. |
| Q40848897 | Bipolar seesaw control on last interglacial sea level. |
| Q58265446 | Carbon isotope ratios suggest no additional methane from boreal wetlands during the rapid Greenland Interstadial 21.2 |
| Q58410223 | Causal feedbacks in climate change |
| Q39119547 | Chemical signals of past climate and environment from polar ice cores and firn air. |
| Q28690134 | Climate change and animals in Saudi Arabia |
| Q28744525 | Climate change: the evidence and our options |
| Q28678655 | Climate sensitivity, sea level and atmospheric carbon dioxide |
| Q56100445 | Climates of the Earth and Cryosphere Evolution |
| Q58422092 | Climatic Effect of Antarctic Meltwater Overwhelmed by Concurrent Northern Hemispheric Melt |
| Q58422098 | Collapse of the North American ice saddle 14,500 years ago caused widespread cooling and reduced ocean overturning circulation |
| Q58087586 | Constraint of the CO2rise by new atmospheric carbon isotopic measurements during the last deglaciation |
| Q42615579 | Contrasting wetland CH4 emission responses to simulated glacial atmospheric CO2 in temperate bogs and fens |
| Q58650467 | Controls on the tropospheric oxidizing capacity during an idealized Dansgaard-Oeschger event, and their implications for the rapid rises in atmospheric methane during the last glacial period |
| Q33979481 | Darwin in mind: new opportunities for evolutionary psychology |
| Q58060272 | Deep water formation in the North Pacific and deglacial CO2 rise |
| Q45342876 | Deglacial Tropical Atlantic subsurface warming links ocean circulation variability to the West African Monsoon |
| Q36068381 | Detecting Causality by Combined Use of Multiple Methods: Climate and Brain Examples |
| Q61051166 | Determining the natural length of the current interglacial |
| Q24289401 | EPICA Dome C record of glacial and interglacial intensities |
| Q58385737 | Earth’s Climate System |
| Q33799311 | Effects of solar UV radiation and climate change on biogeochemical cycling: interactions and feedbacks. |
| Q58412807 | Errors in greenhouse forcing and soil carbon sequestration estimates in freshwater wetlands: a comment on Mitsch et al. (2013) |
| Q56100241 | Evaluation of climate models using palaeoclimatic data |
| Q33493282 | Evidence for obliquity forcing of glacial Termination II. |
| Q39351129 | Evolution of global temperature over the past two million years |
| Q58053617 | Evolution of the stable carbon isotope composition of atmospheric CO2over the last glacial cycle |
| Q33829632 | Extended megadroughts in the southwestern United States during Pleistocene interglacials |
| Q57086702 | Forcing of late Pleistocene ice volume by spatially variable summer energy |
| Q55689143 | Glacial Inception in Marine Isotope Stage 19: An Orbital Analog for a Natural Holocene Climate. |
| Q58320814 | Glacial terminations as southern warmings without northern control |
| Q57251490 | Glacial-interglacial water cycle, global monsoon and atmospheric methane changes |
| Q38695401 | Glacial/interglacial wetland, biomass burning, and geologic methane emissions constrained by dual stable isotopic CH4 ice core records |
| Q47323949 | Global change: Methane and monsoons |
| Q47253695 | Greenhouse gases in the Earth system: a palaeoclimate perspective |
| Q28280161 | High-resolution carbon dioxide concentration record 650,000-800,000 years before present |
| Q58058173 | Historical greenhouse gas concentrations for climate modelling (CMIP6) |
| Q28654264 | Holocene variations in peatland methane cycling associated with the Asian summer monsoon system |
| Q39576300 | Hydroclimate changes across the Amazon lowlands over the past 45,000 years |
| Q57556392 | Hydrological variability over the Apennines during the Early Last Glacial precession minimum, as revealed by a stable isotope record from Sulmona basin, Central Italy |
| Q58616734 | Iberian Margin sea surface temperature during MIS 15 to 9 (580–300 ka): Glacial suborbital variability versus interglacial stability |
| Q47268424 | Ice age terminations |
| Q50026517 | In and out of glacial extremes by way of dust-climate feedbacks. |
| Q58264127 | In search of an ice core signal to differentiate between source-driven and sink-driven changes in atmospheric methane |
| Q58053636 | Independent variations of CH4 emissions and isotopic composition over the past 160,000 years |
| Q55878591 | Influence of Bering Strait flow and North Atlantic circulation on glacial sea-level changes |
| Q60568518 | Insolation and CO2 contribution to the interglacial climate before and after the Mid-Brunhes Event |
| Q56268262 | Interglacial diversity |
| Q55919190 | Interglacials of the last 800,000 years |
| Q58404903 | Inverse modeling of global and regional CH4emissions using SCIAMACHY satellite retrievals |
| Q34162549 | Late Holocene methane rise caused by orbitally controlled increase in tropical sources |
| Q28653174 | Macroevolutionary consequences of profound climate change on niche evolution in marine molluscs over the past three million years |
| Q24289326 | Making sense of palaeoclimate sensitivity |
| Q34625115 | Methane emissions from wetlands: biogeochemical, microbial, and modeling perspectives from local to global scales. |
| Q52589055 | Methane release from the southern Brazilian margin during the last glacial. |
| Q105426325 | Methane, Monsoons, and Modulation of Millennial‐Scale Climate |
| Q99350148 | Millennial climate oscillations controlled the structure and evolution of Termination II |
| Q52595405 | Model evidence for a seasonal bias in Antarctic ice cores. |
| Q36599819 | Molecular insights into the historic demography of bowhead whales: understanding the evolutionary basis of contemporary management practices |
| Q61631382 | Multidecadal variability of atmospheric methane, 1000–1800 C.E |
| Q33981174 | Non-CO2 greenhouse gases and climate change. |
| Q38598609 | Nonlinear climate sensitivity and its implications for future greenhouse warming. |
| Q57250909 | Observing and modeling the influence of layering on bubble trapping in polar firn |
| Q64007047 | Oceanic forcing of the Marine Isotope Stage 11 interglacial |
| Q28603965 | On the causal structure between CO2 and global temperature |
| Q51264253 | Orbital Asian summer monsoon dynamics revealed using an isotope-enabled global climate model. |
| Q39200231 | Orbital control of western North America atmospheric circulation and climate over two glacial cycles |
| Q54969521 | Orbital-scale denitrification changes in the Eastern Arabian Sea during the last 800 kyrs. |
| Q35681258 | Oscillators and relaxation phenomena in Pleistocene climate theory |
| Q56658823 | Palaeoclimate constraints on the impact of 2 °C anthropogenic warming and beyond |
| Q47686839 | Palaeoclimate: windows on the greenhouse |
| Q59133405 | PaleoClim, high spatial resolution paleoclimate surfaces for global land areas |
| Q56100317 | Paleoclimates: what do we learn from deep ice cores? |
| Q37352697 | Photodriven heterogeneous charge transfer with transition-metal compounds anchored to TiO2 semiconductor surfaces |
| Q49527727 | Pollen from the Deep-Sea: A Breakthrough in the Mystery of the Ice Ages |
| Q57950086 | Possible role of wetlands, permafrost, and methane hydrates in the methane cycle under future climate change: A review |
| Q59139357 | Precession phasing offset between Indian summer monsoon and Arabian Sea productivity linked to changes in Atlantic overturning circulation |
| Q57071094 | Precession-band variance missing from East Asian monsoon runoff |
| Q30806155 | Radiometric 81Kr dating identifies 120,000-year-old ice at Taylor Glacier, Antarctica |
| Q57589206 | Reconciling the changes in atmospheric methane sources and sinks between the Last Glacial Maximum and the pre-industrial era |
| Q37258543 | Reconstructing the last interglacial at Summit, Greenland: Insights from GISP2. |
| Q58070991 | Reduction of the temperature sensitivity of minerotrophic fen methane emissions by simulated glacial atmospheric carbon dioxide starvation |
| Q59920944 | Repeated pulses of vertical methane flux recorded in glacial sediments from the southeast Bering Sea |
| Q57874004 | Response of Iberian Margin sediments to orbital and suborbital forcing over the past 420 ka |
| Q62472358 | Sedimentary record from Patagonia, southern Chile supports cosmic-impact triggering of biomass burning, climate change, and megafaunal extinctions at 12.8 ka |
| Q58080567 | Simulating climate and stable water isotopes during the Last Interglacial using a coupled climate-isotope model |
| Q50199716 | Southern Hemisphere climate variability forced by Northern Hemisphere ice-sheet topography. |
| Q46333737 | Speleothems reveal 500,000-year history of Siberian permafrost |
| Q31168244 | State dependence of climatic instability over the past 720,000 years from Antarctic ice cores and climate modeling. |
| Q58388886 | Suborbital climatic variability and centres of biological diversity in the Cape region of southern Africa |
| Q34035857 | Synchronous change of atmospheric CO2 and Antarctic temperature during the last deglacial warming |
| Q57058571 | Terrestrial biogeochemical feedbacks in the climate system |
| Q56268108 | Testing competing forms of the Milankovitch hypothesis: A multivariate approach |
| Q31111358 | The Asian monsoon over the past 640,000 years and ice age terminations |
| Q58650433 | The Spatial Structure of the 128 ka Antarctic Sea Ice Minimum |
| Q57145156 | The climatic cyclicity in semiarid-arid central Asia over the past 500,000 years |
| Q58650487 | The role of atomic chlorine in glacial-interglacial changes in the carbon-13 content of atmospheric methane |
| Q74441846 | The year in Nature |
| Q37676712 | Timing and nature of AMOC recovery across Termination 2 and magnitude of deglacial CO2 change |
| Q58113735 | Toward explaining the Holocene carbon dioxide and carbon isotope records: Results from transient ocean carbon cycle-climate simulations |
| Q28650447 | Tropical Atlantic temperature seasonality at the end of the last interglacial |
| Q33349252 | Tropical ocean temperatures over the past 3.5 million years |
| Q91013879 | Two-million-year-old snapshots of atmospheric gases from Antarctic ice |
| Q34072197 | Wetlands and the global carbon cycle: what might the simulated past tell us about the future? |
| Q24289402 | What caused Earth's temperature variations during the last 800,000 years? Data-based evidence on radiative forcing and constraints on climate sensitivity |
| Q63071778 | Widespread global peatland establishment and persistence over the last 130,000 y |
| Q58412420 | Wind-stress feedback amplification of abrupt millennial-scale climate changes |
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