| scholarly article | Q13442814 |
| P356 | DOI | 10.1007/S10712-011-9140-4 |
| P5875 | ResearchGate publication ID | 225746436 |
| P50 | author | Gilles Ramstein | Q56100170 |
| P2860 | cites work | No climate paradox under the faint early Sun | Q22122182 |
| EPICA Dome C record of glacial and interglacial intensities | Q24289401 | ||
| Marked decline in atmospheric carbon dioxide concentrations during the Paleogene | Q28257130 | ||
| High-resolution carbon dioxide concentration record 650,000-800,000 years before present | Q28280161 | ||
| Stable carbon cycle-climate relationship during the Late Pleistocene | Q28283869 | ||
| Did cooling oceans trigger Ordovician biodiversification? Evidence from conodont thermometry | Q28288401 | ||
| CO2-forced climate thresholds during the Phanerozoic | Q29037834 | ||
| Trends, Rhythms, and Aberrations in Global Climate 65 Ma to Present | Q29546517 | ||
| Orbital and millennial-scale features of atmospheric CH4 over the past 800,000 years | Q31155450 | ||
| A palaeotemperature curve for the Precambrian oceans based on silicon isotopes in cherts | Q33261597 | ||
| High levels of atmospheric carbon dioxide necessary for the termination of global glaciation | Q33979018 | ||
| Earth and Mars: evolution of atmospheres and surface temperatures | Q34006172 | ||
| A neoproterozoic snowball earth | Q34067330 | ||
| Rapid Cenozoic glaciation of Antarctica induced by declining atmospheric CO2. | Q34170751 | ||
| A 'snowball Earth' climate triggered by continental break-up through changes in runoff | Q34306856 | ||
| Late Pliocene Greenland glaciation controlled by a decline in atmospheric CO2 levels | Q34816767 | ||
| Low-latitude glaciation and rapid changes in the Earth's obliquity explained by obliquity-oblateness feedback | Q38528450 | ||
| Atmospheric carbon dioxide concentrations before 2.2 billion years ago. | Q47188746 | ||
| Modelled atmospheric temperatures and global sea levels over the past million years | Q47253262 | ||
| Solar interior structure and luminosity variations | Q53953599 | ||
| A negative feedback mechanism for the long-term stabilization of Earth's surface temperature | Q55878509 | ||
| Climate and atmospheric history of the past 420,000 years from the Vostok ice core, Antarctica | Q55880358 | ||
| GEOCARB II; a revised model of atmospheric CO 2 over Phanerozoic time | Q56001352 | ||
| The snowball Earth hypothesis: testing the limits of global change | Q56066586 | ||
| New MIS 19 EPICA Dome C high resolution deuterium data: Hints for a problematic preservation of climate variability at sub-millennial scale in the “oldest ice” | Q56100314 | ||
| Les glaciations du Protérozoı̈que | Q56100448 | ||
| Coupled modeling of global carbon cycle and climate in the Neoproterozoic: links between Rodinia breakup and major glaciations | Q56100453 | ||
| Impacts of palaeogeography and sea level changes on Mid-Cretaceous climate | Q56100474 | ||
| Amount of CO2emissions irreversibly leading to the total melting of Greenland | Q56100494 | ||
| Fish tooth δ18O revising Late Cretaceous meridional upper ocean water temperature gradients | Q56100507 | ||
| Scenario for the evolution of atmospheric pCO2 during a snowball Earth | Q56100508 | ||
| Causal or casual link between the rise of nannoplankton calcification and a tectonically-driven massive decrease in Late Triassic atmospheric CO2? | Q56527968 | ||
| Oxygen isotopes from biogenic apatites suggest widespread endothermy in Cretaceous dinosaurs | Q57235514 | ||
| From atmosphere, to climate, to Earth system science | Q58339990 | ||
| CLIMBER-2: a climate system model of intermediate complexity. Part I: model description and performance for present climate | Q58410349 | ||
| P433 | issue | 4-5 | |
| P921 | main subject | Earth | Q2 |
| P304 | page(s) | 329-350 | |
| P577 | publication date | 2011-09-01 | |
| P1433 | published in | Surveys in Geophysics | Q15752684 |
| P1476 | title | Climates of the Earth and Cryosphere Evolution | |
| P478 | volume | 32 |
| Q59133450 | Dynamic Greenland ice sheet driven by pCO variations across the Pliocene Pleistocene transition | cites work | P2860 |
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