| P50 | author | Mark Pagani | Q110720981 |
| P2093 | author name string | Ana Christina Ravelo | |
| | Jonathan LaRiviere | |
| | Zhonghui Liu | |
| P2860 | cites work | Regional climate shifts caused by gradual global cooling in the Pliocene epoch | Q39386416 |
| | Paleoatmospheric signatures in neogene fossil leaves | Q47259092 |
| | Effect of Phytoplankton Cell Geometry on Carbon Isotopic Fractionation | Q56621108 |
| | Mid-Pliocene warmth: stronger greenhouse and stronger conveyor | Q56638636 |
| | Effect of the formation of the Isthmus of Panama on Atlantic Ocean thermohaline circulation | Q57073091 |
| | Comparison of mid-Pliocene climate predictions produced by the HadAM3 and GCMAM3 General Circulation Models | Q57411669 |
| | Forcing of late Cenozoic northern hemisphere climate by plateau uplift in southern Asia and the American west | Q59884626 |
| | Late miocene atmospheric CO(2) concentrations and the expansion of C(4) grasses | Q95310232 |
| | Warm upwelling regions in the Pliocene warm period | Q97323697 |
| | Target Atmospheric CO2: Where Should Humanity Aim? | Q24273405 |
| | Atmospheric carbon dioxide concentrations over the past 60 million years | Q28144787 |
| | Closing of the Indonesian seaway as a precursor to east African aridification around 3–4 million years ago | Q29543546 |
| | Permanent El Niño-like conditions during the Pliocene warm period | Q34428679 |
| | Late Pliocene Greenland glaciation controlled by a decline in atmospheric CO2 levels | Q34816767 |
| | Greatly expanded tropical warm pool and weakened Hadley circulation in the early Pliocene. | Q38921244 |
| | North Pacific seasonality and the glaciation of North America 2.7 million years ago. | Q39129854 |
| P433 | issue | 1 | |
| P407 | language of work or name | English | Q1860 |
| P921 | main subject | Pliocene | Q76259 |
| | climate sensitivity | Q521783 |
| P304 | page(s) | 27-30 | |
| P577 | publication date | 2009-12-20 | |
| P1433 | published in | Nature Geoscience | Q1337483 |
| P1476 | title | High Earth-system climate sensitivity determined from Pliocene carbon dioxide concentrations | |
| P478 | volume | 3 | |