| P50 | author | Michael Wagreich | Q13418094 |
| | Phil Gibbard | Q1740096 |
| | Jacques Grinevald | Q3159039 |
| | Will Steffen | Q8003119 |
| | Jan Zalasiewicz | Q11719512 |
| | Mark Williams | Q21518081 |
| | Matthew Edgeworth | Q42415948 |
| | Colin P. Summerhayes | Q42424087 |
| | Alejandro Cearreta | Q42424408 |
| | Clément Poirier | Q42424412 |
| | Erle C. Ellis | Q47451371 |
| | Irka Hajdas | Q47451372 |
| | Catherine Jeandel | Q51163856 |
| | Anthony D. Barnosky | Q57748812 |
| | Agnieszka Gałuszka | Q58424008 |
| | Juliana Ivar do Sul | Q58424021 |
| | Colin N. Waters | Q59754656 |
| | Davor Vidas | Q62034450 |
| P2093 | author name string | Alexander P Wolfe | |
| | Daniel deB Richter | |
| | Reinhold Leinfelder | |
| | Andrew Revkin | |
| | James PM Syvitski | |
| | JR McNeill | |
| P2860 | cites work | Proxy-based reconstructions of hemispheric and global surface temperature variations over the past two millennia | Q24655448 |
| | Defining the Anthropocene | Q29038521 |
| | When did the Anthropocene begin? A mid-twentieth century boundary level is stratigraphically optimal | Q29544455 |
| | Atmospheric CO2 concentrations over the last glacial termination | Q33930236 |
| | Geology of mankind | Q33956753 |
| | Orbital and millennial Antarctic climate variability over the past 800,000 years. | Q34646794 |
| | The maunder minimum | Q34675042 |
| | The Anthropocene concept in ecology and conservation | Q38281915 |
| | Spheroidal carbonaceous fly ash particles provide a globally synchronous stratigraphic marker for the Anthropocene | Q41193052 |
| | Sediment flux and the Anthropocene. | Q43408069 |
| | The Anthropocene and the international law of the sea. | Q44229350 |
| | Geology. Defining the epoch we live in. | Q45011783 |
| | The Anthropocene: are humans now overwhelming the great forces of Nature? | Q47715763 |
| | Can nuclear weapons fallout mark the beginning of the Anthropocene Epoch? | Q55628006 |
| | The Anthropogenic Greenhouse Era Began Thousands of Years Ago | Q55867104 |
| | Are we now living in the Anthropocene | Q55871912 |
| | Natural and anthropogenic changes in atmospheric CO2 over the last 1000 years from air in Antarctic ice and firn | Q55919755 |
| | Inter-hemispheric temperature variability over the past millennium | Q56001264 |
| | Vostok ice core provides 160,000-year record of atmospheric CO2 | Q56048516 |
| | Diachronous beginnings of the Anthropocene: The lower bounding surface of anthropogenic deposits | Q56268256 |
| | A sociometabolic reading of the Anthropocene: Modes of subsistence, population size and human impact on Earth | Q57022668 |
| | A stratigraphical basis for the Anthropocene? | Q57142130 |
| | Global and Hemispheric Temperature Anomalies - Land and Marine Instrumental Records | Q57309074 |
| | Evidence for the Postconquest Demographic Collapse of the Americas in Historical CO2Levels | Q57381604 |
| | Holocene carbon-cycle dynamics based on CO2 trapped in iceat Taylor Dome, Antarctica | Q58114149 |
| | Law Dome CO2, CH4and N2O ice core records extended to 2000 years BP | Q58382142 |
| P433 | issue | 2 | |
| P921 | main subject | anthropocene | Q26841 |
| | Little Ice Age | Q190530 |
| P304 | page(s) | 117-127 | |
| P577 | publication date | 2015-05-29 | |
| P1476 | title | Colonization of the Americas, ‘Little Ice Age’ climate, and bomb-produced carbon: Their role in defining the Anthropocene | |
| P478 | volume | 2 | |