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2. Palaeontological signatures of the Anthropocene are distinct from those of previous epochs

3. Epochs, events and episodes: Marking the geological impact of humans

6. Global Boundary Stratotype Section and Point (GSSP) for the Anthropocene Series: Where and how to look for potential candidates

9. When did the Anthropocene begin? A mid-twentieth century boundary level is stratigraphically optimal

14. The Working Group on the Anthropocene: Summary of evidence and interim recommendations

18. Contributors

33. Contributors

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