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2. The IPCC’s reductive Common Era temperature history

12. Global wood anatomical perspective on the onset of the Late Antique Little Ice Age (LALIA) in the mid-6th century CE

15. MULTI-PROXY TREE-RING DATING DURING THE YOUNGER DRYAS.

17. Temperature-induced germination pulses above the alpine tree line.

18. Contrasting Future Growth of Norway Spruce and Scots Pine Forests Under Warming Climate.

19. Prominent role of volcanism in Common Era climate variability and human history

23. Recent summer warming over the western Mediterranean region is unprecedented since medieval times

24. Eastern USA summer temperatures since 1461 CE show connections to volcanic forcing and jet stream dynamics

25. The influence of decision-making in tree ring-based climate reconstructions

29. Recent summer warming over the western Mediterranean region is unprecedented since medieval times

30. Sudden disappearance of yew (Taxus baccata) woodlands from eastern England coincides with a possible climate event around 4.2 ka ago

31. Dendro-provenancing of Arctic driftwood

34. Central European agroclimate over the past 2,000 years

38. Recognising bias in Common Era temperature reconstructions

41. Reduced Temperature Sensitivity of Maximum Latewood Density Formation in High-Elevation Corsican Pines under Recent Warming

42. The IntCal20 Northern Hemisphere radiocarbon age calibration curve (0-55 kcal BP)

43. The Intcal20 Northern Hemisphere radiocarbon age calibration curve (0-55 cal kBP)

46. Past millennium hydroclimate variability from Corsican pine tree‐ring chronologies.

47. Insights on the timing, global sulfate lifecycle and climate impact of Earth’s largest (pre-) historic volcanic eruptions

48. A millennium-long ‘Blue Ring’ chronology from the Spanish Pyrenees reveals severe ephemeral summer cooling after volcanic eruptions

49. The IntCal20 Northern Hemisphere Radiocarbon Age Calibration Curve (0–55 cal kBP)

50. Illuminating Intcal During the Younger Dryas

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