Published March 31, 2026 | Version v1
Dataset Open

Annual Atmospheric Δ14C Variation in Eastern China During 1850–1933 CE

  • 1. Laboratory of AMS Dating and the Environment, School of Geography and Ocean Science, Nanjing University, Nanjing, China
  • 2. Frontiers Science Center for Critical Earth Material Cycling, Nanjing University, Nanjing, China
  • 3. Laboratory for Climate Risk and Urban-Rural Smart Governance, School of Geography, Jiangsu Second Normal University, Nanjing, China
  • 4. Tianmushan National Nature Reserve Management Bureau, Hangzhou, China

Description

In January 2022, 87 cores from 40 trees (Cryptomeria fortunei) were collected from Mount Tianmu (30.34°N, 119.43°E, 1091 m a.s.l.) in Zhejiang Province, eastern China, to develop a well-dated composite tree-ring width chronology. Subsequently, annual rings from 1850 to 1933 CE in tree-ring sample XTM27A1 (hereafter XTM) were selected for radiocarbon analysis. Details of the pretreatment and radiocarbon analysis protocol are described in Lin et al. (2024).
This dataset provides Δ14C values for XTM tree-ring samples from 1850 to 1933 CE (Table 1), as well as F14C values for 14C blank wood samples (IAEA-C9 and NF142) and reference wood samples (LWQ1796) used for data quality control (Table 2).

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References

  • Bevington, P. R., & Robinson, D. K. (2003). Data reduction and error analysis for the physical sciences (3rd edition). New York: McGraw-Hill.
  • Lin, P., Zhao, Y., Zhang, H., Wieloch, T., Gu, Y., Liang, C., et al. (2024). A tree-ring cellulose extraction device adapted to radiocarbon analysis. Radiocarbon, 66(4), 806–815. https://doi.org/10.1017/RDC.2024.83
  • Stuiver, M., & Polach, H. A. (1977). Discussion reporting of 14C data. Radiocarbon, 3(19), 355–363. https://doi.org/10.1017/S0033822200003672