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A rapid cosmic-ray increase in BC 3372-3371 from ancient buried tree rings in China.
Wang, F Y; Yu, H; Zou, Y C; Dai, Z G; Cheng, K S.
  • Wang FY; School of Astronomy and Space Science, Nanjing University, Nanjing, 210023, China. fayinwang@nju.edu.cn.
  • Yu H; Key Laboratory of Modern Astronomy and Astrophysics (Nanjing University), Ministry of Education, Nanjing, 210023, China. fayinwang@nju.edu.cn.
  • Zou YC; School of Astronomy and Space Science, Nanjing University, Nanjing, 210023, China.
  • Dai ZG; School of Physics, Huazhong University of Science and Technology, Wuhan, 430074, China. zouyc@hust.edu.cn.
  • Cheng KS; School of Astronomy and Space Science, Nanjing University, Nanjing, 210023, China.
Nat Commun ; 8(1): 1487, 2017 11 14.
Article en En | MEDLINE | ID: mdl-29133840
ABSTRACT
Cosmic rays interact with the Earth's atmosphere to produce 14C, which can be absorbed by trees. Therefore, rapid increases of 14C in tree rings can be used to probe previous cosmic-ray events. By this method, three 14C rapidly increasing events have been found. Plausible causes of these events include large solar proton events, supernovae, or short gamma-ray bursts. However, due to the lack of measurements of 14C by year, the occurrence frequency of such 14C rapidly increasing events is poorly known. In addition, rapid increases may be hidden in the IntCal13 data with five-year resolution. Here we report the result of 14C measurements using an ancient buried tree during the period between BC 3388 and 3358. We found a rapid increase of about 9‰ in the 14C content from BC 3372 to BC 3371. We suggest that this event could originate from a large solar proton event.