4.8 Article

Cosmogenic radionuclides reveal an extreme solar particle storm near a solar minimum 9125 years BP

Journal

NATURE COMMUNICATIONS
Volume 13, Issue 1, Pages -

Publisher

NATURE PORTFOLIO
DOI: 10.1038/s41467-021-27891-4

Keywords

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Funding

  1. Royal Physiographic Society of Lund grant
  2. Swedish Research Council [DNR2013-8421, DNR2018-05469, 2020-00420]
  3. RADIATE project under from the EU Research and Innovation programme HORIZON 2020 [824096]
  4. Helmholtz Association [VH-NG-1501]
  5. EGRIP project
  6. Denmark (A. P. MOller Foundation, University of Copenhagen)
  7. USA (US National Science Foundation, Office of Polar Programs)
  8. Germany (Alfred Wegener Institute, Helmholtz Centre for Polar and Marine Research)
  9. Japan (National Institute of Polar Research and Arctic Challenge for Sustainability)
  10. Norway (University of Bergen)
  11. Norway (Trond Mohn Foundation)
  12. Switzerland (Swiss National Science Foundation)
  13. France (French Polar Institute Paul-Emile Victor, Institute for Geosciences and Environmental research)
  14. Canada (University of Manitoba)
  15. China (Chinese Academy of Sciences)
  16. China (Beijing Normal University)
  17. Denmark (SNF)
  18. Belgium (FNRS-CFB)
  19. France (IFRTP)
  20. France (INSU/CNRS)
  21. Germany (AWI)
  22. Iceland (RannIs)
  23. Japan (MEXT)
  24. Sweden (SPRS)
  25. Switzerland (SNF)
  26. United States of America (NSF)
  27. Swedish Research Council [2020-00420] Funding Source: Swedish Research Council

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During solar storms, the Sun releases a large amount of energetic particles that produce cosmogenic radionuclides. By analyzing Be-10 and Cl-36 data from ice cores in Greenland and Antarctica, we have identified one of the largest production peaks caused by an extreme SEP event that occurred around 7176 BCE. This event had a very hard energy spectrum and may have been up to 100 times larger than any SEP event in recorded history. Surprisingly, the event occurred during a solar minimum phase.
During solar storms, the Sun expels large amounts of energetic particles (SEP) that can react with the Earth's atmospheric constituents and produce cosmogenic radionuclides such as C-14, Be-10 and Cl-36. Here we present Be-10 and Cl-36 data measured in ice cores from Greenland and Antarctica. The data consistently show one of the largest Be-10 and Cl-36 production peaks detected so far, most likely produced by an extreme SEP event that hit Earth 9125 years BP (before present, i.e., before 1950 CE), i.e., 7176 BCE. Using the Cl-36/Be-10 ratio, we demonstrate that this event was characterized by a very hard energy spectrum and was possibly up to two orders of magnitude larger than any SEP event during the instrumental period. Furthermore, we provide Be-10-based evidence that, contrary to expectations, the SEP event occurred near a solar minimum. Cosmogenic radionuclides from ice cores and tree rings indicate that an extreme solar proton event has hit Earth about 9200 years ago. Contrary to expectations, the event occurred during a quiet phase of the Sun within the 11 year solar cycle.

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