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A Single-Year Cosmic Ray Event at 5410 BCE Registered in 14C of Tree Rings

Miyake, F. (author)
Nagoya University
Panyushkina, I. P. (author)
University of Arizona
Jull, A. J.T. (author)
Institute for Nuclear Research, Hungarian Academy of Sciences (ATOMKI),University of Arizona
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Adolphi, F. (author)
Alfred-Wegener Institute, Helmholtz Center for Polar and Marine Research, Bremerhaven
Brehm, N. (author)
ETH Zürich
Helama, S. (author)
Natural Resources Institute Finland (Luke)
Kanzawa, K. (author)
Nagoya University
Moriya, T. (author)
Yamagata University
Muscheler, R. (author)
Lund University,Lunds universitet,BECC: Biodiversity and Ecosystem services in a Changing Climate,Centrum för miljö- och klimatvetenskap (CEC),Naturvetenskapliga fakulteten,MERGE: ModElling the Regional and Global Earth system,Kvartärgeologi,Geologiska institutionen,Centre for Environmental and Climate Science (CEC),Faculty of Science,Quaternary Sciences,Department of Geology
Nicolussi, K. (author)
University of Innsbruck
Oinonen, M. (author)
Finnish Museum of Natural History
Salzer, M. (author)
University of Arizona
Takeyama, M. (author)
Yamagata University
Tokanai, F. (author)
Yamagata University
Wacker, L. (author)
ETH Zürich
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 (creator_code:org_t)
2021
2021
English.
In: Geophysical Research Letters. - 0094-8276. ; 48:11
  • Journal article (peer-reviewed)
Abstract Subject headings
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  • The annual 14C data in tree rings is an outstanding proxy for uncovering extreme solar energetic particle (SEP) events in the past. Signatures of extreme SEP events have been reported in 774/775 CE, 992/993 CE, and ∼660 BCE. Here, we report another rapid increase of 14C concentration in tree rings from California, Switzerland, and Finland around 5410 BCE. These 14C data series show a significant increase of ∼6‰ in 5411–5410 BCE. The signature of 14C variation is very similar to the confirmed three SEP events and points to an extreme short-term flux of cosmic ray radiation into the atmosphere. The rapid 14C increase in 5411/5410 BCE rings occurred during a period of high solar activity and 60 years after a grand 14C excursion during 5481–5471 BCE. The similarity of our 14C data to previous events suggests that the origin of the 5410 BCE event is an extreme SEP event.

Subject headings

NATURVETENSKAP  -- Geovetenskap och miljövetenskap -- Klimatforskning (hsv//swe)
NATURAL SCIENCES  -- Earth and Related Environmental Sciences -- Climate Research (hsv//eng)

Keyword

cosmogenic nuclide
radiocarbon
solar activity
solar energetic particle
tree rings

Publication and Content Type

art (subject category)
ref (subject category)

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