1. A Single‐Year Cosmic Ray Event at 5410 BCE Registered in 14C of Tree Rings
- Author
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A. J. T. Jull, Toru Moriya, Kurt Nicolussi, Raimund Muscheler, Fuyuki Tokanai, Samuli Helama, L. Wacker, Matthew W. Salzer, Mirei Takeyama, Markku Oinonen, Irina P. Panyushkina, Florian Adolphi, K. Kanzawa, Nicolas Brehm, and Fusa Miyake
- Subjects
Cosmogenic‐nuclide Exposure Dating ,Dendrochronology ,010504 meteorology & atmospheric sciences ,Energetic Particles ,Geochronology ,Cosmic ray ,010502 geochemistry & geophysics ,01 natural sciences ,law.invention ,Atmosphere ,Paleoceanography ,law ,Research Letter ,Radiocarbon dating ,solar energetic particle ,Cosmogenic nuclide ,0105 earth and related environmental sciences ,Solar Physics, Astrophysics, and Astronomy ,biology ,Excursion ,Bristlecone Pine ,biology.organism_classification ,Solar Cycle Variations ,Solar Activity Cycle ,Cosmic Rays ,Interplanetary Physics ,tree rings ,Geophysics ,13. Climate action ,Climatology ,cosmogenic nuclide ,radiocarbon ,General Earth and Planetary Sciences ,Cosmogenic Isotopes ,solar activity ,Event (particle physics) ,Space Sciences ,Geology ,Chronology - Abstract
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., Key Points Rapid 14C increase of ∼6‰ with significant level was found in tree rings from California, Switzerland, and Finland around 5410 BCEFive thousand, four hundred ten BCE event occurred during a period of high solar activity and 60 years after a grand 14C excursion of ∼20‰ from 5481 to 5471 BCEThe similarity of this 14C signature to already known solar events suggests that the origin of this new 5410 BCE event is an extreme SEP
- Published
- 2021