年輪に閉じ込められた放射性炭素が古代太陽活動を解明(Study sheds light on ancient solar activity using radiocarbon locked in tree-rings)

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2025-04-11 アリゾナ大学

アリゾナ大学とスイスETHチューリッヒの研究により、年輪に含まれる放射性炭素(C-14)を分析することで、紀元前1000年から紀元前2年までの太陽活動の詳細な記録が得られた。特に「ハルシュタット高原」と呼ばれるC-14の変動が乏しい時代でも、太陽の11年周期が安定して存在していたことが判明。新たな分析機器により、過去の太陽嵐の理解が進み、古代の年代表定精度も向上する可能性がある。

<関連情報>

紀元前1千年紀の木の年輪と放射性炭素による古代の太陽周期の追跡 Tracing ancient solar cycles with tree rings and radiocarbon in the first millennium BCE

Nicolas Brehm,Charlotte L. Pearson,Marcus Christl,Alex Bayliss,Kurt Nicolussi,Thomas Pichler,David Brown & Lukas Wacker
Nature Communications  Published:06 January 2025
DOI:https://doi.org/10.1038/s41467-024-55757-y

年輪に閉じ込められた放射性炭素が古代太陽活動を解明(Study sheds light on ancient solar activity using radiocarbon locked in tree-rings)

Abstract

The Sun drives Earth’s energy systems, influencing weather, ocean currents, and agricultural productivity. Understanding solar variability is critical, but direct observations are limited to 400 years of sunspot records. To extend this timeline, cosmic ray-produced radionuclides like 14C in tree-rings provide invaluable insights. However, few records have the resolution or temporal span required to thoroughly investigate important short-term solar phenomena, such as the 11-year solar cycle, or 14C production spikes most likely linked to solar energetic particle (SEP) events. Here we present a continuous, annually resolved atmospheric 14C record from tree-rings spanning the first millennium BCE, confirming no new SEP’s and clearly defining the 11-year solar cycle, with a mean period of 10.5 years, and amplitude of approximately 0.4‰ in 14C concentration. This dataset offers unprecedented detail on solar behavior over long timescales, providing insights for climatic research and solar hazard mitigation, while also offering enhanced radiocarbon calibration and dating accuracy.

1702地球物理及び地球化学
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