木が「話す」とき:研究者たちが太古の木から大規模な太陽嵐についての手がかりを探る(When trees ‘talk:’ Researchers probe ancient wood for clues about massive solar storms)

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2024-11-20 アリゾナ大学

アリゾナ大学の研究チームは、古代の木材の年輪に含まれる放射性炭素(炭素14)を分析し、紀元前664年に発生した極端な太陽嵐の痕跡を特定しました。このような太陽嵐は、地球の大気中の炭素14濃度を急激に増加させ、木の成長過程でその痕跡が年輪に残ります。この発見は、太陽活動の歴史的なパターンを理解し、将来の太陽嵐による地球への影響を予測する上で重要な情報を提供します。

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紀元前660年頃のミヤケ太陽陽子イベントの時期は、紀元前664年から663年の間と推定される The timing of the ca-660 BCE Miyake solar-proton event constrained to between 664 and 663 BCE

Irina P. Panyushkina,A. J. Timothy Jull,Mihaly Molnár,Tamás Varga,Ivan Kontul’,Rashit Hantemirov,Vladymir Kukarskih,Igor Sljusarenko,Vladymir Myglan & Valerie Livina
Communications Earth & Environment  Published:23 August 2024
DOI:https://doi.org/10.1038/s43247-024-01618-x

木が「話す」とき:研究者たちが太古の木から大規模な太陽嵐についての手がかりを探る(When trees ‘talk:’ Researchers probe ancient wood for clues about massive solar storms)

Abstract

Extreme solar energetic particle events, known as Miyake events, are rare phenomena observed by cosmogenic isotopes, with only six documented. The timing of the ca. 660 BCE Miyake event remains undefined until now. Here, we assign its occurrence to 664–663 BCE through new radiocarbon measurements in gymnosperm larch tree rings from arctic-alpine biomes (Yamal and Altai). Using a 22-box carbon cycle model and Bayesian statistics, we calculate the radiocarbon production rate during the event that is 3.2–4.8 times higher than the average solar modulation, and comparable to the 774–775 CE solar-proton event. The prolonged radiocarbon signature manifests a 12‰ rise over two years. The non-uniform signal in the tree rings is likely driven by the low rate of CO2 gas exchange between the trees and the ambient atmosphere, and the high residence time of radiocarbon in the post-event stratosphere. We caution about using the event’s pronounced signature for precise single-year-dating.

1702地球物理及び地球化学
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