エオセンの地磁気極性逆転の異常な長期間
Yuhji Yamamoto1, Slah Boulila2,3, Futoshi Takahashi4
1Marine Core Research Institute, Kochi University, Kochi, Japan.
まとめ
地球の磁場逆転は,これまで考えられていたよりもはるかに長い時間がかかる可能性があり,いくつかの古代の移行は数万年にわたって続きます. この延長された期間は,ジオダイナモの変動性と,放射線の増加による古代の生命への潜在的な影響を示唆しています.
科学分野:
- 地質物理学 地質物理学とは地質物理学です.
- パレオマグネティズム (古磁気学) とは
- 地球科学 地球科学 地球科学
背景:
- 地球の磁場には,極性逆転の歴史があります.
- 以前の研究では,主に最近の地質学的記録に基づいて,1万年未満の逆転期間を示していた.
研究 の 目的:
- 遠い過去における地磁気極性移行の期間を調査する.
- ジオダイナモプロセスの変動性を理解するために.
主な方法:
- 特殊な解像度の高い深海の堆積物の古磁気記録の分析.
- 約4000万年前まで遡る2つの極性移行の年代測定と分析.
主要な成果:
- 約4000万年前に起こった2つの極性移行が特定されました.
- これらの移行は,以前に観察されたものよりも大幅に長く,それぞれ1万8千年と7万年の間続きました.
- 発見は,変数逆転期間を予測する数値ジオダイナモモデルと一致しています.
結論:
- 地磁気逆転の持続時間は一定ではなく,1万年よりもはるかに長くなります.
- 移行期間の長期にわたる地磁場の弱まりは,地球の太陽放射への曝露を増加させた可能性があります.
- フィールドの強度と持続のこの変動は,古代の生命と環境への影響を及ぼす可能性があります.
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