地球の中年期におけるオーロゲン静止
まとめ
地球の山の形成の歴史は,アルカインとファネロゾイクにおける最も厚い地殻を示しています. プロテロゾーイク時代には 超大陸による山岳活動が減少し 生命の進化を阻害した可能性がある.
科学分野:
- 地質学
- 地化学
- 古生物学
背景:
- 山帯は栄養素の循環に不可欠であり,脱毛と水理学に影響を与えます.
- 長期にわたる山の形成過程を理解することは 地球の表面の進化の鍵です
研究 の 目的:
- 地化学のプロキシを用いて 山の形成の歴史を再現する
- 地質学的な時間における大陸地殻の厚さとオロゲン活動との関係を調査する.
主な方法:
- デトリタルジルコンのユーロピウム異常を 山の形成の追跡に利用した
- 地質学的なエオンの間での活動的な大陸の地殻の厚さの変化を分析した.
主要な成果:
- 大陸地殻の厚さはアルカインとファネロゾイク時代にピークに達した.
- プロテロゾイク時代には,地殻の厚さが継続的に減少し,オロゲネシスが最小限であった.
- プロテロゾイクにおける長期のオロゲン静止は,ヌナ・ロディニア超大陸と関連している.
結論:
- 超大陸の循環はマントルの熱構造と石層の強さに大きく影響し,山の形成に影響する.
- プロテロゾーイクにおける 重要な山の形成の欠如は 海洋の栄養素の制限と 進化の進歩を阻害したのかもしれない.
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