比較的酸化した液体で 地球の初期の水熱システムに供給された
Dustin Trail1, Thomas M McCollom2
1Department of Earth and Environmental Sciences, University of Rochester, Rochester, NY 14627, USA.
まとめ
初期の地球
科学分野:
- 地化学
- 天体生物学
- 初期の地球科学
背景:
- 生命の起源を理解するために,初期の地球の石層流体の性質は極めて重要です.
- これらの液体は地球の内部と表面の水熱システムとの間の導体として機能した.
研究 の 目的:
- 約40億年前の 石層流体の特徴を推測する
- 生命の起源に関係する 重要な金属の溶解性と輸送を モデル化する
主な方法:
- ジルコンの化学分析を用いた.
- 実験室での実験を行いました
- 地化学モデリングに従事した.
主要な成果:
- 圧縮された酸素の流動性,塩素含量,初期の石層流体の温度.
- これらの液体は初期の地殻よりも 酸化していることが判明した.
- 水温プールなどの地表付近の水系との相互作用が確認された.
結論:
- 初期の石層液体は,前生物化学に有利な環境における酸化還元グラデーションの増幅に重要な役割を果たした.
- これらの発見は,地球深層の液体と地表の熱水系の相互作用を含む生命の起源のシナリオを支持する.
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