エディアカランの循環を明らかにする
Matthew S Dodd1,2,3,4,5, Wei Shi1,3, Chao Li6,7,8
1State Key Laboratory of Oil and Gas Reservoir Geology and Exploitation, Institute of Sedimentary Geology, Chengdu University of Technology, Chengdu, China.
Nature
|May 31, 2023
まとめ
エディアカラン・シュラムの遠征中に 海洋の濃度が上昇し 酸素が増加した 内部循環だけではなく エディアカランの海洋の酸素化が 制御されていることを示唆しています
科学分野:
- 地化学
- 古代海洋学
- 生地化学
背景:
- 海洋の酸素レベルを 制御する重要な栄養素です
- エディアカラン期には,酸素の上昇と関連した海洋リン酸の増加が提案された.
- この重要な時期におけるの循環は 十分に理解されていない.
研究 の 目的:
- エディアカラン・シュラム (SE) 遠征の時の海洋リン濃度を再構築する.
- この時期の海洋酸素化の要因を調査する.
- リン,炭素同位体,酸素濃度の関係を理解する.
主な方法:
- 炭酸塩関連フォスファート (CAP) の分析
- 海洋のリン濃度の再構築
- 定量的生地化学モデルを適用する.
主要な成果:
- 海洋のリン濃度の急上昇は,SEの間に観察されました.
- モデルでは,有機物質の酸化と土地の気象によるの放出を示唆しています.
- SE全域で異なった無酸素度で同等な濃度が見つかりました.
結論:
- 硫酸エステーションのような 外部刺激により エディアカラの海洋の酸素化が 制御された可能性が高い
- 現代の海とは違って リンと酸素の循環が解き放たれたのかもしれません
- これは大気中の酸素濃度が 長期にわたって上昇していることに 洞察力を与えてくれます
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