海洋のリン酸塩貯蔵庫の進化について
Noah J Planavsky1, Olivier J Rouxel, Andrey Bekker
1Department of Earth Sciences, University of California, Riverside, California 92521, USA.
Nature
|October 29, 2010
まとめ
海洋のリンレベルは,ファネロゾーイクイオン全体で安定していたが,プレカンブリア海洋では急上昇した. この栄養素の余剰は,その後,
科学分野:
- 地質化学 地質化学
- パレオセアノグラフィー
- バイオジオケミカルサイクル
背景:
- は,海洋有機炭素の埋葬と海洋大気の酸化還元状態を調節する重要な栄養素です.
- 堆積岩におけるリンと鉄の比率は,古代の溶解リン酸濃度の代理として機能する.
- 過去のリン酸塩レベルを理解することは,地球の初期の環境条件を再構築するために不可欠です.
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