Don E Canfield1, Shuichang Zhang2, Ross N Mitchell3,4

  • 1Department of Biology, University of Southern Denmark, Odense M 5230, Denmark.

まとめ

過去20億年の間に 大陸の気象と 粒子の海への移動が 大きく変化しました 地殻のダイナミクスと地質学的な活動が 主にこれらの長期的地化学的サイクルを制御していました

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