マリノの氷河期に続く海洋の酸素化
Swapan K Sahoo1, Noah J Planavsky, Brian Kendall
1Department of Geoscience, University of Nevada, Las Vegas, Nevada 89154, USA.
Nature
|September 29, 2012
まとめ
初期の動物の進化は,マリノの氷河期に続く酸素化の出来事によって引き起こされたのかもしれない. エディアカランのシェールからの地化学データは,氷河化,酸素レベル,初期の動物の多様化との関連を裏付ける早期の酸素化イベントを明らかにしています.
科学分野:
- 地質化学 地質化学
- 古代気候学 (paleoclimatology) とは,古代気候学 (paleoclimatology) とは,古代気候学 (paleoclimatology) とは,古代気候学 (paleoclimatology) とは,古代気候学 (paleoclimatology) とは
- 進化生物学の進化生物学について
背景:
- メタゾアンの起源は,冷凍期にさかのぼり,マリノの氷河期 (約6億3500万年前) の後に顕著な多様化がありました.
- この多様化と潜在的な酸素化イベントの間のリンクは,海洋または大気中の酸素の増加の証拠が限られているため,議論の余地があります.
- 初期の生物学的進化を地球システムプロセスと結びつける以前のモデルは論争の的だ.
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