在马里诺海冰期之后的海洋氧化
Swapan K Sahoo1, Noah J Planavsky, Brian Kendall
1Department of Geoscience, University of Nevada, Las Vegas, Nevada 89154, USA.
Nature
|September 29, 2012
概括
早期的动物进化可能是由马里诺冰川之后的氧化事件驱动的. 来自埃迪亚卡兰页岩的地化学数据揭示了早期的氧化事件,支持冰川化,氧气水平和早期动物多样化之间的联系.
科学领域:
- 地质化学 地质化学
- 古气候学 古气候学
- 进化生物学 进化生物学
背景情况:
- 甲动物的起源可追溯到冷时期,在马里诺冰川 (约6.35亿年前) 之后出现了显著的多样化.
- 由于海洋或大气氧气增加的证据有限,这种多样化和潜在的氧化事件之间的联系仍在争论中.
- 以前的模型将早期生物进化与地球系统过程联系起来是有争议的.
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