中部德沃尼亚海洋的氧化使动物能够扩展到更深的水域息地
Kunmanee Bubphamanee1,2, Michael A Kipp2,3,4, Jana Meixnerová1
1Department of Earth and Space Sciences, University of Washington, Seattle, WA 98195-1310.
概括
地球的古代海洋在很大程度上是无毒的,直到纪. 陆地森林的兴起导致了永久的深海氧化,推动了海洋革命和复杂动物的进化.
科学领域:
- 古代海洋学
- 地质化学
- 古生物学
背景情况:
- 地球的氧化历史极大地影响了生物的进化.
- 之前的想法:新生代氧化事件使动物起源.
- 最近的氧化还原代理表明持续的深海氧化不足直到晚代纪.
研究的目的:
- 使用 (Se) 代理物重建古纪深海氧化.
- 研究陆地植物进化与海洋氧气水平之间的联系.
- 澄清了中古海洋革命的时间和驱动因素.
主要方法:
- 在沉积物中分析了丰富度和同位素比率.
- 使用的氧化还原代理数据涵盖了埃迪卡伦到德时期.
- 与陆地古植物记录相关的海洋氧化还原数据.
主要成果:
- 在埃迪亚卡-坎布里亚边界记录过渡性氧化.
- 通过早期德沃尼 (419393万年) 发现了主要的无氧深水条件.
- 确定了从中代纪 (393382万年前) 开始的永久深海氧化,与广泛的陆地森林相吻合.
结论:
- 早期森林的扩散和木质生物质的埋葬将碳封存起来,增加海洋氧气.
- 这种氧化事件促进了大型海洋生物的生态扩张和进化辐射.
- 陆地植物的进化是"中古海洋革命"的关键驱动力.
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