随着时间的推移追踪生物流:海洋沉积物混合和过渡层的演变
Lidya G Tarhan1, Kate H Pippenger1, Alison T Cribb2
1Department of Earth and Planetary Sciences, Yale University, New Haven, CT 06511, USA.
Science advances
|July 30, 2025
概括
生物化,即动物混合海底沉积物,在法内罗纪期间显著演变. 坎布里亚期形成了一个深层的过渡层,而混合层在数亿年的时间里变得更深.
科学领域:
- 古生物学的古生物学
- 海洋地质 海洋地质学
- 生态生态学 生态生态学
背景情况:
- 海底的特性是由生物化,动物的混合和挖掘活动所塑造的.
- 生物化产生了不同的沉积层:一个均质化的混合层和一个更深的洞穴过渡层.
- 了解这些层的历史演变对于解释过去的海底状况至关重要.
研究的目的:
- 为了重建Fanerozoic记录的沉积物混合和过渡层深度.
- 研究生物流强度及其驱动因素的长期进化趋势.
主要方法:
- 对沉积层的分析,以识别和测量整个罗纪的混合和过渡层深度.
- 地质数据与重大进化和环境事件的相关性.
主要成果:
- 沉积物混合层显示了一种跨越数亿年的逐渐加深趋势.
- 坎布里亚早期建立了一个深度过渡层,并保持相对稳定,直到中生代.
- 这些层的进化反映了主要的进化辐射,营养循环的变化和改善的氧化.
结论:
- 生物化在地质时间尺度上深刻改变了海底沉积物结构.
- 深度挖掘结构 (过渡层) 的发展发生在广泛的深层沉积物混合 (混合层) 之前.
- 这些发现突出了生物进化和地化学过程在塑造地球历史的相互作用.
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